自20世纪80年代以来,日下不对称的变暖加剧了大气干燥程度
Ziqian Zhong1, Hans W Chen2, Aiguo Dai3
1Department of Space, Earth and Environment, Division of Geoscience and Remote Sensing, Chalmers University of Technology, SE-412 96, Gothenburg, Sweden.
Nature communications
|September 9, 2025
概括
白天更快的变暖 (最大温度) 会加剧大气干燥 (蒸汽压力缺陷,VPD). 这种不对称的变暖放大了全球变暖.
科学领域:
- 气候科学 气候科学
- 大气科学 大气科学
- 环境科学 环境科学
背景情况:
- 大气蒸汽压力赤字 (VPD) 的上升,这是一个干燥度的度量,与近地表空气温度的增加有关.
- 每日最高 (Tmax) 和最低 (Tmin) 温度之间的差异变暖对其对VPD增加的贡献尚未得到充分评估.
研究的目的:
- 调查Tmax相对于Tmin的更快增加是否导致VPD升高.
- 量化日下不对称变暖对全球陆地VPD加剧的影响.
主要方法:
- 对1980年至2023年的再分析数据进行分析,以评估Tmax,Tmin和VPD的趋势.
- 利用次日站观测来证实重新分析数据的发现.
- 量化不对称变暖对VPD加剧的贡献.
主要成果:
- 与Tmin相比,Tmax在陆上上升的速度较快,从1980年到2023年加剧了VPD.
- 日下不对称的变暖对全球陆地VPD的增加贡献了约18%.
- 站点观测表明,不对称的变暖约占VPD加剧的30%.
结论:
- 日下不对称的变暖显著放大了全球变暖对大气干燥的影响.
- 这些发现强调了温度不对称在推动陆地水资源和碳循环变化的关键作用.
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