Results 11 to 20 of about 973,278 (223)
Remote Sensing of Landscape Change in Permafrost Regions
AbstractAmplification of global warming in Arctic and boreal regions is causing significant changes to permafrost‐affected landscapes. The nature and extent of the change is complicated by ecological responses that take place across strong gradients in environmental conditions and disturbance regimes.
M. Jorgenson, G. Grosse
semanticscholar +4 more sources
Paleolimnology of thermokarst lakes: a window into permafrost landscape evolution
Widespread across northern permafrost landscapes, thermokarst ponds and lakes provide vital wildlife habitat and play a key role in biogeochemical processes.
F. Bouchard +9 more
semanticscholar +3 more sources
Effects of multi-scale heterogeneity on the simulated evolution of ice-rich permafrost lowlands under a warming climate [PDF]
In continuous permafrost lowlands, thawing of ice-rich deposits and melting of massive ground ice lead to abrupt landscape changes called thermokarst, which have widespread consequences on the thermal, hydrological, and biogeochemical state of the ...
J. Nitzbon +10 more
doaj +1 more source
Long-term climate-influenced land cover change in discontinuous permafrost peatland complexes [PDF]
The discontinuous permafrost zone is undergoing rapid transformation as a result of unprecedented permafrost thaw brought on by circumpolar climate warming. Rapid warming over recent decades has significantly decreased the area underlain by permafrost in
O. Carpino +5 more
doaj +1 more source
The current rate and magnitude of temperature rise in the Arctic are disproportionately high compared to global averages. Along with other natural and anthropogenic disturbances, this warming has caused widespread permafrost degradation and soil ...
L. Hughes‐Allen +4 more
semanticscholar +1 more source
The Permafrost and Organic LayEr module for Forest Models (POLE-FM) 1.0 [PDF]
Climate change and increased fire are eroding the resilience of boreal forests. This is problematic because boreal vegetation and the cold soils underneath store approximately 30 % of all terrestrial carbon.
W. D. Hansen +5 more
doaj +1 more source
Soil carbon (C) in permafrost peatlands is vulnerable to decomposition with thaw under a warming climate. The amount and form of C loss likely depends on the site hydrology following permafrost thaw, but antecedent conditions during peat accumulation are
Claire C. Treat +3 more
doaj +1 more source
Evidence for unexpected net permafrost aggradation driven by local hydrology and climatic triggers
Rapid rates of high latitude warming over the past century have led to widespread research on permafrost thaw and its consequences. Studies from lowland plains environments in the discontinuous permafrost zone have highlighted extensive areal loss of ...
Anastasia E Sniderhan +3 more
doaj +1 more source
Ice Volumes in Permafrost Landscapes of Arctic Yakutia
This article is devoted to the study of the distribution of ground ice volumes in the upper layers of 5–10 m permafrost in the permafrost landscapes of Arctic Yakutia. Compilation of such a map will serve as a basis for assessing the vulnerability of permafrost to global warming, anthropogenic impact and forecasting the evolution of permafrost ...
Alexander N. Fedorov +10 more
openaire +3 more sources
Past permafrost dynamics can inform future permafrost carbon-climate feedbacks
Climate warming threatens to destabilize vast northern permafrost areas, potentially releasing large quantities of organic carbon that could further disrupt the climate.
Miriam C. Jones +5 more
doaj +1 more source

