三十年来,南极洲的冰川接地线正在退缩
Eric Rignot1,2,3,4, Bernd Scheuchl1, Jean Baptiste Barre4
1Department of Earth System Science, University of California, Irvine, CA 92697.
概括
南极接地线的撤退在大多数海岸都是最小的,但在西南极洲和东南极洲和半岛的部分地区显著. 这种由温暖的海洋流驱动的冰损失,突出了未来加速的脆弱区域.
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:
- 接地线 (GL) 对冰川的稳定性和质量平衡至关重要.
- 了解GL迁移是预测冰盖行为和海平面上升的关键.
研究的目的:
- 创建一个大陆规模的记录南极接地线迁移从1992年到2025年.
- 识别显著地线退缩的区域及其驱动因素.
主要方法:
- 使用了来自多个卫星任务 (ERS-1/2,Sentinel-1,RADARSAT-1/2,RCM,ALOS PALSAR-2,COSMO-SkyMed,ICEYE) 的微分合成孔径雷达干扰计.
- 组装了一个涵盖南极海岸长度的77 ± 10%的综合数据集.
主要成果:
- 在南极海岸大部分地区 (77 ± 10%) 没有发现显著的GL迁移.
- 在南极半岛,威尔克斯和乔治五世土地以及西南极洲 (特别是阿蒙森和盖茨部门) 观察到集中撤退.
- 在1996年至2025年期间,地面冰总损失为12820±1873平方公里,其中62%来自西南极洲.
结论:
- 退缩与浴度学有关,它将温暖的环极深水引导到逆行着陆区域.
- 为冰盖模型提供了基准,并确定了加速未来撤退的关键领域.
关键词:
在南极洲,南极洲是南极洲.冰川冰川是一个冰川.干涉测量干涉测量干涉测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰测量干扰远程传感是一种遥感技术.海平面的海平面是什么?更多相关视频
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