Limited effectiveness of solar radiation management geoengineering in
preventing sea-level rise from the Greenland Ice Sheet

Authors:
Applegate, Patrick; Keller, Klaus

[email protected]),

EGU General Assembly 2015

04/2015

Abstract

The Greenland Ice Sheet (GIS) is an important contributor to present-day
sea level rise, and the ice sheet's importance for sea level rise will
likely increase with Arctic temperatures. Some scientists have recently
suggested that geoengineering, the deliberate management of Earth's
climate, could prevent sea level rise from the ice sheets. Previous efforts
to assess geoengineering's effects on the GIS and sea level rise have
broken important new ground, but neglect key feedbacks and/or are silent on
the short-term effects of geoengineering that are perhaps most important
for decision-making. Here, we use a simplified, three-dimensional model of
the GIS (SICOPOLIS by Ralf Greve) to examine the response of the Greenland
Ice Sheet under plausible geoengineering scenarios. We find that i) the GIS
generally continues to melt over the first 100 yr after geoengineering
initiation; ii) reductions in GIS sea level contributions over these first
100 yr are small; and iii) there is a delay of decades to centuries between
the initiation of aggressive geoengineering and any regrowth of the ice
sheet, and the rate of this regrowth is slow. However, geoengineering
produces appreciable reductions in the rate of sea level rise contributions
from the GIS within the first few decades. Our results suggest that past
studies have overestimated the effectiveness of geoengineering in
preventing mass loss from the Greenland Ice Sheet and in reversing sea
level rise once it has occurred. We comment on the importance of feedbacks
in the ice sheet system in assessing geoengineering's effectiveness in
reducing sea level rise from the GIS.

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