Matay | |
|---|---|
Village | |
  Matay Location in Kazakhstan | |
| Coordinates: 45°53′42″N78°43′05″E / 45.89500°N 78.71806°E | |
| Country | Kazakhstan |
| Region | Jetisu Region |
| Time zone | UTC+6 (Omsk Time) |
Matay is a village in Jetisu Region, in south-eastern Kazakhstan. [1]
Matay | |
|---|---|
Village | |
| Matay Location in Kazakhstan | |
| Coordinates: 45°53′42″N78°43′05″E / 45.89500°N 78.71806°E | |
| Country | Kazakhstan |
| Region | Jetisu Region |
| Time zone | UTC+6 (Omsk Time) |
Matay is a village in Jetisu Region, in south-eastern Kazakhstan. [1]
Matay has a steppe climate (Köppen: BSk), [2] with hot summers and very cold winters.
| Climate data for Matay (1991–2020) | |||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Month | Jan | Feb | Mar | Apr | May | Jun | Jul | Aug | Sep | Oct | Nov | Dec | Year |
| Mean daily maximum °C (°F) | −6.7 (19.9) | −3.3 (26.1) | 6.9 (44.4) | 19.7 (67.5) | 26.1 (79.0) | 31.8 (89.2) | 33.4 (92.1) | 32.1 (89.8) | 25.7 (78.3) | 17.1 (62.8) | 5.6 (42.1) | −3.3 (26.1) | 15.4 (59.7) |
| Daily mean °C (°F) | −12.5 (9.5) | −9.3 (15.3) | 0.3 (32.5) | 11.7 (53.1) | 18.0 (64.4) | 23.8 (74.8) | 25.6 (78.1) | 23.8 (74.8) | 17.0 (62.6) | 8.9 (48.0) | −0.6 (30.9) | −8.6 (16.5) | 8.2 (46.8) |
| Mean daily minimum °C (°F) | −17.4 (0.7) | −14.4 (6.1) | −5.1 (22.8) | 4.2 (39.6) | 9.8 (49.6) | 15.6 (60.1) | 17.7 (63.9) | 15.3 (59.5) | 8.8 (47.8) | 2.0 (35.6) | −5.4 (22.3) | −12.9 (8.8) | 1.5 (34.7) |
| Average precipitation mm (inches) | 19.6 (0.77) | 16.3 (0.64) | 18.8 (0.74) | 21.3 (0.84) | 23.3 (0.92) | 21.7 (0.85) | 28.1 (1.11) | 11.4 (0.45) | 10.7 (0.42) | 20.6 (0.81) | 28.4 (1.12) | 23.0 (0.91) | 243.2 (9.57) |
| Average precipitation days (≥ 1.0 mm) | 5.5 | 4.5 | 4.9 | 4.3 | 4.8 | 4.4 | 4.5 | 2.7 | 2.3 | 3.9 | 5.5 | 5.4 | 52.7 |
| Source: NOAA [3] | |||||||||||||
In geography, the temperate climates of Earth occur in the middle latitudes, which span between the tropics and the polar regions of Earth. These zones generally have wider temperature ranges throughout the year and more distinct seasonal changes compared to tropical climates, where such variations are often small and usually only have precipitation differences.
The desert climate or arid climate is a dry climate sub-type in which there is a severe excess of evaporation over precipitation. The typically bald, rocky, or sandy surfaces in desert climates are dry and hold little moisture, quickly evaporating the already little rainfall they receive. Covering 14.2% of Earth's land area, hot deserts are the second most common type of climate on Earth after the polar climate.
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