直接观察格陵兰冰盖下方正在演变的冰下排水
Lauren C Andrews1, Ginny A Catania1, Matthew J Hoffman2
11] Institute for Geophysics, Jackson School of Geosciences, The University of Texas at Austin, Austin, Texas 78758, USA [2] Department of Geological Sciences, Jackson School of Geosciences, The University of Texas at Austin, Austin, Texas 78712, USA.
Nature
|October 4, 2014
概括
季节性冰盖的加速取决于融水通过摩林到达床. 冰下水压的变化,特别是在没有通道的地区,会影响冰的速度,影响格陵兰岛.
科学领域:
- 冰川学的冰川学
- 水文学的水文学
- 气候科学 气候科学
背景情况:
- 格陵兰冰盖的季节性加速是由冰下水文学驱动的.
- 通过磨坊将融化水输送到床上,影响了冰的动态.
- 有限的亚冰川水压数据阻碍了对水文系统演变的理解.
研究的目的:
- 研究冰下水压与冰的速度之间的关系.
- 了解亚冰川水文系统的时空演变.
- 确定控制季末冰速变化的因素.
主要方法:
- 同时测量磨床和钻井井的液压头.
- 在格陵兰西部的Paakitsoq地区追踪冰的速度.
- 液压头和冰速之间的相关性分析.
主要成果:
- 冰的速度与滑轮液压头相关,但与钻孔数据相异.
- 磨坊连接到一个高效的,道化下冰川系统,控制白天的冰速.
- 季末降低的冰速与未道化亚冰川系统连接的变化有关.
结论:
- 摩林连接的通道主要控制短期的冰速波动.
- 季末的冰速下降很可能是由于未经道化的亚冰川地区的连接性发生变化.
- 了解冰下压力变化对于预测冰盖动态和海平面上升至关重要.
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