http://onlinelibrary.wiley.com/wol1/doi/10.1002/2015JC011433/abstract

Assessing climate impacts and risks of ocean albedo modification in the
Arctic

N. Mengis1,*, T. Martin1, D.P. Keller1 andA. Oschlies1,2

DOI: 10.1002/2015JC011433
Journal of Geophysical Research: Oceans

Keywords:
Arctic Ocean Albedo Modification

Abstract

The ice albedo feedback is one of the key factors of accelerated
temperature increase in the high northern latitudes under global warming.
This study assesses climate impacts and risks of idealized Arctic Ocean
albedo modification (AOAM), a proposed climate engineering method, during
transient climate change simulations with varying representative
concentration pathway (RCP) scenarios. We find no potential for reversing
trends in all assessed Arctic climate metrics under increasing atmospheric
CO2 concentrations. AOAM only yields an initial offset during the first
years after implementation. Nevertheless, sea ice loss can be delayed by
25(60) years in the RCP8.5(RCP4.5) scenario and the delayed thawing of
permafrost soils in the AOAM simulations prevents up to 40(32) Pg of carbon
from being released by 2100. AOAM initially dampens the decline of the
Atlantic Meridional Overturning and delays the onset of open ocean deep
convection in the Nordic Seas under the RCP scenarios. Both these processes
cause a sub-surface warming signal in the AOAM simulations relative to the
default RCP simulations with the potential to destabilize Arctic marine gas
hydrates. Furthermore, in 2100, the RCP8.5 AOAM simulation diverts more
from the 2005-2015 reference state in many climate metrics than the RCP4.5
run without AOAM. Considering the demonstrated risks, we conclude that
concerning longer time scales, reductions in emissions remain the safest
and most effective way to prevent severe changes in the Arctic.

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