Abstract

Various models based on Budyko framework, widely applied to quantify the impacts of climate change and land use/cover change (LUCC) on runoff, assumed a fixed partition used to distinguish the impacts. Several articles have applied a weighting factor describing arbitrary partitions for developing a total differential Budyko (TDB) model and a complementary Budyko (CB) model. This study introduces the weighting factor into a decomposition Budyko (DB) model and applies these three models to analyze runoff variation due to the impacts in the upper-midstream Heihe River basin. The Pettitt test is first applied to determine a change point of a time series expanded by the runoff coefficient. The cause for the change point is analyzed. Transition matrix is adopted to investigate factors of LUCC. Results suggest the consistency of the CB, TDB, and present DB models in estimating runoff variation due to the impacts. The existing DB model excluding the weighting factor overestimates the impact of climate change on runoff and underestimates the LUCC impact as compared with the present DB model. With two extreme values of the weighting factor, runoff decrease induced by LUCC falls in the range of 65.20%–66.42% predicted by the CB model, 65.01%–66.57% by the TDB model, and 64.83%–66.85% by the present DB model. The transition matrixes indicate the major factors of LUCC are climate warming in the upstream of the study area and cropping in the midstream. Our work provides researchers with a better understanding of runoff variation due to climate change and LUCC.

Highlights

  • Spatiotemporal variation of runoff has been an important component in hydrological cycle [1].Climate change and land use/cover change (LUCC) are two major impacts on runoff [2]

  • With two extreme values of the weighting factor, runoff decrease induced by LUCC falls in the range of 65.20%–66.42% predicted by the complementary Budyko (CB) model, 65.01%–66.57% by the total differential Budyko (TDB) model, and 64.83%–66.85% by the present decomposition Budyko (DB) model

  • It can be reasoned that the runoff variation is related to both climate change and LUCC

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Summary

Introduction

Spatiotemporal variation of runoff has been an important component in hydrological cycle [1].Climate change and land use/cover change (LUCC) are two major impacts on runoff [2]. Variation in temperature due to climate change causes the redistribution of precipitation to evapotranspiration and runoff [3]. Extreme hydrological events such as drought and flood influence runoff and intensify global water cycle [4,5,6]. A large amount of groundwater pumping for irrigation reduces runoff and increases evapotranspiration [8]. These lead us to question how to differentiate and quantify the individual impacts of climate change and LUCC on runoff on reginal or global scale [9]. Exploring runoff variation due to the impacts helps researchers understand complex hydrological processes [10,11]

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