南极洲周围的冰架正在融化
E Rignot1, S Jacobs, J Mouginot
1Department of Earth System Science, University of California, Irvine, CA 92697, USA. erignot@uci.edu
概括
南极冰架融化,主要是基底融化,是南极洲最大的消融过程. 小的,温暖的洞穴冰架对这种融化有着不成比例的贡献,这表明海洋的热力强迫是显著的.
科学领域:
- 冰川学的冰川学
- 海洋学 海洋学 海洋学
- 气候科学 气候科学
背景情况:
- 南极冰架在调节冰盖稳定性方面发挥着至关重要的作用.
- 了解冰架质量平衡对于预测海平面上升至关重要.
研究的目的:
- 量化南极冰架的融化速度和质量平衡.
- 为了确定冰架消融的主要驱动因素和位置.
主要方法:
- 卷流差数据 (2007-2008) 与表面积累 (1979-2010) 和稀释 (2003-2008) 记录的比较.
- 在不同类型的冰架上分析基底融化速率与分娩流量.
主要成果:
- 基本融化 (每年1325±235亿) 显著超过分娩流量 (每年1089±139亿),确定融化为主要的废弃过程.
- 大型冰架 (Ross,Filchner,Ronne) 在净融化中贡献的极小 (15%),而东南太平洋的较小,温暖的洞架 (8%的面积) 占融化水的一半.
- 六个东南极冰架的高融/面积比表明它们的接地线有强烈的,不具特征的海洋热力强迫.
结论:
- 冰架融化是南极冰层消失的主要驱动因素.
- 小,温暖的洞穴冰架是南极融化的关键贡献者.
- 未经证实的海洋热力强迫可能会影响东南极冰架.
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