The Greenland and Antarctic ice sheets under 1.5 C global warming
Even if anthropogenic warming were constrained to less than 2° C above pre-industrial, the
Greenland and Antarctic ice sheets will continue to lose mass this century, with rates similar …
Greenland and Antarctic ice sheets will continue to lose mass this century, with rates similar …
[HTML][HTML] The build-up, configuration, and dynamical sensitivity of the Eurasian ice-sheet complex to Late Weichselian climatic and oceanic forcing
The Eurasian ice-sheet complex (EISC) was the third largest ice mass during the Last
Glacial Maximum (LGM), after the Antarctic and North American ice sheets. Despite its …
Glacial Maximum (LGM), after the Antarctic and North American ice sheets. Despite its …
The EC-earth3 Earth system model for the climate model intercomparison project 6
The Earth System Model EC-Earth3 for contributions to CMIP6 is documented here, with its
flexible coupling framework, major model configurations, a methodology for ensuring the …
flexible coupling framework, major model configurations, a methodology for ensuring the …
Polar regions
MP Meredith, M Sommerkorn… - The ocean and …, 2019 - research.monash.edu
This chapter assesses the state of physical, biological and social knowledge concerning the
Arctic and Antarctic ocean and cryosphere, how they are affected by climate change, and …
Arctic and Antarctic ocean and cryosphere, how they are affected by climate change, and …
BedMachine v3: Complete bed topography and ocean bathymetry mapping of Greenland from multibeam echo sounding combined with mass conservation
M Morlighem, CN Williams, E Rignot… - Geophysical …, 2017 - Wiley Online Library
Greenland's bed topography is a primary control on ice flow, grounding line migration,
calving dynamics, and subglacial drainage. Moreover, fjord bathymetry regulates the …
calving dynamics, and subglacial drainage. Moreover, fjord bathymetry regulates the …
[HTML][HTML] The future sea-level contribution of the Greenland ice sheet: a multi-model ensemble study of ISMIP6
The Greenland ice sheet is one of the largest contributors to global mean sea-level rise
today and is expected to continue to lose mass as the Arctic continues to warm. The two …
today and is expected to continue to lose mass as the Arctic continues to warm. The two …
Contribution of the Greenland Ice Sheet to sea level over the next millennium
The Greenland Ice Sheet holds 7.2 m of sea level equivalent and in recent decades, rising
temperatures have led to accelerated mass loss. Current ice margin recession is led by the …
temperatures have led to accelerated mass loss. Current ice margin recession is led by the …
Ice dynamics will remain a primary driver of Greenland ice sheet mass loss over the next century
The mass loss of the Greenland Ice Sheet is nearly equally partitioned between a decrease
in surface mass balance from enhanced surface melt and an increase in ice dynamics from …
in surface mass balance from enhanced surface melt and an increase in ice dynamics from …
Extensive inland thinning and speed-up of Northeast Greenland Ice Stream
Over the past two decades, ice loss from the Greenland ice sheet (GrIS) has increased
owing to enhanced surface melting and ice discharge to the ocean,,,–. Whether continuing …
owing to enhanced surface melting and ice discharge to the ocean,,,–. Whether continuing …
Rate of mass loss from the Greenland Ice Sheet will exceed Holocene values this century
Abstract The Greenland Ice Sheet (GIS) is losing mass at a high rate 1. Given the short-term
nature of the observational record, it is difficult to assess the historical importance of this …
nature of the observational record, it is difficult to assess the historical importance of this …