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区分黄土高原蒸散量趋势上的植被绿化和气候变化控制因素

Separating Vegetation Greening and Climate Change Controls on Evapotranspiration trend over the Loess Plateau.

作者信息

Jin Zhao, Liang Wei, Yang Yuting, Zhang Weibin, Yan Jianwu, Chen Xuejuan, Li Sha, Mo Xingguo

机构信息

School of Geography and Tourism, Shaanxi Normal University, Xi'an, 710119, China.

National Demonstration Center for Experimental Geography Education, Shaanxi Normal University, Xi'an, 710119, China.

出版信息

Sci Rep. 2017 Aug 15;7(1):8191. doi: 10.1038/s41598-017-08477-x.

Abstract

Evapotranspiration (ET) is a key ecological process connecting the soil-vegetation-atmosphere system, and its changes seriously affects the regional distribution of available water resources, especially in the arid and semiarid regions. With the Grain-for-Green project implemented in the Loess Plateau (LP) since 1999, water and heat distribution across the region have experienced great changes. Here, we investigate the changes and associated driving forces of ET in the LP from 2000 to 2012 using a remote sensing-based evapotranspiration model. Results show that annual ET significantly increased by 3.4 mm per year (p = 0.05) with large interannual fluctuations during the study period. This trend is higher than coincident increases in precipitation (2.0 mm yr), implying a possible pressure of water availability. The correlation analysis showed that vegetation change is the major controlling factor on interannual variability of annual ET with ~52.8% of pixels scattered in the strip region from the northeastern to southwestern parts of the LP. Further factorial analysis suggested that vegetation greening is the primary driver of the rises of ET over the study period relative to climate change. Our study can provide an improved understanding of the effects of vegetation and climate change on terrestrial ecosystem ET in the LP.

摘要

蒸散(ET)是连接土壤-植被-大气系统的关键生态过程,其变化严重影响可用水资源的区域分布,尤其是在干旱和半干旱地区。自1999年黄土高原实施退耕还林工程以来,该地区的水热分布发生了巨大变化。在此,我们使用基于遥感的蒸散模型研究了2000年至2012年黄土高原蒸散的变化及其相关驱动力。结果表明,在研究期间,年蒸散量显著增加,每年增加3.4毫米(p = 0.05),且年际波动较大。这一趋势高于同期降水量的增加(2.0毫米/年),这意味着可能存在水资源可用性压力。相关分析表明,植被变化是年蒸散量年际变化的主要控制因素,约52.8%的像素分布在黄土高原东北部至西南部的带状区域。进一步的因子分析表明,相对于气候变化,植被绿化是研究期间蒸散量增加的主要驱动力。我们的研究可以增进对植被和气候变化对黄土高原陆地生态系统蒸散影响的理解。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/464b/5557839/9d4c7656d4c7/41598_2017_8477_Fig1_HTML.jpg

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