http://iopscience.iop.org/1748-9326/10/8/084018/article?fromSearchPage=true

How effective is albedo modification (solar radiation management
geoengineering) in preventing sea-level rise from the Greenland Ice Sheet?

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Patrick J Applegate and Klaus Keller 2015 Environ. Res. Lett. 10 084018
doi:10.1088/1748-9326/10/8/084018

17 August 2015

Abstract
Albedo modification (AM) is sometimes characterized as a potential means of
avoiding climate threshold responses, including large-scale ice sheet mass
loss. Previous work has investigated the effects of AM on total sea-level
rise over the present century, as well as AM's ability to reduce long-term
(Gt103 yr) contributions to sea-level rise from the Greenland Ice Sheet
(GIS). These studies have broken new ground, but neglect important
feedbacks in the GIS system, or are silent on AM's effectiveness over the
short time scales that may be most relevant for decision-making (<103 yr).
Here, we assess AM's ability to reduce GIS sea-level contributions over
decades to centuries, using a simplified ice sheet model. We drive this
model using a business-as-usual base temperature forcing scenario, as well
as scenarios that reflect AM-induced temperature stabilization or
temperature drawdown. Our model results suggest that (i) AM produces
substantial near-term reductions in the rate of GIS-driven sea-level rise.
However, (ii) sea-level rise contributions from the GIS continue after AM
begins. These continued sea level rise contributions persist for decades to
centuries after temperature stabilization and temperature drawdown begin,
unless AM begins in the next few decades. Moreover, (iii) any regrowth of
the GIS is delayed by decades or centuries after temperature drawdown
begins, and is slow compared to pre-AM rates of mass loss. Combined with
recent work that suggests AM would not prevent mass loss from the West
Antarctic Ice Sheet, our results provide a nuanced picture of AM's possible
effects on future sea-level rise.

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