Transbaikal Bald Mountain tundra

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Transbaikal Bald Mountain tundra
Ozero Medvezh'e zapovednik.JPG
High peaks in Bureya Nature Reserve
Ecoregion PA1112.png
Ecoregion territory (in purple)
Ecology
Realm Palearctic
Biome tundra
Geography
Area217,559 km2 (84,000 sq mi)
CountriesRussia
Coordinates 55°45′N122°15′E / 55.75°N 122.25°E / 55.75; 122.25

The Transbaikal Bald Mountain tundra ecoregion (WWF ID: PA1112) covers the high-altitude peak zones above the treeline in a series of mountain ranges that stretch from the northern reaches of Lake Baikal to the western coastal ranges of the Okhotsk Sea. Floral communities are those of mountain tundra, with bare rock or permafrost under layers of moss and lichen. Because the ecoregion is aligned along a common latitude, it acts as a route for the transmission of species across Siberia. The ecoregion is in the Palearctic realm and the tundra biome. It has an area of 217,559 square kilometres (84,000 sq mi). [1] [2] [3] [4] [5]

Contents

Location and description

The ecoregion stretches almost 1,800 km from west to east, forming a patchwork of sections that are mostly above 975 metres (3,199 ft) in a series of mountain ranges from Lake Baikal to the Okhotsk Sea. This string of high-altitude zones roughly follows 56 degrees north latitude, and much of the tundra climate is due to altitude zoning. The individual mountain ranges include the Stanovoy Range and the Dzhugdzhur Mountains. The highest elevation is 2,700 metres (8,900 ft). [6]

Climate

The region has a Subarctic climate (Koppen classification Dwc). This climate is characterized by high variation in temperature, both daily and seasonally; with long, cold winters and short, cool summers with no month averaging over 22 °C (72 °F); and with low levels of precipitation throughout the year. Mean precipitation in the Transbaikal bald mountain tundra region is about 121 mm/year. The mean temperature at the center of the ecoregion in January is −31.5 °C (−24.7 °F), and 15.8 °C (60.4 °F) in July. [7]

Flora and fauna

In general, the high peaks are bare rock at their highest, most windswept points. At lower elevations, moss and lichen form mats on the thin soil and permafrost. [2] Mammals in this zone include marmots, moose, and musk deer.

Protections

There are several significant nationally protected area that reach into this ecoregion:

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References

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  2. 1 2 "Trans-Baikal Bald Mountain tundra". World Wildlife Federation. Retrieved November 20, 2018.
  3. "Map of Ecoregions 2017". Resolve, using WWF data. Retrieved September 14, 2019.
  4. Kottek, M.; Grieser, J.; Beck, C.; Rudolf, B.; Rubel, F. (2006). "World Map of Koppen-Geiger Climate Classification Updated" (PDF). Gebrüder Borntraeger 2006. Retrieved September 14, 2019.
  5. "Dataset - Koppen climate classifications". World Bank. Retrieved September 14, 2019.
  6. "TRANS-BAIKAL BALD MOUNTAIN TUNDRA". Joint Research Center - Digital Observatory for Protected Areas. Retrieved January 1, 2019.
  7. "Climate Data for Latitude 55.75 Longitude 122.25". GlobalSpecies.org. Retrieved October 20, 2018.