Results 41 to 50 of about 96,608 (241)

A persistent and dynamic East Greenland Ice Sheet over the past 7.5 million years [PDF]

open access: yes, 2016
Climate models show that ice-sheet melt will dominate sea-level rise over the coming centuries, but our understanding of ice-sheet variations before the last interglacial 125,000 years ago remains fragmentary.
Bierman, Paul R.   +4 more
core   +2 more sources

Greenland ice sheet contribution to sea level rise during the last interglacial period: a modelling study driven and constrained by ice core data [PDF]

open access: yesClimate of the Past, 2013
As pointed out by the forth assessment report of the Intergovernmental Panel on Climate Change, IPCC-AR4 (Meehl et al., 2007), the contribution of the two major ice sheets, Antarctica and Greenland, to global sea level rise, is a subject of key ...
A. Quiquet   +3 more
doaj   +1 more source

Circum-Greenland, ice-thickness measurements collected during PROMICE airborne surveys in 2007, 2011 and 2015 [PDF]

open access: yes, 2018
The Greenland ice sheet has experienced an average mass loss of 142 ± 49 Gt/yr from 1992 to 2011 (Shepherd et al. 2012), making it a significant contributor to sea-level rise.
Colgan, William   +6 more
core   +2 more sources

GrSMBMIP: intercomparison of the modelled 1980–2012 surface mass balance over the Greenland Ice Sheet

open access: yesThe Cryosphere, 2020
. Observations and models agree that the Greenland Ice Sheet (GrIS) surface mass balance (SMB) has decreased since the end of the 1990s due to an increase in meltwater runoff and that this trend will accelerate in the future. However, large uncertainties
X. Fettweis   +40 more
semanticscholar   +1 more source

Earliest Holocene south Greenland ice sheet retreat within its late Holocene extent [PDF]

open access: yes, 2014
Early Holocene summer warmth drove dramatic Greenland ice sheet (GIS) retreat. Subsequent insolation-driven cooling caused GIS margin readvance to late Holocene maxima, from which ice margins are now retreating.
Anslow, FS   +8 more
core   +1 more source

Large subglacial source of mercury from the southwestern margin of the Greenland Ice Sheet

open access: yesNature Geoscience, 2021
The Greenland Ice Sheet is currently not accounted for in Arctic mercury budgets, despite large and increasing annual runoff to the ocean and the socio-economic concerns of high mercury levels in Arctic organisms.
J. Hawkings   +21 more
semanticscholar   +1 more source

Constraining GRACE-derived cryosphere-attributed signal to irregularly shaped ice-covered areas [PDF]

open access: yesThe Cryosphere, 2013
We use a Monte Carlo approach to invert a spherical harmonic representation of cryosphere-attributed mass change in order to infer the most likely underlying mass changes within irregularly shaped ice-covered areas at nominal 26 km resolution.
W. Colgan   +3 more
doaj   +1 more source

Subglacial roughness of the Greenland Ice Sheet: relationship with contemporary ice velocity and geology

open access: yesThe Cryosphere, 2019
. The subglacial environment of the Greenland Ice Sheet (GrIS) is poorly constrained both in its bulk properties, for example geology, the presence of sediment, and the presence of water, and interfacial conditions, such as roughness and bed rheology ...
M. Cooper   +5 more
semanticscholar   +1 more source

Greenland Ice Sheet solid ice discharge from 1986 through March 2020

open access: yesEarth System Science Data, 2020
. We present a 1986 through March 2020 estimate of Greenland Ice Sheet ice discharge. Our data include all discharging ice that flows faster than 100 m yr−1 and are generated through an automatic and adaptable method, as opposed to conventional ...
K. Mankoff   +5 more
semanticscholar   +1 more source

Recent deposition of 210Pb on the Greenland ice sheet: variations in space and time [PDF]

open access: yes, 1990
Detailed 210Pb profiles were determined for four Chernobyl dated\u27 snowpits sampled during a wide-ranging survey of the Greenland ice sheet during the 1988 season.
Dibb, Jack E.
core   +2 more sources

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