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Spatial variability and temporal stability of actual evapotranspiration on a hillslope of the Chinese Loess Plateau

ZHANG Yongkun HUANG Mingbin

干旱区科学2021,Vol.13Issue(2):189-204,16.
干旱区科学2021,Vol.13Issue(2):189-204,16.DOI:10.1007/s40333-021-0093-1

Spatial variability and temporal stability of actual evapotranspiration on a hillslope of the Chinese Loess Plateau

Spatial variability and temporal stability of actual evapotranspiration on a hillslope of the Chinese Loess Plateau

ZHANG Yongkun 1HUANG Mingbin2

作者信息

  • 1. State Key Laboratory of Plateau Ecology and Agriculture, Qinghai University, Xining 810016, China
  • 2. Institute of Soil and Water Conservation, Northwest Agriculture and Forestry University, Yangling 712100, China
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摘要

关键词

relative difference/water balance/surface runoff/soil texture/semi-arid areas

Key words

relative difference/water balance/surface runoff/soil texture/semi-arid areas

引用本文复制引用

ZHANG Yongkun,HUANG Mingbin..Spatial variability and temporal stability of actual evapotranspiration on a hillslope of the Chinese Loess Plateau[J].干旱区科学,2021,13(2):189-204,16.

基金项目

This research was financially supported by the Programme of Introducing Talents of Discipline to Universities of China (D18013), the independent subject of State Key Laboratory of Plateau Ecology and Agriculture, Qinghai University, China (2019-ZZ-05), the Project of Qinghai Science & Technology Department (2019-ZJ-Y01), the Natural Science Foundation of Qinghai Province, China (2020-ZJ-967Q), the Thousand High Innovative Talents Program of Qinghai Province (2019), and the Program for Changjiang Scholars and Innovative Research Team in University, Ministry of Education, China (IRT_17R62). The authors would also like to thank the staff of Shenmu Erosion and Environment Station of the Institute of Soil and Water Conservation, Chinese Academy of Sciences. (D18013)

干旱区科学

OACSCDCSTPCDSCI

1674-6767

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