Trends in seasonal sea ice duration in southwestern Hudson Bay

被引：0
|
作者：
Gough, WA
Cornwell, AR
Tsuji, LJS
机构：
[1] Univ Toronto, Dept Phys & Environm Sci, Toronto, ON M1C 1A4, Canada
[2] Univ Toronto, Dept Geog, Toronto, ON M5S 3G3, Canada
[3] Univ Waterloo, Dept Environm & Resource Studies, Waterloo, ON N2L 3G1, Canada
来源：
ARCTIC | 2004年 / 57卷 / 03期
关键词：
Hudson Bay; sea ice; breakup; climate change;
D O I：
暂无
中图分类号：
X [环境科学、安全科学];
学科分类号：
08 ; 0830 ;
摘要：
The southwestern region of Hudson Bay is one of the last areas in the Hudson and James Bay lowlands region to become free of sea ice in the spring. This late breakup is due to the effects of winds and currents. By analyzing time series with three different statistical techniques, we found a statistically significant increase in the length of the ice-free season in this region from 1971 to 2003. Much of this increase was attributed to earlier breakup of the ice, which is consistent with increased spring temperatures in this region. The onset of breakup advanced by at least three days per decade over the study period.
引用
收藏
页码：299 / 305
页数：7
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