Li Yan, Zhao Maosheng, Motesharrei Safa, Mu Qiaozhen, Kalnay Eugenia, Li Shuangcheng
College of Urban and Environmental Sciences, Peking University, Beijing 100871, China.
Department of Atmospheric and Oceanic Science, University of Maryland, College Park, Maryland 20742, USA.
Nat Commun. 2015 Mar 31;6:6603. doi: 10.1038/ncomms7603.
The biophysical effects of forests on climate have been extensively studied with climate models. However, models cannot accurately reproduce local climate effects due to their coarse spatial resolution and uncertainties, and field observations are valuable but often insufficient due to their limited coverage. Here we present new evidence acquired from global satellite data to analyse the biophysical effects of forests on local climate. Results show that tropical forests have a strong cooling effect throughout the year; temperate forests show moderate cooling in summer and moderate warming in winter with net cooling annually; and boreal forests have strong warming in winter and moderate cooling in summer with net warming annually. The spatiotemporal cooling or warming effects are mainly driven by the two competing biophysical effects, evapotranspiration and albedo, which in turn are strongly influenced by rainfall and snow. Implications of our satellite-based study could be useful for informing local forestry policies.
森林对气候的生物物理效应已通过气候模型进行了广泛研究。然而,由于其空间分辨率粗糙和存在不确定性,模型无法准确再现局部气候效应,而实地观测虽有价值,但由于覆盖范围有限往往也不充分。在此,我们展示了从全球卫星数据中获取的新证据,以分析森林对局部气候的生物物理效应。结果表明,热带森林全年都有很强的降温作用;温带森林夏季有适度降温,冬季有适度升温,全年净降温;而北方森林冬季有强烈升温,夏季有适度降温,全年净升温。时空上的降温或升温效应主要由蒸散和反照率这两种相互竞争的生物物理效应驱动,而这两种效应又反过来受到降雨和降雪的强烈影响。我们基于卫星的研究结果可能有助于为地方林业政策提供参考。