Results 21 to 30 of about 231,447 (261)
A minimal model for reconstructing interannual mass balance variability of glaciers in the European Alps [PDF]
We present a minimal model of the glacier surface mass balance. The model relies solely on monthly precipitation and air temperatures as forcing. We first train the model individually for 15 glaciers with existing mass balance measurements.
B. Marzeion +4 more
doaj +4 more sources
The Cordillera Darwin Icefield loses mass at a similar rate as the Northern and Southern Patagonian Icefields, showing contrasting individual glacier responses, particularly between the north-facing and south-facing glaciers, which are subject to ...
Guilherme Netto +2 more
exaly +2 more sources
We present the first-ever mass-balance (MB) observation (2014–19), reconstruction (between 1978 and 2019) and sensitivity of debris-free Stok glacier (33.98°N, 77.45°E), Ladakh Region, India.
Mohd Soheb +5 more
doaj +2 more sources
The mass-balance of Muztag Ata No. 15 (MZ15) glacier in the eastern Pamir is reconstructed between 1980 and 2012 using an energy-based mass-balance model.
MEILIN ZHU +6 more
doaj +2 more sources
Disaggregating geodetic glacier mass balance to annual scale using remote-sensing proxies
Decadal-scale, high-resolution geodetic measurements of glacier thinning have transformed our understanding of glacier response to climate change. Annual glacier mass balance can be estimated using remote-sensing proxies like snow-line altitude.
Argha Banerjee +2 more
doaj +1 more source
Mass balance observations and reconstruction for Batysh Sook Glacier, Tien Shan, from 2004 to 2016
Yaning Chen +2 more
exaly +2 more sources
Glacial extent and mass balance are sensitive climate proxies providing solid information on past climatic conditions. However, series of annual mass-balance measurements of more than 60 years are scarce.
Riccardo Cerrato +6 more
doaj +1 more source
Simulating ice thickness and velocity evolution of Upernavik Isstrøm 1849–2012 by forcing prescribed terminus positions in ISSM [PDF]
Tidewater glacier velocity and mass balance are known to be highly responsive to terminus position change. Yet it remains challenging for ice flow models to reproduce observed ice margin changes. Here, using the Ice Sheet System Model (ISSM; Larour et
K. Haubner +15 more
doaj +1 more source
To get a better overview of atmosphere-driven mass changes at the 79N Glacier (Nioghalvfjerdsfjorden Glacier), the largest outlet glacier of the northeast Greenland ice stream, the surface mass balance (SMB) is modeled by linking the COupled Snowpack and
M. T. Blau +3 more
doaj +1 more source

