Brief communication: Reduction in the future Greenland ice sheet surface melt with the help of solar geoengineering
The Greenland Ice Sheet (GrIS) will be losing mass at an accelerating pace throughout the 21st century, with a direct link between anthropogenic greenhouse gas emissions and the magnitude of Greenland mass loss. Currently, approximately 60 % of the mass loss contribution comes from surface melt and...
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Veröffentlicht in: | The cryosphere 2021-06, Vol.15 (6), p.3013-3019 |
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Zusammenfassung: | The Greenland Ice Sheet (GrIS) will be losing mass at an accelerating pace
throughout the 21st century, with a direct link between anthropogenic
greenhouse gas emissions and the magnitude of Greenland mass loss.
Currently, approximately 60 % of the mass loss contribution comes from
surface melt and subsequent meltwater runoff, while 40 % are due to ice
calving. In the ablation zone covered by bare ice in summer, most of the
surface melt energy is provided by absorbed shortwave fluxes, which could be
reduced by solar geoengineering measures. However, so far very little is
known about the potential impacts of an artificial reduction in the incoming
solar radiation on the GrIS surface energy budget and the subsequent change
in meltwater production. By forcing the regional climate model MAR with the
latest CMIP6 shared socioeconomic pathways (SSP) future emission scenarios
(SSP245, SSP585) and associated G6solar experiment from the CNRM-ESM2-1
Earth system model, we estimate the local impact of a reduced solar constant
on the projected GrIS surface mass balance (SMB) decrease. Overall, our
results show that even in the case of a low-mitigation greenhouse gas emissions
scenario (SSP585), the Greenland surface mass loss can be brought in line
with the medium-mitigation emissions scenario (SSP245) by reducing the solar
downward flux at the top of the atmosphere by ∼ 40 W/m2 or
∼ 1.5 % (using the G6solar experiment). In addition to
reducing global warming in line with SSP245, G6solar also decreases the
efficiency of surface meltwater production over the Greenland ice sheet by
damping the well-known positive melt–albedo feedback. With respect to a MAR
simulation where the solar constant remains unchanged, decreasing the solar
constant according to G6solar in the MAR radiative scheme mitigates the
projected Greenland ice sheet surface melt increase by 6 %. However, only
more constraining geoengineering experiments than G6solar would allow us to
maintain a positive SMB until the end of this century without any reduction in
our greenhouse gas emissions. |
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ISSN: | 1994-0424 1994-0416 1994-0424 1994-0416 |
DOI: | 10.5194/tc-15-3013-2021 |