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Asia is dominated by a varied mix of climate regions. Polar, subarctic, and temperate climates occur along the continent's northern and northeastern fringes; arid and highland climates occur in the continent's interior and southwestern reaches; and a mix of grassland and tropical rainforest climates occur along its southern fringe. (more)
Climate is the long-term pattern of weather in a particular area. Weather can change from hour-to-hour, day-to-day, month-to-month or even year-to-year. A region ’s weather patterns, usually tracked for at least 30 years, are considered its climate. Different parts of the world have different climates.
In Western Asia, the climate can be found on the Black Sea coast of northern Turkey and Georgia, often transitional to humid subtropical. While Cfb zones are rare in Africa, one dominates the coastline of the Eastern Cape in South Africa .
A region’s climate is influenced by many factors, including latitude, elevation, and nearby geographic features. Latitude is how far north or south a place is from the equator. At higher latitudes, sunlight is less direct, leading to cooler climates. Elevation is how high a place is above sea level.
The Southern sections of Asia are mild to hot, while far northeastern areas such as Siberia are very cold, and East Asia has a temperate climate. The highest temperature recorded in Asia was 54 °C (at Ahvaz Airport, Iran on June 29, 2017 and at Tirat Zvi, Israel on June 21, 1942).
The extreme northern fringe, as well as much of the Plateau of Tibet, has a tundra climate, sometimes also called a cold desert because the land is dry like a desert but with cold temperatures. Most of the remainder of Siberia has a subarctic climate.
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In northern areas of Asia such as northern Russia and the Arctic Circle, the climate is colder and very dry. The tundra biome exists here and temperatures can be as low as -60°C.