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Permafrost and Periglacial Processes, 2020
The acceleration of permafrost thaw due to warming, wetting, and disturbance is altering circumpolar landscapes. The effect of thaw is largely determined by ground ice content in near‐surface permafrost, making the characterization and prediction of ...
Jason R. Paul, S. Kokelj, J. Baltzer
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The acceleration of permafrost thaw due to warming, wetting, and disturbance is altering circumpolar landscapes. The effect of thaw is largely determined by ground ice content in near‐surface permafrost, making the characterization and prediction of ...
Jason R. Paul, S. Kokelj, J. Baltzer
semanticscholar +1 more source
, 2020
Ground ice is a key component of permafrost, and its melt induced by climate change and anthropogenic disturbance has been causing increased ground surface subsidence, thermal erosion, and engineering problems.
Zhan-ju Lin +6 more
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Ground ice is a key component of permafrost, and its melt induced by climate change and anthropogenic disturbance has been causing increased ground surface subsidence, thermal erosion, and engineering problems.
Zhan-ju Lin +6 more
semanticscholar +1 more source
Science of the Total Environment, 2020
The stable-isotope data of ground ice from a deep borehole (~46 m) at the Tianshuihai (TSH) lake basin on the northwestern Qinghai-Tibet Plateau (QTP) are presented together with cryolithological information.
Yuzhong Yang +3 more
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The stable-isotope data of ground ice from a deep borehole (~46 m) at the Tianshuihai (TSH) lake basin on the northwestern Qinghai-Tibet Plateau (QTP) are presented together with cryolithological information.
Yuzhong Yang +3 more
semanticscholar +1 more source
(Ground) Ice in the Proglacial Zone
Geography of the Physical Environment, 2018Gärtner-Roer, Isabelle, Bast, Alexander
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Estimation of Permafrost Ground Ice to 10 m Depth on the Qinghai‐Tibet Plateau
Permafrost and Periglacial ProcessesPermafrost ground ice melting could alter hydrological processes in cold regions by releasing water. Currently, there is a lack of gridded data of ground ice from the Qinghai‐Tibet Plateau (QTP).
D. Zou +8 more
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Permafrost and Periglacial Processes, 2019
Knowledge of the amount of unfrozen water and its migration in permafrost soils is important for understanding physico‐chemical and biological processes.
D. Fisher, D. Lacelle, W. Pollard
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Knowledge of the amount of unfrozen water and its migration in permafrost soils is important for understanding physico‐chemical and biological processes.
D. Fisher, D. Lacelle, W. Pollard
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ARCTIC, 1975
In August 1972, the U.S. Coast Guard icebreaker Burton Island confirmed the existence of a large ice formation located at about 160 km northwest of Point Barrow, which had first been observed by 1971 satellite imagery of the U.S. National Ocean and Atmospheric Administration (NOAA-1).
Austin Kovacs +2 more
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In August 1972, the U.S. Coast Guard icebreaker Burton Island confirmed the existence of a large ice formation located at about 160 km northwest of Point Barrow, which had first been observed by 1971 satellite imagery of the U.S. National Ocean and Atmospheric Administration (NOAA-1).
Austin Kovacs +2 more
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Science of the Total Environment, 2019
Ground ice is a distinctive feature of permafrost, and its thawing under climate change can alter the regional hydrological and biogeochemical cycles. Spatial variations and determinants of ground ice isotopes are critical to understand subsurface water ...
Weihua Wang +8 more
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Ground ice is a distinctive feature of permafrost, and its thawing under climate change can alter the regional hydrological and biogeochemical cycles. Spatial variations and determinants of ground ice isotopes are critical to understand subsurface water ...
Weihua Wang +8 more
semanticscholar +1 more source