Results 11 to 20 of about 14,782 (212)

Retreat and frontal ablation rates for Alaska’s lake-terminating glaciers: Investigating potential physical controls with implications for future stability

open access: yesJournal of Glaciology
Globally, glaciers are changing in response to climate warming, with those that terminate in water often undergoing the most rapid change. In Alaska and northwest Canada, proglacial lakes have grown in number and size but their influence on glacier mass ...
Noah G. Caldwell   +7 more
doaj   +3 more sources

Land- to lake-terminating transition triggers dynamic thinning of a Bhutanese glacier [PDF]

open access: yesThe Cryosphere, 2022
There have been rapid increases in both the number and expansion of the proglacial lakes across High Mountain Asia. However, the relationship between proglacial lakes and glacier dynamics remains unclear in the Himalayan region.
Y. Sato   +4 more
doaj   +3 more sources

Contrasting surface velocities between lake- and land-terminating glaciers in the Himalayan region [PDF]

open access: yesThe Cryosphere, 2021
Meltwater from Himalayan glaciers sustains the flow of rivers such as the Ganges and Brahmaputra on which over half a billion people depend for day-to-day needs. Upstream areas are likely to be affected substantially by climate change, and changes in the
J. B. Pronk   +5 more
doaj   +2 more sources

Dulung Proglacial Lake, Suru Sub-Basin, Western Himalaya: Evolution, Controls and Impacts on Glacier Stability

open access: yesFrontiers in Environmental Science, 2022
Proglacial lakes are continually developing and expanding across the Himalayan glaciered terrain in response to climate change. These lakes are known to destabilize the glaciers by enhancing their frontal ablation, causing higher than average glacier ...
Siddhi Garg   +7 more
doaj   +2 more sources

Dynamic Evolution Modeling of a Lake-Terminating Glacier in the Western Himalayas Using a Two-Dimensional Higher-Order Flowline Model

open access: yesRemote Sensing, 2022
To better understand the future evolution of Jiemayangzong Glacier (JMYZG), the headstream of the Yarlung Zangbo River, we simulated its future ice thickness evolution using a two-dimensional higher-order numerical flowline model. Due to the sparsity of in situ observational data, we used a combination of field observations and inversion models of ...
Zhan Yan   +6 more
openaire   +3 more sources

The Formation of an Ice-Contact Proglacial Lake and Its Impact on Glacier Change: A Case Study of the Tanymas Lake and Fedchenko Glacier

open access: yesRemote Sensing, 2023
Lake-terminating glaciers have some peculiar behaviors compared to land-terminating glaciers, but in-depth observation is still limited regarding their formation, which is crucial for understanding the glacier–lake interaction.
Zhijie Li   +3 more
doaj   +2 more sources

Spatial variability in mass loss of glaciers in the Everest region, central Himalayas, between 2000 and 2015 [PDF]

open access: yesThe Cryosphere, 2017
Region-wide averaging of Himalayan glacier mass change has masked any catchment or glacier-scale variability in glacier recession; thus the role of a number of glaciological processes in glacier wastage remains poorly understood.
O. King   +3 more
doaj   +12 more sources

Subglacial discharge controls seasonal variations in the thermal structure of a glacial lake in Patagonia [PDF]

open access: yesNature Communications, 2021
Thermal conditions and circulation near glacier fronts are important to understand the recent rapid retreat of calving glaciers. New observations from a glacial lake suggesting a feedback mechanism between atmospheric warming, glacier front melting and ...
Shin Sugiyama   +7 more
doaj   +2 more sources

Glacier Mass Changes of Lake-Terminating Grey and Tyndall Glaciers at the Southern Patagonia Icefield Derived From Geodetic Observations and Energy and Mass Balance Modeling [PDF]

open access: yesFrontiers in Earth Science, 2018
Published by Frontiers Media ...
Stephanie S. Weidemann   +8 more
openaire   +5 more sources

Lake surface and downstream river temperature response to the retreat of a lake‐terminating glacier

open access: yesHydrological Processes
AbstractGlacier contributions to streamflow moderate summer water temperatures and help keep rivers cool during periods of hot, dry weather. As glaciers retreat, the length of channel exposed to solar radiation above a given point of interest would increase, which should ultimately result in higher water temperatures.
B. M. Pelto   +4 more
openaire   +2 more sources

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