减少的尘埃颗粒通过调节西藏高原上云冰的形成来放大云冷却效应
Jingchuan Chen1, Jianzhong Xu2,3, Zhijun Wu1,4
1State Key Joint Laboratory of Environmental Simulation and Pollution Control, College of Environmental Sciences and Engineering, Peking University, Beijing 100871, China.
Science advances
|September 13, 2024
概括
尘埃颗粒是西藏高原上的主要冰核粒子 (INP),影响云层形成. 减少的尘埃增强了云冷却效应,影响了这个敏感地区的气候反.
科学领域:
- 大气科学 大气科学
- 气候科学 气候科学
- 冰川学的冰川学
背景情况:
- 冰核粒子 (INPs) 对于云冰形成至关重要,影响云辐射效应 (CRE) 和区域气候.
- 西藏高原 (TP) 是一个气候敏感的地区,INP来源,度及其对CRE的影响尚不清楚.
研究的目的:
- 在TP上识别主要的INP来源.
- 调查INP对云属性和CRE的影响.
- 了解气候反机制与大气中的气溶在TP.
主要方法:
- 综合多源卫星观测的整合.
- 来自五个TP冰川的积雪样本的分析.
- 评估尘埃的十年趋势及其与INP度和CRE的相关性.
主要成果:
- 在TP上被确定为主要INP来源的尘埃颗粒.
- 春季的尘埃涌入与混合相云中的冰度增加有关.
- 一个十年的尘埃减少 (2007-2019) 导致INP下降和云冷却放大,每0.01尘埃光学深度下降1.98±0.39W/m2的表面净CRE降低1.98±0.39W/m2.
结论:
- 尘埃在TP的气溶云相互作用中发挥着关键作用.
- 尘埃的变化是气候反的重要途径.
- 研究结果强调了大气INP在了解高海拔地区气候动态方面的重要性.
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