Short-lived pollutants in the Arctic: their climate impact and possible mitigation strategies

被引:264
作者
Quinn, P. K. [1 ]
Bates, T. S. [1 ]
Baum, E. [2 ]
Doubleday, N. [3 ]
Fiore, A. M. [4 ]
Flanner, M. [5 ]
Fridlind, A. [6 ]
Garrett, T. J. [7 ]
Koch, D. [6 ]
Menon, S. [8 ]
Shindell, D. [6 ]
Stohl, A. [9 ]
Warren, S. G. [10 ]
机构
[1] NOAA, Pacific Marine Environm Lab, Seattle, WA 98115 USA
[2] Clean Air Task Force, Boston, MA USA
[3] Carleton Univ, Ottawa, ON K1S 5B6, Canada
[4] NOAA, Geophys Fluid Dynam Lab, Princeton, NJ USA
[5] NCAR, Adv Study Program, Boulder, CO USA
[6] NASA, Goddard Inst Space Studies, New York, NY 10025 USA
[7] Univ Utah, Salt Lake City, UT USA
[8] Univ Calif Berkeley, Lawrence Berkeley Lab, Berkeley, CA 94720 USA
[9] Norwegian Inst Air Res, Kjeller, Norway
[10] Univ Washington, Seattle, WA 98195 USA
关键词
D O I
10.5194/acp-8-1723-2008
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Several short-lived pollutants known to impact Arctic climate may be contributing to the accelerated rates of warming observed in this region relative to the global annually averaged temperature increase. Here, we present a summary of the short-lived pollutants that impact Arctic climate including methane, tropospheric ozone, and tropospheric aerosols. For each pollutant, we provide a description of the major sources and the mechanism of forcing. We also provide the first seasonally averaged forcing and corresponding temperature response estimates focused specifically on the Arctic. The calculations indicate that the forcings due to black carbon, methane, and tropospheric ozone lead to a positive surface temperature response indicating the need to reduce emissions of these species within and outside the Arctic. Additional aerosol species may also lead to surface warming if the aerosol is coincident with thin, low lying clouds. We suggest strategies for reducing the warming based on current knowledge and discuss directions for future research to address the large remaining uncertainties.
引用
收藏
页码:1723 / 1735
页数:13
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