Future loss of Arctic sea-ice cover could drive a substantial decrease in California’s rainfall

Ivana Cvijanovic (), Benjamin D. Santer, Céline Bonfils, Donald D. Lucas, John C. H. Chiang and Susan Zimmerman
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Ivana Cvijanovic: Lawrence Livermore National Laboratory
Benjamin D. Santer: Lawrence Livermore National Laboratory
Céline Bonfils: Lawrence Livermore National Laboratory
Donald D. Lucas: Lawrence Livermore National Laboratory
John C. H. Chiang: University of California
Susan Zimmerman: Lawrence Livermore National Laboratory

Nature Communications, 2017, vol. 8, issue 1, 1-10

Abstract: Abstract From 2012 to 2016, California experienced one of the worst droughts since the start of observational records. As in previous dry periods, precipitation-inducing winter storms were steered away from California by a persistent atmospheric ridging system in the North Pacific. Here we identify a new link between Arctic sea-ice loss and the North Pacific geopotential ridge development. In a two-step teleconnection, sea-ice changes lead to reorganization of tropical convection that in turn triggers an anticyclonic response over the North Pacific, resulting in significant drying over California. These findings suggest that the ability of climate models to accurately estimate future precipitation changes over California is also linked to the fidelity with which future sea-ice changes are simulated. We conclude that sea-ice loss of the magnitude expected in the next decades could substantially impact California’s precipitation, thus highlighting another mechanism by which human-caused climate change could exacerbate future California droughts.

Date: 2017
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DOI: 10.1038/s41467-017-01907-4

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