Results 41 to 50 of about 5,638 (244)
Table S2: Radiocarbon ages of yedoma and thermokarst deposits in Baldwin Peninsula, West-Alaska
Table S2: Radiocarbon ages of yedoma and thermokarst deposits in Baldwin Peninsula, West ...
Strauss, Jens +13 more
core +1 more source
Active construction of new roads and other linear structures requires new techniques for the natural hazard assessment. These techniques can involve both stochastic modeling and remote sensing data (RSD).
Timofey V. Orlov +3 more
doaj +1 more source
Thermokarst lakes are formed following ice-rich permafrost thaw and widely distribute in the cold regions with high latitude and elevation. However, the micro-eukaryotic communities (MECs) in thermokarst lakes are not well studied.
Ze Ren +6 more
doaj +1 more source
ABSTRACT Permafrost in northern peatlands occurs within individual palsas or extensive peat plateaus and controls local carbon storage. These permafrost landforms are complex, and their internal structure remains poorly understood. We used quasi‐3D electrical resistivity tomography (ERT) measurements, supported by UAV‐LiDAR topography, frost probing ...
Cas Renette +5 more
wiley +1 more source
Simulating thermokarst lakes [PDF]
Thermokarst lakes, which form from thawing permafrost, alter landscapes and hydrology and can release significant amounts of methane to the atmosphere. To learn more about the dynamics of thermokarst lakes, Kessler et al. created a three‐dimensional numerical model of these lakes that includes the surrounding topography.
openaire +2 more sources
ABSTRACT The McMurdo Dry Valleys, the largest ice‐free region in Antarctica, are home to a cold‐desert hydrologic system of glaciers, snowbanks, streams, and lakes. Freshwater is also stored as dead glacial ice, which is poorly constrained in terms of ion concentrations and interactions with both in situ and overlying sediments.
Matthew C. Witscheber, Kate M. Swanger
wiley +1 more source
Table S4: GDGT data of yedoma and thermokarst deposits in Baldwin Peninsula, West-Alaska
Table S4: GDGT data of yedoma and thermokarst deposits in Baldwin Peninsula, West ...
Strauss, Jens +13 more
core +1 more source
Accelerating climate change intensifies permafrost degradation and thermokarst hazards on the Qinghai-Tibet Plateau (QTP), threatening ecosystems and infrastructure.
Tiantian Li +9 more
doaj +1 more source
ABSTRACT Pingos are large mounds with cores formed of intrusive ice that form in periglacial landscapes. These ice structures can form in regions of discontinuous permafrost, commonly as hydraulic or open‐system pingos, or in locations of continuous permafrost, commonly as hydrostatic or closed‐system pingos.
Venezia M. Follingstad +12 more
wiley +1 more source
(Table 4) Characteristics of new thermokarst lakes at study sites in Canada, Russia and Sweden
(Table 4) Characteristics of new thermokarst lakes at study sites in Canada, Russia and ...
Kuhry, Peter +3 more
core +1 more source

