南极东部冰盖的降雪驱动增长缓解了近期海平面上升的趋势
Curt H Davis1, Yonghong Li, Joseph R McConnell
1Department of Electrical and Computer Engineering, University of Missouri-Columbia, Columbia, MO 65211, USA. davisch@missouri.edu
概括
东南极冰盖在1992年至2003年期间由于降水量增加而增加了大量,这有助于减缓全球海平面上升.
科学领域:
- 冰川学的冰川学
- 气候科学 气候科学
- 遥感 遥感 遥感 遥感
背景情况:
- 南极冰盖质量平衡对于了解全球海平面变化至关重要.
- 之前的研究已经产生了对南极冰块质量趋势的不同估计.
研究的目的:
- 量化东南极冰盖内部的质量变化.
- 为了研究观察到的质量变化的驱动因素.
- 评估这些变化对全球海平面的影响.
主要方法:
- 卫星雷达高度测量数据从1992年到2003年.
- 与气象模型的降雪估计数据进行比较.
主要成果:
- 东南极冰盖内部 (81.6°S以北) 每年增加45±70亿冰.
- 这种质量增加与降水量增加有关.
- 观测到的质量增加有可能使全球海平面上升减少0.12 ± 0.02毫米/年.
结论:
- 南极东部的冰盖内部一直在积累质量.
- 增加的降雪是这种质量增加的主要驱动因素.
- 这种冰块的积累部分抵消了全球海平面上升.
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