Solar geoengineering in the polar regions: A review
Solar geoengineering refers to proposals, including stratospheric aerosol injection (SAI), to
slow or reverse climate change by reflecting away incoming sunlight. The rapid changes …
slow or reverse climate change by reflecting away incoming sunlight. The rapid changes …
[HTML][HTML] Climate intervention on a high-emissions pathway could delay but not prevent West Antarctic Ice Sheet demise
Solar radiation modification (SRM) is increasingly discussed as a tool to reduce or avert
global warming and concomitantly the risk of ice-sheet collapse, as is considered possible …
global warming and concomitantly the risk of ice-sheet collapse, as is considered possible …
[HTML][HTML] Identifying the sources of uncertainty in climate model simulations of solar radiation modification with the G6sulfur and G6solar Geoengineering Model …
We present here results from the Geoengineering Model Intercomparison Project (GeoMIP)
simulations for the experiments G6sulfur and G6solar for six Earth system models …
simulations for the experiments G6sulfur and G6solar for six Earth system models …
[HTML][HTML] Mass changes of the northern Antarctic Peninsula Ice Sheet derived from repeat bi-static synthetic aperture radar acquisitions for the period 2013–2017
T Seehaus, C Sommer, T Dethinne, P Malz - The Cryosphere, 2023 - tc.copernicus.org
Some of the highest specific mass change rates in Antarctica are reported for the Antarctic
Peninsula. However, the existing estimates for the northern Antarctic Peninsula (< 70∘ S) …
Peninsula. However, the existing estimates for the northern Antarctic Peninsula (< 70∘ S) …
Shallow firn cores 1989–2019 in southwest Greenland's percolation zone reveal decreasing density and ice layer thickness after 2012
Refreezing of meltwater in firn is a major component of Greenland ice-sheet's mass budget,
but in situ observations are rare. Here, we compare the firn density and total ice layer …
but in situ observations are rare. Here, we compare the firn density and total ice layer …
Thermosteric and dynamic sea level under solar geoengineering
C Yue, S Jevrejeva, Y Qu, L Zhao… - npj Climate and …, 2023 - nature.com
The IPCC sixth assessment report forecasts sea level rise (SLR) of up to 2 m along coasts by
2100 relative to 1995–2014 following business as usual (SSP585) scenarios …
2100 relative to 1995–2014 following business as usual (SSP585) scenarios …
Sensitivity of the MAR regional climate model snowpack to the parameterization of the assimilation of satellite-derived wet-snow masks on the Antarctic Peninsula
Both regional climate models (RCMs) and remote sensing (RS) data are essential tools in
understanding the response of polar regions to climate change. RCMs can simulate how …
understanding the response of polar regions to climate change. RCMs can simulate how …
[HTML][HTML] Impact of the melt–albedo feedback on the future evolution of the Greenland Ice Sheet with PISM-dEBM-simple
Surface melting of the Greenland Ice Sheet contributes a large amount to current and future
sea level rise. Increased surface melt may lower the reflectivity of the ice sheet surface and …
sea level rise. Increased surface melt may lower the reflectivity of the ice sheet surface and …
Reduced ice loss from Greenland under stratospheric aerosol injection
Sea level rise (SLR) due to surface melt and to dynamic losses from the ice sheets—that is
via accelerated flow of glaciers into the sea—is something that may be potentially mitigated …
via accelerated flow of glaciers into the sea—is something that may be potentially mitigated …
[HTML][HTML] Assessing bare-ice albedo simulated by MAR over the Greenland ice sheet (2000–2021) and implications for meltwater production estimates
Surface mass loss from the Greenland ice sheet (GrIS) has accelerated over the past
decades, mainly due to enhanced surface melting and liquid water runoff in response to …
decades, mainly due to enhanced surface melting and liquid water runoff in response to …