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Earth System Dynamics An interactive open-access journal of the European Geosciences Union
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Volume 4, issue 2
Earth Syst. Dynam., 4, 301-315, 2013
https://doi.org/10.5194/esd-4-301-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
Earth Syst. Dynam., 4, 301-315, 2013
https://doi.org/10.5194/esd-4-301-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 02 Sep 2013

Research article | 02 Sep 2013

Climate response to imposed solar radiation reductions in high latitudes

M. C. MacCracken1, H.-J. Shin2,3, K. Caldeira2, and G. A. Ban-Weiss2,4 M. C. MacCracken et al.
  • 1Climate Institute, 900 17th St. NW, Suite 700, Washington, DC 20006, USA
  • 2Carnegie Institution for Science, Dept. of Global Ecology, 260 Panama Street, Stanford, CA 94305, USA
  • 3Ocean Circulation and Climate Research Division, Korea Institute of Ocean Science and Technology (KIOST), 787Haean-ro, Sangnok-gu, Ansan-si, Gyeonggi-do, 426-744, South Korea
  • 4Department of Civil and Environmental Engineering, University of Southern California, Los Angeles, CA 90089, USA

Abstract. With human-induced climate change leading to amplified warming in high latitudes, mitigation alone is unlikely to be rapid enough to prevent significant, even irreversible, impacts. Model simulations in which solar insolation was arbitrarily reduced poleward of 51, 61, or 71° latitude in one or both hemispheres not only cooled those regions, but also drew energy from lower latitudes, exerting a cooling influence over much of the particular hemisphere in which the reduction was imposed. The simulations, conducted using the National Center for Atmospheric Research's CAM3.1 atmospheric model coupled to a slab ocean, indicated that high-latitude reductions in absorbed solar radiation have a significantly larger cooling influence than solar reductions of equivalent magnitude spread evenly over the Earth. This amplified influence occurred primarily because concentrated high-latitude reductions in solar radiation led to increased sea ice fraction and surface albedo, thereby amplifying the energy deficit at the top of the atmosphere as compared to the response for an equivalent reduction in solar radiation spread evenly over the globe. Reductions in incoming solar radiation in one polar region (either north or south) resulted in increased poleward energy transport during that hemisphere's cold season and shifted the Inter-Tropical Convergence Zone (ITCZ) away from that pole, whereas comparable solar reductions in both polar regions resulted in increased poleward energy transport, but tended to leave the ITCZ approximately in place. Together, these results suggest that, until emissions reductions are sufficient to limit the warming influence of increasing greenhouse gas concentrations, polar reductions in solar radiation, if they could be efficiently and effectively implemented, warrant further research as an approach to moderating the early stages of both high-latitude and global warming.

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