Water in the Taiga: Both Still and Flowing

The taiga (boreal forest) contains abundant water in both static and dynamic forms, shaped by its cold climate, permafrost patches, and glacial legacy.

Standing Waters

• Lakes: Countless glacial lakes dot the landscape—from Canada's Shield lakes to Siberia's Lake Baikal (world's deepest).
• Bogs and fens: Peatlands store vast carbon; sphagnum moss creates acidic, nutrient-poor pools.
• Thermokarst lakes: Formed by thawing permafrost, expanding as climate warms.

Moving Waters

• Rivers: Major north-flowing rivers (Ob, Yenisey, Lena, Mackenzie) drain to the Arctic Ocean.
• Streams: Spring melt creates torrential seasonal flows.
• Groundwater: Slow movement through taliks (unfrozen zones) beneath permafrost.

This hydrologic diversity supports taiga ecosystems—from migratory waterfowl to spawning fish—and regulates regional climate through evaporation and albedo effects.