Drying of tundra landscapes will limit subsidence-induced acceleration of permafrost thaw
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Arctic permafrost landscapes in transition: towards an integrated

Science Highlights

A Glacic Molliturbel formed in Dry Nonacidic Tundra on Howe Island

Comparison of (a) ALT, (b) annual thaw depth-duration, (c) annual

Tundra vegetation change and impacts on permafrost

Continentality determines warming or cooling impact of heavy

Chapter 2: High Mountain Areas — Special Report on the Ocean and

Frontiers Permafrost and groundwater interaction: current state

NGEE Arctic Improving climate model predictions through advanced

Drying of tundra landscapes will limit subsidence-induced

Drying of tundra landscapes will limit subsidence-induced
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