N Tananaev, E Lotsari - Earth-Science Reviews, 2022 - Elsevier
This paper discusses the potential response of fluvial processes and landforms to the projected permafrost degradation and related hydrological change. Fluvial system structure …
Ice-rich permafrost in the circum-Arctic and sub-Arctic (hereafter pan-Arctic), such as late Pleistocene Yedoma, are especially prone to degradation due to climate change or human …
Yedoma is a permafrost deposit widely distributed across the Arctic and found exclusively within the unglaciated regions in northern Siberia, Alaska, and the Yukon, which are the …
Thermokarst lakes are widespread in Arctic lowlands. Under a warming climate, landscapes with highly ice-rich Yedoma Ice Complex (IC) deposits are particularly vulnerable, and …
Permafrost is warming globally which leads to widespread permafrost thaw. Particularly ice- rich permafrost is vulnerable to rapid thaw and erosion, impacting whole landscapes and …
Arctic permafrost, the largest non-seasonal component of Earth's cryosphere, contains a substantial climate-sensitive carbon pool. The existence of a global tipping point, a warming …
Riverbank erosion in yedoma regions strongly affects landscape evolution, biogeochemical cycling, sediment transport, and organic and nutrient fluxes to the Arctic Ocean. Since 2006 …
The response of permafrost to marine submergence can vary between ice‐rich late Pleistocene deposits and the thermokarst basins that thawed out during the Holocene. We …
SS Kostrova, BK Biskaborn, LA Pestryakova… - Quaternary Science …, 2021 - Elsevier
A new dataset from Lake Emanda provides insights into climate and environmental dynamics in an extreme continental setting in northeastern Siberia. The δ 18 O diatom …