Arctic sea ice decline contributes to thinning lake ice trend in northern Alaska

被引:22
|
作者
Alexeev, Vladimir A. [1 ]
Arp, Christopher D. [2 ]
Jones, Benjamin M. [3 ]
Cai, Lei [1 ]
机构
[1] Univ Alaska Fairbanks, Int Arctic Res Ctr, 930 Koyukuk Dr, Fairbanks, AK 99775 USA
[2] Univ Alaska Fairbanks, Water & Environm Res Ctr, Fairbanks, AK 99775 USA
[3] US Geol Survey, Alaska Sci Ctr, 4210 Univ Dr, Anchorage, AK 99508 USA
来源
ENVIRONMENTAL RESEARCH LETTERS | 2016年 / 11卷 / 07期
基金
美国国家科学基金会;
关键词
Arctic; sea ice decline; winter climate; freshwater ice; thermokarst lakes; WATER AVAILABILITY; COASTAL-PLAIN; SHALLOW LAKES; THAW LAKES; REANALYSIS; THICKNESS; COVER; SLOPE; MODEL; SNOW;
D O I
10.1088/1748-9326/11/7/074022
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Field measurements, satellite observations, and models document a thinning trend in seasonal Arctic lake ice growth, causing a shift from bedfast to floating ice conditions. September sea ice concentrations in the Arctic Ocean since 1991 correlate well (r = +0.69, p < 0.001) to this lake regime shift. To understand how and to what extent sea ice affects lakes, we conducted model experiments to simulate winters with years of high (1991/92) and low (2007/08) sea ice extent for which we also had field measurements and satellite imagery characterizing lake ice conditions. A lake ice growth model forced with Weather Research and Forecasting model output produced a 7% decrease in lake ice growth when 2007/08 sea ice was imposed on 1991/92 climatology and a 9% increase in lake ice growth for the opposing experiment. Here, we clearly link early winter 'ocean-effect' snowfall and warming to reduced lake ice growth. Future reductions in sea ice extent will alter hydrological, biogeochemical, and habitat functioning of Arctic lakes and cause sub-lake permafrost thaw.
引用
收藏
页数:9
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