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格陵兰岛的夏季大气循环是对北极扩大和春季降雪覆盖减少的反应
Jonathon R Preece1, Thomas L Mote2, Judah Cohen3,4
1Department of Geography, University of Georgia, Athens, GA, USA. jonathon.preece@uga.edu.
Nature communications
|June 23, 2023
概括
北极的扩大加剧了格陵兰岛的阻塞,通过波浪较大的大气循环和降低的雪地覆盖. 这些相互关联的机制加快了格陵兰冰盖的质量损失,影响了气候动态.
科学领域:
- 大气科学 大气科学
- 气候动力学 气候动力学
- 冰川学的冰川学
背景情况:
- 北极的扩大与格陵兰冰盖质量损失的加速有关.
- 持续的极端天气被假设是对北极放大带来的动态反应.
研究的目的:
- 研究将高度变暖与格陵兰岛封锁增加联系在一起的机制.
- 探索大气循环和雪地在这种现象中的作用.
主要方法:
- 对北大西洋上空大气循环模式的分析.
- 循环变化与格陵兰岛阻塞事件的相关性.
- 评估陆地积雪覆盖范围的影响.
主要成果:
- 北大西洋夏季大气循环变得波浪化.
- 这种波浪流与更频繁的格陵兰岛封锁有关.
- 降低陆地积雪覆盖增加了变暖,并影响了罗斯比波反应.
结论:
- 两个协同作用的机制将北极变暖与格陵兰岛封锁的增加联系起来.
- 波浪较大的大气流和雪地覆盖变化的动态导致冰盖质量损失.
- 了解这些过程对于预测未来气候变化影响至关重要.
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