相关实验视频
Updated: Jul 24, 2026

Measuring the Densities of Aqueous Glasses at Cryogenic Temperatures
Published on: June 28, 2017
格陵兰冰盖在高海拔地区的质量平衡
1EG&G Services, Wallops Flight Facility, Building N-159, Wallops Island, VA 23337, USA. Jet Propulsion Laboratory, M/S 300-325, 4800 Oak Grove Drive, Pasadena, CA 91109, USA. Byrd Polar Research Center, Ohio State University, Columbus, OH 42310, USA. ESSIC, University of Maryland, College Park, MD 20742, USA. Radar Systems and Remote Sensing Laboratory, University of Kansas, Lawrence, KS 66045, USA.
格陵兰冰盖显示了近几十年来冰厚变化的区域差异. 虽然一些地区正在变厚,但其他地区,特别是东南地区,正在显著变薄.
科学领域:
- 冰川学的冰川学
- 气候科学 气候科学
- 地球系统科学 地球系统科学
背景情况:
- 格陵兰冰盖的质量平衡对于了解全球海平面上升至关重要.
- 以前对冰厚化和薄化速率的估计显示出区域差异.
研究的目的:
- 为了比较整个格陵兰冰盖的冰排放与积雪积累.
- 为了估计近几十年来冰的加厚和稀释速度.
主要方法:
- 将高海拔地区的冰排放与总积雪量进行比较.
- 使用来自重复的高度计调查的数据.
主要成果:
- 格陵兰岛的冰盖平均处于平衡状态.
- 存在显著的区域差异:西南地区每年变厚21厘米,东南地区每年变薄30厘米.
- 北方的变化较小:每年变厚2厘米 (东北),每年变薄5厘米 (西北).
- 与高度计调查数据相比,在极南地区发现了差异.
结论:
- 格陵兰冰盖在其质量平衡中表现出复杂的区域动态.
- 格陵兰东南部正在经历大量的冰层流失,导致海平面上升的担忧.
- 高度计数据可能需要在特定的极端南部地区进行细化.
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