Observations of recent Arctic sea ice volume loss and its impact on ocean-atmosphere energy exchange and ice production

被引:55
作者
Kurtz, N. T. [1 ,2 ]
Markus, T. [2 ]
Farrell, S. L. [2 ,3 ]
Worthen, D. L. [2 ,4 ]
Boisvert, L. N. [2 ,5 ]
机构
[1] Univ Maryland Baltimore Cty, Joint Ctr Earth Syst Technol, Baltimore, MD 21228 USA
[2] NASA, Goddard Space Flight Ctr, Hydrospher & Biospher Sci Lab, Greenbelt, MD 20771 USA
[3] Univ Maryland, Earth Syst Sci Interdisciplinary Ctr, Cooperat Inst Climate Studies, College Pk, MD 20742 USA
[4] RS Informat Syst, Mclean, VA USA
[5] Univ Maryland, Dept Atmospher & Ocean Sci, College Pk, MD 20742 USA
基金
美国国家科学基金会;
关键词
MODEL; FLUX; AMPLIFICATION; THICKNESS; CLIMATE; BALANCE; SHEBA; SNOW;
D O I
10.1029/2010JC006235
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
Using recently developed techniques we estimate snow and sea ice thickness distributions for the Arctic basin through the combination of freeboard data from the Ice, Cloud, and land Elevation Satellite (ICESat) and a snow depth model. These data are used with meteorological data and a thermodynamic sea ice model to calculate ocean-atmosphere heat exchange and ice volume production during the 2003-2008 fall and winter seasons. The calculated heat fluxes and ice growth rates are in agreement with previous observations over multiyear ice. In this study, we calculate heat fluxes and ice growth rates for the full distribution of ice thicknesses covering the Arctic basin and determine the impact of ice thickness change on the calculated values. Thinning of the sea ice is observed which greatly increases the 2005-2007 fall period ocean-atmosphere heat fluxes compared to those observed in 2003. Although there was also a decline in sea ice thickness for the winter periods, the winter time heat flux was found to be less impacted by the observed changes in ice thickness. A large increase in the net Arctic ocean-atmosphere heat output is also observed in the fall periods due to changes in the areal coverage of sea ice. The anomalously low sea ice coverage in 2007 led to a net ocean-atmosphere heat output approximately 3 times greater than was observed in previous years and suggests that sea ice losses are now playing a role in increasing surface air temperatures in the Arctic.
引用
收藏
页数:19
相关论文
共 52 条
[41]   Retreat of the cold halocline layer in the Arctic Ocean [J].
Steele, M ;
Boyd, T .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 1998, 103 (C5) :10419-10435
[42]  
Stroeve J., 2008, Eos, V89, P13, DOI DOI 10.1029/2008EO020001
[43]   Thermal conductivity and heat transfer through the snow on the ice of the Beaufort Sea [J].
Sturm, M ;
Perovich, DK ;
Holmgren, J .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 2002, 107 (C21)
[44]   RELATIONSHIP BETWEEN SEA ICE FREEBOARD AND DRAFT IN THE ARCTIC BASIN, AND IMPLICATIONS FOR ICE THICKNESS MONITORING [J].
WADHAMS, P ;
TUCKER, WB ;
KRABILL, WB ;
SWIFT, RN ;
COMISO, JC ;
DAVIS, NR .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 1992, 97 (C12) :20325-20334
[45]  
Warren SG, 1999, J CLIMATE, V12, P1814, DOI 10.1175/1520-0442(1999)012<1814:SDOASI>2.0.CO
[46]  
2
[47]  
Weeks W.F., 1958, Arctic, V11, P92
[48]  
Weller G., 1972, AIDJEX Bull, V14, P28
[49]  
WENTZ F, 2004, AMSR E AQUA DAILY L3
[50]  
Wentz F., 2000, REMOTE SENS SYST