基底排水系统应对格陵兰冰盖表面日益化的表面融化
T Meierbachtol1, J Harper, N Humphrey
1Department of Geosciences, the University of Montana, Missoula, MT 59812, USA. toby.meierbachtol@umontana.edu
概括
表面的融水通过影响基底水压来影响格陵兰冰盖的运动. 目前的模型可能无法完全捕捉内陆水文如何影响冰流动力学.
科学领域:
- 冰川学的冰川学
- 水文学的水文学
- 地球科学 地球科学 地球科学
背景情况:
- 到达格陵兰岛冰盖床的表面融水对于基底运动至关重要.
- 冰盖的滑动速度取决于冰/床的合,受冰下水文系统的影响.
- 现有的格陵兰基底水文模型通常基于山地冰川研究.
研究的目的:
- 为了研究格陵兰冰盖下面的基底水压和水文系统配置.
- 评估亚冰川水文系统运输融化水排放内陆能力.
- 评估山脉冰川衍生的水文模型对格陵兰冰盖的适用性.
主要方法:
- 现场观测使用23个钻孔在格陵兰冰盖床的四个站点截面.
- 数字分析,结合现实的冰盖几何.
- 分析基底水压和冰壁融化回收率.
主要成果:
- 观察到的基底水压对深冰下内陆排水管道的发展不利.
- 缓慢的冰壁回融限制了管道的生长,限制了它们管理化水排放增加的能力.
- 这些发现表明,目前的概念模型主要适用于靠近冰盖边缘的废弃区.
结论:
- 在格陵兰岛内陆深处的冰层下方的冰川系统可能无法有效地运输大量的融化水.
- 冰下管道的生长和功能受到冰盖几何和融化动态的限制.
- 考虑到格陵兰岛独特的冰盖特征,需要对格陵兰岛基底水文学的修订理解.
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