Tundra vegetation productivity and composition are responding rapidly to climatic changes in the Arctic. These changes can, in turn, mitigate or amplify permafrost thaw. In this Review, we synthesize remotely-sensed and field-observed vegetation change across the tundra biome, and outline how these shifts could influence permafrost thaw. Permafrost ice content appears to be an important control on local vegetation changes; woody vegetation generally increases in ice-poor uplands, whereas replacement of woody vegetation by (aquatic) graminoids following abrupt permafrost thaw is more frequent in ice-rich Arctic lowlands. These locally observed vegetation changes contribute to regional satellite-observed greening trends, although the interpretation of greening and browning is complicated. Increases in vegetation cover and height generally mitigate permafrost thaw in summer, yet increase annual soil temperatures through snow-related winter soil warming effects. Strong vegetation-soil feedbacks currently alleviate the consequences of thaw-related disturbances. However, if the increasing scale and frequency of disturbances in a warming Arctic exceeds the capacity for vegetation and permafrost recovery, changes to Arctic ecosystems could be irreversible. To better disentangle vegetation-soil-permafrost interactions, ecological field studies remain crucial, but require better integration with geophysical assessments.
[H1] IntroductionArctic tundra is changing rapidly, with a pervasive trend toward more abundant and taller vegetation as shrubs and trees expand northward 1 . Field and satellite observations suggest that tundra vegetation has become more productive, a phenomenon known as tundra greening. Such increases in the biomass and stature of Arctic tundra vegetation can alter the thermal properties of the ground surface. Canopies can mediate the effect of increasing summer air temperatures on soil temperatures 2-4 and contribute to insulation of soils in winter through trapping of snow [5][6][7][8] .Vegetation and soil characteristics also influence surface energy partitioning and the thermal diffusivity of the soil 9,10 . Permafrost (permanently frozen ground) underlies soil and vegetation, and is the foundation of Arctic tundra ecosystems. In turn, vegetation and near-surface soils insulate permafrost 11 , regulating the effects of atmospheric conditions. However, the Arctic is warming more than twice as fast as the global average, amplified by loss of sea ice cover 1 . Even if Arctic temperatures were to stabilize at 2°C of warming, as aimed for with the Paris Agreement, approximately 40% of near-surface permafrost is still projected to thaw 12 . Permafrost-dominated ecosystems are thus at risk 13 , even under modest CO2 emission scenarios 1 , with consequences for Arctic inhabitants 14 .