在东南极洲太平洋海岸的出口冰川中,气候驱动的快速变化
B W J Miles1, C R Stokes, A Vieli
1Department of Geography, Durham University, Science Site, South Road, Durham DH1 3LE, UK.
Nature
|August 30, 2013
概括
东南极冰川在终点位置上呈现出显著,同步的变化,其中大多数在1990年后出现. 这些变化表明,冰盖的某些部分可能容易受到气候强迫的影响.
科学领域:
- 冰川学的冰川学
- 气候科学 气候科学
- 南极研究南极研究
背景情况:
- 格陵兰岛和西南极洲的终结海洋的冰川正在加速海平面上升.
- 在东南极冰盖边缘观察到稀释,但终点行为在很大程度上是未知的.
- 以前的研究缺乏关于质量损失或迫使东南极冰川变化的背景.
研究的目的:
- 分析东南极冰川出口的终点位置的多十年趋势.
- 调查冰川行为的广泛和同步变化.
- 评估冰川变化与气候/海洋强迫之间的关系.
主要方法:
- 对175个结束海洋的出口冰川的终点位置趋势的分析.
- 在东南极洲5,400公里的冰盖边缘上绘制冰川变化.
- 冰川趋势与空气温度,海冰和南环形态数据的相关性.
主要成果:
- 在175个冰川中观察到广泛和同步的终点变化.
- 63%的人退出了1974-1990年; 72%的人进入了1990-2000年; 58%的人进入了2000-2010年.
- 与罗斯海冰川不同的是,太平洋海岸冰川显示出与空气温度和海冰相关的明显变化.
结论:
- 东南极冰川表现出时代性的退缩和前进模式.
- 太平洋海岸的冰川动态对气候变化非常敏感,特别是南方年轮模式.
- 南极东部冰盖的部分地区可能比以前认为的更容易受到外部强迫的影响.
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