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There are taiga areas of eastern Siberia and interior Alaska-Yukon where the mean annual temperature reaches down to −10 °C (14 °F), [11] [12] and the lowest reliably recorded temperatures in the Northern Hemisphere were recorded in the taiga of northeastern Russia. Taiga has a subarctic climate with very large temperature range between ...
This vast ecoregion is located in the heart of Siberia, stretching over 20° of latitude and 50° of longitude [1] (52° to 72° N, and 80° to 130° E). The climate in the East Siberian taiga is subarctic (the trees growing there are coniferous and deciduous) and displays high continentality, with extremes ranging from 40 °C (104 °F) to −65 °C (−85 °F) and possibly lower.
[25] [26] On 28 July 2010, Oymyakon recorded a record high temperature of 34.6 °C (94.3 °F), [27] yielding a temperature range of 102.3 °C (184.1 °F). Verkhoyansk, Yakutsk, Delyankir, Tegyulte, and Fort Vermilion, Canada are the only other known places in the world that have a temperature amplitude higher than 100 °C (180 °F).
The ecoregion is centered on the West Siberian Plain, a flat lowland that only ranges from 100 meters to 300 meters above sea level. The western edge of the region is the Urals mountains, and the western half of the region is dominated by the Ob River and its main tributary the Irtysh River.
The Scandinavian and Russian taiga is an ecoregion within the taiga and boreal forests biome as defined by the WWF classification (ecoregion PA0608). [1] It is situated in Northern Europe between tundra in the north and temperate mixed forests in the south and occupies about 2,156,900 km 2 (832,800 sq mi) in Norway, Sweden, Finland and the northern part of European Russia, being the largest ...
Most of Northern European Russia and Siberia between the Scandinavian Peninsula and the Pacific Ocean has a subarctic climate, with extremely severe winters (Dfd, Dwd, Dsd) in the inner regions of Northeast Siberia (mostly the Sakha Republic) with the record low temperature of −67.8 °C or −90.0 °F), and more moderate (Dwc, Dfc, Dsc ...
The dominant vegetation is light coniferous taiga with Larix gmelini forming the canopy in areas with low snow cover. This ecoregion is rich in minerals. [3] The climate of the Central Siberia Reserve is Subarctic climate, without dry season (Köppen climate classification Subarctic climate (Dfc)). This climate is characterized by mild summers ...
The climate of the Okhotsk-Manchurian taiga is Humid continental climate, warm summer (Köppen climate classification), with a dry winter.This climate is characterized by large seasonal temperature differentials and a warm summer (at least four months averaging over 10 °C (50 °F), but no month averaging over 22 °C (72 °F), and cold winters having monthly precipitation less than one-tenth ...