Coupled regional climate–ice-sheet simulation shows limited Greenland ice loss during the Eemian [PDF]
During the last interglacial period (Eemian, 130–115 kyr BP) eustatic global sea level likely peaked at > 6 m above the present-day level, but estimates of the contribution of the Greenland Ice Sheet vary widely.
M. M. Helsen +4 more
doaj +1 more source
Eemian Greenland ice sheet simulated with a higher-order model shows strong sensitivity to surface mass balance forcing [PDF]
The Greenland ice sheet contributes increasingly to global sea level rise. Its history during past warm intervals is a valuable reference for future sea level projections.
A. Plach +6 more
doaj +1 more source
Design and results of the ice sheet model initialisation initMIP-Greenland: an ISMIP6 intercomparison [PDF]
Earlier large-scale Greenland ice sheet sea-level projections (e.g. those run during the ice2sea and SeaRISE initiatives) have shown that ice sheet initial conditions have a large effect on the projections and give rise to important uncertainties. The
H. Goelzer +37 more
doaj +1 more source
Exceptionally high heat flux needed to sustain the Northeast Greenland Ice Stream [PDF]
The Northeast Greenland Ice Stream (NEGIS) currently drains more than 10 % of the Greenland Ice Sheet area and has recently undergone significant dynamic changes.
S. Smith-Johnsen +5 more
doaj +1 more source
Economics of the disintegration of the Greenland ice sheet. [PDF]
Concerns about the impact on large-scale earth systems have taken center stage in the scientific and economic analysis of climate change. The present study analyzes the economic impact of a potential disintegration of the Greenland ice sheet (GIS).
Nordhaus W.
europepmc +4 more sources
An ice sheet model validation framework for the Greenland ice sheet [PDF]
Abstract. We propose a new ice sheet model validation framework – the Cryospheric Model Comparison Tool (CmCt) – that takes advantage of ice sheet altimetry and gravimetry observations collected over the past several decades and is applied here to modeling of the Greenland ice sheet.
Stephen F. Price +17 more
openaire +7 more sources
Algal photophysiology drives darkening and melt of the Greenland Ice Sheet [PDF]
Christopher J Williamson +2 more
exaly +2 more sources
Potential subglacial lake locations and meltwater drainage pathways beneath the Antarctic and Greenland ice sheets [PDF]
We use the Shreve hydraulic potential equation as a simplified approach to investigate potential subglacial lake locations and meltwater drainage pathways beneath the Antarctic and Greenland ice sheets. We validate the method by demonstrating its ability
S. J. Livingstone +3 more
doaj +1 more source
Threatened loss of the Greenland ice-sheet [PDF]
The Greenland ice-sheet would melt faster in a warmer climate and is likely to be eliminated — except for residual glaciers in the mountains — if the annual average temperature in Greenland increases by more than about 3 °C. This could raise the global average sea-level by 7 metres over a period of 1,000 years or more.
Gregory, Jonathan +2 more
openaire +2 more sources
Constraining GRACE-derived cryosphere-attributed signal to irregularly shaped ice-covered areas [PDF]
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

