环境科学
降水
泰加语
气候变化
北方的
气候学
生态系统
热带气候
农业
大气科学
气候模式
森林生态学
热带
潜热
水循环
全球变暖
热带森林
作者
Xintao Li,Taixia WU,Ke Xia,Hongzhao Tang,Xuege Wang,S. Wang,Vincent Lyne,Ying Zu
出处
期刊:Science Advances
[American Association for the Advancement of Science (AAAS)]
日期:2026-01-07
卷期号:12 (2): eadv7998-eadv7998
标识
DOI:10.1126/sciadv.adv7998
摘要
Global forest loss increases the risk of meteorological drought by altering surface energy balances. While local impacts on temperature and precipitation are known, the extent and underlying mechanisms of its influence on meteorological drought remain unclear. Here, we analyzed 3696 paired forest loss and intact sites across boreal, temperate, and tropical zones. Forest loss intensified meteorological drought in more than 52% of affected regions. Drought prevalence in boreal zones rose by 5% over 20 years—three times greater than in tropical zones—because of reduced latent heat flux and increased surface albedo, which together suppressed convective rainfall. In contrast, tropical forests demonstrated greater ecological resilience, mitigating ~40% of meteorological drought intensification. Notably, forest loss–induced meteorological drought may further evolve into more severe agricultural and hydrological droughts. Therefore, we recommend implementing strategies tailored for each climate zone, including native forest conservation, proactive ecological restoration, and connectivity enhancement, to effectively reduce drought risk.
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