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The river flows in the northern area of Sumatra with predominantly tropical rainforest climate (designated as Af in the Köppen-Geiger climate classification). [5] The annual average temperature in the area is 22 °C. The warmest month is March, when the average temperature is around 23 °C, and the coldest is June, at 21 °C. [6]
The climate of the interior of Alaska is best described as extreme and is the best example of a true subarctic climate, as the highest and lowest temperatures of any of these countries have a significant influence over climate and weather conditions and climate conditions and are generally considered the best conditions in this area for ...
The subtropics are geographic and climate zones located roughly between the Tropic of Cancer and Tropic of Capricorn and the 40th parallel in both hemispheres. Subtropical climate regions can exist at high elevations within the tropics, such as across the Mexican Plateau and the Ethiopian Highlands and in Da Lat of the Vietnamese Central ...
The Köppen climate classification system was modified further within the Trewartha climate classification system in 1966 (revised in 1980). The Trewartha system sought to create a more refined middle latitude climate zone, which was one of the criticisms of the Köppen system (the climate group C was too general). [10]: 200–1
Alas (Yakut: Алаас) is a shallow depression which occurs primarily in Yakutia, which is formed by subsidence of the Arctic permafrost owing to repeated melting and refreezing. An alas first develops as a shallow lake as melt water fills the depression. The lake eventually dries out and is replaced by grasses and other herbaceous vegetation.
Glennallen features a dry-summer subarctic climate (Köppen climate classification: Dsc) The city is located in the continental climate zone, with long, cold winters, and relatively warm summers. Climate data for Glennallen, Alaska (1991–2020 normals, extremes 1965–present)
U.S. Rep. Katherine Clark was in Natick for the announcement of $400,000 in federal funding granted to the Charles River Watershed Association.
The climate and ecology of different locations on the globe naturally separate into life zones, depending on elevation, latitude, and location.The generally strong dependency on elevation is known as altitudinal zonation: the average temperature of a location decreases as the elevation increases.