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冰盖. 冰盖. 在冰盖. 南极冰架的体积损失正在加速
Fernando S Paolo1, Helen A Fricker2, Laurie Padman3
1Scripps Institution of Oceanography, University of California, San Diego, CA, USA. fpaolo@ucsd.edu.
概括
南极冰架正在快速减小,加快了冰流向海洋的速度. 卫星数据显示,海平面显著变薄,特别是在西南极洲,威胁到未来的海平面上升.
科学领域:
- 冰川学和气候科学 冰川学和气候科学
- 地球观测和远程传感
背景情况:
- 浮动的冰架起到了关键的支柱作用,减缓了地面冰流入海洋的速度.
- 冰架薄化减少了这种支作用,导致冰排放增加和海平面潜在上升.
研究的目的:
- 为了量化南极冰架厚度和体积的十年级变化.
- 评估18年间冰层消失的加快速度及其区域差异.
主要方法:
- 利用了 18 年的连续卫星雷达高度计观测.
- 计算了南极大陆冰架厚度的十年级变化.
主要成果:
- 平均冰架体积损失的速度显著加速,从25 ± 64公里3/年 (1994-2003) 增加到310 ± 74公里3/年 (2003-2012).
- 在过去的十年中,西南极冰架的损失增加了大约70%.
- 南极东部冰架从体积增长过渡到损失;阿蒙森和贝林斯豪森地区的一些冰架损失高达18%的厚度.
结论:
- 南极冰架正在经历加速的体积损失,这表明支效应正在减弱.
- 观察到的变化,特别是在西南极洲,意味着一个具有潜在全球海平面影响的关键转变.
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