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基于 MODIS 数据的全球干旱对生态系统水分利用效率响应的研究

A global examination of the response of ecosystem water-use efficiency to drought based on MODIS data.

机构信息

State Key Laboratory of Earth Surface Processes and Resource Ecology, College of Global Change and Earth System Science, Beijing Normal University, Beijing 100875, China.

State Key Laboratory of Earth Surface Processes and Resource Ecology, College of Global Change and Earth System Science, Beijing Normal University, Beijing 100875, China.

出版信息

Sci Total Environ. 2017 Dec 1;601-602:1097-1107. doi: 10.1016/j.scitotenv.2017.05.084. Epub 2017 Jun 9.

Abstract

Ecosystem water-use efficiency (WUE) plays an important role in carbon and water cycles. Currently, the response of WUE to drought disturbance remains controversial. Based on the global ecosystem gross primary productivity (GPP) product and the evapotranspiration product (ET), both of which were retrieved from the moderate resolution imaging spectroradiometer (MODIS), as well as the drought index, this study comprehensively examined the relationship between ecosystem WUE (WUE=GPP/ET) and drought at the global scale. The response of WUE to drought showed large differences in various regions and biomes. WUE for arid ecosystems typically showed a negative response to drought, whereas WUE for humid ecosystems showed both positive and negative response to drought. Legacy effects of drought on ecosystem WUE were observed. Furthermore, ecosystems showed a sensitive response to abrupt changes in hydrological climatic conditions. The transition from wet to dry years should increase ecosystem WUE, and the opposite change in WUE should occur when an ecosystem experiences a transition from dry to wet years. This indicates the resilience of ecosystems to drought disturbance. Knowledge from this study should provide an in-depth understanding of ecosystem strategies for coping with drought.

摘要

生态系统水分利用效率(WUE)在碳和水循环中起着重要作用。目前,WUE 对干旱干扰的响应仍存在争议。本研究基于全球生态系统总初级生产力(GPP)产品和蒸散产品(ET),以及干旱指数,综合考察了全球尺度上生态系统 WUE(WUE=GPP/ET)与干旱的关系。WUE 对干旱的响应在不同地区和生物群落中存在较大差异。干旱生态系统的 WUE 通常对干旱呈负响应,而湿润生态系统的 WUE 对干旱则呈正、负响应。干旱对生态系统 WUE 的滞后效应也被观察到。此外,生态系统对水文气候条件的突然变化表现出敏感响应。从湿润到干旱年份的转变应会增加生态系统的 WUE,而当生态系统经历从干旱到湿润年份的转变时,WUE 则会发生相反的变化。这表明生态系统对干旱干扰具有恢复力。本研究的知识应提供对生态系统应对干旱策略的深入了解。

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