在极度反射的格陵兰岛上观察到的短波云变暖效应.
Haotian Zhang1, Chuanfeng Zhao2, Jing Li1
1Department of Atmospheric and Oceanic Sciences, School of Physics, Peking University, Beijing 100871, China.
Science bulletin
|February 8, 2025
概括
在格陵兰岛上空,某些云层通过反射阳光而导致温暖,而不是冷却. 这种短波云变暖效应对冰融和极地能源预算具有重要意义.
科学领域:
- 大气科学 大气科学
- 气候科学 气候科学
- 地球科学 地球科学 地球科学
背景情况:
- 云通常通过反射太阳辐射和捕获热量来冷却地球.
- 地球的能源预算受到云层辐射效应的重大影响.
研究的目的:
- 为了研究格陵兰岛上空的短波云辐射效应.
- 为了确定云在哪些条件下会导致变暖而不是变冷.
主要方法:
- 对2013-2022年格陵兰岛卫星观测结果的分析.
- 基于表面白度和大气顶层反射率计算短波云辐射效应.
- 确定导致积极短波云辐射效应的条件.
主要成果:
- 在格陵兰岛上发现云层带来的短波变暖效应,与典型的冷却相反.
- 光学上薄薄的云层和相对于大气顶层反射率的高表面白度是关键因素.
- 观察到高达25W/m2的变暖效应,集中在冰融地区.
结论:
- 云层可以在格陵兰岛等明亮的表面上引起变暖,影响极地冰融化.
- 这些发现挑战了人们对极地云层辐射效应的传统理解.
- 需要改进的气候模型来纳入这种短波变暖现象,以准确地预测能源预算和冰川融化.
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