气候变化下的塔里木盆地西南部内陆河流域径流组分特征分析

doi:10.13866/j.azr.2022. 01.12

Abstract

Abstract:

Climate change has a significant impact on the water cycle in the alpine region of Central Asia, which intensifies the disparity between the supply and demand of regional water resources. Understanding the characteristics of runoff components in regional inland rivers is of great importance for water resource management. Based on meteorological data and runoff data from the Tiznafu River Basin in the southwest of the Tarim Basin from the past 60 years (1957-2016), regional climate change and runoff responses were evaluated in this study. Results showed that the temperature of the whole basin and the precipitation in mountainous areas had an obvious upward trend; moreover, the regional warming and humidification trends had become more pronounced since 2010. Given these changes, the runoff of the Tiznafu River had increased significantly in summer and autumn, although there was no significant change in spring. Using isotope samples, we investigated variation in isotopes in different water sources and analyzed the contribution of different water sources based on isotope hydrograph separation. Melt water, groundwater, and rainfall contributed 17%, 40%, and 43% of the annual stream flow, respectively. There were obvious differences in runoff components in different seasons and the contribution of precipitation to runoff was more substantial in summer. As a typical alpine inland river in the southwest of the Tarim River Basin, regional climate change, especially changes in precipitation, will greatly affect the utilization of the Tizinafu River and its resources in the future.

Key words: Tiznafu River Basin, climate change, runoff, isotope, hydrograph separation, Tarim Basin

SUN Congjian,CHEN Wei,WANG Shiyu. Stream component characteristics of the inland river basin of the Tarim Basin under regional climate change[J].Arid Zone Research, 2022, 39(1): 113-122.

Figures/Tables 11

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References 30

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站点类型	名称	地理位置	地形	时间段
气象站	塔什库尔干	37°46′N, 75°14′E	山区(3091 m)	1957—2016年
气象站	莎车	38°26′N, 77°16′E	平原(1231 m)	1957—2016年
水文站	江卡	37°44′N, 77°15′E	出山口(1504 m)	1974—2016年

位置	类型	气温				降水
位置	类型	C_v	比率/[℃·(10a)^-1]	突变点（年）		C_v	比率/[mm·(10a)^-1]	突变点（年）	比例/%
平原	年均	0.04	0.29	1996^**		0.56	5.66	None	-
	春季	0.13	0.35	1996^**		1.33	0.06	None	18
	夏季	0.03	0.12	None		0.80	3.72	None	63
	秋季	0.17	0.29	1997^**		1.29	1.38	1974^*	14
	冬季	0.25	0.39	1978^**		1.51	0.50	None	5
山区	年均	0.24	0.31	1987^**		0.32	7.30	1997^**	-
	春季	2.29	0.33	1992^**	0.74		1.19	None	14
	夏季	0.07	0.19	1993^**	0.46		4.95	None	66
	秋季	0.23	0.44	1986^**	0.92		0.69	None	12
	冬季	0.17	0.27	None	1.39		0.45	None	8

类型	C_v	变化率/(10⁹m³·a^-1)	突变点（年）	比例/%
年径流	0.18	0.06	1998^**
春季径流	0.31	0.008	None	5
夏季径流	0.17	0.045	1998^*	79
秋季径流	0.34	0.01	1997^**	13
冬季径流	0.20	0.003	1996^**	3

月份	河水					降水					地下水					融冰雪水（河冰）
	δD	δ¹⁸O	TDS	N		δD	δ¹⁸O	TDS	N		δD	δ¹⁸O	TDS	N		δD	δ¹⁸O	TDS	N
	/‰	/‰	/(mg·L^-1)	N	/‰		/‰	/(mg·L^-1)	N	/‰	/‰		/(mg·L^-1)	N	/‰	/‰	/(mg·L^-1)		N
1						-19.9	-25.74	70	1
2						-115.45	-15.2	75	6
3	-39.07	-6.88	410	6		-96.16	-13.34	70	2		-63.2	-9.3	715	2		-28.05	-5.38	170	2
4	-55.44	-9.15	412	6		-87.89	-11.72	110	1		-39.06	-7.72	720	2		-28.52	-5.5	174	2
5	-56	-8.94	400	6		-78.37	-10.09	120	4		-41.24	-7.56	715	2		-41.2	-7.87	150	2
6	-49.14	-8.54	370	6		-44.21	-7.2	120	1		-41.24	-7.57	730	2		-79.9	-10.24	170	2
7	-47.84	-8.18	370	6		-33.27	-5.97	120	4		-49.91	-8.54	740	2		-121..30	-12.22	160	2
8	-37.77	-7.31	380	6		-27.45	-4.79	130	5		-58.01	-9.3	725	2		-115.2	-11.35	170	2
9	-39.33	-7.24	390	6		-30.62	-5.47	119	4		-60.23	-9.4	720	2		-80.9	-10.49	160	2
10	-38.66	-7.01	400	6		-112.48	-14.94	110	1		-61.1	-9.45	715	2		-28.32	-5.3	170	2
11	-39.2	-7.24	400	6		-194.34	-24.41	110	1		-61	-9.4	715	2		-29.85	-5.71	170	2
12	-	-	-	-		-194.11	-24.31	80	2		-	-	-	-		-	-	-	-

Stream component characteristics of the inland river basin of the Tarim Basin under regional climate change

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