Bayesian Approach to Estimate Proglacial Lake Volume (BE‐GLAV)
We present a new model called Bayesian Estimated Glacial Lake Volume (BE‐GLAV) to estimate the volume of proglacial lakes. Presuming the lake cross‐section as trapezoidal, BE‐GLAV uses a Bayesian calibration approach to adjust the cross‐sectional ...
Prateek Gantayat +4 more
doaj +3 more sources
Ice‐Marginal Proglacial Lakes Across Greenland: Present Status and a Possible Future [PDF]
Ice‐marginal lakes can affect glacier dynamics but are ignored in studies of the evolution of the Greenland ice sheet (GrIS) and of peripheral mountain glaciers and ice caps (PGICs).
Jonathan L. Carrivick +8 more
doaj +6 more sources
Diversity, Function and Activity of DNA Viruses in the Qiangyong Proglacial Lake Sediment, the Tibetan Plateau. [PDF]
This study identified DNA viruses from Qiangyong proglacial lake sediments on the Tibetan Plateau, revealing a highly diverse and previously uncharacterized viral community. These viruses influence microbial community structure and function by infecting key nutrient‐transforming taxa and encoding auxiliary metabolic genes that modulate host metabolism.
Zhao Y +6 more
europepmc +2 more sources
Evaluation of lacustrine groundwater discharge, hydrologic partitioning, and nutrient budgets in a proglacial lake in the Qinghai–Tibet Plateau: using 222Rn and stable isotopes [PDF]
Proglacial lakes are good natural laboratories to investigate groundwater and glacier dynamics under current climate conditions and to explore biogeochemical cycling under pristine lake status. This study conducted a series of investigations of 222Rn,
X. Luo +14 more
doaj +1 more source
Links between proglacial lakes and glacier dynamics are poorly understood but are necessary to predict how mountain glaciers will react to a warmer, wetter climate, where such lakes are expected to increase both in number and volume.
Brittany Main +11 more
doaj +1 more source
Deglaciation and proglacial lakes [PDF]
Glaciers and ice sheets are important constituents of the Earth's land surface. Current worldwide retreat of glaciers has implications for the environment and for civilisation. There are a range of geomorphic changes occurring in cold environments and it is anticipated that these will be accentuated as a consequence of climate change.
TWEED, Fiona, Carrivick, Jonathan L.
openaire +2 more sources
Deglacial ice sheet instabilities induced by proglacial lakes [PDF]
AbstractDuring the last deglaciation (21–7 kaBP), the gradual retreat of Northern Hemisphere ice sheet margins produced large proglacial lakes. While the climatic impacts of these lakes have been widely acknowledged, their role on ice sheet grounding line dynamics has received very little attention so far.
Quiquet, Aurélien +5 more
openaire +4 more sources
Gulf of Alaska ice-marginal lake area change over the Landsat record and potential physical controls [PDF]
Lakes in contact with glacier margins can impact glacier evolution as well as the downstream biophysical systems, flood hazard, and water resources. Recent work suggests positive feedbacks between glacier wastage and ice-marginal lake evolution, although
H. R. Field +5 more
doaj +1 more source
Buoyant calving and ice-contact lake evolution at Pasterze Glacier (Austria) in the period 1998–2019 [PDF]
Rapid growth of proglacial lakes in the current warming climate can pose significant outburst flood hazards, increase rates of ice mass loss, and alter the dynamic state of glaciers. We studied the nature and rate of proglacial lake evolution at Pasterze
A. Kellerer-Pirklbauer +5 more
doaj +1 more source
Warm Arctic Proglacial Lakes in the ASTER Surface Temperature Product [PDF]
Despite an increase in heatwaves and rising air temperatures in the Arctic, little research has been conducted into the temperatures of proglacial lakes in the region. An assumption persists that they are cold and uniformly feature a temperature of 1 °C. This is important to test, given the rising air temperatures in the region (reported in this study)
Adrian Dye +4 more
openaire +4 more sources

