在大气CO2升下,全球森林的生物物理冷却效益减少
Fei Kan1, Hao Xu2, Shuchang Tang1
1Institute of Carbon Neutrality, Sino-French Institute for Earth System Science, College of Urban and Environmental Sciences, Peking University, Beijing, 100871, China.
Nature communications
|May 13, 2025
概括
全球森林化可以通过降低陆地表面Ta来降低近地表空气温度 (Ta). 然而,二氧化碳 (CO2) 水平的上升会减少这种冷却效应,需要动态森林管理策略来缓解气候变化.
科学领域:
- 气候科学 气候科学
- 生态生态学 生态生态学
- 地球系统科学 地球系统科学
背景情况:
- 森林化是通过碳捕获来缓解全球变暖的一个关键战略.
- 森林植被对地表能量平衡的生物物理影响,特别是在 CO2 增加的情况下,需要进一步研究.
研究的目的:
- 为了研究全球潜在的森林植被对近地表空气温度 (Ta) 在不断增加的CO2度下的生物物理效应.
- 了解二氧化碳水平如何影响森林的降温效益.
主要方法:
- 利用陆地大气合模型与板块海洋模块.
- 在不同的CO2度下模拟了全球完全潜力森林化的生物物理效应.
主要成果:
- 在当前的气候条件下,全球森林化可以使陆地表面Ta减少0.062°C.
- 森林的降温效益随着二氧化碳水平的上升而减少.
- 非局部机制,主要是由于背景气候变化而改变的水平温度转移,主导着降温的减少.
结论:
- 森林的冷却效应是由二氧化碳水平和背景气候变化所调节的.
- 动态森林管理策略对于优化气候变化减缓潜力至关重要.
- 了解森林,二氧化碳和气候动态之间的相互作用是必不可少的.
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