Results 31 to 40 of about 1,094,470 (270)
Biodegradability of dissolved organic carbon in permafrost soils and aquatic systems: A meta-analysis [PDF]
As Arctic regions warm and frozen soils thaw, the large organic carbon pool stored in permafrost becomes increasingly vulnerable to decomposition or transport.
Tank, Suzanne +39 more
core +4 more sources
Ground ice, organic carbon and soluble cations in tundra permafrost soils and sediments near a Laurentide ice divide in the Slave Geological Province, Northwest Territories, Canada [PDF]
The central Slave Geological Province is situated 450–650 km from the presumed spreading centre of the Keewatin Dome of the Laurentide Ice Sheet, and it differs from the western Canadian Arctic, where recent thaw-induced landscape changes in ...
R. Subedi +3 more
doaj +1 more source
Решение многих вопросов рационального землепользования основано на информации о состоянии ландшафтных комплексов. Возможности получения достоверной информации о пространственной структуре мерзлотных ландшафтов становятся особенно актуальными для оценки состояния и тенденций развития.
openaire +2 more sources
Rapid Saline Permafrost Thaw Below a Shallow Thermokarst Lake in Arctic Alaska
Permafrost warming and degradation is well documented across the Arctic. However, observation‐ and model‐based studies typically consider thaw to occur at 0°C, neglecting the widespread occurrence of saline permafrost in coastal plain regions.
Benjamin M. Jones +7 more
doaj +1 more source
Rapid and Gradual Permafrost Thaw: A Tale of Two Sites
Warming temperatures and increasing disturbance by wildfire and extreme weather events is driving permafrost change across northern latitudes. The state of permafrost varies widely in space and time, depending on landscape, climate, hydrologic, and ...
B. J. Minsley +6 more
doaj +1 more source
Isotropic thaw subsidence in undisturbed permafrost landscapes [PDF]
AbstractObservations in undisturbed terrain within some regions of the Arctic reveal limited correlation between increasing air temperature and the thickness of the seasonally thawed layer above ice‐rich permafrost. Here we describe landscape‐scale, thaw‐induced subsidence lacking the topographic contrasts associated with thermokarst terrain.
Nikolay I. Shiklomanov +3 more
openaire +1 more source
Frozen Ground - The News Bulletin of the International Permafrost Association, No.19 [PDF]
Frozen Ground - The News Bulletin of the International Permafrost Association, No ...
International Permafrost Association, IPA
core +1 more source
In the Arctic, the spatiotemporal variation of net methane uptake in upland soils depends on unresolved interactive controls between edaphic and microbial factors not yet included in current models, underpinning the uncertainty of upscaling the Arctic ...
Ludovica D’Imperio +11 more
doaj +1 more source
Arctic Landscapes in Transition: Responses to Thawing Permafrost [PDF]
Observations indicate that over the past several decades, geomorphic processes in the Arctic have been changing or intensifying. Coastal erosion, which currently supplies most of the sediment and carbon to the Arctic Ocean [Rachold et al., 2000], may have doubled since 1955 [Mars and Houseknecht, 2007].
J. C. Rowland +16 more
openaire +1 more source
The Western Siberian Lowlands (WSL) store large quantities of organic carbon that will be exposed and mobilized by the thawing of permafrost. The fate of mobilized carbon, however, is not well understood, partly because of inadequate knowledge of ...
P Ala-aho +11 more
doaj +1 more source

