Characteristics of runoff change in the Shiyang River Basin

doi:10.7522/j.issn.1000-694X.2022.00142

Journal of Desert Research ›› 2023, Vol. 43 ›› Issue (3): 57-68.DOI: 10.7522/j.issn.1000-694X.2022.00142

Characteristics of runoff change in the Shiyang River Basin

Ran Duan¹(), Zongjie Li¹(), Yu Wang¹, Xiaoying Liu¹, Juan Gui², Pengfei Liang², Yuchen Li², Jian Xue², Mengqing Liu¹, Bin Xu¹

^1.School of Energy and Power Engineering，Lanzhou University of Technology，Lanzhou 730050，China
^2.Key Laboratory of Ecohydrology of Inland River Basin / Gansu Qilian Mountains Ecology Research Center，Northwest Institute of Eco-Environment and Resources，Chinese Academy of Sciences，Lanzhou 730000，China

Received:2022-08-31 Revised:2022-10-14 Online:2023-05-20 Published:2023-05-31
Contact: Zongjie Li

Abstract

Abstract:

Based on the month-by-month precipitation and runoff data from 12 hydrological stations and 35 rainfall stations in the main stream and eight tributaries of the Shiyang River Basin， wavelet analysis and double accumulation curve were used to study the change characteristics of runoff in the Shiyang River Basin. The results showed that：（1） The overall trend of runoff in the Shiyang River Basin was decreasing， with an average decrease of 0.37 billion m³ per 10 a.The runoff in the main stream of Shiyang River， Jinta River， Zamu River， Huangyang River and Gulang River decreased， and the runoff in the Xida River， Dongda River， Xiying River and Dajing River increased. （2） Nine hydrological stations in the Shiyang River Basin have periodic variations on time scales of 2-10 a and 10-30 a， among which the Zamusi station and the Huangyanghe reservoir station also have long periodic variations of 30-60 a， and the nine hydrological stations have the most obvious changes in abundance and depletion on time scales of 24， 21， 21， 21， 43， 45， 22， 17， 21 a， respectively. （3） The abrupt changes in the Shiyang River main stream and eight major tributaries occurred in 1971， 2014， 2000， 2018， 1960， 1959， 1962， 1994 and 1965， respectively， in which the runoff decreased after abrupt changes in the Shiyang River main stream， Jinta River， Zamu River， Huangyang River and Gulang River， increased after abrupt changes in the Xida River， Xiyang River and Dajing River， and did not have abrupt changes in the Dongda River. The results of the study can provide reference for the scientific management and optimal allocation of water resources in the Shiyang River basin and the implementation of subsequent ecological projects.

Key words: Shiyang River Basin, climate change, runoff change

CLC Number:

P333.1

Ran Duan, Zongjie Li, Yu Wang, Xiaoying Liu, Juan Gui, Pengfei Liang, Yuchen Li, Jian Xue, Mengqing Liu, Bin Xu. Characteristics of runoff change in the Shiyang River Basin[J]. Journal of Desert Research, 2023, 43(3): 57-68.

Figures/Tables 11

Fig.1 Location of the study area and distribution of hydrological and rainfall stations

Table 1 Hydrographical stations location information of Shiyang River Basin

河段	流域	水文站	经度(E)/（°）	纬度(N)/（°）	资料年份
支流（上游）	西大河	西大河水库	101.38	38.05	1982—2020
	东大河	金川峡	101.99	38.24	1958—2020
	西营河	九条岭	102.05	37.87	1956—2020
	金塔河	南营水库	102.52	37.80	1955—2020
	杂木河	杂木寺	102.57	37.70	1952—2020
	黄羊河	黄羊河水库	102.72	37.57	1950—2020
	古浪河	古浪	102.90	37.43	1989—2020
	大靖河	大靖峡水库	103.35	37.38	1962—2006
干流（中下游）	石羊河	蔡旗	102.75	38.22	1956—2020

Fig.2 Inter-annual change of runoff in the Shiyang River Basin

Fig.3 Annual distribution of runoff in the Shiyang River Basin

Table 2 The magnitude of seasonal change of runoff in the Shiyang River Basin after the 1990s compared to the pre-1990s

流域	春季	夏季	秋季	冬季
干流	31.8%	70.7%	65.9%	-64.2%
西大河	-6.4%	-11.6%	23.2%	-4.7%
东大河	-7.4%	47.8%	50.1%	7.8%
西营河	-5.2%	-9.1%	10.7%	13.6%
金塔河	-15.0%	-11.2%	2.5%	-4.3%
杂木河	-6.0%	-17.1%	4.3%	6.3%
黄羊河	-67.1%	45.2%	48.3%	30.6%
古浪河	-39.7%	6.8%	24.2%	-58.8%
大靖河	-19.5%	-0.9%	8.6%	29.96%

Fig.4 Annual distribution of runoff and precipitation in the Shiyang River Basin

Fig.5 Wavelet cycle change of runoff in the Shiyang River Basin

Fig.6 Wavelet variance of runoff in the Shiyang River Basin

Fig.7 Abrupt change of runoff in the Shiyang River Basin

Fig.8 Abundance， flatness and dryness of runoff in the Shiyang River Basin

Fig.9 Runoff-precipitation double accumulation curve in the Shiyang River Basin

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Characteristics of runoff change in the Shiyang River Basin

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