Results 21 to 30 of about 6,744,784 (307)
Four decades of Antarctic Ice Sheet mass balance from 1979–2017
Significance Statement We evaluate the state of the mass balance of the Antarctic Ice Sheet over the last four decades using a comprehensive, precise satellite record and output products from a regional atmospheric climate model to document its impact on
E. Rignot +5 more
semanticscholar +1 more source
Forty-six years of Greenland Ice Sheet mass balance from 1972 to 2018
Significance We reconstruct the mass balance of the Greenland Ice Sheet for the past 46 years by comparing glacier ice discharge into the ocean with interior accumulation of snowfall from regional atmospheric climate models over 260 drainage basins.
J. Mouginot +8 more
semanticscholar +1 more source
Marsh Sedimentation Controls Delta Top Morphology, Slope, and Mass Balance
Rising sea levels, subsidence, and decreased fluvial sediment load threaten river deltas and their wetlands. However, the feedbacks between fluvial and non‐fluvial (marsh) deposition remain weakly constrained.
K. M. Sanks +5 more
doaj +1 more source
The Himalayan glaciers contribute significantly to regional water resources. However, limited field observations restrict our understanding of glacier dynamics and behaviour.
Arindan Mandal +9 more
semanticscholar +1 more source
Haxilegen Glacier No.51 (43.731°N, 84.391°E; CN5Y741C0051) is located in the Kuytun river basin, Erenharbirga range, eastern Tien Shan. This study presents the annual mass balance of Haxilegen Glacier No.51 for 7 hydrological years and uses a temperature-
HUI ZHANG +4 more
doaj +1 more source
Potential of the retention capability of a Neotropical reservoir (São Paulo State, Brazil) [PDF]
: Aim Man-made reservoirs lead to several changes in their downstream rivers that depend on the hydraulic characteristics of the reservoirs. However, their multiple uses can also provide facilities that influence the ecosystem services that they provide.
Flavia Bottino +4 more
doaj +1 more source
Region-Wide Annual Glacier Surface Mass Balance for the European Alps From 2000 to 2016
Studying glacier mass changes at regional scale provides critical insights into the impact of climate change on glacierized regions, but is impractical using in situ estimates alone due to logistical and human constraints.
L. Davaze +4 more
semanticscholar +1 more source
. Antarctic ice sheet mass loss is currently equivalent to around 1 mm year−1 of global mean sea level rise. Most mass is lost due to sub-ice shelf melting and calving of icebergs.
R. Mottram +16 more
semanticscholar +1 more source
We show results from a positive degree-day (PDD) model of Greenland ice sheet (GrIS) surface mass balance (SMB), 1870–2012, forced with reanalysis data. The model includes an improved daily temperature parameterization as compared with a previous version
DAVID J. WILTON +6 more
doaj +1 more source
Debris Emergence Elevations and Glacier Change
Debris-covered glaciers represent potentially significant stores of freshwater in river basins throughout High Mountain Asia (HMA). Direct glacier mass balance measurements are extremely difficult to maintain on debris-covered glaciers, and optical ...
Joseph M. Shea +3 more
doaj +1 more source

