Vast portions of Arctic and sub-Arctic Siberia, Alaska and the Yukon Territory are covered by ice-rich silts that are penetrated by large ice wedges, resulting from syngenetic sedimentation and freezing. Accompanied by wedge-ice growth, the sedimentation process was driven by cold continental climatic and environmental conditions in unglaciated regions during the late Pleistocene, inducing the accumulation of the unique Yedoma permafrost deposits up to 50 meter thick. Because of fast incorporation of organic material into permafrost during formation, Yedoma deposits include low-decomposed organic matter. Moreover, ice-rich permafrost deposits like Yedoma are especially prone to degradation triggered by climate changes or human activity. W...
With ongoing climate change, the Arctic will continue to warm approximately twice as fast as the low...
Rapid changes are observed in the Polar Regions. With ongoing climate change, the Arctic will contin...
With ongoing climate change, the Arctic will continue to warm approximately twice as fast as the low...
Large parts of (sub-)Arctic Siberia, Alaska and the Yukon Territory are covered by ice-rich silts th...
Vast regions of Arctic Siberia, Alaska, and the Yukon Territory are covered by ice-rich silts penetr...
Vast portions of Arctic and sub-Arctic Siberia, Alaska and the Yukon Territory are covered by ice-ri...
Vast portions of Arctic and sub-Arctic Siberia, Alaska and the Yukon Territory are covered by ice-ri...
Permafrost is a distinct feature of the terrestrial Arctic and is vulnerable to climate warming. Per...
Arctic landscapes underlain by permafrost are threatened by climate warming and may degrade in diffe...
With ongoing climate change, the Arctic will continue to warm approximately twice as fast as the low...
Permafrost landscapes are threatened by climate warming and degrade in different ways. This includes...
An estimation of the carbon stored in Arctic permafrost and its biogeochemical characteristics are e...
The estimation of organic carbon stored in Arctic permafrost and its biogeochemical characteristics ...
Permafrost is a distinct feature of the terrestrial Arctic and is vulnerable to climate warming. Per...
The permafrost region approximately makes up one quarter of the land surface of the Northern Hemisph...
With ongoing climate change, the Arctic will continue to warm approximately twice as fast as the low...
Rapid changes are observed in the Polar Regions. With ongoing climate change, the Arctic will contin...
With ongoing climate change, the Arctic will continue to warm approximately twice as fast as the low...
Large parts of (sub-)Arctic Siberia, Alaska and the Yukon Territory are covered by ice-rich silts th...
Vast regions of Arctic Siberia, Alaska, and the Yukon Territory are covered by ice-rich silts penetr...
Vast portions of Arctic and sub-Arctic Siberia, Alaska and the Yukon Territory are covered by ice-ri...
Vast portions of Arctic and sub-Arctic Siberia, Alaska and the Yukon Territory are covered by ice-ri...
Permafrost is a distinct feature of the terrestrial Arctic and is vulnerable to climate warming. Per...
Arctic landscapes underlain by permafrost are threatened by climate warming and may degrade in diffe...
With ongoing climate change, the Arctic will continue to warm approximately twice as fast as the low...
Permafrost landscapes are threatened by climate warming and degrade in different ways. This includes...
An estimation of the carbon stored in Arctic permafrost and its biogeochemical characteristics are e...
The estimation of organic carbon stored in Arctic permafrost and its biogeochemical characteristics ...
Permafrost is a distinct feature of the terrestrial Arctic and is vulnerable to climate warming. Per...
The permafrost region approximately makes up one quarter of the land surface of the Northern Hemisph...
With ongoing climate change, the Arctic will continue to warm approximately twice as fast as the low...
Rapid changes are observed in the Polar Regions. With ongoing climate change, the Arctic will contin...
With ongoing climate change, the Arctic will continue to warm approximately twice as fast as the low...