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Climate of Cyprus
Climate of Cyprus
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Cyprus from Space
Solar Map of the Island
Mountainous Geography on the northern coast
Seacoast from Southern Side
Sunsets on the island
Seacoast from Eastern side

Cyprus has a subtropical climate, Mediterranean and semi-arid type (Csa and BSh) according to Köppen climate classification,[1][2] with very mild winters on sea level and warm to hot summers. Snow is possible only in the Troodos Mountains in the central part of the island. Rain occurs mainly in winter, with summer being generally dry.

Temperatures

[edit]

Cyprus has one of the warmest climates and warmest winters in the Mediterranean part of the European Union. The average annual temperature on the coast is around 26 °C (79 °F) during the day and 17 °C (63 °F) at night. Generally, the warm season lasts about eight months. It begins in April, with average temperatures of 23–25 °C (73–77 °F) during the day and 13–15 °C (55–59 °F) at night, and ends in November, with average temperatures of 24–25 °C (75–77 °F) during the day and 14–17 °C (57–63 °F) at night. In the remaining four months of the year, the temperatures tend to remain mild, while sometimes exceeding 21 °C (70 °F) during the day. In Limassol, in the period January–February, the average maximum temperature is 18–20 °C (64–68 °F) during the day and 11–13 °C (52–55 °F) at night. In other coastal locations in Cyprus, the temperature is generally 16–18 °C (61–64 °F) during the day and 9–11 °C (48–52 °F) at night. In March and December in Limassol the average is 22–23 °C (72–73 °F) during the day and 12–14 °C (54–57 °F) at night; other coastal locations in Cyprus are generally 17–21 °C (63–70 °F) during the day and 8–11 °C (46–52 °F) at night.

The middle of summer (July and August) is usually hot, with an average maximum coastal temperature of around 37 °C (99 °F) during the day and around 28 °C (82 °F) at night. In the centre of the island (the highlands) the average temperature exceeds 37 °C (99 °F)). In June and September on the coast the average maximum temperature is usually around 30–32 °C (86–90 °F) during the day and around 19–21 °C (66–70 °F) at night. While large temperature fluctuations are rare on the coast, the centre of Cyprus has more variations – typically cool winters and hotter summers.[3]

Temperature of sea

[edit]

The average annual temperature of the sea around Cyprus is 21–22 °C (70–72 °F), from 17 °C (63 °F) in February to 27–28 °C (81–82 °F) in August (depending on the location). In the seven months from May to November the average sea temperature exceeds 20 °C (68 °F).[4]

Sea temperature
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec
Paphos [1] 18 17 17 18 20 24 26 27 26 24 22 19
Larnaca [2] 18 17 17 18 20 24 26 27 27 25 22 19
Limassol [3] 18 17 17 18 20 24 26 27 27 25 22 19
Argaka [4]
Ayia Napa [5]
Coral Bay [6]
Famagusta [7] Archived 2011-12-24 at the Wayback Machine
Kyrenia [8] 29
Latchi [9]
Nissi Bay [10]
Peyia [11]
Polis [12]
Protaras [13]

Sunshine

[edit]

In winter, Cyprus receives an average of 5–6 hours of sunlight per day, half of the 12–13 hours experienced at the height of summer.[4] This is about double that of cities in the northern half of Europe; for comparison, London has 1,461 hours.[5] However, in winter there can be more than four times more sunshine; for comparison, London has 37 hours[5] while coastal locations in Cyprus have around 180 hours of sunshine in December (that is, as much as in May in London).

Charts of selected locations

[edit]

On the coast

[edit]
Climate data for Paphos airport - near sea (Satellite view)
Month Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year
Mean daily maximum °C (°F) 17.0
(62.6)
16.9
(62.4)
18.5
(65.3)
21.3
(70.3)
24.4
(75.9)
27.7
(81.9)
29.9
(85.8)
30.4
(86.7)
28.8
(83.8)
26.6
(79.9)
22.4
(72.3)
18.6
(65.5)
23.6
(74.5)
Daily mean °C (°F) 12.5
(54.5)
12.3
(54.1)
13.6
(56.5)
16.3
(61.3)
19.5
(67.1)
22.8
(73.0)
25.2
(77.4)
25.7
(78.3)
23.8
(74.8)
21.5
(70.7)
17.5
(63.5)
14.2
(57.6)
18.7
(65.7)
Mean daily minimum °C (°F) 8.0
(46.4)
7.6
(45.7)
8.7
(47.7)
11.3
(52.3)
14.5
(58.1)
17.8
(64.0)
20.4
(68.7)
21.0
(69.8)
18.8
(65.8)
16.4
(61.5)
12.6
(54.7)
9.7
(49.5)
13.9
(57.0)
Average precipitation mm (inches) 80.2
(3.16)
64.2
(2.53)
34.3
(1.35)
18.7
(0.74)
5.30
(0.21)
1.60
(0.06)
0.30
(0.01)
0.00
(0.00)
3.80
(0.15)
18.0
(0.71)
66.4
(2.61)
93.9
(3.70)
386.7
(15.22)
Average precipitation days (≥ 1 mm) 9.9 8.0 5.5 4.1 1.3 0.3 0.1 0.0 0.6 2.5 5.8 8.7 46.6
Mean monthly sunshine hours 195.3 211.7 244.9 270.0 344.1 381.0 390.6 365.8 315.0 285.2 225.0 186.0 3,414.6
Source: Meteorological Service (Cyprus)[6]
Climate data for Larnaca airport - near sea (Satellite view)
Month Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year
Mean daily maximum °C (°F) 16.8
(62.2)
16.8
(62.2)
19.1
(66.4)
22.5
(72.5)
26.5
(79.7)
30.3
(86.5)
32.4
(90.3)
32.7
(90.9)
30.9
(87.6)
28.1
(82.6)
22.6
(72.7)
18.3
(64.9)
24.7
(76.5)
Daily mean °C (°F) 12.1
(53.8)
11.8
(53.2)
13.9
(57.0)
17.1
(62.8)
21.2
(70.2)
25.0
(77.0)
27.3
(81.1)
27.6
(81.7)
25.4
(77.7)
22.6
(72.7)
17.5
(63.5)
13.7
(56.7)
19.6
(67.3)
Mean daily minimum °C (°F) 7.5
(45.5)
6.9
(44.4)
8.7
(47.7)
11.7
(53.1)
16.0
(60.8)
19.8
(67.6)
22.2
(72.0)
22.6
(72.7)
19.9
(67.8)
17.1
(62.8)
12.5
(54.5)
9.2
(48.6)
14.5
(58.1)
Average precipitation mm (inches) 77.6
(3.06)
40.9
(1.61)
34.4
(1.35)
17.7
(0.70)
8.80
(0.35)
2.70
(0.11)
0.60
(0.02)
0.40
(0.02)
7.10
(0.28)
13.8
(0.54)
53.1
(2.09)
94.5
(3.72)
351.5
(13.84)
Average precipitation days (≥ 1 mm) 7.9 5.7 4.5 3.1 0.7 0.3 0.1 0.1 0.5 2.1 4.7 8.0 37.6
Mean monthly sunshine hours 195.3 208.8 238.7 267.0 331.7 378.0 387.5 365.8 312.0 275.9 216.0 179.8 3,356.5
Source: Meteorological Service (Cyprus)[6]
Climate data for Polis (Satellite view)
Month Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year
Mean daily maximum °C (°F) 16.4
(61.5)
16.3
(61.3)
18.5
(65.3)
21.5
(70.7)
26.1
(79.0)
30.5
(86.9)
33.5
(92.3)
33.3
(91.9)
29.9
(85.8)
26.5
(79.7)
21.9
(71.4)
17.8
(64.0)
24.3
(75.7)
Daily mean °C (°F) 12.1
(53.8)
11.8
(53.2)
13.5
(56.3)
16.3
(61.3)
20.4
(68.7)
24.7
(76.5)
27.6
(81.7)
27.6
(81.7)
24.6
(76.3)
21.4
(70.5)
17.2
(63.0)
13.6
(56.5)
19.2
(66.6)
Mean daily minimum °C (°F) 7.9
(46.2)
7.3
(45.1)
8.6
(47.5)
11.1
(52.0)
14.7
(58.5)
18.8
(65.8)
21.6
(70.9)
21.8
(71.2)
19.3
(66.7)
16.3
(61.3)
12.4
(54.3)
9.4
(48.9)
14.1
(57.4)
Average precipitation mm (inches) 79.9
(3.15)
67.1
(2.64)
37.6
(1.48)
24.7
(0.97)
7.20
(0.28)
1.50
(0.06)
0.20
(0.01)
0.00
(0.00)
4.40
(0.17)
21.8
(0.86)
55.3
(2.18)
94.4
(3.72)
394.2
(15.52)
Average precipitation days (≥ 1 mm) 10.1 8.3 6.5 4.2 1.8 0.2 0.1 0.0 0.6 2.9 5.7 9.1 49.4
Mean monthly sunshine hours 192.2 211.7 254.2 291.0 359.6 387.0 399.9 378.2 318.0 279.0 219.0 182.9 3,472.7
Source: Meteorological Service (Cyprus)[6]
Climate data for Paralimni - ~4 km from sea, elevation: 70 m (Satellite view)
Month Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year
Mean daily maximum °C (°F) 16.0
(60.8)
16.1
(61.0)
18.7
(65.7)
22.2
(72.0)
26.8
(80.2)
30.8
(87.4)
33.1
(91.6)
33.3
(91.9)
31.2
(88.2)
27.7
(81.9)
21.7
(71.1)
17.3
(63.1)
24.6
(76.3)
Daily mean °C (°F) 12.3
(54.1)
12.0
(53.6)
14.2
(57.6)
17.4
(63.3)
21.8
(71.2)
25.7
(78.3)
28.2
(82.8)
28.5
(83.3)
26.1
(79.0)
22.8
(73.0)
17.6
(63.7)
13.7
(56.7)
20.0
(68.0)
Mean daily minimum °C (°F) 8.6
(47.5)
7.9
(46.2)
9.7
(49.5)
12.5
(54.5)
16.8
(62.2)
20.6
(69.1)
23.4
(74.1)
23.7
(74.7)
20.9
(69.6)
18.0
(64.4)
13.4
(56.1)
10.1
(50.2)
15.5
(59.9)
Average precipitation mm (inches) 70.0
(2.76)
62.0
(2.44)
35.0
(1.38)
15.0
(0.59)
7.50
(0.30)
2.50
(0.10)
0.50
(0.02)
0.30
(0.01)
1.20
(0.05)
25.0
(0.98)
45.0
(1.77)
87.0
(3.43)
351.0
(13.82)
Average precipitation days (≥ 1 mm) 8.2 5.6 4.7 3.5 1.2 0.3 0.1 0.1 0.6 2.5 4.9 7.3 38.9
Source: Meteorological Service (Cyprus)[6]
Climate data for Limassol - ~1 km from sea (Satellite view)
Month Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year
Mean daily maximum °C (°F) 17.6
(63.7)
17.8
(64.0)
20.0
(68.0)
22.9
(73.2)
26.9
(80.4)
30.8
(87.4)
33.2
(91.8)
33.3
(91.9)
31.3
(88.3)
28.6
(83.5)
23.5
(74.3)
18.9
(66.0)
25.4
(77.7)
Daily mean °C (°F) 13.2
(55.8)
13.1
(55.6)
15.2
(59.4)
18.0
(64.4)
21.8
(71.2)
25.5
(77.9)
27.8
(82.0)
28.0
(82.4)
26.0
(78.8)
23.2
(73.8)
18.5
(65.3)
14.5
(58.1)
20.4
(68.7)
Mean daily minimum °C (°F) 8.8
(47.8)
8.5
(47.3)
10.4
(50.7)
13.1
(55.6)
16.7
(62.1)
20.1
(68.2)
22.4
(72.3)
22.7
(72.9)
20.6
(69.1)
17.7
(63.9)
13.5
(56.3)
10.1
(50.2)
15.4
(59.7)
Average precipitation mm (inches) 86.7
(3.41)
66.9
(2.63)
35.8
(1.41)
18.4
(0.72)
5.1
(0.20)
1.4
(0.06)
0.0
(0.0)
0.0
(0.0)
2.9
(0.11)
13.1
(0.52)
77.5
(3.05)
99.7
(3.93)
407.5
(16.04)
Average precipitation days (≥ 1 mm) 9.3 7.1 5.6 3.3 1.1 0.2 0.0 0.0 0.3 1.9 5.5 8.8 43.1
Source: Meteorological Service (Cyprus)[6]

Inland

[edit]
Climate data for Nicosia, elevation: 162 m (Satellite view)
Month Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year
Mean daily maximum °C (°F) 15.5
(59.9)
15.9
(60.6)
19.2
(66.6)
24.0
(75.2)
29.7
(85.5)
34.3
(93.7)
37.2
(99.0)
36.9
(98.4)
33.9
(93.0)
29.0
(84.2)
22.1
(71.8)
17.0
(62.6)
26.2
(79.2)
Daily mean °C (°F) 10.6
(51.1)
10.6
(51.1)
13.1
(55.6)
17.1
(62.8)
22.3
(72.1)
26.9
(80.4)
29.7
(85.5)
29.4
(84.9)
26.2
(79.2)
22.3
(72.1)
16.3
(61.3)
12.0
(53.6)
19.7
(67.5)
Mean daily minimum °C (°F) 5.7
(42.3)
5.2
(41.4)
7.0
(44.6)
10.2
(50.4)
14.8
(58.6)
19.4
(66.9)
22.2
(72.0)
21.9
(71.4)
18.8
(65.8)
15.6
(60.1)
10.4
(50.7)
7.1
(44.8)
13.2
(55.8)
Average precipitation mm (inches) 54.7
(2.15)
41.6
(1.64)
28.3
(1.11)
19.9
(0.78)
23.5
(0.93)
17.6
(0.69)
5.80
(0.23)
1.30
(0.05)
11.7
(0.46)
17.4
(0.69)
54.6
(2.15)
65.8
(2.59)
342.2
(13.47)
Average precipitation days (≥ 1 mm) 7.3 6.5 5.4 3.5 2.7 1.3 0.5 0.1 0.6 2.8 4.7 7.7 43.1
Mean monthly sunshine hours 182.9 200.1 238.7 267.0 331.7 369.0 387.5 365.8 312.0 275.9 213.0 170.5 3,314.1
Source: Meteorological Service (Cyprus)[6]
Climate data for Saittas near Moniatis and Trimiklini, elevation: 640 m (Satellite view)
Month Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year
Mean daily maximum °C (°F) 13.6
(56.5)
13.9
(57.0)
17.1
(62.8)
21.5
(70.7)
27.0
(80.6)
31.5
(88.7)
34.6
(94.3)
34.3
(93.7)
31.2
(88.2)
26.8
(80.2)
20.2
(68.4)
15.2
(59.4)
23.9
(75.0)
Daily mean °C (°F) 8.4
(47.1)
8.5
(47.3)
10.9
(51.6)
14.8
(58.6)
19.6
(67.3)
23.8
(74.8)
26.8
(80.2)
26.5
(79.7)
23.4
(74.1)
19.7
(67.5)
14.1
(57.4)
10.0
(50.0)
17.2
(63.0)
Mean daily minimum °C (°F) 3.2
(37.8)
3.1
(37.6)
4.7
(40.5)
8.0
(46.4)
12.2
(54.0)
16.1
(61.0)
18.9
(66.0)
18.7
(65.7)
15.7
(60.3)
12.5
(54.5)
8.1
(46.6)
4.7
(40.5)
10.5
(50.9)
Average precipitation mm (inches) 117.6
(4.63)
89.0
(3.50)
70.3
(2.77)
38.4
(1.51)
20.1
(0.79)
27.2
(1.07)
4.9
(0.19)
10.3
(0.41)
11.7
(0.46)
25.7
(1.01)
93.9
(3.70)
144.0
(5.67)
653.2
(25.72)
Average precipitation days (≥ 1 mm) 10.3 9.1 8.4 5.5 2.7 2.1 0.7 1.1 1.4 3.3 7.0 9.2 60.9
Mean monthly sunshine hours 142.6 168.2 213.9 261.0 310.0 351.0 362.7 347.2 300.0 248.0 165.0 124.0 2,993.6
Source: Meteorological Service (Cyprus)[6]
Climate data for Prodromos in Troodos Mountains, elevation: 1380 m (Satellite view)
Month Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year
Mean daily maximum °C (°F) 6.3
(43.3)
6.6
(43.9)
10.3
(50.5)
15.1
(59.2)
20.5
(68.9)
25.0
(77.0)
28.1
(82.6)
27.9
(82.2)
24.4
(75.9)
19.6
(67.3)
12.8
(55.0)
8.0
(46.4)
17.1
(62.8)
Daily mean °C (°F) 3.5
(38.3)
3.5
(38.3)
6.6
(43.9)
10.7
(51.3)
15.8
(60.4)
20.1
(68.2)
23.3
(73.9)
23.1
(73.6)
19.6
(67.3)
15.4
(59.7)
9.5
(49.1)
5.3
(41.5)
13.0
(55.4)
Mean daily minimum °C (°F) 0.7
(33.3)
0.3
(32.5)
2.8
(37.0)
6.3
(43.3)
11.1
(52.0)
15.2
(59.4)
18.4
(65.1)
18.2
(64.8)
14.9
(58.8)
11.3
(52.3)
6.2
(43.2)
2.5
(36.5)
9.0
(48.2)
Average precipitation mm (inches) 133.4
(5.25)
123.6
(4.87)
82.3
(3.24)
56.9
(2.24)
26.0
(1.02)
40.0
(1.57)
12.1
(0.48)
10.0
(0.39)
9.5
(0.37)
24.0
(0.94)
102.5
(4.04)
169.7
(6.68)
790.1
(31.11)
Average precipitation days (≥ 1 mm) 12.4 11.2 9.8 6.7 3.7 2.1 0.7 0.7 1.4 3.5 7.4 11.2 70.7
Mean monthly sunshine hours 130.2 150.8 195.3 231.0 275.9 315.0 328.6 310.0 255.0 220.1 165.0 136.4 2,713.3
Source: Meteorological Service (Cyprus)[6]

Precipitation

[edit]

The higher mountain areas are cooler and moister than the rest of the island. They receive the heaviest annual rainfall, which may be as much as 1,000 millimeters (39.4 in). Sharp frost also occurs in the higher districts, which are usually blanketed with snow during the first months of the year. Precipitation increases from 450 millimeters (17.7 in) up the south-western windward slopes to nearly 1,100 millimeters (43.3 in) at the top of the Troodos massif. The narrow ridge of the Kyrenia range, stretching 160 km (99 mi) from west to east along the extreme north of the island produces a relatively small increase in rainfall of around 550 millimeters (21.7 in) along its ridge at an elevation of 1,000 meters (3,281 ft). Plains along the northern coast and in the Karpass Peninsula area average 400 to 450 millimeters (15.7 to 17.7 in) of annual rainfall. The least rainfall occurs in the Mesaoria, with 300 to 400 millimeters (11.8 to 15.7 in) a year. Variability in annual rainfall is characteristic for the island, however, and droughts are frequent and sometimes severe. Statistical analysis of rainfall in Cyprus reveals a decreasing trend of rainfall amounts in the last 30 years.

Rainfall in the warmer months contributes little or nothing to water resources and agriculture. Autumn and winter rainfall, on which agriculture and water supply generally depend, is somewhat variable from year to year.

Other information

[edit]
Sandstorm in the Levant, October 19, 2002

The Mediterranean climate, warm and rather dry, with rainfall mainly between November and March, favors agriculture. In general, the island experiences mild wet winters and dry hot summers. Variations in temperature and rainfall are governed by altitude and, to a lesser extent, distance from the coast. Hot, dry summers from mid-May to mid-September and rainy, rather changeable winters from November to mid-March are separated by short autumn and spring seasons.

In summer the island is mainly under the influence of a shallow trough of low pressure extending from the great continental depression centred over Western Asia. It is a season of high temperatures with almost cloudless skies.

In winter Cyprus is near the track of fairly frequent small depressions which cross the Mediterranean Sea from west to east between the continental anticyclone of Eurasia and the generally low pressure belt of North Africa. These depressions give periods of disturbed weather usually lasting for a day or so and produce most of the annual precipitation, the average rainfall from December to February being about 60% of the average annual total precipitation for the island as a whole, which is 500 millimeters (19.7 in).

Humidity

[edit]

Relative humidity of the air is on average between 60% and 80% in winter and between 40% and 60% in summer with even lower values over inland areas around midday. Fog is infrequent and visibility is generally very good. Sunshine is abundant during the whole year and particularly from April to September when the average duration of bright sunshine exceeds 12 hours per day.

Winds

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Winds are generally light to moderate and variable in direction. Strong winds may occur sometimes, but gales are infrequent over Cyprus and are mainly confined to exposed coastal areas as well as areas at high elevation.

Carbon waste emissions

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In 2024, carbon waste emissions (excluding LULUCF and excluding emissions from forestry and land use change) rank and amount in the Cyprus island are recorded as:
Republic of Cyprus: 109th 1.92 MT CO2e
Turkish Republic of Northern Cyprus: 210th 13301.70 T CO2e
(Note: 1. China: 394.77 MT CO2e; 2. the USA: 161.72 MT CO2e; 50. Kenya: 6.96 MT CO2e; 100. Niger: 2.42 MT CO2e; 150. Djibouti 554235.76 T CO2e; 200. Dominica 30419.80 T CO2e)[7]

Temperature and precipitation charts

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Paphos
Climate chart (explanation)
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66
 
 
23
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94
 
 
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Average max. and min. temperatures in °C
Precipitation totals in mm
Source: World Meteorological Organization
Imperial conversion
JFMAMJJASOND
 
 
3.2
 
 
63
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2.6
 
 
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3.7
 
 
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Larnaca
Climate chart (explanation)
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Average max. and min. temperatures in °C
Precipitation totals in mm
Source: World Meteorological Organization
Imperial conversion
JFMAMJJASOND
 
 
3.1
 
 
62
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1.6
 
 
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0.3
 
 
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2.1
 
 
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3.7
 
 
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Limassol
Climate chart (explanation)
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19
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Average max. and min. temperatures in °C
Precipitation totals in mm
Source: World Meteorological Organization
Imperial conversion
JFMAMJJASOND
 
 
3.4
 
 
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2.6
 
 
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Nicosia
Climate chart (explanation)
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17
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Average max. and min. temperatures in °C
Precipitation totals in mm
Source: World Meteorological Organization
Imperial conversion
JFMAMJJASOND
 
 
1.9
 
 
60
41
 
 
1.9
 
 
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1.5
 
 
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Troodos Mountains
Climate chart (explanation)
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Average max. and min. temperatures in °C
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Source: World Meteorological Organization
Imperial conversion
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5.3
 
 
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Amargeti
Climate chart (explanation)
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Source: Climate Data
Imperial conversion
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5.7
 
 
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Average max. and min. temperatures in °F
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See also

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References

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Revisions and contributorsEdit on WikipediaRead on Wikipedia
from Grokipedia
The climate of Cyprus is classified as hot-summer Mediterranean (Köppen Csa), characterized by long, hot, and dry summers from mid-May to mid-October and mild, wet winters from December to February, with transitional spring and autumn seasons. This subtropical regime results in significant seasonal temperature contrasts, with coastal and lowland areas averaging daily highs of 16–19°C and lows of 5–10°C in , rising to 30–32°C highs and 19–22°C lows in July and ; inland areas average around 10°C in , while mountainous regions like the Troodos range are cooler at around 3°C, with potential snowfall above 1,000 meters. is highly seasonal, totaling about 400 mm annually on the coast but up to 1,000 mm in higher elevations, with over 70% falling as between and , while summers remain nearly rainless; sea surface temperatures peak at 27°C in and drop to 16–17°C in winter. Cyprus enjoys abundant sunshine, averaging 3,300 hours yearly or 9 hours per day, contributing to its appeal as a sunny destination, though occasional heatwaves exceeding 40°C and winter storms can occur due to its position. Recent trends indicate warming, with average annual temperatures rising by about 1.5°C since the early 20th century, exacerbating drought risks and shifting some inland areas toward semi-arid conditions (BSh), though the core Mediterranean pattern persists.

Overview

Climate Classification

The climate of Cyprus is primarily classified under the Köppen-Geiger system, which delineates global climates based on native vegetation, temperature thresholds, and seasonal precipitation patterns. The island exhibits a hot-summer Mediterranean climate (Csa) along its coasts and in lowlands, a hot semi-arid climate (BSh) across interior plains such as the Mesaoria, and a temperate oceanic climate (Cfb) in the elevated regions of the Troodos Mountains. The Csa classification characterizes areas with hot, dry summers—where the mean temperature of the hottest month surpasses 22°C and the driest month receives less than 30 mm of —paired with mild, wet winters in which the coldest month averages above 0°C and at least one month exceeds 10°C on average. This regime reflects the influence of subtropical high-pressure systems dominating summer, limiting rainfall to winter frontal activity. In Cyprus's BSh zones, particularly the Mesaoria plain, arises from annual below 400 mm, exacerbated by high rates driven by persistently warm temperatures (all months above 0°C, with the hottest exceeding 18°C). These conditions support steppe-like , distinguishing them from more humid coastal areas through reduced winter rainfall and intensified summer . Cyprus's varied topography fosters transition zones and microclimates, with orographic uplift in the enhancing precipitation to create wetter Csa conditions at mid-elevations, grading into cooler Cfb at higher altitudes where temperatures remain moderate year-round (no month above 22°C) and rainfall distribution is less seasonally skewed.

General Characteristics

Cyprus possesses a prototypical , defined by distinct seasonal contrasts between mild, wet winters and hot, dry summers. Winters, occurring from November to March, bring daytime temperatures averaging 16-20°C, accompanied by the majority of the island's rainfall. Summers, extending from May to , are marked by daytime highs of 30-37°C under predominantly clear skies, with negligible . Annual mean temperatures reflect regional variations influenced by and proximity to the sea. Coastal areas experience an average of approximately 18-19°C, while inland plains register around 17-18°C. Mountainous regions, such as the Troodos, are notably cooler, with annual means of 10-15°C. Transitional seasons of spring (March to May) and autumn (September to November) provide moderate conditions, with temperatures ranging from 20-25°C and occasional rainfall. The climate's overall is pronounced in summer, when relative humidity drops to 15-30% during midday, contrasted by higher levels of 60-80% in winter. enjoys abundant sunshine, averaging 11.5 hours per day in summer months, owing to its isolated position as the third-largest island in the basin, which limits continental influences and enhances maritime moderation.

Factors Influencing the Climate

Geographical and Topographical Effects

Cyprus is located in the Sea, spanning latitudes 34° to 35° N and longitudes 32° to 34° E, positioning it at the crossroads of subtropical influences from the Mediterranean and exposure to continental heat lows originating from western . This geographical placement contributes to a characterized by hot, dry summers and mild, wet winters, with the island's proximity to the Asian landmass enhancing summer heat through the extension of low-pressure systems. As a relatively small island covering 9,251 km², Cyprus experiences rapid transitions in weather patterns due to the limited spatial scale, which allows atmospheric systems to move across the terrain quickly and reduces the persistence of extreme events compared to larger landmasses. The island's topography profoundly shapes its climate through distinct physiographic features. The Troodos Mountains in the south, rising to 1,952 m at Mount Olympus, induce orographic lift on prevailing northerly and northwesterly winds, leading to enhanced precipitation on windward slopes and cooler temperatures at higher elevations, where snow accumulation is common above 1,000 m during winter months from mid-December to late March. In contrast, the Kyrenia Range (also known as Pentadactylos) along the northern coast, reaching up to 1,000 m, intercepts moist air from the north, promoting rainfall on its northern flanks while contributing to drier conditions southward. The intervening Mesaoria Plain, a low-lying central area, lies in the rain shadow of both ranges, resulting in aridity with annual precipitation often limited to 350 mm or less. These topographical variations foster diverse microclimates across . Coastal areas benefit from moderating breezes that alleviate summer heat, maintaining relatively milder temperatures along the shores compared to inland regions. Inland valleys and the Mesaoria Plain, however, trap heat during the day due to their flat and distance from the , leading to higher maximum temperatures. North-facing slopes of the mountain ranges receive more than south-facing ones, as they directly confront moist onshore flows, enhancing local and vegetation in those areas.

Atmospheric and Oceanic Influences

The climate of Cyprus is significantly shaped by atmospheric pressure systems that drive seasonal weather patterns. During the winter months from November to March, Mediterranean depressions originating from the Atlantic Ocean frequently traverse the region, bringing periods of unstable weather characterized by rainfall and associated thunderstorms. These baroclinic systems account for 70-80% of the island's annual , with the rainy season concentrated in this period. In contrast, summer conditions from May to September are dominated by the , a semi-permanent subtropical anticyclone that intensifies and shifts eastward, promoting and stable atmospheric layers over the . This high-pressure system interacts with an extension of the Asian centered over Southwest Asia, creating a shallow trough that inhibits convective activity and results in prolonged dry, clear skies with minimal . These dynamics contribute to the arid summer regime, where is negligible. The Sea plays a key moderating role in Cyprus's through its thermal interactions with the overlying atmosphere. In summer, the warming sea surface, reaching 27-28°C, heats the lower atmosphere, exacerbating and contributing to high levels along coastal areas. During winter, cooler sea temperatures around 17°C help temper air masses, providing relative mildness despite occasional cold intrusions. currents, such as the Levantine Intermediate Water formed in the northern Levantine Basin, have a limited direct impact on surface temperatures around due to the semi-enclosed nature of the sea and weak circulation in the region. Rare atmospheric events further influence variability. Sirocco winds, warm and dust-laden southerly flows from , occasionally affect Cyprus, particularly in spring and autumn, transporting and elevating temperatures temporarily. Additionally, infrequent cold air outbreaks from , associated with deep depressions, can lead to sudden temperature drops and wintry even at low elevations.

Temperature

Air Temperature Patterns

Cyprus's air temperature patterns reflect its , with mild winters, hot summers, and significant spatial variations across coastal, inland, and mountainous regions. Coastal areas, moderated by the surrounding sea, maintain relatively stable temperatures throughout the year, while inland plains experience greater extremes due to continental influences, and the are consistently cooler owing to . The annual mean air temperature along the averages 18–19°C, providing a baseline for the island's temperate conditions. In winter (), daytime temperatures on the typically range from 16–20°C, with nighttime lows of 7–10°C, fostering comfortable conditions despite occasional cooler spells. Summers (July–August) bring intense heat, with coastal daytime highs of 30–33°C and nighttime temperatures of 20–23°C, often accompanied by heat waves exceeding 40°C that strain urban infrastructure and agriculture; inland areas can reach 37°C. These seasonal shifts are influenced by the nearby sea surface temperatures, which help temper coastal extremes but have a lesser effect inland. The diurnal temperature range varies markedly by location, reaching up to 15°C inland where rapid heating and cooling occur away from maritime moderation, compared to 8–10°C along the coast. In the , temperatures are generally 5–10°C cooler than coastal levels year-round, with summer highs rarely surpassing 25°C and winter lows dipping below freezing, potentially reaching -10°C or lower. Urban areas like exhibit an effect, elevating temperatures by 2–3°C compared to rural surroundings, particularly during summer nights. Extreme temperatures underscore the island's vulnerability to climatic variability. The record high of 46.2°C was recorded at Athalassa in 2020, while frequently push inland areas above 40°C in summer; in August 2025, temperatures reached 46°C in Lefkara, approaching the record. The lowest recorded temperatures in the have reached below -10°C, highlighting the potential for cold snaps at higher elevations despite the overall mild climate.

Sea Surface Temperatures

The sea surface temperatures (SST) surrounding typically average 21–22°C annually, reflecting the island's position in the warm Levantine Basin of the Sea. These temperatures exhibit a pronounced seasonal cycle, ranging from a minimum of approximately 17°C in to a maximum of 28°C in . SST remains below 20°C from through , influenced by winter cooling and atmospheric heat loss, before rising above 20°C from May to November as solar insolation intensifies. The cycle peaks in late summer, particularly , due to persistent surface heating and reduced vertical mixing from thermal stratification. Spatially, SST shows subtle variations around the island, with slightly warmer conditions to the and east under the influence of the broader circulation, where temperatures can exceed basin averages by 1–2°C in eddies of . In contrast, waters to the north are cooler by up to 5°C, primarily due to the cyclonic Gyre, which advects colder waters from the region through and gyre dynamics. These SST patterns significantly influence the coastal climate, warming adjacent air masses during winter to moderate temperatures along the shoreline and extending the viable swimming season from through early autumn when waters exceed 20°C. Additionally, higher summer SST enhances , contributing to elevated local levels near the coast.

Precipitation

Rainfall Distribution and Amounts

Cyprus exhibits significant spatial variations in annual rainfall due to its diverse topography, with precipitation amounts ranging from as low as 250 mm in the inland plains to over 1,000 mm in the mountainous regions. The Troodos Mountains in the central-southern part of the island receive the highest totals, typically between 750 and 1,100 mm annually, owing to orographic enhancement where moist air from prevailing westerly winds is forced upward, leading to increased condensation and precipitation. In contrast, the northern (Pentadactylos) Mountains experience moderately high rainfall of 500 to 650 mm per year, influenced by similar orographic effects but moderated by the island's overall eastward-decreasing moisture gradient. Coastal plains along the south and west average 400 to 500 mm annually, while the eastern and southern coasts see slightly less due to proximity to drier air masses. The Mesaoria Plain in the interior, lying in a east of the Troodos, records the lowest amounts at 250 to 400 mm, creating a pronounced west-to-east and mountain-to-plain gradient across the island. These spatial patterns are derived from long-term observations by the Cyprus Department of Meteorology, utilizing data from over 30 years of rain gauge records spanning multiple stations to establish reliable averages. Analysis of records since the early reveals a decreasing trend in annual , with reductions of 10 to 20% observed since the 1970s, particularly pronounced in the (15-25% decline) and less so in the plains (around 10%), attributed to a step change around 1970 affecting wetter winter months more significantly. Recent analyses up to 2023 confirm an overall 18% decline since the early , with annual averages dropping to around 476 mm. The interior plains, such as the Mesaoria, are particularly drought-prone, often receiving less than 300 mm in dry years, exacerbating in these low-precipitation zones. Overall, rainfall is predominantly concentrated in the winter season, aligning with the regime.

Seasonal Patterns and Extremes

The precipitation regime in is markedly seasonal, with 70-80% of the annual total falling between and , driven by Mediterranean depressions that bring moist air masses during the winter period. This accounts for the bulk of hydrological recharge, while the remainder of the year remains largely arid. Orographic enhancement in mountainous areas amplifies this pattern, as noted in broader rainfall distribution analyses. Within the wet season, rainfall peaks in and January, particularly in the where monthly totals can reach 100-200 mm due to enhanced uplift of moist air. Coastal regions typically experience 50-60 mm per month during these winter months, whereas the interior plains receive 30-40 mm, reflecting topographic and exposure differences. In contrast, summer months from to see negligible , often less than 1 mm per month across the island, contributing to prolonged dry conditions. Extreme events underscore the variability of this pattern, with the highest recorded annual rainfall reaching 759 mm island-wide in 1968/69, though mountainous areas like Troodos can exceed 1,000 mm in exceptionally wet years such as 2001/02 in nearby watersheds. Conversely, the driest year saw only 182 mm in 1972/73, with the Mesaoria plain particularly vulnerable to lows around 150 mm during drought periods like 1989. Intense winter storms occasionally trigger flash floods, as evidenced by severe events in December 2018 that caused widespread inundation and fatalities. Interannual fluctuations can exceed 50%, largely modulated by the North Atlantic Oscillation (NAO), which influences the track and intensity of winter cyclones affecting the region.

Sunshine and Insolation

Sunshine Duration

Cyprus experiences abundant sunshine throughout the year, with an annual average of 3,000 to 3,300 hours, and coastal areas typically receiving around 3,200 hours. This high level of solar exposure contributes to the island's , characterized by extended dry summers that enhance outdoor activities. Seasonally, varies significantly, with winter months (December to February) averaging 5 to 6 hours per day—for instance, December records approximately 180 hours total. In contrast, summer months ( to August) offer 12 to 13 hours per day, peaking in at around 380 hours. These patterns reflect the island's subtropical location, where longer daylight in summer aligns closely with actual sunshine received. Cloud cover influences these durations, reducing winter sunshine to 50-60% of the possible astronomical daylight, while clear summer skies achieve nearly 90% utilization. In the , sunshine is notably less due to frequent orographic cloud formation, with winter averages dropping to 4-5 hours per day compared to 6 hours on the and plains. Relative to , Cyprus's winter sunshine is roughly double, where locations like average only about 1-2 hours per day in , making the island a favored winter destination.

Solar Radiation Levels

Cyprus experiences elevated solar radiation levels characteristic of its Mediterranean location, with annual global horizontal irradiation (GHI) averaging 5.0 to 5.4 kWh/m²/day across the island. This places Cyprus among the regions with the highest solar potential in , surpassing many northern and central European countries due to its southern and minimal . Seasonally, solar radiation peaks in summer, reaching 7 to 8 kWh/m²/day in , driven by high solar elevation and prolonged clear skies, while winter minima drop to 2 to 3 kWh/m²/day in and due to shorter days and occasional cloudiness. These variations correlate with the island's extended , enhancing the overall energy input to the climate system. Several factors contribute to these high levels: the island's around 35°N allows for intense insolation, while predominantly clear atmospheric conditions—reflected in average clearness indices of 0.49 to 0.64—minimize by clouds and aerosols. Additionally, elevated terrains in the Troodos and receive slightly higher radiation due to reduced atmospheric path length, with increases of approximately 5-10% per kilometer of altitude for broadband solar flux. The abundant solar radiation supports Cyprus's substantial potential for generation, enabling photovoltaic yields of 1,650 to 1,710 kWh/kWp annually. Furthermore, this high insolation drives elevated rates of surface , contributing to the arid conditions during dry seasons and influencing the local heat budget through increased latent and fluxes.

Humidity

Relative Humidity Variations

Relative humidity in Cyprus exhibits significant spatial and temporal variations, influenced by its Mediterranean location and topography. On the coast, annual averages typically range from 60% to 70%, as observed in locations like where the yearly mean is approximately 61.4%. Inland areas, such as , experience lower annual averages of around 50% to 60%, with a mean of about 55%. These differences arise primarily from proximity to the sea, which moderates humidity levels along the coastline compared to drier and valleys. Seasonally, relative is highest during winter (November to ), averaging 70% to 80%, particularly at night when cooler temperatures allow moisture to condense, reaching up to 95% in coastal areas throughout the year. In contrast, summer months ( to ) see lower levels, typically 40% to 60% during the day, with coastal sites like recording 53% to 55% in July and August. Inland, summer humidity dips even further, reflecting reduced marine influence and higher rates in the warmer, drier air masses. Diurnal cycles are pronounced, especially in summer, where humidity drops significantly during midday due to intense solar heating. Inland in , midday relative humidity can fall to 30% to 40% during summer afternoons, driven by dry katabatic winds from the . At night, humidity rises sharply across , often to 70% or more, as temperatures decrease and the air's capacity to hold moisture diminishes, creating a daily amplitude of 20% to 30% or greater inland. On the coast, such as in , midday summer values hover around 50% to 55%, with less extreme diurnal swings due to sea breezes that transport moist air onshore. Overall spatial patterns show decreasing from coastal zones toward inland valleys and plains, where annual ranges are wider (up to 30% variation between winter highs and summer lows in ). Coastal areas benefit from a narrower annual range of about 20%, maintaining more stable moisture levels year-round. These variations are subtly influenced by adjacent sea surface temperatures, which enhance and coastal during warmer periods.

Fog and Visibility Conditions

Fog is a rare phenomenon in Cyprus, occurring on fewer than 10 days per year along the , primarily during winter mornings due to temperature inversions associated with sea breezes. These conditions arise when cool, moist air from the interacts with warmer surfaces, leading to near the ground. High winter levels further facilitate this process, though dissipates quickly with rising temperatures and solar heating. The predominant type of fog in Cyprus is advection fog, formed when warm, moist maritime air moves over cooler coastal or land surfaces, often during periods of light winds. This is most common along the southern and eastern coasts, such as in and , where sea surface temperatures contrast with overlying air masses. Radiation fog, which develops inland under clear skies and calm conditions allowing of the ground, is even rarer and typically confined to valleys or lowlands like the Mesaoria plain during cold winter nights. Visibility in Cyprus is generally excellent, often exceeding 10 km and averaging around 35 km in the eastern Mediterranean region during summer months, supported by the subtropical high-pressure systems that promote clear skies. However, it can be reduced to 1-5 km during winter rainfall events, when precipitation scatters light and limits sightlines, or in summer due to Saharan dust outbreaks that transport fine particles across the island, lowering visibility to as little as 5-14 km in moderate cases. These low-visibility events have minimal impacts on and driving, given their infrequency and short duration, rarely necessitating widespread disruptions.

Winds

Prevailing Wind Patterns

The prevailing in are typically light to moderate, with average speeds ranging from 3 to 5 m/s (approximately 11 to 18 km/h), though they can occasionally reach 15 to 30 km/h (about 4 to 8 m/s) in more exposed areas. Westerly dominate for much of the year, accounting for about 22% of wind directions in northern regions, while northerly components become more prominent during certain seasons. Annual average speeds across the generally fall between 4 and 6 m/s, reflecting the influence of the Mediterranean's subtropical . Seasonally, winter winds (December to February) are variable and often influenced by passing atmospheric depressions, leading to gusts of 30 to 50 km/h, primarily from westerly or northwesterly directions. These depressions introduce instability, with wind directions shifting frequently due to frontal systems moving across the . In contrast, summer winds ( to August) are steadier, featuring daytime sea breezes flowing from the coast inland at speeds up to 9 m/s near the surface, and nocturnal land breezes reversing the flow at 3 to 4 m/s. The summer regime is marked by northerlies, including the (Meltemi) winds, which prevail from to September as persistent northwesterly flows exceeding 10 m/s in coastal areas, driven by the South Asian monsoon and midlatitude pressure gradients. Regionally, the channel katabatic drainage winds, particularly at night, with speeds of 2 to 5 m/s flowing downslope through valleys and reaching coastal zones up to 20 km offshore, where they fan out and moderate local conditions. Coastal locations experience enhanced sea and land breeze circulations due to the island's and proximity , while inland areas see more variable flows influenced by orographic channeling. The risk of tornadoes is generally low, though occurrences have increased recently, with notable events in February and July 2024 despite the island's exposure to Mediterranean cyclonic activity.

Extreme Wind Events

Extreme wind events in Cyprus are relatively infrequent, with gales exceeding 34 knots (approximately 63 km/h) occurring primarily during winter along exposed coastal areas and in mountainous regions such as the . These events are typically associated with Mediterranean depressions that bring unsettled weather, including strong winds lasting 2–5 days, and are more pronounced in the western and southern coasts. Such gales affect the island on a limited number of days annually, reflecting the overall light to moderate prevailing wind regime. The primary types of extreme wind events stem from these Mediterranean storms, which often feature southerly or southwesterly winds reaching sustained speeds of 50–70 km/h, particularly during winter low-pressure systems. Rare tropical-like cyclones, known as medicanes, occasionally impact the , including , with gusts exceeding 90 km/h; such intense cyclone occurrences remain uncommon due to the region's cooler sea surface temperatures and subtropical high-pressure influences. Additionally, winds—hot, dry southerlies originating from —can generate dust storms that carry Saharan particles to , significantly reducing visibility to below 1 km and exacerbating air quality issues. Recent examples include tornadoes in (February 2024) and (July 2024), and strong winds exacerbating wildfires in July 2025. Historical records indicate notable gusts in elevated areas, such as speeds approaching 100 km/h in the during winter storms. Dust storms from events, while not always reaching force, frequently impair visibility and contribute to localized hazards, occurring several times per year, mainly in spring and autumn. Cyprus's subtropical position precludes major hurricanes, limiting development despite occasional medicane formation. These events generally cause minor impacts, including from storm surges and wave action, as well as power outages due to fallen trees and damaged lines, as seen in multiple incidents where winds uprooted vegetation and disrupted electricity in urban areas like and . Localized crop damage and infrastructure strain occur, but widespread devastation is rare owing to the events' brevity and the island's , which channels winds but also provides shelter in valleys.

Climatic Data and Variations

Coastal Locations

Coastal locations in Cyprus, including in the southwest, in the south, in the southeast, and further east, feature a moderated by the , resulting in relatively uniform temperatures and reduced seasonal extremes compared to inland regions. Based on 1991-2020 normals derived from observed station , these areas experience mild winters with average daily highs around 18°C in and hot, dry summers with highs reaching 32–33°C in and . Annual mean temperatures hover near 20°C, with minimums rarely dropping below 6–9°C in winter due to the sea's thermal regulation. is low overall, averaging 350–450 mm annually and mostly occurring from to , while sunshine duration is extensive, typically exceeding 3,300 hours per year across these stations. The following table summarizes representative monthly climate normals for coastal Cyprus (aggregated from station observations in , , , and nearby sites; data reflect typical values for these locations, with minor variations by station). Temperatures are daily averages (mean derived from max/min), and is monthly totals.
MonthAvg Max Temp (°C)Avg Min Temp (°C)Mean Temp (°C) (mm)
January1861280
February1861260
March2191540
April24121820
May29152210
June3218255
July322126.50
August322126.50
September32182510
October27152140
November22121760
December19914100
Annual261420425
For example, in , July records typical highs of 32°C and lows of 22°C, while sees about 100 mm of in , the wettest month. averages around 3,300 hours of sunshine annually, with daily durations peaking at 12–13 hours in summer. , being more exposed, shows similar patterns but slightly higher summer humidity due to its southeastern position. These values highlight the low variance in coastal climates, where diurnal temperature ranges seldom exceed 10–15°C, influenced by the . Recent trends indicate a slight warming of approximately 0.5°C per decade in coastal temperatures since the 1980s, particularly in summer maxima, while precipitation totals remain stable at historical levels but exhibit high year-to-year variability, with occasional intense winter events. This moderation by the sea keeps coastal extremes lower than those observed inland.

Inland and Mountainous Locations

Inland and mountainous locations in Cyprus, such as the central plain around Nicosia and the Troodos Mountains, display climatic patterns shaped by elevation, with cooler temperatures and higher precipitation in higher altitudes compared to coastal areas. Nicosia, at an elevation of approximately 180 m, represents typical inland conditions, characterized by hot, dry summers and mild winters, while Prodromos in the Troodos range, at about 1,000 m, experiences more temperate summers and cold winters with snowfall. These areas benefit from abundant sunshine, but the mountains receive more precipitation due to orographic effects. The 1991-2020 climate normals for key stations highlight these differences. In , the annual mean temperature is 20.9°C, with extreme heat in summer; the hottest month is , averaging a maximum of 38°C and minimum of 24°C. In contrast, Prodromos has a cooler annual mean of around 12°C, with as the coldest month, averaging 8°C maximum and -2°C minimum. Diurnal temperature ranges are greater inland, often exceeding 15°C in Nicosia during summer due to low humidity and clear skies.
MonthNicosia Max (°C)Nicosia Min (°C)Prodromos Max (°C)Prodromos Min (°C)
Jan1668-2
Feb1769-1
Mar208121
Apr2512175
May3016229
Jun34202613
Jul37222916
Aug38243017
Sep34212714
Oct29172210
Nov2312165
Dec188111
Data based on 1991-2020 normals from station observations. Precipitation is low in inland plains but increases significantly in the mountains. Nicosia receives an annual total of 475 mm, mostly during winter months, while the Troodos Mountains average around 800 mm annually, with higher amounts at elevations above 1,000 m supporting coniferous forests and seasonal snow cover. Snowfall in the Troodos typically occurs from December to March, with 20-50 snow days per year at higher elevations, enabling winter sports.
MonthNicosia Precip. (mm)Troodos Precip. (mm)
Jan110150
Feb80120
Mar60100
Apr3060
May1540
Jun110
Jul05
Aug05
Sep520
Oct2550
Nov60100
Dec94140
Annual475800
Monthly values derived from 1991-2020 station data; summer months are nearly dry in both areas. Sunshine duration is high across these regions, contributing to the warm conditions. averages 3,260 hours annually, with peaks of over 370 hours in . The Troodos receives slightly less due to occasional in winter, but still around 3,140 hours per year.
MonthNicosia Sunshine (h)Troodos Sunshine (h)
Jan170160
Feb190180
Mar240230
Apr280270
May340330
Jun370360
Jul390380
Aug360350
Sep300290
Oct250240
Nov200190
Dec170160
Annual3,2603,140
Based on 1991-2020 observations. Recent observations indicate that inland and mountainous areas are warming faster than coastal regions, with a temperature increase of 0.4–0.6°C per decade from 1991 to 2020, driven by rising minimum temperatures. This trend has led to fewer frost days in the Troodos and more heat stress in .

Climate Change Impacts

Over the past several decades, has experienced a notable warming trend, with the annual mean temperature increasing by approximately 1.2°C from 1960 to 2020, based on records from the Cyprus Department of Meteorology. This rise has been particularly pronounced during summer months, where maximum temperatures have shown the fastest rate of increase, contributing to more frequent and intense heat events. For instance, the number of days exceeding 35°C has roughly doubled since 1980, with trends indicating an addition of about 9.8 such days per decade in locations like . However, these observations may include some bias, particularly in coastal and urban stations, as noted in analyses of long-term meteorological data up to 2023. In 2024, July marked the warmest month on record since 1983, with average temperatures reaching 40.0°C at the Athalassa station. Precipitation patterns have also shifted, with annual rainfall declining by 15-20% since the 1970s, according to data from the Department of spanning 1971-2020. This reduction has been accompanied by shorter winter rainy seasons and a tendency toward more intense, episodic downpours rather than consistent rainfall, exacerbating in an already arid climate. Compared to the 1991-2020 baseline period, earlier decades show even steeper declines, with average annual totals dropping from around 559 mm in 1901-1930 to 463 mm in 1971-2000; the decreasing trend has continued into the 2022-2023 hydrometeorological year. Drought frequency has increased in recent decades, with severe events becoming more common and prolonged. A prominent example is the 2008-2010 , which marked four consecutive years of below-average rainfall, reducing levels to as low as 3% capacity and severely impacting and water supplies. Such episodes highlight the growing vulnerability of Cyprus's to these trends. Additionally, coastal areas face rising challenges from increase, measured at about 2.4 mm per year since the late based on data, with recent Mediterranean-wide observations indicating rates of approximately 4.6 mm per year from 1992 to 2022, leading to erosion and inundation risks along low-lying shores.

Future Projections

Climate projections for Cyprus, aligned with IPCC scenarios, indicate significant warming by the end of the . Under the RCP4.5 , mean annual temperatures are expected to rise by approximately 0.5-3.0°C, while under the more pessimistic RCP8.5 , increases could reach 4°C or more by 2100 relative to the 1981–2010 baseline, with the strongest warming in summer and high-elevation areas where maximum temperatures may exceed 4.5°C. Summers exceeding 40°C will become more frequent, driven by an increase in heatwave days—potentially adding 2-34 such days by mid-century and 23-56 or more annually in lowland areas by late century (2080) under RCP8.5. Precipitation is projected to decline substantially, with annual totals decreasing by 20–30% by 2100 across both RCP4.5 and RCP8.5 scenarios, leading to drier winters and overall reduced water availability. EU-aligned reports suggest a 25% drop in rainfall by 2050, exacerbating as demand rises. While total falls, variability will increase, with fewer rainy days (up to 20 fewer per year by 2100) but potential for more intense events, raising the risk of flash floods from maximum daily up to 80% higher in some regions. Sea surface temperatures around are anticipated to warm by 2–3°C by 2100 under RCP8.5, accelerating evaporation and contributing to heightened . These changes will intensify extreme events, including prolonged heatwaves and droughts, with adaptation strategies emphasizing improved water management through measures like and to mitigate impacts on sectors such as .

References

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