蒸发式冷却超过了全球干旱地区绿化区域的白色诱导变暖
Mojolaoluwa T Daramola1,2,3, Renqiang Li2, Ming Xu4,5,6
1Irish Climate Analysis and Research Units (ICARUS), Department of Geography, Maynooth University, Maynooth, Ireland.
Scientific reports
|February 14, 2026
概括
全球干旱地的绿化显著影响气候温度. 由土壤水分驱动的蒸发转化是主导因素,日间温度的降温超过了白色变化.
科学领域:
- 气候科学 气候科学
- 生态生态学 生态生态学
- 遥感 遥感 遥感 遥感
背景情况:
- 绿化影响了地表-大气的能量交换和气候反.
- 全球干旱地区的绿化对温度的反影响尚不清楚.
研究的目的:
- 检查二十年来全球干旱土地绿化趋势.
- 评估生物物理性质的变化及其对温度反的影响.
主要方法:
- 使用卫星和重新分析数据.
- 分析了绿化趋势和生物物理性质变化.
主要成果:
- 绿化改变了表面的白度和净短波辐射.
- 由土壤水分驱动的蒸发透气变化主导着温度反 (54-83%).
- 显著的绿化使白天的温度降低了0.530.8°C/十年;棕色增加了0.861.32°C/十年.
结论:
- 土壤水分的可用性对于干旱地区的蒸发转化温度反至关重要.
- 干旱地区的变暖和湿度可用性影响植物功能和区域气候.
- 了解这些反对于干旱地区的可持续性至关重要.
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