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Ismaiylov, G. Kh.; Fedorov, V. M.

doi:10.1023/a:1012342203595

Cited by 11 publications

(2 citation statements)

References 1 publication

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“…In recent years, hydrologists have put great efforts into attribution analysis of changes in runoff [16][17][18][19][20][21][22][23][24][25][26]. Broadly, the attribution analysis methods can be mainly divided into five categories: (1) Paired catchment studies.…”

Section: Introductionmentioning

confidence: 99%

Attribution of Runoff Change for the Xinshui River Catchment on the Loess Plateau of China in a Changing Environment

Wang

Zhang

Yang

2016

Water

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Abstract:Stream flow plays a crucial role in the environment, society, and the economy, and identifying the causes of changes in runoff is important to understanding the impact of climate change and human activity. This study examines the variation trends in recorded runoff for the Xinshui River, a tributary of the Yellow River on the Loess Plateau, and uses hydrological simulations to investigate how climate change and human activity have contributed to those trends. Results show that the recorded runoff at the Daning station on the Xinshui River declined significantly from 1955-2008 with an abrupt change occurring in 1973. The Simplified Water Balance Model (SWBM) simulates monthly discharge well with a Nash-Sutcliffe efficiency (NSE) coefficient of 78% and a relative error of volumetric fit (RE) of 0.32%. Runoff depth over the catchment in 1973-2008 fell by 25.5 mm relative to the previous period, with human activity and climate change contributing 60.6% and 39.4% of the total runoff reduction, respectively. However, the impacts induced by climate change and human activities are both tending to increase. Therefore, efforts to improve the ecology of the Loess Plateau should give sufficient attention to the impacts of climate change and human activity.

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Section: Introductionmentioning

confidence: 99%

Attribution of Runoff Change for the Xinshui River Catchment on the Loess Plateau of China in a Changing Environment

Wang

Zhang

Yang

2016

Water

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“…In recent decades, the annual average maximum temperature, minimum temperature, mean temperature, and annual precipitation in the ARB have exhibited generally increasing trends [18][19][20][21]. Moreover, significant regional, seasonal, and interannual variations in temperature and precipitation have been investigated in portions of the ARB [1,7,[22][23][24][25]. Furthermore, driven by the different policies, regional characteristics, and economic development statuses in China, Russia, and Mongolia, the land was reclaimed, resulting in significant fragmentation of the remaining wetlands [27,29,49].…”

Section: Introductionmentioning

confidence: 99%

Impacts of Climate and Land-Use Changes on the Hydrological Processes in the Amur River Basin

Zhou

Zhang

Guo

2019

Water

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Under the joint effects resulted from different changes of climate and land-use regimes, spatial-temporal variations of hydrological processes took place in certain principles. Identifying the impact of changes in individual land-use types/climatic factors on hydrological processes is significant for water management and sustainability of watersheds. In this study, seven simulation scenarios were developed using the soil and water assessment tool (SWAT) model to distinguish the impacts of climate and land-use changes on the hydrological processes in the Amur River Basin (ARB) for four periods of 1980–1990, 1991–1999, 2000–2006, and 2007–2013, respectively. Based on the multi-period simulation scenario data, partial least squares regression and ridge regression analyses were performed to further evaluate the effects of changes in individual land-use types/climatic factors on hydrologic components. The results suggested that summer precipitation and summer average temperature were the dominant climatic factors, and crops and wetlands were the principal land-use types contributing to the hydrological responses. In addition, the drastic changes in crop and wetland areas and a clear decline in summer precipitation between the periods of 1991–1999 and 2000–2006 may account for the highest-intensity impacts of climate and land-use changes on the runoff at the outlet (−31.38% and 16.17%, respectively) during the four periods.

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Quantifying the effects of climate and watershed structure changes on runoff variations in the Tao River basin by using three different methods under the Budyko framework

Guan

Zhang

Yang

et al. 2022

Theor Appl Climatol

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Cited by 11 publications

References 1 publication

Attribution of Runoff Change for the Xinshui River Catchment on the Loess Plateau of China in a Changing Environment

Attribution of Runoff Change for the Xinshui River Catchment on the Loess Plateau of China in a Changing Environment

Impacts of Climate and Land-Use Changes on the Hydrological Processes in the Amur River Basin

Quantifying the effects of climate and watershed structure changes on runoff variations in the Tao River basin by using three different methods under the Budyko framework

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