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.

[1] [2][3][4][5] 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 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.

At lower elevations, moss and lichen form mats on the thin soil and permafrost.