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2001-2013 年中国土地利用/土地覆被变化和气候对蒸散的响应。

Response of evapotranspiration to changes in land use and land cover and climate in China during 2001-2013.

机构信息

Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters, Key Laboratory of Meteorological Disaster, Ministry of Education, 210044 Nanjing, China; WMO-NUIST Global Research Institute of Applied Meteorology, Jiangsu Key Laboratory of Agricultural Meteorology, College of Applied Meteorology, Nanjing University of Information Science and Technology, 210044 Nanjing, China.

Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters, Key Laboratory of Meteorological Disaster, Ministry of Education, 210044 Nanjing, China; WMO-NUIST Global Research Institute of Applied Meteorology, Jiangsu Key Laboratory of Agricultural Meteorology, College of Applied Meteorology, Nanjing University of Information Science and Technology, 210044 Nanjing, China.

出版信息

Sci Total Environ. 2017 Oct 15;596-597:256-265. doi: 10.1016/j.scitotenv.2017.04.080. Epub 2017 Apr 21.

Abstract

Land surface evapotranspiration (ET) is a central component of the Earth's global energy balance and water cycle. Understanding ET is important in quantifying the impacts of human influences on the hydrological cycle and thus helps improving water use efficiency and strengthening water use planning and watershed management. China has experienced tremendous land use and land cover changes (LUCC) as a result of urbanization and ecological restoration under a broad background of climate change. This study used MODIS data products to analyze how LUCC and climate change affected ET in China in the period 2001-2013. We examined the separate contribution to the estimated ET changes by combining LUCC and climate data. Results showed that the average annual ET in China decreased at a rate of -0.6mm/yr from 2001 to 2013. Areas in which ET decreased significantly were mainly distributed in the northwest China, the central of southwest China, and most regions of south central and east China. The trends of four climatic factors including air temperature, wind speed, sunshine duration, and relative humidity were determined, while the contributions of these four factors to ET were quantified by combining the ET and climate datasets. Among the four climatic factors, sunshine duration and wind speed had the greatest influence on ET. LUCC data from 2001 to 2013 showed that forests, grasslands and croplands in China mutually replaced each other. The reduction of forests had much greater effects on ET than change by other land cover types. Finally, through quantitative separation of the distinct effects of climate change and LUCC on ET, we conclude that climate change was the more significant than LULC change in influencing ET in China during the period 2001-2013. Effective water resource management and vegetation-based ecological restoration efforts in China must consider the effects of climate change on ET and water availability.

摘要

陆地表面蒸散(ET)是地球全球能量平衡和水循环的核心组成部分。了解 ET 对于量化人类活动对水文循环的影响非常重要,这有助于提高用水效率,加强用水规划和流域管理。

在中国,城市化和生态恢复在气候变化的广泛背景下,经历了巨大的土地利用和土地覆盖变化(LUCC)。本研究利用 MODIS 数据产品分析了 2001-2013 年期间 LUCC 和气候变化如何影响中国的 ET。我们通过结合 LUCC 和气候数据来检验估计的 ET 变化的单独贡献。结果表明,2001 年至 2013 年期间,中国的年平均 ET 以-0.6mm/yr 的速度减少。ET 显著减少的地区主要分布在中国西北部、中国西南部中部和中国中南部和东部的大部分地区。确定了四个气候因素(包括空气温度、风速、日照时间和相对湿度)的趋势,同时通过结合 ET 和气候数据集,量化了这四个因素对 ET 的贡献。在这四个气候因素中,日照时间和风速对 ET 的影响最大。2001 年至 2013 年的 LUCC 数据显示,中国的森林、草地和耕地相互替代。森林减少对 ET 的影响比其他土地覆盖类型的变化更大。最后,通过对气候变化和 LUCC 对 ET 的明显影响进行定量分离,我们得出结论,在 2001-2013 年期间,气候变化对中国 ET 的影响大于 LULC 变化的影响。中国有效的水资源管理和基于植被的生态恢复工作必须考虑气候变化对 ET 和水可用性的影响。

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