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在更高度地区观察到森林砍伐局部降温效应的增加
Xuhui Lee1, Michael L Goulden, David Y Hollinger
1School of Forestry and Environmental Studies, Yale University, New Haven, Connecticut 06511, USA. xuhui.lee@yale.edu
Nature
|November 19, 2011
概括
森林砍伐,特别是在中高度地区,可以通过改变生物物理过程来冷却地球表面. 这项研究观察到,与附近的森林相比,开放式土地上的表面空气温度较低,这表明土地清理的降温效应.
科学领域:
- 气候科学 气候科学
- 生态生态学 生态生态学
- 生物物理学的生物物理.
背景情况:
- 森林砍伐对全球气候的影响是有争议的,模型表明通过白色变化来降温,但当地土地利用变化可能不会引发必要的反.
- 之前的研究缺乏关于森林砍伐对大面积气候影响的直接观察证据.
研究的目的:
- 通过使用观测数据,调查森林砍伐对地表空气温度的直接影响.
- 为了确定森林砍伐的内在生物物理机制是否可以独立于大规模反改变表面温度.
主要方法:
- 在美国和加拿大的森林和附近的地表气象站 (清理土地的代理) 之间比较表面空气温度.
- 分析了不同度的温度数据,以评估森林砍伐效应的度依赖性.
主要成果:
- 在开的土地上,表面空气温度低于不同度的相邻森林.
- 在北45度以北观察到0.85±0.44K的冷却效应,在北45度以南观察到0.21±0.53K的冷却效应.
- 独立于白度的夜间温度下降,对整体冷却效应作出了显著的贡献.
结论:
- 森林砍伐对地表空气温度有明显的降温作用,特别是在中高度地区.
- 观察到的冷却与通过对流和辐射改变能量损失的理论预期一致.
- 在模型中,夜间温度变化是森林砍伐对气候影响的关键,但往往不确定的组成部分.
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