http://iopscience.iop.org/1748-9326/10/4/044020/

Environmental Research Letters Volume 10 Number 4
Ivana Cvijanovic et al 2015 Environ. Res. Lett. 10 044020
doi:10.1088/1748-9326/10/4/044020

Impacts of ocean albedo alteration on Arctic sea ice restoration and
Northern Hemisphere climate

OPEN ACCESS
Ivana Cvijanovic, Ken Caldeira and Douglas G MacMartin

Abstract

The Arctic Ocean is expected to transition into a seasonally ice-free state
by mid-century, enhancing Arctic warming and leading to substantial
ecological and socio-economic challenges across the Arctic region. It has
been proposed that artificially increasing high latitude ocean albedo could
restore sea ice, but the climate impacts of such a strategy have not been
previously explored. Motivated by this, we investigate the impacts of
idealized high latitude ocean albedo changes on Arctic sea ice restoration
and climate. In our simulated 4xCO2 climate, imposing surface albedo
alterations over the Arctic Ocean leads to partial sea ice recovery and a
modest reduction in Arctic warming. With the most extreme ocean albedo
changes, imposed over the area 70°–90°N, September sea ice cover stabilizes
at ~40% of its preindustrial value (compared to ~3% without imposed albedo
modifications). This is accompanied by an annual mean Arctic surface
temperature decrease of ~2 °C but no substantial global mean temperature
decrease. Imposed albedo changes and sea ice recovery alter climate outside
the Arctic region too, affecting precipitation distribution over parts of
the continental United States and Northeastern Pacific. For example,
following sea ice recovery, wetter and milder winter conditions are present
in the Southwest United States while the East Coast experiences cooling. We
conclude that although ocean albedo alteration could lead to some sea ice
recovery, it does not appear to be an effective way of offsetting the
overall effects of CO2 induced global warming.

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