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Heat wave
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A heat wave or heatwave, sometimes described as extreme heat, is a period of abnormally hot weather [1]: 2911 that lasts for multiple days. A heat wave is usually measured relative to the usual climate in the area and to normal temperatures for the season.[2] The main difficulties with this broad definition emerge when one must quantify what the 'normal' temperature state is, and what the spatial extent of the event may or must be. Temperatures that humans from a hotter climate consider normal can be regarded as a heat wave in a cooler area. This would be the case if the warm temperatures are outside the normal climate pattern for that area. Heat waves have become more frequent, and more intense over land, across almost every area on Earth since the 1950s, the increase in frequency and duration being caused by climate change.[3]: 8–10 [4]
Heat waves form when a high-pressure area in the upper atmosphere strengthens and remains over a region for several days up to several weeks.[5] This traps heat near the earth's surface. It is usually possible to forecast heat waves, thus allowing the authorities to issue a warning in advance.
Heat waves have an impact on the economy. They can reduce labour productivity, disrupt agricultural and industrial processes and damage infrastructure.[6][7] Severe heat waves have caused catastrophic crop failures and thousands of deaths from hyperthermia. They have increased the risk of wildfires in areas with drought. They can lead to widespread electricity outages because more air conditioning is used. A heat wave counts as extreme weather. It poses a danger to human health, because heat and sunlight overwhelm the thermoregulation in humans.
Definitions
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There are several definitions of heat waves:
- The IPCC defines a heatwave as "a period of abnormally hot weather, often defined with reference to a relative temperature threshold, lasting from two days to months."[8][1]: 2911
- A definition based on the Heat Wave Duration Index is that a heat wave occurs when the daily maximum temperature of more than five consecutive days exceeds the average maximum temperature by 5 °C (9 °F), the normal period being 1961–1990.[9] The same definition is used by the World Meteorological Organization.[10]
- A definition from the Glossary of Meteorology is:[11] "A period of abnormally and uncomfortably hot and usually humid weather."
- Marine heatwaves are generally described as prolonged discrete periods of unusually warm sea surface temperatures in a specific region. At this time the most commonly accepted definition is that proposed by Hobday et. al.[12] which refers to an algorithm that uses percentile values for temperatures, and defines a threshold set as the 90th percentile for a given day of the year, above which one can say a marine heatwave is occurring. This definition can be used with temperature data acquired anywhere in the world, allowing for comparisons across different observations and latitudes.
Definitions by country
[edit]Europe
[edit]Denmark defines a national heat wave (hedebølge) as a period of at least 3 consecutive days in which the average maximum temperature across more than half the country exceeds 28 °C (82.4 °F). The Danish Meteorological Institute also has a definition for a "warmth wave" (varmebølge). It defines this using the same criteria for a 25 °C (77.0 °F) temperature.[13] Sweden defines a heat wave as at least five days in a row with a daily high exceeding 25 °C (77.0 °F).[14]
In Greece, the Hellenic National Meteorological Service defines a heat wave as occurring over three consecutive days with temperatures at 39 °C (102 °F) or higher. In the same period the minimum temperature is 26 °C (79 °F) or more. During this period, there are either no winds or only weak winds. These conditions occur in a broad area.
The Netherlands defines a heat wave as a period of at least five consecutive days in which the maximum temperature in De Bilt exceeds 25 °C (77 °F). During this period the maximum temperature in De Bilt must exceed 30 °C (86 °F) for at least three days. Belgium also uses this definition of a heat wave with Ukkel as a reference point. So does Luxembourg.
In the United Kingdom, the Met Office operates a Heat Health Watch system. This places each Local Authority region into one of four levels. Heat wave conditions occur when the maximum daytime temperature and minimum nighttime temperature rise above the threshold for a particular region. The length of time above that threshold determines the level. Level 1 represents normal summer conditions. Level 2 occurs when there is a 60% or higher risk that the temperature will be above the threshold levels for two days and the intervening night. Level 3 arises when the temperature has been above the threshold for the preceding day and night, and there is a 90% or higher chance that it will stay above the threshold in the following day. Level 4 is triggered if conditions are more severe than those of the preceding three levels. Each of the first three levels gives rise to a particular state of readiness and response by the social and health services. Level 4 involves a more widespread response.[15] The threshold for a heat wave occurs when there are at least three days above 25 °C (77 °F) across much of the country. Greater London has a threshold of 28 °C (82 °F).[16]
In Ireland, a heat wave is defined as temperatures exceeding 25 °C (77 °F) for five or more consecutive days.[17]
North America
[edit]In the United States, definitions also vary by region. They usually involve a period of at least two or more days of excessively hot weather.[18] In the Northeast, a heat wave is typically when the temperature reaches or exceeds 90 °F (32.2 °C) for three or more consecutive days. This is not always the case. This is because the high temperature ties in with humidity levels to determine a heat index threshold.[19] The same does not apply to drier climates. A heat storm is a Californian term for an extended heat wave. Heat storms occur when the temperature reaches 100 °F (37.8 °C) for three or more consecutive days over a wide area (tens of thousands of square miles).[20] The National Weather Service issues heat advisories and excessive heat warnings when it expects unusual periods of hot weather.
In Canada, heat waves are defined using the daily maximum and minimum temperatures, and in most of the country, the humidex as well, exceeding a regional threshold for two or more days. The threshold in which daily maximum temperatures must exceed ranges between 28 °C (82 °F) in Newfoundland and 35 °C (95 °F) in interior British Columbia, though this threshold is much lower in Nunavut, ranging between 22 °C (72 °F) and 26 °C (79 °F).[21]
Oceania
[edit]In Adelaide, South Australia, a heat wave is five consecutive days at or above 35 °C (95 °F), or three consecutive days at or over 40 °C (104 °F).[22] The Australian Bureau of Meteorology defines a heat wave as three or more days of unusual maximum and minimum temperatures.[23] Before this new Pilot Heatwave Forecast there was no national definition for heat waves or measures of heat wave severity.[23]
In New Zealand, heat waves thresholds depend on local climatology, with the temperature threshold ranging between 27 °C (81 °F) in Greymouth and 32 °C (90 °F) in Gisborne.[24]
Marine Heatwaves
[edit]Marine heatwaves have become a prominent subject of research in recent years, reflecting the fact that since the turn of this century many ocean areas have experienced peaks of temperatures, along with more frequent, more intense, and more prolonged warming events than ever met on record.[25] The genesis of marine heatwaves is mainly driven by a combination of oceanic and atmospheric factors, often triggered by high pressure systems that will reduce cloud cover and increase solar absorption by the sea surface. Human-induced climate change appears bound to play a growing role in the development of marine heatwaves, with increasing impacts on marine ecosystems, such as mass mortality in benthic communities, coral bleaching events, disruptions in fishery catches, and shifts in species distributions.
Observations
[edit]
It is possible to compare heat waves in different regions of the world with different climates thanks to a general indicator that appeared in 2015.[28] With these indicators, experts estimated heat waves at the global scale from 1901 to 2010. They found a substantial and sharp increase in the number of affected areas in the last two decades.[29]
One study in 2021 investigated 13,115 cities. It found that extreme heat exposure of a wet bulb globe temperature above 30 Celsius tripled between 1983 and 2016, and if the effect of population growth (increasing the urban heat island effect) during those years is excluded, the exposure increased a further 50%. The researchers compiled a comprehensive list of past urban extreme heat events.[30][31]
Causes
[edit]Heat waves form when a high pressure area at an altitude of 3,000–7,600 metres (9,800–24,900 feet) strengthens and remains over a region for several days and up to several weeks.[5] This is common in summer in both the Northern and Southern Hemispheres. This is because the jet stream 'follows the sun'. The high pressure area is on the equator side of the jet stream in the upper layers of the atmosphere.
Weather patterns are generally slower to change in summer than in winter. So, this upper level high pressure also moves slowly. Under high pressure, the air sinks toward the surface. It warms and dries adiabatically. This inhibits convection and prevents the formation of clouds. A reduction of clouds increases the shortwave radiation reaching the surface. A low pressure area at the surface leads to surface wind from lower latitudes that brings warm air, enhancing the warming. The surface winds could also blow from the hot continental interior towards the coastal zone. This would lead to heat waves on the coast. They could also blow from high towards low elevations. This enhances the subsidence or sinking of the air and therefore the adiabatic warming.[32][33]
In the eastern regions of the United States a heat wave can occur when a high pressure system originating in the Gulf of Mexico becomes stationary just off the Atlantic Seaboard. Hot humid air masses form over the Gulf of Mexico and the Caribbean Sea. At the same time hot dry air masses form over the desert Southwest and northern Mexico. The southwest winds on the back side of the high continue to pump hot, humid Gulf air northeastwards. This results in a spell of hot and humid weather for much of the eastern United States and into southeastern Canada.[34]
In the Western Cape Province of South Africa, a heat wave can occur when the low-pressure area offshore and the high-pressure area inland combine to form a bergwind. The air warms as it descends from the Karoo interior. The temperature will rise about 10 Celsius from the interior to the coast. Humidity is usually very low. The temperature can be over 40 Celsius in summer. The highest temperature recorded in South Africa (51.5 Celsius) occurred one summer during a berg wind along the Eastern Cape coastline.[35][36]
The level of soil moisture can intensify heat waves in Europe.[37][38] Low soil moisture leads to a number of complex feedback mechanisms. These in turn can result in increased surface temperatures. One of the main mechanisms is reduced evaporative cooling of the atmosphere.[37] When water evaporates, it consumes energy. So, it will lower the surrounding temperature. If the soil is very dry, then incoming radiation from the sun will warm the air. But there will be little or no cooling effect from moisture evaporating from the soil.
Climate change
[edit]Heatwaves over land have become more frequent and more intense in almost all world regions since the 1950s, due to climate change. Heat waves are more likely to occur simultaneously with droughts. Marine heatwaves are twice as likely as they were in 1980.[41] Climate change will lead to more very hot days and fewer very cold days.[42]: 7 There are fewer cold waves.[43]: 8
Experts can often attribute the intensity of individual heat waves to global warming. Some extreme events would have been nearly impossible without human influence on the climate system. A heatwave that would occur once every ten years before global warming started now occurs 2.8 times as often. Under further warming, heatwaves are set to become more frequent. An event that would occur every ten years would occur every other year if global warming reaches 2 °C (3.6 °F).[44]Impacts on human health
[edit]
Heat-related health effects for vulnerable humans
[edit]Heat illness is a spectrum of disorders due to increased body temperature. It can be caused by either environmental conditions or by exertion. It includes minor conditions such as heat cramps, heat syncope, and heat exhaustion as well as the more severe condition known as heat stroke.[45] It can affect any or all anatomical systems.[46] Heat illnesses include:[47][48] heat stroke, heat exhaustion, heat syncope, heat edema, heat cramps, heat rash, heat tetany.
Prevention includes avoiding medications that can increase the risk of heat illness, gradual adjustment to heat, and sufficient fluids and electrolytes.[49][50]Exposure to extreme heat poses an acute health hazard, especially for people deemed as vulnerable.[51][52] Vulnerable people with regard to heat illnesses include people with low incomes, minority groups, women (in particular pregnant women), children, older adults (over 65 years old), people with chronic diseases, disabilities and multiple long-term health conditions.[51]: 13 Other people at risk include those living in urban environments (due to the urban heat island effect), outdoor workers and people who take certain prescription drugs.[51]
Climate change increases the frequency and severity of heatwaves and thus heat stress for people. A 2022 global study found that heat-related deaths increased significantly between 2000 and 2019, particularly in tropical and low-income countries, underscoring the growing health burden from rising temperatures.[53]
Human responses to heat stress can include heat stroke and overheating (hyperthermia). Extreme heat is also linked to acute kidney injury, low quality sleep,[54][55] and complications with pregnancy.[56]: 1051 Furthermore, it may cause the deterioration of pre-existing cardiovascular and respiratory disease.[56]: 1624 Adverse pregnancy outcomes due to high ambient temperatures include for example low birth weight and pre-term birth.[56]: 1051 Heat waves have also resulted in epidemics of chronic kidney disease (CKD).[57][58] Prolonged heat exposure, physical exertion, and dehydration are sufficient factors for the development of CKD.[57][58]Mortality
[edit]
Health experts warn that "exposure to extreme heat increases the risk of death from cardiovascular, cerebrovascular, and respiratory conditions and all-cause mortality. Heat-related deaths in people older than 65 years reached a record high of an estimated 345 000 deaths in 2019".[51]: 9 More than 70,000 Europeans died as a result of the 2003 European heat wave.[59] Also more than 2,000 people died in Karachi, Pakistan in June 2015 due to a severe heat wave with temperatures as high as 49 °C (120 °F).[60][61]
Due to climate change temperatures rose in Europe and heat mortality increased. From 2003–12 to 2013–22 alone, it increased by 17 deaths per 100,000 people, while women are more vulnerable than men.[62]Underreporting of fatalities
[edit]The number of heat fatalities is probably highly underreported. This is due to a lack of reports and to misreporting.[63] When considering heat-related illnesses as well, actual death tolls from extreme heat may be six times higher than official figures. This is based on studies of California[64] and Japan.[65]
Part of the mortality during a heat wave may be due to short-term forward mortality displacement. In some heat waves there is a decrease in overall mortality in the weeks after a heat wave. These compensatory reductions in mortality suggest that heat affects people who would have died anyway, and brings their deaths forward.[66]
Social institutions and structures influence the effects of risks. This factor can also help explain the underreporting of heat waves as a health risk. The deadly French heat wave in 2003 showed that heat wave dangers result from a combination of natural and social factors.[67] Social invisibility is one such factor. Heat-related deaths can occur indoors, for instance among elderly people living alone. In these cases it can be challenging to assign heat as a contributing factor.[68]
Heat index for temperature and relative humidity
[edit]Temperature Relative humidity
|
80 °F (27 °C) | 82 °F (28 °C) | 84 °F (29 °C) | 86 °F (30 °C) | 88 °F (31 °C) | 90 °F (32 °C) | 92 °F (33 °C) | 94 °F (34 °C) | 96 °F (36 °C) | 98 °F (37 °C) | 100 °F (38 °C) | 102 °F (39 °C) | 104 °F (40 °C) | 106 °F (41 °C) | 108 °F (42 °C) | 110 °F (43 °C) |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 40% | 80 °F (27 °C) | 81 °F (27 °C) | 83 °F (28 °C) | 85 °F (29 °C) | 88 °F (31 °C) | 91 °F (33 °C) | 94 °F (34 °C) | 97 °F (36 °C) | 101 °F (38 °C) | 105 °F (41 °C) | 109 °F (43 °C) | 114 °F (46 °C) | 119 °F (48 °C) | 124 °F (51 °C) | 130 °F (54 °C) | 136 °F (58 °C) |
| 45% | 80 °F (27 °C) | 82 °F (28 °C) | 84 °F (29 °C) | 87 °F (31 °C) | 89 °F (32 °C) | 93 °F (34 °C) | 96 °F (36 °C) | 100 °F (38 °C) | 104 °F (40 °C) | 109 °F (43 °C) | 114 °F (46 °C) | 119 °F (48 °C) | 124 °F (51 °C) | 130 °F (54 °C) | 137 °F (58 °C) | |
| 50% | 81 °F (27 °C) | 83 °F (28 °C) | 85 °F (29 °C) | 88 °F (31 °C) | 91 °F (33 °C) | 95 °F (35 °C) | 99 °F (37 °C) | 103 °F (39 °C) | 108 °F (42 °C) | 113 °F (45 °C) | 118 °F (48 °C) | 124 °F (51 °C) | 131 °F (55 °C) | 137 °F (58 °C) | ||
| 55% | 81 °F (27 °C) | 84 °F (29 °C) | 86 °F (30 °C) | 89 °F (32 °C) | 93 °F (34 °C) | 97 °F (36 °C) | 101 °F (38 °C) | 106 °F (41 °C) | 112 °F (44 °C) | 117 °F (47 °C) | 124 °F (51 °C) | 130 °F (54 °C) | 137 °F (58 °C) | |||
| 60% | 82 °F (28 °C) | 84 °F (29 °C) | 88 °F (31 °C) | 91 °F (33 °C) | 95 °F (35 °C) | 100 °F (38 °C) | 105 °F (41 °C) | 110 °F (43 °C) | 116 °F (47 °C) | 123 °F (51 °C) | 129 °F (54 °C) | 137 °F (58 °C) | ||||
| 65% | 82 °F (28 °C) | 85 °F (29 °C) | 89 °F (32 °C) | 93 °F (34 °C) | 98 °F (37 °C) | 103 °F (39 °C) | 108 °F (42 °C) | 114 °F (46 °C) | 121 °F (49 °C) | 128 °F (53 °C) | 136 °F (58 °C) | |||||
| 70% | 83 °F (28 °C) | 86 °F (30 °C) | 90 °F (32 °C) | 95 °F (35 °C) | 100 °F (38 °C) | 105 °F (41 °C) | 112 °F (44 °C) | 119 °F (48 °C) | 126 °F (52 °C) | 134 °F (57 °C) | ||||||
| 75% | 84 °F (29 °C) | 88 °F (31 °C) | 92 °F (33 °C) | 97 °F (36 °C) | 103 °F (39 °C) | 109 °F (43 °C) | 116 °F (47 °C) | 124 °F (51 °C) | 132 °F (56 °C) | |||||||
| 80% | 84 °F (29 °C) | 89 °F (32 °C) | 94 °F (34 °C) | 100 °F (38 °C) | 106 °F (41 °C) | 113 °F (45 °C) | 121 °F (49 °C) | 129 °F (54 °C) | ||||||||
| 85% | 85 °F (29 °C) | 90 °F (32 °C) | 96 °F (36 °C) | 102 °F (39 °C) | 110 °F (43 °C) | 117 °F (47 °C) | 126 °F (52 °C) | 135 °F (57 °C) | ||||||||
| 90% | 86 °F (30 °C) | 91 °F (33 °C) | 98 °F (37 °C) | 105 °F (41 °C) | 113 °F (45 °C) | 122 °F (50 °C) | 131 °F (55 °C) | |||||||||
| 95% | 86 °F (30 °C) | 93 °F (34 °C) | 100 °F (38 °C) | 108 °F (42 °C) | 117 °F (47 °C) | 127 °F (53 °C) | ||||||||||
| 100% | 87 °F (31 °C) | 95 °F (35 °C) | 103 °F (39 °C) | 112 °F (44 °C) | 121 °F (49 °C) | 132 °F (56 °C) |
The heat index in the table above is a measure of how hot it feels when relative humidity is factored with the actual air temperature.
Psychological and sociological effects
[edit]Excessive heat causes psychological stress as well as physical stress. This can affect performance. It may also lead to an increase in violent crime.[69] High temperatures are associated with increased conflict between individuals and at the social level. In every society, crime rates go up when temperatures go up. This is particularly the case with violent crimes such as assault, murder and rape. In politically unstable countries, high temperatures can exacerbate factors that lead to civil war.[70]
High temperatures also have a significant effect on income. A study of countries in the United States found that the economic productivity of individual days declines by about 1.7 percent for each degree Celsius above 15 °C (59 °F).[71]
Surface ozone (air pollution)
[edit]High temperatures also make the effects of ozone pollution in urban areas worse. This raises heat-related mortality during heat waves.[72] During heat waves in urban areas, ground level ozone pollution can be 20 percent higher than usual.[73]
One study looked at fine particle concentrations and ozone concentrations from 1860 to 2000. It found that the global population-weighted fine particle concentrations increased by 5 percent due to climate change. Near-surface ozone concentrations rose by 2 percent.[74]
An investigation to assess the joint mortality effects of ozone and heat during the European heat waves in 2003 concluded that these appear to be additive.[75]
Impacts on societies
[edit]Reduced economic outputs
[edit]Calculations from 2022 suggest that heat waves will shrink the global economy by about 1 percent decrease by the middle of the 21st century.[76][77][7]
Heat waves often have complex effects on economies. They reduce labour productivity, disrupt agricultural and industrial processes and damage infrastructure that is not suitable for extreme heat.[6][7] In 2016, a marine heatwave in Chile and its subsequent harmful algal bloom caused $800 million (USD) in export losses for the aquaculture industry as salmon and shellfish died off.[78]
Reduced agricultural outputs
[edit]Heat waves are a big threat to agricultural production. In 2019 heat waves in the Mulanje region of Malawi involved temperatures as high as 40 °C (104 °F). This and a late rain season scorched tea leaves and reduced yields.[79]
Farmed animals
[edit]
Once the body temperature of livestock animals is 3–4 °C (5.4–7.2 °F) above normal, this soon leads to "heat stroke, heat exhaustion, heat syncope, heat cramps, and ultimately organ dysfunction". Livestock mortality rates are already known to be higher during the hottest months of the year, as well as during heatwaves. During the 2003 European heat wave, for instance, thousands of pigs, poultry, and rabbits died in the French regions of Brittany and Pays-de-la-Loire alone.[80]
Livestock can also suffer multiple sublethal impacts from heat stress, such as reduced milk production. Once the temperatures exceed 30 °C (86 °F), cattle, sheep, goats, pigs and chickens all begin to consume 3–5% less feed for each subsequent degree of temperature increase.[81] At the same time, they increase respiratory and sweating rates, and the combination of these responses can lead to metabolic disorders. One examples is ketosis, or the rapid accumulation of ketone bodies, caused by the animal's body rapidly catabolizing its fat stores to sustain itself.[80] Heat stress also causes an increase in antioxidant enzyme activities, which can result in an imbalance of oxidant and antioxidant molecules, otherwise known as oxidative stress. Feed supplementation with antioxidants like chromium can help address oxidative stress and prevent it from leading to other pathological conditions, but only in a limited way.[82]
The immune system is also known to be impaired in heat-stressed animals, rendering them more susceptible to various infections.[80] Similarly, vaccination of livestock is less effective when they suffer from heat stress.[83] So far, heat stress had been estimated by researchers using inconsistent definitions, and current livestock models have limited correlation with experimental data.[84] Notably, since livestock like cows spend much of their day laying down, comprehensive heat stress estimation needs to take account of ground temperature as well,[85] but the first model to do so was only published in 2021, and it still tends to systematically overestimate body temperature while underestimating breathing rate.[86]Infrastructural damage
[edit]Heat waves cause roads and highways to buckle and melt,[87] water lines to burst, and power transformers to detonate, causing fires. A heat wave can also damage railways, by buckling and kinking rails. This can slow down or delay traffic. It can even lead to cancellations of service when rails are too dangerous to traverse by trains.
Power outages
[edit]Heat waves often lead to spikes in electricity demand because there is more use of air conditioning. This can create power outages, making the problem worse. During the 2006 North American heat wave, thousands of homes and businesses went without power, especially in California. In Los Angeles, electrical transformers failed, leaving thousands without power for as long as five days.[88] The early 2009 southeastern Australia heat wave caused major power disruptions in the city of Melbourne. They left over half a million people without power as the heat wave blew transformers and overloaded a power grid.
Impacts on the environment
[edit]Wildfires
[edit]A heat wave occurring during a drought can contribute to bushfires and wildfires. This is because a drought dries out vegetation, so it is more likely to catch fire. During the disastrous heat wave that struck Europe in 2003, fires raged through Portugal. They destroyed over 3,010 square kilometres (1,160 sq mi) of forest and 440 square kilometres (170 sq mi) of agricultural land. They caused about €1 billion worth of damage.[89] High end farmlands have irrigation systems to back up crops.
Floods
[edit]Heat waves can also contribute to flooding. Because hot air is able to carry more moisture, heatwaves may be followed by extreme rainfall especially in mid-latitude regions.[90] For example, the record-breaking heat wave that afflicted Pakistan beginning in May 2022 led to glacier melt and moisture flow. These were factors in the devastating floods that began in June and claimed over 1,100 lives.[91]
Wild animals on land
[edit]Researchers have predicted that roughly 10-40% of all land vertebrate species will be affected by heat waves by 2099, depending on the amount of future greenhouse gas emissions.[92] Heatwaves present an additional form of stress and evolutionary pressure for species that already deal with habitat loss and climate change.
Species have a thermal range of tolerance that describes the temperatures where they perform best. Temperature conditions that are outside of this range may experience decreased fitness and the inability to reproduce.[93][94] The species with sufficient genetic variation will be able to ensure some individuals can survive frequent days of high temperatures in the future.[95]
Oceans
[edit]Marine heatwaves may cause mass mortality in fish populations, especially for species that are better adapted to cooler temperatures.[96] Species that have adapted to warmer temperatures may expand their range during a heatwave. These invasive species may outcompete the native species that experience higher mortality during a heatwave, which disrupts ecosystem functioning.[96] Marine heatwaves have also been correlated with negative impacts on foundation species such as coral and kelp.[97]
Options for reducing impacts on humans
[edit]A possible public health measure during heat waves is to set up air-conditioned public cooling centres. Adding air conditioning in schools provides a cooler work place.[98] But it can result in additional greenhouse gas emissions unless solar energy is used.
Policymakers, funders and researchers have created the Extreme Heat Resilience Alliance coalition under the Atlantic Council. This advocates for naming heat waves, measuring them, and ranking them to build better awareness of their impacts.[99][100]
Recent examples by country or region
[edit]Around the world in 2024
[edit]

- Since March 2024, severe heat waves impacted Mexico, the Southern United States, and Central America, leading to dozens of broken temperature records,[103] mass deaths of animals from several threatened species,[citation needed] water shortages requiring rationing,[104] increased forest fires, and over 48 deaths in Mexico with over 950 people suffering from heat-related ailments.[105]
- Since April 2024 Southeast Asia has faced a severe heatwave, resulting in unprecedented high temperatures of up to 38.8 °C (101.8 °F) that have caused school closures and prompted urgent health advisories throughout the region.[106][107][108]
- 2024 Indian heat wave - Since May 2024, the longest heat wave has occurred in India and Pakistan with a new record temperature for India's capital New Delhi of 49 °C (120 °F) (an even higher record of 53 °C (127 °F) had initially been reported in New Delhi on May 29 but was later found to be attributable to a faulty sensor), and temperatures in Pakistan getting as high as 52.2 °C (126.0 °F).[109][110][111]
- 2024 European heatwaves - Since mid-June 2024, Greece has been experiencing a heatwave, Europe's first heatwave of the year. Temperatures in Greece are forecast to reach to 43 °C (109 °F).[112] Turkey has also been affected with temperatures hitting 44 °C (111 °F).
- In mid-June, high temperatures in Mecca, characterized as a heat wave, resulted in the deaths of pilgrims in the city for Hajj from countries including Indonesia, Jordan, Tunisia, and India.[113][114][115] It is reported that as many as 1300 people may have died.[116] Saudi authorities have said most who died were not officially authorized to perform Hajj.[117] Forecasts predicted temperatures as high as 113 °F (45 °C) on 19 June 2024.[115] The heat also impacted Kuwait, where heightened demand caused officials at the Ministry of Electricity, Water and Renewable Energy to temporarily stop distribution of electricity to portions of the nation.[118]
- 2024 Pakistan heat wave - In June 2024, Pakistan experienced a heat wave.[119] The Edhi Foundation in Karachi said it transported a higher-than-normal number of bodies to the morgue during the period of 20 to 25 June.[120]
- During the 2024 Summer Olympics, host city Paris, along with portions of Southern France and England, experienced a heatwave.[121][122]
- 2024 Japan heatwaves - At least 59 heat-related deaths were recorded in Japan, with at least 62 temperature observation posts across Japan breaking temperature records in July 2024. According to the Japan Meteorological Agency (JMA), the average temperatures reached during the heatwaves represented the hottest for Japan in April and July since its record-keeping began in 1898.[123][124]
India
[edit]From April 2024 to June 2024,[125][126] a severe and long heat wave affected India.[127] The heat wave occurred during the Indian dry season, which typically lasts from March to July, with peak temperatures in April and May. The year marked the third consecutive year of extreme heat waves in the country, a trend partly attributed to climate change.[125][126].
Churu district in Rajasthan recorded a temperature of 50.5 °C (122.9 °F), the highest in India in eight years.[128]. A temperature of 52.9°C was recorded in Mungeshpur, Delhi, and was initially thought to be record-breaking. However, it was later found to be approximately 3°C too high due to a faulty sensor.[129][130]Southeast Asia
[edit]Since April 2024,[until when?] several Southeast Asian countries have experienced record-breaking temperatures which have left several people dead.[131][132] Heat indices peaked at 53 °C (127 °F) in Iba in the Philippines on 28 April 2024. The heat wave has been attributed to a combination of causes, including climate change and El Niño.[131]
In some countries, the high heat has caused excessive energy demand. Drought conditions have worsened across the region. In Indonesia, dengue infections increased. In Myanmar, the heat wave exacerbated the humanitarian crisis caused by the ongoing civil war. Many government agencies have declared local emergencies and advised safety measures to protect residents from the heat, and some countries have closed schools or shortened their hours.China
[edit]A study found the average resident in China was exposed to 16 days of heat waves in 2023, with more than 37,000 heat wave-related deaths. Besides, the number of work hours lost due to heat stress in China was 36.9 billion in 2023, and China's citizens experienced a 60% surge in lost safe outdoor activity hours, with each person losing 2.2 hours on average each day. The study predicted that by the 2060s, annual heat wave-related mortality is expected to reach 29,000 to 38,000 in China, with a 28% to 37% increase in work hours lost.[133]
United States
[edit]In July 2019, there were over 50 million people in the United States in jurisdictions with heat advisories. Scientists predicted that many records for highest low temperatures would be broken in the days following these warnings. This means the lowest temperature in a 24-hour period will be higher than any low temperature measured before.[135]
According to a 2022 study, 107 million people in the US will experience extremely dangerous heat in the year 2053.[136]
Heat waves are the most lethal type of weather phenomenon in the United States. Between 1992 and 2001, deaths from excessive heat in the United States numbered 2,190, compared with 880 deaths from floods and 150 from tropical cyclones.[137] About 400 deaths a year on average are directly due to heat in the United States.[63] The 1995 Chicago heat wave, one of the worst in US history, led to approximately 739 heat-related deaths over 5 days.[138] In the United States, the loss of human life in hot spells in summer exceeds that caused by all other weather events. These include lightning, rain, floods, hurricanes, and tornadoes.[139][140]
About 6,200 Americans need hospital treatment each summer, according to data from 2008. This is due to excessive heat, and those at highest risk are poor, uninsured or elderly.[141]
The relationship between extreme temperature and mortality in the United States varies by location. Heat is more likely to increase the risk of death in cities in the northern part of the country than in southern regions. As a whole, people in the United States appear to be adapting to hotter temperatures further north each decade. This might be due to better infrastructure, more modern building design and better public awareness.[142]
See also
[edit]References
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Heat wave
View on GrokipediaDefinitions
Core Criteria and Metrics
A heat wave is generally defined as a prolonged period of abnormally high temperatures relative to the expected climate of a given location, typically lasting at least two consecutive days and often extending to three or more to distinguish it from isolated hot days.[14][15] The World Meteorological Organization describes it as a sequence of unusually hot days and nights where excess heat accumulates locally, amplifying risks beyond mere daytime highs by incorporating sustained warmth.[2] Core criteria emphasize both duration and intensity, with thresholds calibrated to exceed historical norms rather than arbitrary absolutes, ensuring the event represents an outlier in the local climatology.[16] Intensity is most commonly measured using percentile-based thresholds applied to daily maximum temperatures, such as exceeding the 90th or 95th percentile of historical maxima for the relevant season and location, calculated over a baseline period like 30-50 years.[15][17] This relative approach, preferred by organizations like the U.S. Environmental Protection Agency and NOAA's National Centers for Environmental Information, accounts for regional climate variations—e.g., a 90th percentile threshold in the U.S. Southwest might equate to 105°F (41°C), while in the Midwest it could be 95°F (35°C)—and is often centered on a 31-day climatological window to capture seasonal peaks.[18][19] Fixed absolute thresholds, such as daily maxima 5°C above the long-term average for five or more days (per some WMO guidelines), are used in operational forecasting but criticized for ignoring acclimatization differences across latitudes.[20] Minimum nighttime temperatures exceeding the 90th percentile are increasingly incorporated to reflect heat accumulation, as persistent warm nights prevent physiological recovery.[17][21] Key metrics extend beyond raw temperature to assess human and ecological impacts, incorporating humidity via indices like the heat index (combining air temperature and relative humidity to estimate perceived heat) or wet-bulb temperature (a direct measure of heat stress potential, where values approaching 35°C (95°F) approach human survivability limits for prolonged exposure due to impaired evaporative cooling).[22][23] The wet-bulb globe temperature (WBGT), which factors in radiant heat, wind, and humidity, serves as a standard for occupational risk assessment, with thresholds like WBGT >30°C indicating high strain for moderate work.[24][25] These physiological metrics outperform simple temperature in predicting health outcomes, as evidenced by studies linking wet-bulb exceedances to elevated heat stroke rates even at moderate air temperatures around 28°C in humid conditions.[26] Percentile metrics for heat waves align with broader extreme event analysis, such as the EPA's use of the 85th percentile for summer temperatures to track event frequency.[18]| Metric | Description | Typical Threshold for Heat Wave Contribution |
|---|---|---|
| Temperature Percentile | Exceedance of historical daily max/min over baseline period | 90th-95th percentile for 3+ consecutive days[17][27] |
| Heat Index | Apparent temperature accounting for humidity | >103°F (39°C) for advisory levels, sustained over duration[22] |
| Wet-Bulb Temperature | Evaporative cooling limit indicator | >31°C (88°F) for severe risk; ~35°C unsustainable for hours[23][28] |
| WBGT | Composite for work/exertion stress | >28°C moderate risk; >32°C extreme for unacclimatized individuals[24] |
Regional and Temporal Variations
Heat wave definitions incorporate regional variations to account for baseline climatic norms, population acclimatization, and local impacts, as uniform global thresholds would overlook differences in vulnerability; for instance, a temperature exceeding 35°C (95°F) might constitute a heat wave in cooler temperate zones but not in tropical regions where such levels are normative.[10][16] In the United States, the National Weather Service often employs criteria such as two or more consecutive days with apparent temperatures above 105°F (41°C) or heat index values exceeding regional thresholds, while the Environmental Protection Agency standardizes analyses using periods of two or more days where daily high and low temperatures rank among the warmest 5% of historical occurrences for consistency across diverse subregions like the Northeast versus the Southwest.[18][30] European definitions, such as those from the Copernicus Climate Change Service, frequently rely on relative excesses over seasonal averages (e.g., 5°C above the 1971–2000 mean for several days) or percentile-based thresholds tailored to subcontinental variations, emphasizing night-time recovery failures in densely urbanized areas.[21] In Australia, the Bureau of Meteorology defines heat waves as three or more consecutive days where maximum temperatures exceed the highest Bureau of Meteorology forecast for that location or surpass the 90th percentile of historical maxima, reflecting the continent's arid interiors and coastal humidity contrasts.[10] Asian regions, including China, adapt definitions to monsoon influences and urban density; for example, some frameworks use region-specific percentiles (e.g., 95th for frequency) combined with duration, acknowledging that fixed absolute thresholds underestimate risks in acclimatized tropical populations versus mid-latitude ones.[31] These regional adjustments stem from empirical evidence that heat-related mortality correlates more strongly with deviations from local norms than absolute values, with studies across 112 countries revealing diverse variables like wet-bulb temperature in humid tropics versus dry-bulb in arid zones.[32][33] Temporal criteria in heat wave definitions emphasize duration and persistence to distinguish transient hot spells from cumulative stress events, typically requiring 2–5 consecutive days of elevated temperatures, though shorter periods suffice in vulnerable demographics; for example, some indices mandate three days for intensity metrics but extend to five for severe classifications.[30] Diurnal variations are incorporated by including minimum night-time temperatures failing to drop below thresholds (e.g., below the 10th percentile), as sustained warmth prevents physiological recovery and amplifies risks.[2] Over longer timescales, definitions have evolved to reflect climatic shifts, with adaptive thresholds like moving minimum mortality temperatures rising alongside observed warming, indicating partial human acclimatization; however, fixed historical baselines in many protocols can lead to temporal inconsistencies in classifying events amid rising baselines.[34][16] Seasonal confines predominate, confining most definitions to summer months (June–August in the Northern Hemisphere), but exceptions apply in equatorial zones where "heat waves" may occur year-round due to absent cool seasons.[18]Meteorological Mechanisms
Large-Scale Atmospheric Patterns
Persistent high-pressure systems, or anticyclones, dominate large-scale atmospheric patterns during heat waves, inducing subsidence that compresses descending air and generates adiabatic warming at the surface.[12] These systems suppress vertical motion, inhibit cloud development, and block precipitation, fostering prolonged clear skies and enhanced solar insolation.[35] In mid-latitudes, such anticyclones often manifest as blocking highs, which become quasi-stationary and impede the westerly flow of the jet stream, trapping heat over expansive regions for days or weeks.[36] For instance, the 2021 Pacific Northwest heat wave involved a blocking anticyclone that stalled weather progression, amplifying temperatures through persistent ridging.[37] Rossby waves, planetary-scale undulations in the extratropical circulation driven by the Coriolis effect and Earth's rotation, play a key role in establishing these persistent patterns.[38] High-amplitude Rossby wave trains propagate eastward, creating meridional meanders that favor ridging and blocking configurations conducive to heat domes—intensified upper-level highs that cap and heat the troposphere below.[39] Zonal propagation of Rossby wave packets influences the positioning and longevity of these features, with amplified waves linking to concurrent extremes across hemispheres.[36] Observational analyses indicate that blocking events, often Rossby wave-induced, actively sustain mid- and high-latitude heat waves by diverting synoptic systems and prolonging stagnant conditions.[36] Regional variations in these patterns arise from interactions with topography and climatological flows; for example, in the Northeastern United States, heat waves frequently align with four distinct circulation types, including dominant high-pressure ridges over the Ohio Valley that enhance subsidence.[40] Over Asia, increased persistence of large-scale regimes, such as subtropical highs, has been documented since the 1980s, correlating with extended heat episodes through stalled anticyclonic circulations.[41] These dynamics underscore that heat waves stem from amplified natural variability in atmospheric circulation rather than isolated local forcings, though external influences like sea surface temperatures can modulate wave propagation and blocking frequency.[42] Empirical reanalyses, such as ERA5, confirm Rossby wave packets' association with propagating heat wave pathways, highlighting their role in sequential extreme events.[43]Local and Microscale Factors
Local and microscale factors modulate heat wave intensity by altering surface energy budgets, airflow patterns, and heat retention at scales below synoptic systems, often amplifying large-scale warming through feedbacks like reduced evaporative cooling and trapped heat. In urban environments, the urban heat island (UHI) effect arises from the replacement of vegetated surfaces with impervious materials such as asphalt and concrete, which absorb and re-radiate solar radiation while limiting evapotranspiration.[44] This results in urban temperatures exceeding rural counterparts by 2–10°C during heat waves, depending on city size, building density, and nighttime conditions, as anthropogenic heat from vehicles and air conditioning further sustains elevated minima.[45] Reduced wind speeds in densely built areas exacerbate UHI by limiting convective mixing, creating synergistic interactions that prolong heat exposure.[46] Soil moisture deficits at the local scale play a critical role by diminishing latent heat loss via transpiration and evaporation, redirecting energy toward sensible heating of the air. During dry antecedent conditions, such as those preceding the 2021 Pacific Northwest heat dome, low soil moisture initiated positive feedbacks that elevated near-surface temperatures by enhancing downward solar radiation absorption and reducing boundary layer cooling.[47] Peer-reviewed analyses confirm that regions with depleted topsoil layers experience amplified heat wave magnitude and duration, as evapotranspiration drops sharply once soil moisture falls below wilting points, with correlations showing negative relationships between soil wetness and maximum temperatures.[48] Vegetation cover mitigates this through shading and moisture retention, but land-use changes like deforestation or urbanization diminish such effects, intensifying local hotspots.[49] Topographic features influence microscale heat accumulation by affecting downslope drainage of cool air and promoting subsidence in valleys or basins, which suppresses cloud formation and enhances radiative heating. In complex terrain, such as urban-adjacent hillslopes, reduced katabatic flows during calm conditions trap heat, while south-facing exposures receive prolonged insolation, elevating surface temperatures independently of broader atmospheric patterns.[50] Local airflow disruptions, including sea breezes or urban canyons channeling heat, further contribute, though these are modulated by surrounding land cover; for instance, sparse vegetation on slopes heightens sensitivity to soil dryness, diminishing microclimate buffering.[51] Empirical modeling underscores that integrating these factors—UHI, soil states, and relief—yields more accurate predictions of intra-regional heat disparities during events.[52]Historical Context
Ancient and Pre-Modern Records
Historical records of heat waves from ancient times are sparse and primarily indirect, derived from chronicles, agricultural reports, and proxy indicators such as phenological shifts or crop failures, which often imply prolonged excessive heat accompanying drought. In the Mediterranean during the Roman Climatic Optimum (approximately 250 BCE to 400 CE), summers featured notable heat, as evidenced by architectural adaptations like narrow streets to mitigate urban warming and references in texts to the "dog days" linked to the rising of Sirius, a period of stifling temperatures prompting rituals and public health measures.[53][54] However, specific quantified events remain undocumented due to the absence of instrumental data, with evidence limited to qualitative accounts of hot, dry conditions exacerbating famines and migrations. Medieval European records provide clearer examples of extreme heat episodes. In spring 1473, much of Europe endured a severe heat wave and drought, accelerating vegetation growth and causing widespread crop stress, as noted in contemporary chronicles from regions including Switzerland, France, and the Holy Roman Empire; this event contributed to social unrest and economic strain amid already warm conditions in the early 1470s.[55] Similarly, Chinese historical annals from the 5th century CE detail recurrent droughts signaling heat waves, such as those in 463–464 CE across multiple provinces, where prolonged dry heat led to 60–70% population losses from famine in affected areas.[56] The 1540 European event represents one of the most extensively documented pre-modern heat waves, lasting nearly a year with extreme dryness and warmth across the continent; Central Europe saw no significant rainfall from March to late September, drying rivers like the Rhine and Elbe, devastating harvests, and prompting calls for prayer against famine, with reconstructed summer temperatures likely exceeding those of 2003 by 2–4°C in proxy-based estimates.[57][58] This megadrought, linked to persistent high-pressure systems, affected agriculture from Ireland to Poland, highlighting vulnerabilities in pre-industrial societies despite occurring during the cooler Little Ice Age phase.[59] Such records underscore that while heat waves occurred historically, their documentation relied on non-instrumental sources prone to regional bias, with peer-reviewed reconstructions using grape harvest dates and tree-ring data providing the most reliable modern validations.[60]Modern Era Events Prior to 1950
The 1936 North American heat wave, occurring primarily from June to August amid the Dust Bowl drought, brought extreme temperatures across the United States and Canada, with record highs reaching 121°F (49.4°C) in North Dakota and Kansas.[61] This event, exacerbated by persistent high pressure and dry soils amplifying surface heating, resulted in approximately 5,000 deaths nationwide, many from heatstroke in urban areas lacking modern cooling.[62] In Chicago, temperatures exceeded 100°F (37.8°C) for eight consecutive days in July, contributing to over 200 local fatalities and straining public health resources during the Great Depression.[63] Earlier, the 1911 Eastern North American heat wave struck the U.S. East Coast in July, with temperatures lingering in the 90s°F (32–37°C) for extended periods, causing at least 211 deaths in New York City alone through dehydration and exhaustion. Concurrently, a severe heat wave and drought affected Europe, including the United Kingdom, where temperatures in England reached 36.6°C (97.9°F) on August 9, leading to widespread crop failures, reduced livestock yields, and elevated mortality, particularly among the vulnerable.[64] These conditions persisted for weeks, with minimal rainfall intensifying the thermal stress in populated regions. The 1896 Eastern North America heat wave, spanning August 4–14, delivered unrelenting humidity and highs above 100°F (37.8°C) from Chicago to New England, claiming around 1,500 lives in New York City, predominantly among tenement residents without access to relief.[65] Urban heat islands worsened the impacts, as asphalt and dense housing trapped heat, prompting public measures like opening fire hydrants and rooftop sleeping, though mortality remained high due to limited medical interventions at the time.[66] Such events underscored early vulnerabilities to prolonged heat in industrializing societies, often linked to stagnant anticyclones and antecedent dry conditions rather than isolated anomalies.[67]Observed Trends
Global and Regional Frequency Data
Observational records indicate that the frequency of heatwaves has increased globally since the 1950s, with medium confidence in this trend derived from station data and reanalyses.[68] This increase is most pronounced in mid-latitude and subtropical regions, where datasets show a rise in the occurrence of prolonged hot periods exceeding historical baselines.[69] In North America, particularly the United States, heatwave frequency has risen from an average of two events per year in the 1960s to six per year in the 2010s and 2020s, based on analyses of populated metropolitan statistical areas using thresholds of four or more consecutive days above the 90th percentile of local temperatures.[18] European records similarly document significant upward trends, with heatwaves becoming more frequent across midlatitudes, as evidenced by consistent increases in event counts since the late 20th century.[69] In Asia, observational trends reveal escalating heatwave frequency, especially in subtropical and mid-latitude zones, with disparities across subregions showing sharper rises in densely populated areas like South and East Asia.[70] These patterns align with broader global shifts, though regional variations persist due to differences in data coverage and definitions, such as consecutive days above the 95th or 99th percentile of daily maximum temperatures.[68]Intensity and Duration Metrics
Heat wave intensity is commonly assessed using metrics such as peak or average temperature excesses above historical baselines (e.g., the 95th percentile of daily maxima), heat index incorporating humidity, or the Excess Heat Factor (EHF), which combines absolute excess heat with relative deviations from recent climatological norms to account for acclimatization.[71][72] EHF, validated against health outcomes in mid-latitude regions, emphasizes cumulative thermal stress over isolated peaks.[73] Duration metrics measure consecutive days meeting these thresholds, often spanning 2–5 or more days, with longer spells indicating prolonged exposure risks.[30] Observational trends in the United States, drawn from daily temperature records at 97 locations spanning 1961–2020, reveal significant increases in heat wave intensity (average event temperature above the 95th percentile) in 20 locations and duration in 28, based on events exceeding two or more consecutive days above the local 95th percentile.[18] The heat wave season length, defined as days between the first and last event annually, extended significantly in 46 locations over the same period.[18] These patterns align with broader North American analyses using reanalysis data, showing modest but positive trends in event magnitude and persistence since the mid-20th century.[30] Globally, peer-reviewed analyses of gridded temperature datasets indicate upward trends in intensity and duration, particularly in mid-latitudes and subtropical regions; for example, extra heat generated during events has risen most sharply in the Middle East, northern Africa, and parts of South America from 1979–2017.[10] A 2025 statistical examination of historical and projected data confirms nonlinear acceleration in long-duration heat wave changes with rising global temperatures, outpacing linear warming expectations.[74] Metric selection critically affects trend attribution, as cumulative or averaged indices (e.g., total excess heat) detect stronger increases than maximum temperature anomalies alone, highlighting the need for context-specific definitions to avoid understating compound risks.[72] Regional variability persists, with some areas showing stable or slower shifts due to local circulation influences.[10]Confounding Factors in Trend Analysis
The urban heat island (UHI) effect represents a primary confounding factor in heat wave trend analysis, as urban development replaces vegetated surfaces with heat-absorbing materials like concrete and asphalt, elevating local temperatures by 1–3°C or more relative to rural areas, with intensification during calm, clear nights and heat wave conditions.[12] Expansion of urban areas has increased the proportion of weather stations affected by UHI, particularly since the mid-20th century, leading to upward biases in observed minimum temperatures and heat wave durations in composite datasets; for instance, analyses of global land stations estimate that urbanization accounts for 10–50% of the reported warming in minimum temperatures across various regions, depending on correction methods applied.[75] [76] This bias is amplified in heat wave metrics because UHI exacerbates nighttime warming, prolonging periods above thresholds, yet many trend studies rely on raw or partially adjusted data where rural-urban contrasts are insufficiently disentangled.[77] Changes in weather station siting and surrounding environments introduce additional non-climatic discontinuities, as stations relocated to airports, industrial zones, or urban peripheries since the 1950s often experience altered microclimates, such as proximity to heat-emitting infrastructure, resulting in spurious warming signals of 0.1–0.5°C per decade in affected records.[78] In the United States, for example, evaluations of the U.S. Historical Climatology Network reveal that over 40% of stations exhibit poor siting quality by modern standards (e.g., within 10 meters of asphalt or exhaust sources), correlating with inflated heat wave frequencies in unadjusted series from 1960–2020.[79] Data homogenization algorithms, intended to correct these inhomogeneities by referencing neighboring stations, can propagate urban biases into ostensibly rural records through "urban blending," where urban-influenced breakpoints are smoothed across networks, underestimating true climatic variability.[79] [80] Instrumental and procedural shifts, including transitions from manual to automated observations and changes in daily observation times (e.g., from afternoon to morning), further confound heat wave detection by altering the capture of daily maxima and minima; time-of-observation bias alone can inflate apparent trends by up to 0.2°C per century in maximum temperature series if uncorrected.[76] Uneven spatial coverage, with denser networks in urbanized mid-latitude regions, exacerbates these issues, as sparser rural or remote areas underrepresented in global datasets like HadCRUT contribute to cool biases in early records, amplifying apparent recent heat wave uptrends.[81] Rigorous trend attribution thus requires pairwise rural-urban comparisons and robust breakpoint detection, though institutional datasets often apply standardized adjustments that skeptics argue inadequately isolate these artifacts from greenhouse-driven signals.[82]Causal Factors
Natural Variability and Cycles
The El Niño-Southern Oscillation (ENSO) represents a primary mode of interannual climate variability, with El Niño phases characterized by anomalous warming of equatorial Pacific sea surface temperatures, occurring irregularly every 2 to 7 years. These events disrupt global atmospheric circulation, often promoting persistent anticyclonic conditions that exacerbate heat waves in regions such as the southwestern United States, northeastern Australia, and parts of South Asia by suppressing cloud cover and enhancing solar heating at the surface.[83] For instance, delayed teleconnections from ENSO can increase the frequency of extreme hot days in the Asian monsoon region through mechanisms like the Indo-Pacific Oscillation and Rossby wave propagation, which reduce soil moisture and amplify temperature anomalies.[84] Compound drought-heat wave events in northeast Australia show significantly higher frequency, duration, and severity during strong El Niño periods compared to neutral or La Niña conditions.[85] On decadal to multidecadal timescales, the Atlantic Multidecadal Oscillation (AMO), a ~60- to 80-year cycle in North Atlantic sea surface temperatures, modulates heat wave occurrence through altered meridional temperature gradients and atmospheric blocking patterns. Positive AMO phases, featuring warmer Atlantic waters, have been linked to increased heat wave frequency across eastern North America and Europe by strengthening subtropical high-pressure systems and reducing storm track activity.[86] Large-ensemble climate simulations indicate that AMO warm phases can elevate the probability of multi-day heat waves in the central and eastern United States by up to 50% relative to cold phases, independent of mean warming trends.[87] Similarly, the Pacific Decadal Oscillation (PDO) influences North Pacific heat waves via shifts in jet stream positioning, with positive (warm) phases correlating to drier conditions and higher extreme temperatures in the northwestern United States.[88] Solar variability, driven by the 11-year sunspot cycle, introduces small fluctuations in total solar irradiance of about 1 W/m² at Earth's surface, corresponding to global temperature variations of approximately 0.1°C. Peaks in solar activity, such as the anticipated maximum in Solar Cycle 25 around 2025, can marginally enhance tropospheric heating and influence regional circulation patterns, potentially contributing to hotter summers in mid-latitudes through stratospheric-tropospheric coupling. However, these effects are dwarfed by internal ocean-atmosphere dynamics and do not explain multidecadal heat wave trends. Volcanic eruptions provide episodic cooling via stratospheric aerosols, indirectly modulating heat wave baselines by altering radiative forcing, though their influence on wave frequency is secondary to oscillatory modes.[88] These natural cycles superimpose on baseline climate states, generating variability that has historically produced severe heat waves, such as the 1930s Dust Bowl events in the U.S., which aligned with a positive AMO phase and strong El Niño influences without elevated greenhouse gas levels.[86] Attribution studies emphasize that while anthropogenic forcing amplifies extremes, natural variability accounts for substantial year-to-year and decadal fluctuations in heat wave metrics, necessitating its isolation in trend analyses to avoid conflating internal dynamics with external drivers.[91]Anthropogenic Greenhouse Gas Effects
![Frequency of extreme weather for different degrees of global warming - IPCC AR6][float-right] Anthropogenic emissions of greenhouse gases, particularly carbon dioxide (CO₂) from fossil fuel combustion and land-use changes, have elevated atmospheric CO₂ concentrations from about 280 parts per million (ppm) pre-industrially to over 420 ppm by 2023, exerting a radiative forcing of approximately 2.0 W/m².[68] This forcing enhances the greenhouse effect by absorbing and re-emitting infrared radiation, thereby increasing Earth's energy imbalance and driving global surface warming of roughly 1.1°C since 1850–1900, with GHGs responsible for the net positive forcing.[92] In relation to heat waves, this anthropogenic warming shifts the statistical distribution of surface temperatures toward higher values, amplifying the probability, intensity, and persistence of extreme heat events that exceed regional thresholds.[93] The Intergovernmental Panel on Climate Change's Sixth Assessment Report (AR6) concludes with virtual certainty that the frequency and intensity of hot extremes, including heat waves, have increased globally since the 1950s, primarily due to human-induced GHG emissions, while cold extremes have decreased.[94] Attribution studies further quantify this effect, showing that GHG-driven climate change made 213 documented heat waves from 2000 to 2023 more likely and intensified their severity, with emissions from major fossil fuel producers contributing to about half of the post-pre-industrial increase in heat wave intensity.[95] Projections based on climate models indicate that for every additional 1°C of global warming—largely from continued GHG emissions—the frequency of heat waves could increase by factors of 2 to 10 times in various regions, alongside extensions in duration and rises in maximum temperatures by 1–3°C beyond baseline warming.[68] Empirical evidence from event attribution supports this, as seen in analyses of specific heat waves where anthropogenic forcing elevated risks; for example, GHG influences have been linked to longer-lasting and more spatially extensive heat events through altered atmospheric dynamics.[96] While natural variability modulates individual events, the long-term trend in heat wave characteristics is dominated by GHG-induced forcing, as confirmed by detection and attribution methods comparing observed trends against model simulations with and without anthropogenic aerosols and GHGs.[97]Land Use Changes and Urbanization
Urbanization contributes to the exacerbation of heat waves through the urban heat island (UHI) effect, where built environments with impervious surfaces such as concrete and asphalt absorb and retain solar radiation, reducing surface albedo and limiting evaporative cooling from vegetation. This leads to elevated local temperatures, particularly at night due to stored heat release and anthropogenic sources like air conditioning and vehicles. During heat waves, the UHI intensity often amplifies, with studies observing enhancements of up to 0.94°C in urban areas of China compared to non-heat wave periods, nearly doubling the baseline effect.[98] Similarly, nocturnal UHI has intensified in 28 of 32 analyzed cities during extreme high temperatures, driven by reduced rural cooling relative to urban persistence.[99] The synergy between UHI and heat waves creates compounded overheating, where baseline urban-rural temperature differentials widen under synoptic heat conditions, increasing urban exposure beyond regional averages. For instance, urbanization in the Yangtze River Delta has enhanced compound heat wave frequency and intensity, with urban fractions explaining significant portions of observed trends in night-time events. In wetter climates, urbanization's role in heat wave trends is disproportionately stronger, modulating local hydroclimatic feedbacks that sustain elevated temperatures. Empirical analyses in Indian cities further quantify this, attributing increased heat wave severity to urban expansion, which overrides some natural variability signals in regional data.[100][101][102] Land use changes, particularly deforestation and conversion to agriculture or urban development, diminish latent heat fluxes from evapotranspiration, resulting in net surface warming and drier conditions that prolong heat wave durations locally. In tropical regions, 15 years of deforestation has induced warming sufficient to eliminate safe thermal working conditions for 2.8 million outdoor laborers, with effects detectable up to 50 km from deforested patches. Observational data link such changes to 28,000 annual heat-related deaths globally, primarily through amplified local extremes rather than broad atmospheric forcing. While some modeling suggests complex tropical responses where deforestation might slightly mitigate wet-bulb stress via reduced humidity, empirical evidence predominates in highlighting warming and ecosystem stress amplification during heat events.[103][104][105]Human Health Impacts
Direct Physiological Effects
During heat exposure, the human body maintains thermal balance primarily through cutaneous vasodilation and sweating, which facilitate heat dissipation via radiation, convection, and evaporation. Vasodilation redirects blood flow to the skin, increasing cardiac output by 1-2 L/min per °C rise in core temperature to support skin blood flow exceeding 7 L/min, while sweating rates can reach 1-2 L/hour in acclimatized individuals to evaporate heat. These responses are effective up to wet-bulb temperatures around 31-35°C, beyond which evaporative cooling diminishes due to high humidity, leading to net heat gain and progressive hyperthermia.[106]01208-3/fulltext) When thermoregulatory mechanisms are overwhelmed, core body temperature rises above 38-40°C, triggering cellular stress responses including heat shock protein activation, but prolonged elevation causes protein denaturation, membrane instability, and mitochondrial dysfunction, culminating in multi-organ injury. Cardiovascular strain intensifies as heart rate elevates by approximately 10-20% per 1°C core temperature increase, straining preload and afterload, which can precipitate arrhythmias, myocardial ischemia, or decompensated heart failure, particularly in those with preexisting conditions. Dehydration from insensible fluid loss exacerbates hypovolemia, reducing stroke volume and glomerular filtration rate by up to 50%, while electrolyte imbalances like hyponatremia or hyperkalemia disrupt neuromuscular function.[107][106][108] Neurological effects manifest as central nervous system dysfunction, with hyperthermia impairing cerebral blood flow regulation and inducing excitotoxicity via glutamate release, progressing from confusion and seizures to coma in severe cases like heat stroke, where core temperatures exceed 40°C. Respiratory compensation involves tachypnea to augment evaporative loss, but this can lead to respiratory alkalosis and fatigue, compounding hypoxemia from pulmonary edema or aspiration. Renal tubular damage from hypoperfusion and direct thermal injury results in acute kidney injury, with biomarkers like NGAL rising within hours of heat stress. These direct effects underscore heat's causal role in acute physiological derangement, independent of behavioral factors.[109][110]01208-3/fulltext)Mortality Patterns and Vulnerabilities
Older adults, particularly those aged 65 and above, account for the majority of heat wave-related excess deaths due to diminished physiological capacity for thermoregulation, including reduced sweat production and impaired cardiovascular responses to heat stress.[111] Pre-existing conditions such as cardiovascular disease and diabetes amplify this vulnerability, with epidemiological studies showing risk ratios for mortality increasing by up to 2.5 times during intense heat events among this demographic.[112] Children under five and infants also face elevated risks from dehydration and heat exhaustion, though their share of fatalities remains lower than the elderly.[7] Urban populations experience disproportionately higher mortality rates compared to rural counterparts, attributable to the urban heat island (UHI) effect, which elevates nighttime temperatures and prolongs exposure; analyses of the 2003 European heat wave indicate that UHI contributed around 50% of heat-related deaths in affected urban regions like the West Midlands, UK.[113] Across 93 European cities, UHI effects are estimated to cause approximately 6,700 premature deaths annually from amplified heat stress.[114] In the United States, from 2008 to 2017, extreme heat days correlated with elevated all-cause mortality, with urban areas showing 1.1 to 5.1 more heat exposure days for vulnerable subgroups, including older adults of color and the uninsured.[115][116] Socioeconomic factors intersect with demographic vulnerabilities to heighten mortality risks; individuals in poverty, those living in substandard housing without air conditioning, and socially isolated elderly—often residing alone without support networks—exhibit the highest excess death rates, as low AC prevalence mitigates up to 80% of heat-mortality associations in some U.S. communities.[117][118] Gender patterns vary by region, with females in certain populations, such as India, facing 10-20% higher cardiovascular mortality risks from heat than males across age groups.[112] Globally, heat wave excess deaths totaled millions attributable between 1990 and 2019, with declining per capita rates in some areas due to adaptation, yet persistent burdens in under-resourced settings.[119]Relative Risks Compared to Cold Extremes
A multi-country study analyzing over 74 million deaths across 13 nations from 1985 to 2012 found that the population attributable fraction for cold temperatures was 7.29% (95% empirical confidence interval 6.96–7.62%), compared to 0.42% (0.39–0.44%) for heat, indicating that cold-related deaths outnumbered heat-related deaths by a ratio of approximately 17 to 1 in the studied populations.62114-0/fulltext) This disparity arises because moderately cold temperatures contribute substantially to cumulative mortality through mechanisms like respiratory and cardiovascular strain, whereas heat effects are more concentrated during rare extremes. Globally, non-optimal temperatures account for about 9.4% of all deaths, or roughly 5 million annually, with cold responsible for the vast majority.00054-3/fulltext) In Europe, a health impact assessment of 854 cities estimated 203,620 annual excess deaths from cold and 20,173 from heat between 2000 and 2019, yielding a cold-to-heat ratio exceeding 10 to 1, with the highest burdens in eastern regions.00023-2/fulltext) Cold extremes, including snaps, elevate mortality risks primarily via hypothermia, infection exacerbation, and reduced physical activity, while heat waves trigger acute failures like heat stroke and dehydration; however, the relative risk increase per degree deviation is often steeper for heat (e.g., 8.9–12.1% mortality rise during heat events versus more gradual cold impacts).62114-0/fulltext) Despite this, cold events' higher frequency in temperate zones sustains their greater overall toll.[120] Projections under climate change scenarios suggest declining cold-related deaths may offset rising heat-related ones, but cold extremes are expected to remain the dominant temperature-mortality driver through 2100 in most regions, assuming no major adaptation shifts.00081-4/fulltext) For instance, in the United States, extreme cold days correlate with 0.26–0.27% higher mortality among older adults, comparable to heat effects, yet baseline cold exposure amplifies total impacts.[121] These patterns underscore that while heat waves garner attention for acute spikes, empirical data consistently affirm cold extremes' superior aggregate risk.[122]Societal and Economic Impacts
Infrastructure and Energy Demands
Heat waves significantly elevate electricity demand, primarily due to increased use of air conditioning and cooling systems in residential, commercial, and industrial sectors. In the Eastern United States, a heat wave in June 2025 caused electricity demand to surge, with regional grids experiencing peaks driven by cooling loads that strained supply capacities. Globally, electricity consumption rose by 4.3% in 2024 compared to the prior year, nearly double the decade-long average, as heat waves amplified air conditioning needs across regions like China, the United States, and India. In August 2024 alone, global electricity demand increased by 79 terawatt-hours (9%) over August 2023, with 44 terawatt-hours attributable to cooling demands. This surge often leads to record demand response activations; for instance, U.S. utilities dispatched demand response programs 411 times in summer 2024, curtailing 11,000 megawatt-hours to avert shortages, a marked rise from 2023 levels. Power generation and transmission infrastructure face compounded stresses during such events, as high temperatures reduce the efficiency of thermal power plants and cause transmission lines to sag, increasing outage risks. Peer-reviewed analysis indicates heat waves elevate outage frequency by 3.9% to 4.0% and extend durations by 7.9% to 8.3%, particularly in systems reliant on overhead lines and fossil fuel generation. Utilities may implement rolling blackouts or emergency measures to manage peaks, as seen in historical U.S. events where cooling demands overwhelmed grid capacity, prompting urban conservation appeals. Water scarcity exacerbates these issues, as thermoelectric plants require substantial cooling water that competes with heightened municipal and agricultural needs during droughts often coinciding with heat waves. Transportation infrastructure is also vulnerable, with extreme heat causing asphalt roads to soften and buckle, rail tracks to warp and expand, and necessitating speed reductions to prevent derailments. In mid-latitude regions, including Europe and North America, such failures have disrupted freight and passenger services, with railways imposing operational limits during prolonged high temperatures to mitigate buckling risks. Bridges and airport runways similarly suffer from thermal expansion, leading to closures or repairs; for example, documented cases in the U.S. and Europe show heat-induced deformations compromising structural integrity and delaying critical logistics. These disruptions amplify economic costs by hindering supply chains and emergency responses, underscoring the need for heat-resilient materials in aging infrastructure networks.Agricultural and Labor Productivity Losses
Heat waves during critical growth stages, such as pollination and grain filling, significantly reduce crop yields by accelerating senescence, disrupting photosynthesis, and increasing sterility. For instance, compound droughts and heatwaves have amplified maize yield losses by up to 44% compared to normal conditions in affected regions.[123] The 2012 U.S. heatwave substantially decreased revenues from corn and soybeans, with panel analyses showing persistent negative effects on crop values from such extreme events.[124] In tropical and subtropical areas, increased heat stress is projected to strongly reduce future yields of rice, maize, and cotton due to lowered plant productivity.[125] Livestock production faces direct declines from heat stress, which elevates body temperatures, reduces feed intake, and impairs metabolic functions. Dairy cows experience notable drops in milk yield and quality; U.S. studies indicate heat stress lowered dairy productivity in 2010, with an average 1% of annual milk yield lost from 2012–2016, projected to rise by about 30% by 2050 relative to 2016 levels.[126][127] Heat stress also diminishes liveweight gain in beef cattle and increases somatic cell counts in milk, further eroding farm incomes, particularly for smaller operations.[128][129] Labor productivity losses from heat waves primarily affect outdoor sectors like agriculture and construction, where workers face physiological limits on safe exertion. Extreme heat can cause 29% to 41% reductions in productivity on high-heat days, driven by heat strain, dehydration, and reduced work capacity.[130] Globally, heat stress is expected to result in a 2.2% loss of total working hours by 2030, equivalent to 80 million full-time jobs, with outdoor workers in agriculture and construction bearing 60% and 19% of these losses, respectively.[131][132] In the U.S., extreme heat notably impairs construction sector output, a key economic driver, through decreased work rates and increased downtime.[133] Older workers and those with heavy workloads exhibit heightened vulnerability, with productivity drops linked to cardiovascular strain and fatigue.[134]Quantified Economic Burdens
Heat waves impose significant economic burdens through direct damages, productivity losses, and indirect effects such as increased energy demands and supply chain disruptions. A peer-reviewed analysis of global economic data from 1992 to 2013 estimated that extreme heat events coincided with cumulative losses of approximately $16 trillion in GDP, equivalent to about 1.5% of per capita GDP on average for the world's poorest countries during affected periods.[135] These figures account for reduced labor productivity, agricultural shortfalls, and health-related costs, with disproportionate impacts on lower-income regions where adaptation measures are limited.[136] In Europe, heat waves in selected years between 1980 and 2018 resulted in total economic damages estimated at 0.3% to 0.5% of regional GDP, primarily from lost work hours and sector-specific disruptions in construction, tourism, and energy.[137] For instance, the 2003 European heat wave, which caused widespread crop failures and excess mortality, led to insured losses exceeding €13 billion alongside broader uninsured economic hits in agriculture and infrastructure.[137] Similarly, in Australia, annual economic losses from occupational heat stress totaled around US$6.2 billion as of recent assessments, driven by reduced worker output and health expenditures.[138] United States data from the National Oceanic and Atmospheric Administration (NOAA) tracks heat-related events within billion-dollar disasters, with cumulative costs since 1980 surpassing hundreds of billions in inflation-adjusted dollars; for example, the 2021 Pacific Northwest heat dome contributed over $8 billion in damages from wildfires, power outages, and agricultural losses exacerbated by the extreme temperatures.[139] Conservative estimates place annual U.S. economic losses from extreme heat at over $100 billion, encompassing productivity declines in outdoor labor sectors and heightened cooling demands that strain electricity grids.[140]| Region/Period | Estimated Economic Loss | Key Drivers | Source |
|---|---|---|---|
| Global (1992–2013) | $16 trillion cumulative | Productivity and growth reductions | Science Advances |
| Europe (selected years 1980–2018) | 0.3–0.5% of GDP | Labor and sectoral disruptions | Nature Communications |
| U.S. (annual average) | >$100 billion | Productivity, energy, health | One Billion Resilient |
| Australia (annual) | $6.2 billion | Occupational heat stress | PMC |
Environmental Impacts
Terrestrial Wildlife and Ecosystems
Heat waves impose acute physiological stress on terrestrial wildlife, often exceeding thermal tolerances and leading to direct mortality, particularly in species with limited evaporative cooling capacities such as birds and small mammals. Ectothermic animals like insects face disrupted development, reproduction, and survival when temperatures surpass lethal thresholds, with studies documenting reduced population densities and altered community structures in affected habitats. For instance, severe heat events in desert environments have triggered catastrophic avian die-offs, where body temperatures rise uncontrollably, as modeled in projections linking intensified heat waves to heightened extinction risks for heat-sensitive species.[142][143] Mammalian responses vary by body size and habitat, with larger endotherms experiencing chronic sub-lethal effects like reduced foraging and reproductive success due to impaired heat dissipation, prompting evolutionary shifts toward smaller body sizes in warming climates. In forested ecosystems, compounded heat and drought exacerbate tree mortality through hydraulic failure and pathogen outbreaks, such as bark beetle infestations, diminishing canopy cover and altering understory composition. Empirical data from U.S. assessments indicate that warming-driven extremes have amplified wildfire frequency and insect outbreaks, reducing biodiversity and shifting dominant species toward more heat-resilient taxa.[144][145][146] Ecosystem-level disruptions include phenological mismatches, where heat-accelerated plant flowering desynchronizes with pollinator activity, cascading to reduced seed set and prey availability for herbivores. Invertebrate declines from heat stress propagate through food webs, impacting predators and scavengers, while habitat fragmentation limits migration to cooler refugia. Observations from North American heat domes, such as the 2021 event, revealed elevated small mammal and reptile mortality, underscoring vulnerabilities in mid-latitude biomes where adaptive behaviors like burrowing or shade-seeking prove insufficient against prolonged extremes. Long-term, these pressures contribute to range contractions and local extirpations, with peer-reviewed syntheses forecasting accelerated species turnover in terrestrial communities under continued warming.[147][148]Aquatic and Marine Heatwaves
Aquatic heatwaves occur in freshwater systems such as lakes and rivers, characterized by prolonged periods of water temperatures exceeding seasonal climatological norms, typically defined relative to the 99th percentile threshold for at least five consecutive days, leading to disruptions in thermal stratification and oxygen solubility.[149] These events have increased in frequency and intensity globally, with lake surface water warming accelerating deoxygenation rates by enhancing metabolic demands and reducing dissolved oxygen saturation, as evidenced by analyses of over 11,000 lakes showing rapid declines in hypolimnetic oxygen during heatwaves.[150] In rivers, heatwaves outpace atmospheric counterparts, with documented rises linked to direct fish mortality, impaired reproduction, and shifts in macroinvertebrate assemblages, exacerbating vulnerabilities in thermally sensitive species like salmonids.[149] Marine heatwaves, defined as anomalous sea surface temperature excursions above the 99th percentile for five or more days, have similarly intensified, with global annual frequency rising 54% and cumulative intensity adding 17 extra days per year from 1925 to 2016 based on reanalysis data.[151] Observations from 1982 to 2023 reveal escalating cumulative intensity in U.S. coastal waters, particularly in the Northeast Pacific and Gulf of Maine, correlating with expanded spatial extent and prolonged durations driven by reduced heat dissipation and atmospheric blocking patterns.[152] NOAA monitoring confirms these trends extend globally, with events like the 2012 "Blob" in the Northeast Pacific demonstrating how persistent warm anomalies alter circulation and nutrient upwelling.[153] Ecological consequences in marine environments include mass mortality of foundation species, such as kelp forests and seagrasses, with meta-analyses of 79 events from 1980 to 2020 showing significant declines in biomass and cover, particularly during summer peaks that compound stress from low oxygen and acidification.[154] Coral reefs suffer acute bleaching, as thermal stress exceeds physiological tolerances, triggering symbiotic algae expulsion and skeletal whitening, with prolonged exposure reducing calcification rates by up to 50% in affected colonies.[155] Fisheries face cascading effects, including range shifts and recruitment failures in species like sardines and anchovies, as heatwaves suppress primary productivity through stratification-induced nutrient trapping.[156] In freshwater ecosystems, heatwaves amplify eutrophication by favoring cyanobacterial blooms under warmer, stratified conditions, as seen in deep reservoirs where phytoplankton biomass variability correlates with thermal extremes, potentially releasing toxins harmful to higher trophic levels.[157] These events also degrade water quality through elevated organic matter decomposition and reduced dilution flows, with global river analyses indicating worsened concentrations of nutrients and pollutants during compound drought-heatwave occurrences.[158] Overall, both aquatic and marine heatwaves disrupt biogeochemical cycles, with empirical data underscoring their role in regime shifts, such as from kelp-dominated to urchin barrens in oceans or from cold-water to warm-water fish communities in lakes, though recovery trajectories depend on event severity and pre-existing stressors.[155][159]Feedback Loops with Other Hazards
Heat waves often compound with droughts, forming a positive feedback loop wherein elevated temperatures accelerate soil moisture evaporation and reduce vegetation transpiration, thereby intensifying drought conditions, while diminished soil moisture in turn limits evaporative cooling, prolonging and amplifying subsequent heat episodes.[160][68] This interaction has been observed to increase in frequency globally, with concurrent heat waves and droughts occurring more often since the mid-20th century, particularly in regions like the Mediterranean, southern Africa, and parts of North America, under high confidence from observational data.[68] Similarly, heat waves interact with wildfires through heightened fire weather conditions—characterized by low humidity, high temperatures, and dry fuels—that elevate ignition risks and fire spread rates, while wildfire smoke and particulates can trap heat or alter local atmospheric dynamics, exacerbating thermal stress in affected areas.[161][68] For instance, during the 2021 Pacific Northwest heat dome, antecedent drought and extreme heat fueled unprecedented wildfire activity across Canada and the U.S., releasing approximately 1.8 billion tons of CO2 equivalent and contributing to cascading air quality degradation that compounded heat-related mortality.[162] These compound events demonstrate how heat-driven desiccation primes ecosystems for combustion, with post-fire landscapes exhibiting reduced albedo and increased erosion vulnerability, potentially feeding back into longer-term drought persistence.[163] Heat waves can also precede or coincide with pluvial hazards like flash floods via soil preconditioning: prolonged dry heat compacts and hardens soils, reducing infiltration capacity and elevating runoff during intense rainfall, thus transforming antecedent aridity into heightened flood severity.[164] Empirical records, such as the 2021 European floods following heat-induced dryness in Germany, illustrate this dynamic, where antecedent heat waves contributed to 20-30% higher peak discharges in urbanized basins compared to non-preconditioned events.[165] Such feedbacks underscore the non-linear amplification in compound hazard risks, with models projecting 2-5 times greater likelihood of these sequences under 2°C global warming relative to pre-industrial levels.[68]Adaptation and Mitigation Strategies
Technological and Behavioral Adaptations
Air conditioning systems have demonstrably reduced heat-related mortality during extreme heat events. In the United States, widespread adoption of residential air conditioning accounted for approximately 28.6% of the decline in deaths due to high temperatures between 1960 and 2004.[166] Similarly, in Japan, air conditioning use was associated with a 36% reduction in heat-related deaths under baseline scenarios, with potential for further decreases through optimized thermostat settings.[167] These systems lower indoor temperatures by circulating cooled air, mitigating hyperthermia risks, though their efficacy depends on accessibility and energy infrastructure reliability during prolonged heat waves.[168] Reflective roofing materials, known as cool roofs, mitigate urban heat islands by increasing solar reflectance, thereby reducing surface temperatures and cooling demands. Solar-reflective cool roofs can decrease peak cooling energy needs in air-conditioned buildings by 11-27%, with higher reflectance values (e.g., 0.85) potentially cutting annual energy use by up to 12% in hot climates.[169][170] These coatings or membranes reflect sunlight rather than absorbing it, lowering ambient outdoor temperatures and easing strain on electrical grids during heat waves.[171] Heat-health early warning systems (HHEWS) integrate weather forecasts with health risk thresholds to issue alerts, enabling proactive measures that avert fatalities. Evaluations indicate HHEWS can reduce heat-related mortality by triggering public health responses, such as opening cooling centers, with cost-benefit analyses showing substantial savings in morbidity and healthcare utilization.[172][173] In European cities, alert effectiveness varies by local factors like population vulnerability, but overall implementation has correlated with decreased excess deaths during forecasted events.[174] Personal cooling devices, including evaporative vests and phase-change materials, provide targeted relief for outdoor workers exposed to heat stress. These garments absorb body heat through evaporation or material transitions, reducing core temperature rises and fatigue in personal protective equipment scenarios.[175] Field tests demonstrate they extend safe work durations in high-heat environments by countering metabolic heat buildup.[176] Behavioral adaptations encompass individual actions like scheduling activities outside peak heat hours, maintaining hydration, and seeking shaded or air-conditioned spaces. Studies categorize these into awareness-raising and personal risk reduction, such as wearing light clothing and limiting exertion, which collectively lower heat strain incidence.[177] Community-level behaviors, including use of cooling centers during alerts, further amplify protection for vulnerable groups, though adherence depends on education and accessibility.[178] Natural ventilation and shading strategies can reduce reliance on mechanical cooling by up to 80% in simulations of heat wave conditions.[179]Urban Design and Policy Interventions
Urban design strategies to mitigate heat waves focus on countering the urban heat island (UHI) effect, where impervious surfaces like asphalt and concrete absorb and re-radiate solar heat, elevating local temperatures by 1–7°C compared to rural areas.[180] Interventions such as increasing urban vegetation cover through tree planting and parks provide shade and evapotranspiration cooling, with studies showing parks can lower surrounding air temperatures by 1–4°C during peak heat.[181] Cool pavements and roofs, using high-albedo materials to reflect sunlight, have demonstrated reductions in surface temperatures by up to 10–20°C and ambient air by 1–2°C in modeled urban scenarios.[182] Green roofs, vegetated rooftops that insulate buildings and promote evaporative cooling, can decrease roof surface temperatures by 30–40°C and reduce building cooling energy demands by up to 70%, though their ambient air cooling effect is more modest at 0–1°C citywide without widespread adoption.[183] Cool roofs, coated with reflective materials, outperform green roofs in rapid daytime cooling, achieving average near-surface temperature drops of 1.2°C across urban areas, with minimal nighttime warming, based on simulations integrating radiative and convective heat transfer principles.[184] Combining these—such as cool roofs with street-level vegetation—yields synergistic effects, reducing UHI intensity by 2–5°C in high-density zones, as evidenced by field measurements and energy balance models.[185] Policy interventions enforce these designs through building codes, zoning regulations, and incentives. For instance, mandates for minimum green coverage in new developments, as implemented in cities like Singapore and parts of Europe, have correlated with 10–20% UHI reductions via expanded canopy cover.[181] Heat action plans, which integrate urban design with emergency protocols, provide empirical success: Ahmedabad's 2013 plan, emphasizing early warnings, cooling centers, and greening incentives, reduced heat-related deaths by approximately 20% during subsequent waves by prioritizing vulnerable areas.[186] In the U.S., federal programs like EPA's Heat Island Reduction initiatives offer grants for cool roof retrofits, yielding 23–25% drops in UHI-attributable mortality risks during modeled heat events.[187] [178] However, effectiveness varies by implementation scale; partial adoption (e.g., <50% roof coverage) limits benefits to under 0.5°C cooling, underscoring the need for comprehensive, data-driven policies over sporadic efforts.[188]Empirical Evidence of Effectiveness
Air conditioning represents one of the most empirically validated adaptation measures against heatwave mortality. A multi-country study across 388 locations in 12 countries, analyzing data from 2000 to 2016, found that a 10% increase in air conditioning prevalence was associated with a 1.8% reduction in heat-related mortality risk, independent of other socioeconomic factors.[189] In the United States, historical expansion of residential air conditioning since the 1960s correlates with a 75-80% decline in heat-related death rates, even as temperatures rose, with per capita heat deaths dropping from 7.3 per million in the 1920s to under 2 per million by 2005.[168] Japanese modeling of urban heat scenarios estimates that air conditioning could avert 36-47% of heat-related deaths under projected warming, based on exposure-response functions from national health data.[167] These findings hold across diverse climates, though access disparities—such as lower penetration in low-income or elderly households—limit broader protective effects.[190] Heat warning and early alert systems exhibit variable effectiveness, with systematic reviews synthesizing epidemiological evidence from multiple events concluding they reduce mortality by prompting behavioral changes like staying indoors or hydrating.[191] For instance, a review of 12 studies found consistent associations between warnings and lower heat-attributable deaths, particularly in systems integrated with community outreach.[192] However, evaluations of U.S. National Weather Service alerts from 2001-2006 across 63 cities showed no significant mortality reduction in most locations, attributing this to inadequate public response or confounding by acclimatization.[193] Recent implementations, such as China's graded heat-health forecasts, demonstrate stronger impacts when tailored to vulnerability indices, averting an estimated 10-20% of excess hospitalizations during peaks.[194] Effectiveness hinges on dissemination reach and behavioral compliance, with urban-rural gaps persisting. Urban design interventions targeting heat islands provide empirical cooling benefits, though health outcome linkages are often modeled rather than directly observed. Green and blue infrastructure, including vegetation and reflective surfaces, reduced daytime surface temperatures by 1-4°C in empirical assessments of European and North American cities, with peak effects during heatwaves.[181] A study of urban squares found that increasing albedo and vegetation cover improved air temperatures by up to 2°C and lowered physiological stress indices for pedestrians.[195] Cool and green roofs, simulated via regional climate models validated against observations, mitigated urban heat islands by 0.5-1.5°C regionally, with greater efficacy in high-density areas.[196] Longitudinal data on mortality remains sparse, but proxy indicators like reduced emergency calls correlate with greening projects in cities like Toronto post-2003 heatwave adaptations.[197] Community-based behavioral interventions, such as education on hydration and timing activities, show modest empirical gains in vulnerability reduction. A systematic review of trials found short-term knowledge improvements but inconsistent long-term adherence, with effect sizes on self-reported heat stress around 10-15% in targeted groups like the elderly.[198] Planned adaptations overall have decreased population heat sensitivity in Europe by 20-50% since the 1970s, per time-series analyses, though attribution to specific policies versus acclimatization is inconclusive.[197] For mitigation strategies aimed at curbing greenhouse gas emissions, direct empirical evidence of reduced heatwave intensity or frequency remains limited, as global efforts post-Kyoto have coincided with rising temperatures and events. Local-scale emission controls, however, contribute to urban heat island attenuation, with observational data from low-carbon districts showing 0.5-1°C cooler peaks compared to high-emission baselines.[199] Broader causal impacts rely on attribution models rather than randomized or quasi-experimental designs, highlighting methodological challenges in isolating human forcing from natural variability.[200]Attribution Debates
Methodological Challenges in Blaming Climate Change
Attribution of heat waves to anthropogenic climate change typically employs probabilistic frameworks, such as those comparing the likelihood and intensity of an observed event in factual (with human emissions) versus counterfactual (pre-industrial) model simulations. These methods, advanced since the early 2010s, quantify changes in risk but encounter fundamental limitations in isolating causal contributions amid natural variability and model uncertainties.[201][202] A primary challenge stems from biases in global climate models (GCMs) used for simulations, which often underestimate internal climate variability, leading to overconfident attributions that systematically inflate the anthropogenic signal. For example, multi-model ensembles exhibit reduced spread in variability compared to observations, resulting in higher fractions of events deemed attributable to external forcing rather than natural fluctuations.[203] This issue is compounded by model errors in representing physical processes relevant to extremes, such as soil moisture feedbacks or atmospheric circulation patterns like Rossby waves, which can bias heat wave simulations in regions like Europe during summer.[204][205] Event definition poses another hurdle, as heat waves vary in spatial scale, duration, and metrics (e.g., daily maximums for health impacts versus multi-day averages for agriculture), complicating consistent analysis across local and regional contexts. Observational records, essential for validating trends, suffer from inhomogeneities due to factors like urbanization-induced heat island effects or changes in measurement practices, which can artifactually amplify apparent warming signals without adjustment.[206] Sparse data networks in the Global South further limit robust trend detection, exacerbating reliance on potentially flawed models for attribution in data-poor areas.[205] Natural variability, including modes like the El Niño-Southern Oscillation (ENSO) or Atlantic Multidecadal Oscillation (AMO), often dominates decadal-scale heat wave occurrences and is challenging to fully disentangle from anthropogenic trends in short-term events. Explicit inclusion of such variability in attribution frameworks increases overall uncertainty, as models may inadequately capture teleconnections or decadal oscillations, potentially leading to overstated human influence.[207] Real-time attribution, demanded by media post-event, is particularly constrained by computational demands for high-resolution ensembles and the need for rapid bias corrections, often yielding preliminary results with wide confidence intervals.[202][208] These methodological issues contribute to debates over attribution robustness, with heat waves—despite clearer signals than precipitation extremes—still subject to interpretive variability across studies. Discrepancies between modeled and observed trends, such as lower model-simulated heat wave intensification in parts of Europe, underscore the need for improved process representation and hybrid statistical-dynamical approaches to reduce over-reliance on imperfect simulations.[206][205]Role of Natural Forcing vs. Human Activity
Natural forcing encompasses external drivers such as solar irradiance variations and volcanic aerosol injections, which can modulate global temperatures over decadal to centennial scales, while internal variability arises from chaotic atmospheric and oceanic processes, including the El Niño-Southern Oscillation (ENSO), Pacific Decadal Oscillation (PDO), and Atlantic Multidecadal Oscillation (AMO).[209][210] These natural elements have historically produced intense heat waves without significant anthropogenic influence; for instance, the 1930s Dust Bowl era in the United States featured the most severe heat waves in recorded history, with widespread temperatures exceeding 40°C (104°F) driven by persistent drought, soil degradation, and atmospheric blocking patterns rather than elevated greenhouse gas levels, which were then comparable to early industrial emissions.[18][211] Positive phases of the AMO since the mid-1990s have contributed substantially to regional warming in the North Atlantic and North America, accounting for up to 72% of contiguous U.S. summer temperature increases in some analyses, amplifying heat wave frequency through enhanced sea surface temperatures and jet stream persistence.[212][213] Anthropogenic forcing, dominated by greenhouse gas emissions, establishes a long-term warming trend that increases the baseline for heat wave potential, but event attribution studies often overemphasize its role in specific occurrences by relying on climate models that inadequately capture local-scale natural variability, which can predominate and explain event timing and magnitude.[205][214] For example, ENSO events like the strong 2015-2016 El Niño exacerbated global heat waves through teleconnections that shifted weather patterns, independent of the anthropogenic signal, while PDO shifts have modulated Pacific-influenced extremes.[209] On regional scales, natural decadal variations rival or exceed forced anthropogenic changes, as seen in simulations distinguishing internal oscillations from external forcings.[215] Critiques highlight methodological pitfalls, including insufficient adjustment for urban heat island (UHI) effects in observational data—where urbanization can inflate recorded temperatures by 1-3°C in cities during heat waves—and model biases that underestimate variability, leading to probabilistic claims like "doubled risk" that conflate trend enhancement with causation.[214][216] Solar forcing contributes modestly to multidecadal temperature fluctuations, with cycle peaks like the ongoing Solar Cycle 25 (peaking around 2024-2025) potentially adding 0.1°C to global means via increased irradiance, though its net effect since the 1950s has been near-neutral compared to greenhouse gases.[217] Volcanic eruptions provide transient cooling that interrupts heat wave trends, as in the 1991 Mount Pinatubo event, which lowered global temperatures by ~0.5°C for 1-2 years.[210] Overall, while anthropogenic forcing elevates heat wave probabilities in a probabilistic sense, empirical evidence underscores that natural factors remain primary modulators for individual events, with attribution overconfidence stemming from institutional preferences for forced responses in simulations that poorly resolve chaotic dynamics.[205][206]Critiques of Overstated Projections
Climate models have been critiqued for systematically overestimating the frequency and duration of heat waves due to biases in simulating atmospheric circulation. A 2015 analysis in Climate Dynamics found that many global climate models exhibit overly persistent blocking patterns, leading to simulated heat waves that last longer and occur more often than historical observations indicate; for instance, models projected European summer heat waves persisting beyond observed durations by factors of 2-3 times in certain CMIP5 ensembles. This circulation bias persists in subsequent model generations, contributing to inflated projections of extreme heat persistence under future warming scenarios.[218] [219] Projections of heat wave impacts often overlook historical adaptation trends, resulting in overstated mortality and economic forecasts. In the United States, heat-related deaths declined by over 80% from the 1960s to the 2010s despite rising baseline temperatures, driven by air conditioning proliferation, early warning systems, and urban planning changes—factors frequently underweighted in integrated assessment models. Roger Pielke Jr. has argued that event attribution studies and IPCC-linked projections downplay such adaptations, projecting unmitigated increases in heat wave fatalities that contradict empirical reductions; for example, a 2021 review noted that assuming static vulnerability in models yields death toll estimates 3-5 times higher than adjusted scenarios incorporating behavioral responses. This omission stems partly from model reliance on thermodynamic scaling alone, neglecting dynamic human factors.[220][221] Uncertainties from internal climate variability and model equilibrium assumptions further amplify overestimation risks in near-term heat wave forecasts. Judith Curry highlights that projections spanning 20-30 years often attribute extremes predominantly to anthropogenic forcing while underplaying natural oscillations like the Atlantic Multidecadal Oscillation, which can account for 30-50% of decadal heat wave variability in mid-latitudes; ignoring this leads to inflated confidence in upward trends. Peer-reviewed critiques, including those in Earth's Future, note that overestimation of temperature variability in CMIP6 models erodes reliability for projecting heat wave intensity, with some ensembles simulating extremes exceeding observed distributions by 1-2 standard deviations. These issues are compounded by selective sourcing in media and policy summaries, which prioritize high-end model outcomes from ensembles known to run "hot" due to cloud feedback parameterizations.[222][205]Notable Events
Pre-2020 Milestones
The 1936 North American heat wave, occurring amid the Dust Bowl era, stands as one of the deadliest and most severe in U.S. history, with temperatures exceeding 100°F (38°C) for extended periods across the Midwest and Great Plains, reaching 121°F (49°C) in North Dakota and sustaining highs above 100°F in Chicago for eight consecutive days.[63] This event contributed to approximately 5,000 deaths nationwide, exacerbated by drought, poor air quality from dust storms, and limited access to cooling or medical care during the Great Depression.[62] It set numerous state and city temperature records that persisted for decades, highlighting vulnerabilities in rural and urban areas to prolonged extreme heat without modern infrastructure.[63] In 1980, a multi-month heat wave and drought gripped the central and eastern United States from June to September, marking the deadliest such event in modern U.S. records with over 1,250 fatalities, primarily in Missouri and Tennessee, due to heat stress and associated cardiovascular failures among the elderly and those without air conditioning.[223] Average temperatures deviated 6–10°F (3–6°C) above normal, leading to crop failures, energy shortages, and an estimated $20 billion in damages (in 2023 dollars), underscoring the compounding effects of heat on agriculture and public health infrastructure.[224] The 1995 Chicago heat wave, lasting from July 12–16, saw temperatures climb to 106°F (41°C) with high humidity, resulting in over 700 deaths in the city alone, disproportionately affecting low-income and isolated residents in urban heat islands lacking ventilation or social support.[223] This event prompted early advancements in urban heat emergency protocols, revealing systemic issues in emergency response and housing quality.[225] Europe's 2003 summer heat wave, peaking in August, brought temperatures of 35–40°C (95–104°F) across France, Germany, and other nations, causing an estimated 70,000 excess deaths continent-wide, including 14,800 in France from dehydration, heatstroke, and overwhelmed hospitals.[226] [227] Forest fires, reduced hydropower, and agricultural losses amplified economic impacts exceeding €13 billion, while the event's persistence—driven by stagnant high-pressure systems—exposed gaps in heat preparedness for aging populations in urban settings.[228] Russia's 2010 heat wave, from June to August, shattered national temperature records with averages 7–10°C (13–18°F) above normal in western regions, leading to roughly 55,000 excess deaths from heat-related illnesses, compounded by wildfire smoke and air pollution that degraded respiratory health.[229] Drought-induced crop failures slashed wheat production by 25–30%, triggering global food price spikes, while economic losses topped $15 billion from fires that scorched over 17 million acres; analyses attributed the anomaly partly to natural atmospheric blocking patterns rather than solely anthropogenic forcing.[230]2020s Developments Including 2024-2025 Anomalies
The decade of the 2020s has witnessed intensified heat wave activity in various regions, with events characterized by prolonged high temperatures exceeding local thresholds by margins larger than historical norms. In the United States, the average heat wave intensity rose to 2.5°F above thresholds during this period, affecting 46 of 50 monitored metropolitan areas. Globally, the spatial extent of heat waves has expanded, with average sizes increasing by 1.5 to 2 times across most land areas in recent years, driven by shifts in atmospheric circulation patterns.[18][231] A prominent early event was the 2021 Western North America heat dome, which peaked from June 24 to 30, setting all-time records in Canada and the U.S. Pacific Northwest; Lytton, British Columbia, reached 49.6°C on June 29, contributing to over 600 heat-related deaths in British Columbia alone. In Europe, the 2022 heat wave from July 12 to 19 shattered the UK's all-time high at 40.3°C in Coningsby on July 19, while Portugal recorded 47.3°C in Pinhão, exacerbating wildfires and resulting in thousands of excess deaths across the continent. The 2023 Northern Hemisphere summer featured simultaneous extremes, including Canada's Yellowknife reaching 37.1°C amid unprecedented wildfires and southern Europe's temperatures surpassing 48°C in Sicily, linked to over 61,000 heat-attributable deaths region-wide.[232][233] The year 2024 marked the warmest on instrumental record, with global average temperatures reaching approximately 1.55°C above pre-industrial levels, surpassing 2023's previous high; this included a new daily global peak of 17.16°C on July 22. Continental records fell across all monitored regions, with heat waves compounding marine anomalies like the persistent Kuroshio Extension event, fueled by anticyclonic eddies and enhanced shortwave radiation. In the U.S., 26 cities endured dangerous extreme heat waves from June to August, while China broke monthly temperature records in April, May, and August. These events amplified risks, adding an estimated 41 days of dangerous heat globally per analyses from weather attribution groups.[234][235][236] Into 2025, anomalies persisted but moderated post the 2023-2024 El Niño, with January-June global anomalies at +1.21°C, ranking second-highest but trailing 2024's pace. The U.S. summer opened with a heat dome affecting over 255 million people in June, featuring multi-day events in the Midwest and West; Wisconsin's first major heat wave of the season brought 80-90°F with high humidity around late June. An unusual October heat surge projected temperatures above 80°F across 46 states through mid-month, exceeding 90°F in 24, marking unprecedented late-season warmth for millions. Marine anomalies reemerged with the "Blob" expansion in the North Pacific by early October, covering coasts from Alaska to California and breaking multidecadal warming trends in sea surface temperatures. These developments highlight variability, as 2025's trajectory aligns more closely with gradual warming expectations absent strong ENSO forcing.[237][238][239][240][241][242] ![1940-2024 Global surface temperature - stacked - Copernicus.jpg][center] Such anomalies underscore debates on attribution, where natural oscillations like Rossby waves contributed to regional persistence, alongside long-term trends; however, empirical records confirm elevated frequencies without isolating causal dominance.[235][231]References
- https://science.[nasa](/page/NASA).gov/climate-change/faq/is-the-sun-causing-global-warming/
- https://www.[climate](/page/Climate).gov/news-features/understanding-climate/climate-change-incoming-sunlight
