High resolution seismic and ground penetrating radar-geophysical profiling of a thermokarst lake in the western Lena Delta, Northern Siberia [PDF]
High resolution seismic and ground-penetrating radar (GPR) have been acquired over Lake Nikolay in the western Lena Delta (Siberia) in order to study the uppermost basin fill and the bordering frozen margins. GPR measurements were completed on the frozen
Dix, J.K. +7 more
core +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
Thermokarst lake detection : a remote sensing approach [PDF]
Rock glaciers are apparent occurrences, and thus indicators of permafrost conditions in mountain regions. Active rock glaciers contain ice and are moving, while inactive rock glaciers are immobile but still contain ice. They can be summarized as intact rock glaciers.
Obwegs, Maria
core +4 more sources
A new Stefan equation to characterize the evolution of thermokarst lake and talik geometry [PDF]
Thermokarst lake dynamics, which play an essential role in carbon release due to permafrost thaw, are affected by various geomorphological processes. In this study, we derive a three-dimensional (3D) Stefan equation to characterize talik geometry under a
N. Ohara +10 more
doaj +1 more source
Evolution of thermokarst in East Siberian ice-rich permafrost [PDF]
Thermokarst lakes and basins are major components of ice-rich permafrost landscapes in East Siberian coastal lowlands and are regarded as indicators of regional climatic changes.
Irina Fedorova (6975533) +17 more
core +1 more source
Grain size distribution of sediment core PG2412 beneath thermokarst lake Goltsovoye Lake on the Bykovsky Pensinula, northeastern Siberia [PDF]
These datasets describe a 31.5 m long sediment core taken from beneath thermokarst lake Goltsovoye Lake (71.74515 N, 129.30217 E) on the Bykovsky Peninsula, northeastern Siberia. The thermokarst lake was 510 cm deep.
Strauss, Jens +2 more
core +1 more source
(Table 3) Changes in thermokarst lake extent, infilling with fen vegetation and lateral erosion at study sites in Canada, Russia and Sweden [PDF]
Thermokarst lakes = surrounded by peat plateau along >75% of the shoreline. For all study sites the changes in lake area were statistically significant (p < 0.001), except for in the 2 km × 2 km area in Rogovaya (p = 0.63).
Kuhry, Peter +3 more
core +1 more source
Mapping thermokarst lakes in different physical states on the central Tibetan plateau
Mapping and monitoring the spatial–temporal evolution of thermokarst lakes on the Tibetan Plateau can significantly contribute to the estimation of climate change impacts on permafrost degradation.
Yuanyuan Qin, Ping Lu, Jicang Wu
doaj +1 more source
Decadal-scale hotspot methane ebullition within lakes following abrupt permafrost thaw
Thermokarst lakes accelerate deep permafrost thaw and the mobilization of previously frozen soil organic carbon. This leads to microbial decomposition and large releases of carbon dioxide (CO _2 ) and methane (CH _4 ) that enhance climate warming ...
K M Walter Anthony +18 more
doaj +1 more source
The evolution of a thermokarst-lake landscape: late Quaternary permafrost degradation and stabilization in interior Alaska [PDF]
Thermokarst processes characterize a variety of ice-rich permafrost terrains and often lead to lake formation. The long-term evolution of thermokarst landscapes and the stability and longevity of lakes depend upon climate, vegetation and ground ...
Jones, Benjamin M. +3 more
core +1 more source

