脱离植被和土壤-水分相互作用的蒸发转化年间的变化
Xiaowen Huang1,2, Shijing Liang2,3,4, Alan D Ziegler5
1State Key Laboratory of Soil Pollution Control and Safety, Southern University of Science and Technology, Shenzhen, China.
iScience
|July 31, 2025
概括
植被显著影响通过陆地-大气合 (LAC) 的蒸发转化 (ET) 变化. 了解这种动态对于预测气候变化和极端天气事件在变暖的世界中至关重要.
科学领域:
- 地球系统科学 地球系统科学
- 气候科学 气候科学
- 生态生态学 生态生态学
背景情况:
- 蒸发转化 (ET) 是通过陆地-大气合 (LAC) 的气候变化的一个关键驱动因素.
- 在LAC的植被,土壤水分和ET之间的相互作用尚未完全理解.
- 现有的研究往往低估了植被在ET动态中的作用.
研究的目的:
- 区分土壤水分和植被对ET年间变化的影响.
- 量化土壤水分与植被对不同气候区的ET变异性的贡献.
- 评估植被在ET中的作用对气候变化预测的影响.
主要方法:
- 使用社区地球系统模型 (CESM) 进行全球模拟.
- 分析了土壤水分,植被和ET之间的合强度.
- 来自土壤蒸发和植物透气的差异化ET变异性贡献.
主要成果:
- 在全球范围内,55.7%的土地表现出土壤水分,植被和ET之间的强烈合.
- 土壤湿度-ET合在低度的LAC地区占主导地位.
- 在干旱和高度地区,植被与外来物种的结合占主导地位,在炎热干燥的地区,透气的变化比土壤蒸发的变化更大.
结论:
- 植被在ET动态中起着关键的,往往被低估的作用.
- 目前的LAC评估可能会忽视植被的影响,这可能导致低估极端事件风险.
- 准确地描述植被对ET的影响对于可靠的气候变化建模和适应策略至关重要.
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