Changing environmental conditions in the Arctic have profound impacts on permafrost coasts, which erode at great pace. Although numbers exist on annual carbon and sediment fluxes from coastal erosion, little is known on how terrestrial organic matter (OM) is transformed by thermokarst and –erosional processes on transit from land to sea. Here, we investigated a retrogressive thaw slump (RTS) on Qikiqtaruk - Herschel Island in the western Canadian Arctic
Collapse of permafrost coasts delivers large quantities of particulate organic carbon (POC) to arcti...
Warming air and sea temperatures, longer open-water seasons and sea-level rise collectively promote ...
Collapse of permafrost coasts delivers large quantities of particulate organic carbon (POC) to Arcti...
Retrogressive thaw slumps (RTS) are spectacular lateral thermokarst features occurring in ice-rich p...
The changing climate in the Arctic has a profound impact on permafrost coasts, which are subject to ...
Enhanced warming of the Northern high latitudes has intensified thermokarst processes throughout the...
The mechanism of carbon dioxide and methane release to the atmosphere in permafrost regions is not s...
Permafrost soils, which store almost half of the global belowground organic carbon (OC), are suscept...
Climate change has a strong impact on permafrost coasts in the Arctic. With increasing air and water...
Climate warming has a strong impact on permafrost coasts in the Arctic. With increasing air and wate...
Retrogressive thaw slumps (RTSs) are among the most active thermokarst landforms in the Arctic and ...
Along Arctic coastlines retrogressive thaw slumps (RTS) are common thermokarst landform. They delive...
The Canadian Yukon Coast is an ice-rich permafrost coast. This is a fragile ecosystem and reacts st...
Ice-rich permafrost thaw is highly sensitive to the creation of local landscape subsidence in the Ar...
Warming and wetting in the western Canadian Arctic are accelerating thaw-driven mass wasting by perm...
Collapse of permafrost coasts delivers large quantities of particulate organic carbon (POC) to arcti...
Warming air and sea temperatures, longer open-water seasons and sea-level rise collectively promote ...
Collapse of permafrost coasts delivers large quantities of particulate organic carbon (POC) to Arcti...
Retrogressive thaw slumps (RTS) are spectacular lateral thermokarst features occurring in ice-rich p...
The changing climate in the Arctic has a profound impact on permafrost coasts, which are subject to ...
Enhanced warming of the Northern high latitudes has intensified thermokarst processes throughout the...
The mechanism of carbon dioxide and methane release to the atmosphere in permafrost regions is not s...
Permafrost soils, which store almost half of the global belowground organic carbon (OC), are suscept...
Climate change has a strong impact on permafrost coasts in the Arctic. With increasing air and water...
Climate warming has a strong impact on permafrost coasts in the Arctic. With increasing air and wate...
Retrogressive thaw slumps (RTSs) are among the most active thermokarst landforms in the Arctic and ...
Along Arctic coastlines retrogressive thaw slumps (RTS) are common thermokarst landform. They delive...
The Canadian Yukon Coast is an ice-rich permafrost coast. This is a fragile ecosystem and reacts st...
Ice-rich permafrost thaw is highly sensitive to the creation of local landscape subsidence in the Ar...
Warming and wetting in the western Canadian Arctic are accelerating thaw-driven mass wasting by perm...
Collapse of permafrost coasts delivers large quantities of particulate organic carbon (POC) to arcti...
Warming air and sea temperatures, longer open-water seasons and sea-level rise collectively promote ...
Collapse of permafrost coasts delivers large quantities of particulate organic carbon (POC) to Arcti...