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Tropical Asia
Tropical Asia refers to the entirety of the areas in Asia with a tropical climate. These areas are of geographic and economic importance due to their natural resources and biodiversity, which include many species of agricultural value. There are 16 countries in tropical Asia, ranging in size from around 610 square kilometres (240 square miles) (Singapore) to 3,000,000 km2 (1,200,000 sq mi) (India). The total population as of 2006 was 1.6 billion, predominantly rural, and projected to reach 2.4 billion by 2025.[needs update] Climate in tropical Asia is subject to seasonal weather patterns with the two monsoons and the amount of tropical cyclones in the three core areas of cyclogenesis (the Bay of Bengal, north Pacific Ocean and South China Sea). Stressors on the environment include growing urbanization, land industrialization, economic development, land degradation, environmental issues, and increased pollution, all of which are contributing to changes in climate.
In tropical Asia, the distribution and character of the rain forest changes with elevation in the mountains. In Thailand, for instance, the area of tropical forests could increase from 45% to 80% of the total forest cover, while in Sri Lanka, a substantial change in dry forest and decrease in wet forest might occur. With predictable increases in evapotranspiration and rainfall changeability, likely a negative impact on the viability of freshwater wetlands will occur, resulting in contraction and desiccation. Sea level and temperature rises are the most likely major climate change-related stresses on ecosystems. Coral reefs might be capable of surviving this intensification, but suffer bleaching from high temperatures. Landward migration of mangroves and tidal wetlands is likely to be inhibited by human infrastructure and human activities.
Coastal lands in particular are extremely vulnerable to sea-level rise as a result of climate change. Densely settled and intensively used low-level coastal plains, deltas, and islands are particularly susceptible to coastal erosion and land loss, sea flooding and barrage, especially vulnerable to coastal erosion and land loss, inundation and sea flooding, upstream movement of the saline/freshwater front and seawater incursion into freshwater lenses. Mainly at risk are large delta regions of Bangladesh, Myanmar, Vietnam and Thailand, and the low-lying areas of Indonesia, Malaysia and the Philippines. Socio-economic effects may be noticeable to major cities and ports, tourist resorts, artisanal and commercial fishing and coastal agriculture, and infra-structure development. Global studies project that by 2100, up to 410 million people (59 per cent in tropical Asia) may be affected by a 1-metre rise in sea level.
In tropical Asia, the Himalayas are crucial to the provision of water during the continental monsoon season in Asia. Augmented temperatures and seasonal variability could cause a backdrop of glaciers and increasing danger from glacial lake outburst floods. Then, a diminution of average flow of snow-fed rivers, mixed with an increase in peak flows and sediment yield, could have major effects on hydropower generation, urban water supply and agriculture. Supply of hydropower generation from snow-fed rivers can occur in the short term, though not in the long term—run off snow-fed rivers might change as well. As stated before, an increased amount economic, agriculture, and industrial resources, can affect climate, but it can put an extra stress on water. Lower level basins are expected to be most affected. Hydrological changes on island and drainage basins will be relatively low to tropical Asia, despite those related to sea rise.
The sensitivity of major cereal and tree crops, changes in temperature, moisture and CO2 concentration of the magnitudes estimated for the region has been done in many studies. One instance is the influences on rice fields, wheat yield and sorghum yield imply that any increase in production associated with CO2 fertilization will most likely be offset by reductions in yield from temperature or moisture changes. Even though climate impression may result huge changes in crop yields, storage, and distribution., the continuing effect of the region-wide changes is tentative because of varietal disparity; local disparity in emergent season, crop management, etc. (the lack of inclusion of possible diseases, pests, and microorganisms in crop model simulations); and the vulnerability of agricultural (especially low-income rural population) areas to periodic environmental hazards such as floods, droughts and cyclones.
The occurrence and level of some vector-borne diseases have risen with global warming. Diseases such as malaria, schistosomiasis and dengue, which are significant causes of mortality and morbidity in tropical Asia, are very climate-sensitive and likely to spread into new regions on the margins of currently widespread areas as a result of climate change. Populations that are newly affected will initially experience higher fatality rates. According to one study specifically focused on climate influences on infectious disease in presently vulnerable regions, a growth in epidemic potential of 12-27 per cent for malaria and 31 to 47 per cent for dengue and a decrease of schistosomiasis of 11-17 per cent are expected under a range of Global Climate Model (GCM) scenarios through climate change. Waterborne and water-related infectious diseases, already accounting for the majority of epidemic emergencies in the area, are also expected to increase when higher temperatures and higher humidity are placed over on existing conditions and estimated upsurge in population, urbanization, deduction of water quality and other trends.
Tropical Asia has an abundance of edible resources. The following section involves various edible resource plants.
Bananas are the most famous members of Musa with 21 species and edible subspecies. Especially in the Mayan area, it is probably native to Southeast Asia and widely refined in the tropics. Black pepper is vine to the East Indies—made by drying the whole fruit (peppercorn); white pepper is made by first hulling the fruit, then grinding. The majority of production is in India and Indonesia; outside the region, America is a chief importer. Four of the main cultivators of this plant are capsicum annuum: cayenne pepper, sweet pepper, paprika, and jalapenos grown in temperate regions.
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Tropical Asia AI simulator
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Tropical Asia
Tropical Asia refers to the entirety of the areas in Asia with a tropical climate. These areas are of geographic and economic importance due to their natural resources and biodiversity, which include many species of agricultural value. There are 16 countries in tropical Asia, ranging in size from around 610 square kilometres (240 square miles) (Singapore) to 3,000,000 km2 (1,200,000 sq mi) (India). The total population as of 2006 was 1.6 billion, predominantly rural, and projected to reach 2.4 billion by 2025.[needs update] Climate in tropical Asia is subject to seasonal weather patterns with the two monsoons and the amount of tropical cyclones in the three core areas of cyclogenesis (the Bay of Bengal, north Pacific Ocean and South China Sea). Stressors on the environment include growing urbanization, land industrialization, economic development, land degradation, environmental issues, and increased pollution, all of which are contributing to changes in climate.
In tropical Asia, the distribution and character of the rain forest changes with elevation in the mountains. In Thailand, for instance, the area of tropical forests could increase from 45% to 80% of the total forest cover, while in Sri Lanka, a substantial change in dry forest and decrease in wet forest might occur. With predictable increases in evapotranspiration and rainfall changeability, likely a negative impact on the viability of freshwater wetlands will occur, resulting in contraction and desiccation. Sea level and temperature rises are the most likely major climate change-related stresses on ecosystems. Coral reefs might be capable of surviving this intensification, but suffer bleaching from high temperatures. Landward migration of mangroves and tidal wetlands is likely to be inhibited by human infrastructure and human activities.
Coastal lands in particular are extremely vulnerable to sea-level rise as a result of climate change. Densely settled and intensively used low-level coastal plains, deltas, and islands are particularly susceptible to coastal erosion and land loss, sea flooding and barrage, especially vulnerable to coastal erosion and land loss, inundation and sea flooding, upstream movement of the saline/freshwater front and seawater incursion into freshwater lenses. Mainly at risk are large delta regions of Bangladesh, Myanmar, Vietnam and Thailand, and the low-lying areas of Indonesia, Malaysia and the Philippines. Socio-economic effects may be noticeable to major cities and ports, tourist resorts, artisanal and commercial fishing and coastal agriculture, and infra-structure development. Global studies project that by 2100, up to 410 million people (59 per cent in tropical Asia) may be affected by a 1-metre rise in sea level.
In tropical Asia, the Himalayas are crucial to the provision of water during the continental monsoon season in Asia. Augmented temperatures and seasonal variability could cause a backdrop of glaciers and increasing danger from glacial lake outburst floods. Then, a diminution of average flow of snow-fed rivers, mixed with an increase in peak flows and sediment yield, could have major effects on hydropower generation, urban water supply and agriculture. Supply of hydropower generation from snow-fed rivers can occur in the short term, though not in the long term—run off snow-fed rivers might change as well. As stated before, an increased amount economic, agriculture, and industrial resources, can affect climate, but it can put an extra stress on water. Lower level basins are expected to be most affected. Hydrological changes on island and drainage basins will be relatively low to tropical Asia, despite those related to sea rise.
The sensitivity of major cereal and tree crops, changes in temperature, moisture and CO2 concentration of the magnitudes estimated for the region has been done in many studies. One instance is the influences on rice fields, wheat yield and sorghum yield imply that any increase in production associated with CO2 fertilization will most likely be offset by reductions in yield from temperature or moisture changes. Even though climate impression may result huge changes in crop yields, storage, and distribution., the continuing effect of the region-wide changes is tentative because of varietal disparity; local disparity in emergent season, crop management, etc. (the lack of inclusion of possible diseases, pests, and microorganisms in crop model simulations); and the vulnerability of agricultural (especially low-income rural population) areas to periodic environmental hazards such as floods, droughts and cyclones.
The occurrence and level of some vector-borne diseases have risen with global warming. Diseases such as malaria, schistosomiasis and dengue, which are significant causes of mortality and morbidity in tropical Asia, are very climate-sensitive and likely to spread into new regions on the margins of currently widespread areas as a result of climate change. Populations that are newly affected will initially experience higher fatality rates. According to one study specifically focused on climate influences on infectious disease in presently vulnerable regions, a growth in epidemic potential of 12-27 per cent for malaria and 31 to 47 per cent for dengue and a decrease of schistosomiasis of 11-17 per cent are expected under a range of Global Climate Model (GCM) scenarios through climate change. Waterborne and water-related infectious diseases, already accounting for the majority of epidemic emergencies in the area, are also expected to increase when higher temperatures and higher humidity are placed over on existing conditions and estimated upsurge in population, urbanization, deduction of water quality and other trends.
Tropical Asia has an abundance of edible resources. The following section involves various edible resource plants.
Bananas are the most famous members of Musa with 21 species and edible subspecies. Especially in the Mayan area, it is probably native to Southeast Asia and widely refined in the tropics. Black pepper is vine to the East Indies—made by drying the whole fruit (peppercorn); white pepper is made by first hulling the fruit, then grinding. The majority of production is in India and Indonesia; outside the region, America is a chief importer. Four of the main cultivators of this plant are capsicum annuum: cayenne pepper, sweet pepper, paprika, and jalapenos grown in temperate regions.