越来越多的裂越来越快地穿越格陵兰冰盖边缘
Thomas R Chudley1,2, Ian M Howat2,3, Michalea D King4
1Department of Geography, Durham University, Durham, UK.
概括
在2016年至2021年期间,格陵兰冰盖的表面裂在某些地区显著增加,这与加速的冰流有关. 这一发现对于理解冰盖质量损失及其影响至关重要.
科学领域:
- 冰川学的冰川学
- 气候科学 气候科学
- 地球观测 地球观测
背景情况:
- 表面裂是格陵兰冰盖质量损失的主要未知因素.
- 现有的数据缺乏关于裂位置和演变的全面观察.
研究的目的:
- 测量2016年至2021年间格陵兰冰盖中裂体积的变化.
- 了解冰流动力学与裂发展之间的关系.
主要方法:
- 利用高分辨率的数字海拔模型 (DEMs) 来绘制裂领域的地图.
- 分析了2016年和2021年的3D裂体积.
- 与冰排放数据相关的裂体积变化.
主要成果:
- 在加速流动的海洋终端部门观察到裂体积的显著增加 (例如,东南地区的+25.3%).
- 在中西部部门 (-14.2%) 发现了裂体积的减少,特别是在雅各布沙文·伊斯布雷.
- 整个冰盖的裂体积变化在测量误差范围内 (+4.3%).
结论:
- 格陵兰岛的冰流加速在五年内引发了大量的裂增加.
- 裂纹进化为10年以下的质量损失反提供了一个机制.
- 这些发现有助于更好地理解分娩,冰流和基底水转移.
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