冬季云层不透明度的增加增加了北极长期天文台的表面长波辐射.
Leah Bertrand1,2, Jennifer E Kay3,4, Gijs de Boer5
1Department of Atmospheric and Oceanic Sciences, University of Colorado, Boulder, Boulder, CO, USA. leah.bertrand@colorado.edu.
Nature communications
|November 2, 2025
概括
北极的变暖正在增加冬季的表面辐射,这是由云层辐射效应的上升驱动的,云层不透明度更大. 这种北极云反放大了变暖,正如从阿拉斯加观察到的.
科学领域:
- * 大气科学 大气科学
- * 北极的气候动力学
- * 云物理 云物理
背景情况:
- *北极放大导致冬季云的特性发生显著变化.
- * 北极云反机制的不确定性阻碍了气候预测.
- *观察北极低云是很有挑战性的,特别是在太空.
研究的目的:
- * 限制和解释北极冬季长波 (LW) 辐射流变化.
- * 调查云辐射效应 (CRE) 在表面变暖中的作用.
- * 确定增加云层不透明性的驱动因素.
主要方法:
- *利用了阿拉斯加北坡的二十年 (1998-2023) 的地面观测.
- *分析了长波流量变化及其与温度,温室气体和云的相关性.
- * 量化了云辐射效应对表面能量平衡的贡献.
主要成果:
- * 观察到长波向下辐射流量在表面显著增加.
- * 发现仅仅温度和温室气体无法解释观察到的流量增加.
- * 证明,增加云辐射效应 (0.96 ± 0.64 W/m2/K) 是必要的,以解释升温趋势,由冰单体云和混合相云的增强云不透明度驱动.
结论:
- * 增加云的不透明度是北极冬季扩大表面变暖的关键驱动因素.
- * 基于表面的观测为了解北极云的反提供了关键的限制.
- *这些发现表明,积极的云反循环有助于北极放大.
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