Abstract

Improving understanding of changes in intra-annual variability (IAV) of evapotranspiration (ET) and the underlying drivers is an essential step for modeling hydrological processes in response to global change. Previous studies paid special attention to climatic regulations of IAV of ET. However, ignoring the role of landscape characteristics (e.g., vegetation coverage) can introduce great uncertainty in the explanation of ET variance. In this work, the Poyang Lake Basin, which is a typical humid basin in China, was taken as the study area. It has experienced an obvious climate change and revegetation since the 1980s. Here, trends of IAV of ET and their responses to four climatic variables (i.e., air temperature, precipitation, downward shortwave radiation and wind speed) and vegetation coverage were explored from 1983 to 2014. The results show that IAV of ET exhibited contrary trends during the past decades. It significantly (p < 0.05) declined with a significant linear slope of −0.52 mm/year before 2000, and then slightly increased (slope = 0.06 mm/year, p > 0.05) over the basin, which was generally consistent with the IAV of temperature and radiation. The proposed variables could well capture the change in IAV of ET, while their dominators were different during the two contrasting phases mentioned above. The IAV of radiation and temperature dominated the change of the IAV of ET over 77.82% and 35.14% of the basin, respectively, before and after the turning point. Meanwhile, the rapid increase in vegetation coverage, which was associated with afforestation, significantly (p < 0.05) reduced IAV of ET over about 35% of the study area. The achievements of this study should be beneficial for a sophisticated awareness of responses of intra-annual variability of ET to climate and land cover changes at the basin scale.

Highlights

  • Evapotranspiration (ET) is the only way in which terrestrial water returns to the atmosphere in the earth system [1]

  • The trend of intra-annual variability (IAV) of ET remarkably changed over the Poyang Lake Basin during the study period

  • This study presented changes of intra-annual variability (IAV) of ET and the responses to climatic variables and vegetation coverage over the Poyang Lake Basin in China from 1983 to 2014

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Summary

Introduction

Evapotranspiration (ET) is the only way in which terrestrial water returns to the atmosphere in the earth system [1]. It is a crucial component to maintain land surface water and energy balance [2,3]. Terrestrial ET is mainly composed of two parts [4]. The first is plant transpiration, which is mainly controlled by leaf stomata, and the other is water evaporation from moist surfaces of vegetation and/or soil. Transpiration and evaporation are regulated by both abiotic (e.g., climate and soil) and biotic (e.g., leaf area and coverage) variables [5]. It is meaningful and challenging to understand comprehensive and complex responses of terrestrial ET to changes in climate and land cover

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