Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1016/j.gloplacha.2013.06.008 |
Response of evapotranspiration and water availability to changing climate and land cover on the Mongolian Plateau during the 21st century | |
Liu, Yaling1; Zhuang, Qianlai1,2; Chen, Min1; Pan, Zhihua3,4; Tchebakova, Nadja5; Sokolov, Andrei6; Kicklighter, David7; Melillo, Jerry7; Sirin, Andrey8; Zhou, Guangsheng9; He, Yujie1; Chen, Jiquan10; Bowling, Laura2; Miralles, Diego G.11; Parfenova, Elena5 | |
通讯作者 | Liu, Yaling |
来源期刊 | GLOBAL AND PLANETARY CHANGE
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ISSN | 0921-8181 |
EISSN | 1872-6364 |
出版年 | 2013 |
卷号 | 108页码:85-99 |
英文摘要 | Adequate quantification of evapotranspiration (ET) is crucial to assess how climate change and land cover change (LCC) interact with the hydrological cycle of terrestrial ecosystems. The Mongolian Plateau plays a unique role in the global climate system due to its ecological vulnerability, high sensitivity to climate change and disturbances, and limited water resources. Here, we used a version of the Terrestrial Ecosystem Model that has been modified to use Penman-Monteith (PM) based algorithms to calculate ET. Comparison of site-level ET estimates from the modified model with ET measured at eddy covariance (EC) sites showed better agreement than ET estimates from the MODIS ET product, which overestimates ET during the winter months. The modified model was then used to simulate ET during the 21st century under six climate change scenarios by excluding/including climate-induced LCC. We found that regional annual ET varies from 188 to 286 mm yr(-1) across all scenarios, and that it increases between 0.11 mm yr(-2) and 0.55 mm yr(-2) during the 21st century. A spatial gradient of ET that increases from the southwest to the northeast is consistent in all scenarios. Regional ET in grasslands, boreal forests and semi-desert/deserts ranges from 242 to 374 mm yr(-1), 213 to 278 mm yr(-1) and 100 to 199 mm yr(-1), respectively; and the degree of the ET increase follows the order of grassland, semi-desert/desert, and boreal forest. Across the plateau, climate-induced LCC does not lead to a substantial change (<5%) in ET relative to a static land cover, suggesting that climate change is more important than LCC in determining regional ET. Furthermore, the differences between precipitation and ET suggest that the available water for human use (water availability) on the plateau will not change significantly during the 21st century. However, more water is available and less area is threatened by water shortage in the Business-As-Usual emission scenarios relative to level-one stabilization emission scenarios. (C) 2013 Elsevier B.V. All rights reserved. |
英文关键词 | Evapotranspiration Mongolian Plateau Terrestrial Ecosystem Model MODIS Climate change Land cover change |
类型 | Article |
语种 | 英语 |
国家 | USA ; Peoples R China ; Russia ; England |
收录类别 | SCI-E |
WOS记录号 | WOS:000323470800007 |
WOS关键词 | LEAF-AREA INDEX ; REFLECTANCE DISTRIBUTION FUNCTION ; FARMING-PASTORAL ECOTONE ; NET PRIMARY PRODUCTIVITY ; SPACE-TIME CLIMATE ; INNER-MONGOLIA ; TERRESTRIAL ECOSYSTEMS ; STOMATAL CONDUCTANCE ; SURFACE CONDUCTANCE ; FLUX MEASUREMENTS |
WOS类目 | Geography, Physical ; Geosciences, Multidisciplinary |
WOS研究方向 | Physical Geography ; Geology |
来源机构 | 中国农业大学 ; 中国科学院植物研究所 |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/177425 |
作者单位 | 1.Purdue Univ, Dept Earth Atmospher & Planetary Sci, W Lafayette, IN 47907 USA; 2.Purdue Univ, Dept Agron, W Lafayette, IN 47907 USA; 3.China Agr Univ, Coll Resources & Environm Sci, Beijing 100193, Peoples R China; 4.Minist Agr, Key Ecol & Environm Expt Stn Field Sci Observat H, Inner Mongolia 011705, Peoples R China; 5.Russian Acad Sci, VN Sukachev Inst Forest, Siberian Branch, Krasnoyarsk 660036, Russia; 6.MIT, Dept Earth Atmospher & Planetary Sci, Cambridge, MA 02139 USA; 7.Marine Biol Lab, Ctr Ecosyst, Woods Hole, MA 02543 USA; 8.Russian Acad Sci, Inst Forest Sci, Lab Peatland Forestry & Ameliorat, Uspenskoye 143030, Moscow Oblast, Russia; 9.Chinese Acad Sci, State Key Lab Vegetat & Environm Change, Inst Bot, Beijing 100093, Peoples R China; 10.Univ Toledo, Dept Environm Sci, Toledo, OH 43606 USA; 11.Univ Bristol, Sch Geog Sci, Bristol, Avon, England |
推荐引用方式 GB/T 7714 | Liu, Yaling,Zhuang, Qianlai,Chen, Min,et al. Response of evapotranspiration and water availability to changing climate and land cover on the Mongolian Plateau during the 21st century[J]. 中国农业大学, 中国科学院植物研究所,2013,108:85-99. |
APA | Liu, Yaling.,Zhuang, Qianlai.,Chen, Min.,Pan, Zhihua.,Tchebakova, Nadja.,...&Parfenova, Elena.(2013).Response of evapotranspiration and water availability to changing climate and land cover on the Mongolian Plateau during the 21st century.GLOBAL AND PLANETARY CHANGE,108,85-99. |
MLA | Liu, Yaling,et al."Response of evapotranspiration and water availability to changing climate and land cover on the Mongolian Plateau during the 21st century".GLOBAL AND PLANETARY CHANGE 108(2013):85-99. |
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