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温带地区的造林和地表冷却:机制与意义。

Reforestation and surface cooling in temperate zones: Mechanisms and implications.

机构信息

State Key Laboratory of Water Resources and Hydropower Engineering Science, Wuhan University, Wuhan, China.

O'Neill School of Public and Environmental Affairs, Indiana University, Bloomington, IN, USA.

出版信息

Glob Chang Biol. 2020 Jun;26(6):3384-3401. doi: 10.1111/gcb.15069. Epub 2020 Apr 6.

Abstract

Land-use/cover change (LUCC) is an important driver of environmental change, occurring at the same time as, and often interacting with, global climate change. Reforestation and deforestation have been critical aspects of LUCC over the past two centuries and are widely studied for their potential to perturb the global carbon cycle. More recently, there has been keen interest in understanding the extent to which reforestation affects terrestrial energy cycling and thus surface temperature directly by altering surface physical properties (e.g., albedo and emissivity) and land-atmosphere energy exchange. The impacts of reforestation on land surface temperature and their mechanisms are relatively well understood in tropical and boreal climates, but the effects of reforestation on warming and/or cooling in temperate zones are less certain. This study is designed to elucidate the biophysical mechanisms that link land cover and surface temperature in temperate ecosystems. To achieve this goal, we used data from six paired eddy-covariance towers over co-located forests and grasslands in the temperate eastern United States, where radiation components, latent and sensible heat fluxes, and meteorological conditions were measured. The results show that, at the annual time scale, the surface of the forests is 1-2°C cooler than grasslands, indicating a substantial cooling effect of reforestation. The enhanced latent and sensible heat fluxes of forests have an average cooling effect of -2.5°C, which offsets the net warming effect (+1.5°C) of albedo warming (+2.3°C) and emissivity cooling effect (-0.8°C) associated with surface properties. Additional daytime cooling over forests is driven by local feedbacks to incoming radiation. We further show that the forest cooling effect is most pronounced when land surface temperature is higher, often exceeding -5°C. Our results contribute important observational evidence that reforestation in the temperate zone offers opportunities for local climate mitigation and adaptation.

摘要

土地利用/覆被变化(LUCC)是环境变化的重要驱动因素,它与全球气候变化同时发生,并且经常相互作用。在过去的两个世纪中,造林和毁林一直是 LUCC 的关键方面,并且由于其对全球碳循环的潜在影响而得到广泛研究。最近,人们越来越感兴趣地了解造林在多大程度上通过改变地表物理特性(例如反照率和发射率)和陆地-大气能量交换,直接影响陆地能量循环并因此直接影响地表温度。造林对地表温度及其机制的影响在热带和北方气候中相对较为清楚,但造林对温带地区变暖或降温的影响则不太确定。本研究旨在阐明将陆地覆盖与温带生态系统地表温度联系起来的生物物理机制。为了实现这一目标,我们使用了来自美国东部温带地区六个对林地和草地进行配对的涡动协方差塔的数据,其中测量了辐射分量、潜热和感热通量以及气象条件。结果表明,在年时间尺度上,森林表面比草地低 1-2°C,表明造林具有明显的降温作用。森林增强的潜热和感热通量具有平均降温效应-2.5°C,这抵消了与地表特性相关的反照率变暖(+2.3°C)和发射率冷却效应(-0.8°C)的净变暖效应(+1.5°C)。森林额外的日间降温是由入射辐射的局部反馈驱动的。我们进一步表明,当地表温度较高时,森林的降温效果最为明显,通常超过-5°C。我们的研究结果提供了重要的观测证据,表明温带地区的造林为当地气候缓解和适应提供了机会。

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