Impacts of Deforestation and Climate Variability on Terrestrial Evapotranspiration in Subarctic China

Although deforestation affects hydrological and climatic variables over tropical regions, its actual contributions to changes in evapotranspiration (ET) over subarctic China remain unknown. To establish a quantitative relationship between deforestation and terrestrial ET variations, we estimated ET...

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Bibliographic Details
Published in:Forests
Main Authors: Yao, Yunjun, Liang, Shunlin, Cheng, Jie, Lin, Yi, Jia, Kun, Liu, Meng
Other Authors: Yao, YJ (reprint author), Beijing Normal Univ, State Key Lab Remote Sensing Sci, Coll Global Change & Earth Syst Sci, 19 Xinjiekou St, Beijing 100875, Peoples R China., Beijing Normal Univ, State Key Lab Remote Sensing Sci, Coll Global Change & Earth Syst Sci, Beijing 100875, Peoples R China., Univ Maryland, Dept Geog Sci, College Pk, MD 20742 USA., Peking Univ, Inst Remote Sensing & GIS, Beijing 100871, Peoples R China., Beijing Normal Univ, State Key Lab Remote Sensing Sci, Coll Global Change & Earth Syst Sci, 19 Xinjiekou St, Beijing 100875, Peoples R China.
Format: Journal/Newspaper
Language:English
Published: forests 2014
Subjects:
Online Access:https://hdl.handle.net/20.500.11897/388049
https://doi.org/10.3390/f5102542
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Summary:Although deforestation affects hydrological and climatic variables over tropical regions, its actual contributions to changes in evapotranspiration (ET) over subarctic China remain unknown. To establish a quantitative relationship between deforestation and terrestrial ET variations, we estimated ET using a semi-empirical Penman (SEMI-PM) algorithm driven by meteorological and satellite data at both local and regional scales. The results indicate that the estimated ET can be used to analyse the observed inter-annual variations. There is a statistically significant positive relationship between local-scale forest cover changes (F) and annual ET variations (ET) of the following form: ET = 0.0377F - 2.11 (R-2 = 0.43, p < 0.05). This relationship may be due to deforestation-induced increases in surface albedo and a reduction in the fractional vegetation cover (FVC). However, the El Nino/Southern Oscillation (ENSO), rather than deforestation, dominates the multi-decadal ET variability due to regional-scale wind speed changes, but the exact effects of deforestation and ENSO on ET are challenging to quantify. http://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcApp=PARTNER_APP&SrcAuth=LinksAMR&KeyUT=WOS:000344352900008&DestLinkType=FullRecord&DestApp=ALL_WOS&UsrCustomerID=8e1609b174ce4e31116a60747a720701 Forestry SCI(E) EI 0 ARTICLE yaoyunjun@bnu.edu.cn; sliang@umd.edu; brucechan2003@126.com; yi.lin@pku.edu.cn; jiakun@bnu.edu.cn; xinyin_liumeng@163.com 10 2542-2560 5