Changes in intra-annual runoff and its response to climate change and human activities in the headstream areas of the Tarim River Basin, China
Intra-annual runoff trends and periods in the headstream areas of the Tarim River Basin were investigated by non-parametric tests and wavelet analysis. The analysis was based on runoff data collected from six hydrological stations in the mountain headstreams and at the Alar station in the main strea...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Ling, Hongbo [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2014transfer abstract |
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| Umfang: |
13 |
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| Übergeordnetes Werk: |
Enthalten in: Biocompatible and noncytotoxic nucleoside-based AIEgens sensor for lighting-up nucleic acids - Xiao, Qiuyun ELSEVIER, 2021, the journal of the International Union for Quaternary Research, Amsterdam [u.a.] |
|---|---|
| Übergeordnetes Werk: |
volume:336 ; year:2014 ; day:26 ; month:06 ; pages:158-170 ; extent:13 |
| Links: |
|---|
| DOI / URN: |
10.1016/j.quaint.2013.08.003 |
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| 245 | 1 | 0 | |a Changes in intra-annual runoff and its response to climate change and human activities in the headstream areas of the Tarim River Basin, China |
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| 520 | |a Intra-annual runoff trends and periods in the headstream areas of the Tarim River Basin were investigated by non-parametric tests and wavelet analysis. The analysis was based on runoff data collected from six hydrological stations in the mountain headstreams and at the Alar station in the main stream of Tarim River Basin combined with the regional meteorological data collected from 1957 to 2008. The impacts of human activities and climate change on the runoff quantities during high-flow periods were investigated by structuring models. The results showed that (1) the runoff, air temperature and precipitation of the headstreams increased remarkably during both high-flow and low-flow periods. (2) In mountain headstreams, the concentration degree index (CDI) at the Xiehela hydrological station increased slightly, while the indexes at the other five stations (Shanliguilank, Kaqun, Yuzmenlek, Tongguzlek and Wuluwati) showed decreasing trends. (3) The CDIs of runoff in the mountain headstreams had significant periods of 3–8 years, which were similar to those of air temperature during high- and low-flow periods, but differed from those of precipitation. (4) Both climate change and human activities had significant effects on the total runoff of oasis headstreams during the period of 1993–2007, and climate change was a leading factor driving runoff evolution of oasis headstreams during high-flow periods. Overall, the results of this study provide a scientific basis for realizing reasonable allocation of water resources in the Tarim River Basin. | ||
| 520 | |a Intra-annual runoff trends and periods in the headstream areas of the Tarim River Basin were investigated by non-parametric tests and wavelet analysis. The analysis was based on runoff data collected from six hydrological stations in the mountain headstreams and at the Alar station in the main stream of Tarim River Basin combined with the regional meteorological data collected from 1957 to 2008. The impacts of human activities and climate change on the runoff quantities during high-flow periods were investigated by structuring models. The results showed that (1) the runoff, air temperature and precipitation of the headstreams increased remarkably during both high-flow and low-flow periods. (2) In mountain headstreams, the concentration degree index (CDI) at the Xiehela hydrological station increased slightly, while the indexes at the other five stations (Shanliguilank, Kaqun, Yuzmenlek, Tongguzlek and Wuluwati) showed decreasing trends. (3) The CDIs of runoff in the mountain headstreams had significant periods of 3–8 years, which were similar to those of air temperature during high- and low-flow periods, but differed from those of precipitation. (4) Both climate change and human activities had significant effects on the total runoff of oasis headstreams during the period of 1993–2007, and climate change was a leading factor driving runoff evolution of oasis headstreams during high-flow periods. Overall, the results of this study provide a scientific basis for realizing reasonable allocation of water resources in the Tarim River Basin. | ||
| 700 | 1 | |a Xu, Hailiang |4 oth | |
| 700 | 1 | |a Fu, Jinyi |4 oth | |
| 773 | 0 | 8 | |i Enthalten in |n Elsevier Science |a Xiao, Qiuyun ELSEVIER |t Biocompatible and noncytotoxic nucleoside-based AIEgens sensor for lighting-up nucleic acids |d 2021 |d the journal of the International Union for Quaternary Research |g Amsterdam [u.a.] |w (DE-627)ELV005958261 |
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10.1016/j.quaint.2013.08.003 doi GBVA2014017000015.pica (DE-627)ELV03411145X (ELSEVIER)S1040-6182(13)00541-7 DE-627 ger DE-627 rakwb eng 550 550 DE-600 540 VZ 6,25 ssgn ASIEN DE-1a fid 35.00 bkl 35.04 bkl Ling, Hongbo verfasserin aut Changes in intra-annual runoff and its response to climate change and human activities in the headstream areas of the Tarim River Basin, China 2014transfer abstract 13 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Intra-annual runoff trends and periods in the headstream areas of the Tarim River Basin were investigated by non-parametric tests and wavelet analysis. The analysis was based on runoff data collected from six hydrological stations in the mountain headstreams and at the Alar station in the main stream of Tarim River Basin combined with the regional meteorological data collected from 1957 to 2008. The impacts of human activities and climate change on the runoff quantities during high-flow periods were investigated by structuring models. The results showed that (1) the runoff, air temperature and precipitation of the headstreams increased remarkably during both high-flow and low-flow periods. (2) In mountain headstreams, the concentration degree index (CDI) at the Xiehela hydrological station increased slightly, while the indexes at the other five stations (Shanliguilank, Kaqun, Yuzmenlek, Tongguzlek and Wuluwati) showed decreasing trends. (3) The CDIs of runoff in the mountain headstreams had significant periods of 3–8 years, which were similar to those of air temperature during high- and low-flow periods, but differed from those of precipitation. (4) Both climate change and human activities had significant effects on the total runoff of oasis headstreams during the period of 1993–2007, and climate change was a leading factor driving runoff evolution of oasis headstreams during high-flow periods. Overall, the results of this study provide a scientific basis for realizing reasonable allocation of water resources in the Tarim River Basin. Intra-annual runoff trends and periods in the headstream areas of the Tarim River Basin were investigated by non-parametric tests and wavelet analysis. The analysis was based on runoff data collected from six hydrological stations in the mountain headstreams and at the Alar station in the main stream of Tarim River Basin combined with the regional meteorological data collected from 1957 to 2008. The impacts of human activities and climate change on the runoff quantities during high-flow periods were investigated by structuring models. The results showed that (1) the runoff, air temperature and precipitation of the headstreams increased remarkably during both high-flow and low-flow periods. (2) In mountain headstreams, the concentration degree index (CDI) at the Xiehela hydrological station increased slightly, while the indexes at the other five stations (Shanliguilank, Kaqun, Yuzmenlek, Tongguzlek and Wuluwati) showed decreasing trends. (3) The CDIs of runoff in the mountain headstreams had significant periods of 3–8 years, which were similar to those of air temperature during high- and low-flow periods, but differed from those of precipitation. (4) Both climate change and human activities had significant effects on the total runoff of oasis headstreams during the period of 1993–2007, and climate change was a leading factor driving runoff evolution of oasis headstreams during high-flow periods. Overall, the results of this study provide a scientific basis for realizing reasonable allocation of water resources in the Tarim River Basin. Xu, Hailiang oth Fu, Jinyi oth Enthalten in Elsevier Science Xiao, Qiuyun ELSEVIER Biocompatible and noncytotoxic nucleoside-based AIEgens sensor for lighting-up nucleic acids 2021 the journal of the International Union for Quaternary Research Amsterdam [u.a.] (DE-627)ELV005958261 volume:336 year:2014 day:26 month:06 pages:158-170 extent:13 https://doi.org/10.1016/j.quaint.2013.08.003 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-ASIEN 35.00 Chemie: Allgemeines VZ 35.04 Ausbildung Beruf Organisationen Chemie VZ AR 336 2014 26 0626 158-170 13 045F 550 |
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10.1016/j.quaint.2013.08.003 doi GBVA2014017000015.pica (DE-627)ELV03411145X (ELSEVIER)S1040-6182(13)00541-7 DE-627 ger DE-627 rakwb eng 550 550 DE-600 540 VZ 6,25 ssgn ASIEN DE-1a fid 35.00 bkl 35.04 bkl Ling, Hongbo verfasserin aut Changes in intra-annual runoff and its response to climate change and human activities in the headstream areas of the Tarim River Basin, China 2014transfer abstract 13 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Intra-annual runoff trends and periods in the headstream areas of the Tarim River Basin were investigated by non-parametric tests and wavelet analysis. The analysis was based on runoff data collected from six hydrological stations in the mountain headstreams and at the Alar station in the main stream of Tarim River Basin combined with the regional meteorological data collected from 1957 to 2008. The impacts of human activities and climate change on the runoff quantities during high-flow periods were investigated by structuring models. The results showed that (1) the runoff, air temperature and precipitation of the headstreams increased remarkably during both high-flow and low-flow periods. (2) In mountain headstreams, the concentration degree index (CDI) at the Xiehela hydrological station increased slightly, while the indexes at the other five stations (Shanliguilank, Kaqun, Yuzmenlek, Tongguzlek and Wuluwati) showed decreasing trends. (3) The CDIs of runoff in the mountain headstreams had significant periods of 3–8 years, which were similar to those of air temperature during high- and low-flow periods, but differed from those of precipitation. (4) Both climate change and human activities had significant effects on the total runoff of oasis headstreams during the period of 1993–2007, and climate change was a leading factor driving runoff evolution of oasis headstreams during high-flow periods. Overall, the results of this study provide a scientific basis for realizing reasonable allocation of water resources in the Tarim River Basin. Intra-annual runoff trends and periods in the headstream areas of the Tarim River Basin were investigated by non-parametric tests and wavelet analysis. The analysis was based on runoff data collected from six hydrological stations in the mountain headstreams and at the Alar station in the main stream of Tarim River Basin combined with the regional meteorological data collected from 1957 to 2008. The impacts of human activities and climate change on the runoff quantities during high-flow periods were investigated by structuring models. The results showed that (1) the runoff, air temperature and precipitation of the headstreams increased remarkably during both high-flow and low-flow periods. (2) In mountain headstreams, the concentration degree index (CDI) at the Xiehela hydrological station increased slightly, while the indexes at the other five stations (Shanliguilank, Kaqun, Yuzmenlek, Tongguzlek and Wuluwati) showed decreasing trends. (3) The CDIs of runoff in the mountain headstreams had significant periods of 3–8 years, which were similar to those of air temperature during high- and low-flow periods, but differed from those of precipitation. (4) Both climate change and human activities had significant effects on the total runoff of oasis headstreams during the period of 1993–2007, and climate change was a leading factor driving runoff evolution of oasis headstreams during high-flow periods. Overall, the results of this study provide a scientific basis for realizing reasonable allocation of water resources in the Tarim River Basin. Xu, Hailiang oth Fu, Jinyi oth Enthalten in Elsevier Science Xiao, Qiuyun ELSEVIER Biocompatible and noncytotoxic nucleoside-based AIEgens sensor for lighting-up nucleic acids 2021 the journal of the International Union for Quaternary Research Amsterdam [u.a.] (DE-627)ELV005958261 volume:336 year:2014 day:26 month:06 pages:158-170 extent:13 https://doi.org/10.1016/j.quaint.2013.08.003 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-ASIEN 35.00 Chemie: Allgemeines VZ 35.04 Ausbildung Beruf Organisationen Chemie VZ AR 336 2014 26 0626 158-170 13 045F 550 |
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10.1016/j.quaint.2013.08.003 doi GBVA2014017000015.pica (DE-627)ELV03411145X (ELSEVIER)S1040-6182(13)00541-7 DE-627 ger DE-627 rakwb eng 550 550 DE-600 540 VZ 6,25 ssgn ASIEN DE-1a fid 35.00 bkl 35.04 bkl Ling, Hongbo verfasserin aut Changes in intra-annual runoff and its response to climate change and human activities in the headstream areas of the Tarim River Basin, China 2014transfer abstract 13 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Intra-annual runoff trends and periods in the headstream areas of the Tarim River Basin were investigated by non-parametric tests and wavelet analysis. The analysis was based on runoff data collected from six hydrological stations in the mountain headstreams and at the Alar station in the main stream of Tarim River Basin combined with the regional meteorological data collected from 1957 to 2008. The impacts of human activities and climate change on the runoff quantities during high-flow periods were investigated by structuring models. The results showed that (1) the runoff, air temperature and precipitation of the headstreams increased remarkably during both high-flow and low-flow periods. (2) In mountain headstreams, the concentration degree index (CDI) at the Xiehela hydrological station increased slightly, while the indexes at the other five stations (Shanliguilank, Kaqun, Yuzmenlek, Tongguzlek and Wuluwati) showed decreasing trends. (3) The CDIs of runoff in the mountain headstreams had significant periods of 3–8 years, which were similar to those of air temperature during high- and low-flow periods, but differed from those of precipitation. (4) Both climate change and human activities had significant effects on the total runoff of oasis headstreams during the period of 1993–2007, and climate change was a leading factor driving runoff evolution of oasis headstreams during high-flow periods. Overall, the results of this study provide a scientific basis for realizing reasonable allocation of water resources in the Tarim River Basin. Intra-annual runoff trends and periods in the headstream areas of the Tarim River Basin were investigated by non-parametric tests and wavelet analysis. The analysis was based on runoff data collected from six hydrological stations in the mountain headstreams and at the Alar station in the main stream of Tarim River Basin combined with the regional meteorological data collected from 1957 to 2008. The impacts of human activities and climate change on the runoff quantities during high-flow periods were investigated by structuring models. The results showed that (1) the runoff, air temperature and precipitation of the headstreams increased remarkably during both high-flow and low-flow periods. (2) In mountain headstreams, the concentration degree index (CDI) at the Xiehela hydrological station increased slightly, while the indexes at the other five stations (Shanliguilank, Kaqun, Yuzmenlek, Tongguzlek and Wuluwati) showed decreasing trends. (3) The CDIs of runoff in the mountain headstreams had significant periods of 3–8 years, which were similar to those of air temperature during high- and low-flow periods, but differed from those of precipitation. (4) Both climate change and human activities had significant effects on the total runoff of oasis headstreams during the period of 1993–2007, and climate change was a leading factor driving runoff evolution of oasis headstreams during high-flow periods. Overall, the results of this study provide a scientific basis for realizing reasonable allocation of water resources in the Tarim River Basin. Xu, Hailiang oth Fu, Jinyi oth Enthalten in Elsevier Science Xiao, Qiuyun ELSEVIER Biocompatible and noncytotoxic nucleoside-based AIEgens sensor for lighting-up nucleic acids 2021 the journal of the International Union for Quaternary Research Amsterdam [u.a.] (DE-627)ELV005958261 volume:336 year:2014 day:26 month:06 pages:158-170 extent:13 https://doi.org/10.1016/j.quaint.2013.08.003 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-ASIEN 35.00 Chemie: Allgemeines VZ 35.04 Ausbildung Beruf Organisationen Chemie VZ AR 336 2014 26 0626 158-170 13 045F 550 |
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10.1016/j.quaint.2013.08.003 doi GBVA2014017000015.pica (DE-627)ELV03411145X (ELSEVIER)S1040-6182(13)00541-7 DE-627 ger DE-627 rakwb eng 550 550 DE-600 540 VZ 6,25 ssgn ASIEN DE-1a fid 35.00 bkl 35.04 bkl Ling, Hongbo verfasserin aut Changes in intra-annual runoff and its response to climate change and human activities in the headstream areas of the Tarim River Basin, China 2014transfer abstract 13 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Intra-annual runoff trends and periods in the headstream areas of the Tarim River Basin were investigated by non-parametric tests and wavelet analysis. The analysis was based on runoff data collected from six hydrological stations in the mountain headstreams and at the Alar station in the main stream of Tarim River Basin combined with the regional meteorological data collected from 1957 to 2008. The impacts of human activities and climate change on the runoff quantities during high-flow periods were investigated by structuring models. The results showed that (1) the runoff, air temperature and precipitation of the headstreams increased remarkably during both high-flow and low-flow periods. (2) In mountain headstreams, the concentration degree index (CDI) at the Xiehela hydrological station increased slightly, while the indexes at the other five stations (Shanliguilank, Kaqun, Yuzmenlek, Tongguzlek and Wuluwati) showed decreasing trends. (3) The CDIs of runoff in the mountain headstreams had significant periods of 3–8 years, which were similar to those of air temperature during high- and low-flow periods, but differed from those of precipitation. (4) Both climate change and human activities had significant effects on the total runoff of oasis headstreams during the period of 1993–2007, and climate change was a leading factor driving runoff evolution of oasis headstreams during high-flow periods. Overall, the results of this study provide a scientific basis for realizing reasonable allocation of water resources in the Tarim River Basin. Intra-annual runoff trends and periods in the headstream areas of the Tarim River Basin were investigated by non-parametric tests and wavelet analysis. The analysis was based on runoff data collected from six hydrological stations in the mountain headstreams and at the Alar station in the main stream of Tarim River Basin combined with the regional meteorological data collected from 1957 to 2008. The impacts of human activities and climate change on the runoff quantities during high-flow periods were investigated by structuring models. The results showed that (1) the runoff, air temperature and precipitation of the headstreams increased remarkably during both high-flow and low-flow periods. (2) In mountain headstreams, the concentration degree index (CDI) at the Xiehela hydrological station increased slightly, while the indexes at the other five stations (Shanliguilank, Kaqun, Yuzmenlek, Tongguzlek and Wuluwati) showed decreasing trends. (3) The CDIs of runoff in the mountain headstreams had significant periods of 3–8 years, which were similar to those of air temperature during high- and low-flow periods, but differed from those of precipitation. (4) Both climate change and human activities had significant effects on the total runoff of oasis headstreams during the period of 1993–2007, and climate change was a leading factor driving runoff evolution of oasis headstreams during high-flow periods. Overall, the results of this study provide a scientific basis for realizing reasonable allocation of water resources in the Tarim River Basin. Xu, Hailiang oth Fu, Jinyi oth Enthalten in Elsevier Science Xiao, Qiuyun ELSEVIER Biocompatible and noncytotoxic nucleoside-based AIEgens sensor for lighting-up nucleic acids 2021 the journal of the International Union for Quaternary Research Amsterdam [u.a.] (DE-627)ELV005958261 volume:336 year:2014 day:26 month:06 pages:158-170 extent:13 https://doi.org/10.1016/j.quaint.2013.08.003 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-ASIEN 35.00 Chemie: Allgemeines VZ 35.04 Ausbildung Beruf Organisationen Chemie VZ AR 336 2014 26 0626 158-170 13 045F 550 |
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10.1016/j.quaint.2013.08.003 doi GBVA2014017000015.pica (DE-627)ELV03411145X (ELSEVIER)S1040-6182(13)00541-7 DE-627 ger DE-627 rakwb eng 550 550 DE-600 540 VZ 6,25 ssgn ASIEN DE-1a fid 35.00 bkl 35.04 bkl Ling, Hongbo verfasserin aut Changes in intra-annual runoff and its response to climate change and human activities in the headstream areas of the Tarim River Basin, China 2014transfer abstract 13 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier Intra-annual runoff trends and periods in the headstream areas of the Tarim River Basin were investigated by non-parametric tests and wavelet analysis. The analysis was based on runoff data collected from six hydrological stations in the mountain headstreams and at the Alar station in the main stream of Tarim River Basin combined with the regional meteorological data collected from 1957 to 2008. The impacts of human activities and climate change on the runoff quantities during high-flow periods were investigated by structuring models. The results showed that (1) the runoff, air temperature and precipitation of the headstreams increased remarkably during both high-flow and low-flow periods. (2) In mountain headstreams, the concentration degree index (CDI) at the Xiehela hydrological station increased slightly, while the indexes at the other five stations (Shanliguilank, Kaqun, Yuzmenlek, Tongguzlek and Wuluwati) showed decreasing trends. (3) The CDIs of runoff in the mountain headstreams had significant periods of 3–8 years, which were similar to those of air temperature during high- and low-flow periods, but differed from those of precipitation. (4) Both climate change and human activities had significant effects on the total runoff of oasis headstreams during the period of 1993–2007, and climate change was a leading factor driving runoff evolution of oasis headstreams during high-flow periods. Overall, the results of this study provide a scientific basis for realizing reasonable allocation of water resources in the Tarim River Basin. Intra-annual runoff trends and periods in the headstream areas of the Tarim River Basin were investigated by non-parametric tests and wavelet analysis. The analysis was based on runoff data collected from six hydrological stations in the mountain headstreams and at the Alar station in the main stream of Tarim River Basin combined with the regional meteorological data collected from 1957 to 2008. The impacts of human activities and climate change on the runoff quantities during high-flow periods were investigated by structuring models. The results showed that (1) the runoff, air temperature and precipitation of the headstreams increased remarkably during both high-flow and low-flow periods. (2) In mountain headstreams, the concentration degree index (CDI) at the Xiehela hydrological station increased slightly, while the indexes at the other five stations (Shanliguilank, Kaqun, Yuzmenlek, Tongguzlek and Wuluwati) showed decreasing trends. (3) The CDIs of runoff in the mountain headstreams had significant periods of 3–8 years, which were similar to those of air temperature during high- and low-flow periods, but differed from those of precipitation. (4) Both climate change and human activities had significant effects on the total runoff of oasis headstreams during the period of 1993–2007, and climate change was a leading factor driving runoff evolution of oasis headstreams during high-flow periods. Overall, the results of this study provide a scientific basis for realizing reasonable allocation of water resources in the Tarim River Basin. Xu, Hailiang oth Fu, Jinyi oth Enthalten in Elsevier Science Xiao, Qiuyun ELSEVIER Biocompatible and noncytotoxic nucleoside-based AIEgens sensor for lighting-up nucleic acids 2021 the journal of the International Union for Quaternary Research Amsterdam [u.a.] (DE-627)ELV005958261 volume:336 year:2014 day:26 month:06 pages:158-170 extent:13 https://doi.org/10.1016/j.quaint.2013.08.003 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U FID-ASIEN 35.00 Chemie: Allgemeines VZ 35.04 Ausbildung Beruf Organisationen Chemie VZ AR 336 2014 26 0626 158-170 13 045F 550 |
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Biocompatible and noncytotoxic nucleoside-based AIEgens sensor for lighting-up nucleic acids |
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changes in intra-annual runoff and its response to climate change and human activities in the headstream areas of the tarim river basin, china |
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Changes in intra-annual runoff and its response to climate change and human activities in the headstream areas of the Tarim River Basin, China |
| abstract |
Intra-annual runoff trends and periods in the headstream areas of the Tarim River Basin were investigated by non-parametric tests and wavelet analysis. The analysis was based on runoff data collected from six hydrological stations in the mountain headstreams and at the Alar station in the main stream of Tarim River Basin combined with the regional meteorological data collected from 1957 to 2008. The impacts of human activities and climate change on the runoff quantities during high-flow periods were investigated by structuring models. The results showed that (1) the runoff, air temperature and precipitation of the headstreams increased remarkably during both high-flow and low-flow periods. (2) In mountain headstreams, the concentration degree index (CDI) at the Xiehela hydrological station increased slightly, while the indexes at the other five stations (Shanliguilank, Kaqun, Yuzmenlek, Tongguzlek and Wuluwati) showed decreasing trends. (3) The CDIs of runoff in the mountain headstreams had significant periods of 3–8 years, which were similar to those of air temperature during high- and low-flow periods, but differed from those of precipitation. (4) Both climate change and human activities had significant effects on the total runoff of oasis headstreams during the period of 1993–2007, and climate change was a leading factor driving runoff evolution of oasis headstreams during high-flow periods. Overall, the results of this study provide a scientific basis for realizing reasonable allocation of water resources in the Tarim River Basin. |
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Intra-annual runoff trends and periods in the headstream areas of the Tarim River Basin were investigated by non-parametric tests and wavelet analysis. The analysis was based on runoff data collected from six hydrological stations in the mountain headstreams and at the Alar station in the main stream of Tarim River Basin combined with the regional meteorological data collected from 1957 to 2008. The impacts of human activities and climate change on the runoff quantities during high-flow periods were investigated by structuring models. The results showed that (1) the runoff, air temperature and precipitation of the headstreams increased remarkably during both high-flow and low-flow periods. (2) In mountain headstreams, the concentration degree index (CDI) at the Xiehela hydrological station increased slightly, while the indexes at the other five stations (Shanliguilank, Kaqun, Yuzmenlek, Tongguzlek and Wuluwati) showed decreasing trends. (3) The CDIs of runoff in the mountain headstreams had significant periods of 3–8 years, which were similar to those of air temperature during high- and low-flow periods, but differed from those of precipitation. (4) Both climate change and human activities had significant effects on the total runoff of oasis headstreams during the period of 1993–2007, and climate change was a leading factor driving runoff evolution of oasis headstreams during high-flow periods. Overall, the results of this study provide a scientific basis for realizing reasonable allocation of water resources in the Tarim River Basin. |
| abstract_unstemmed |
Intra-annual runoff trends and periods in the headstream areas of the Tarim River Basin were investigated by non-parametric tests and wavelet analysis. The analysis was based on runoff data collected from six hydrological stations in the mountain headstreams and at the Alar station in the main stream of Tarim River Basin combined with the regional meteorological data collected from 1957 to 2008. The impacts of human activities and climate change on the runoff quantities during high-flow periods were investigated by structuring models. The results showed that (1) the runoff, air temperature and precipitation of the headstreams increased remarkably during both high-flow and low-flow periods. (2) In mountain headstreams, the concentration degree index (CDI) at the Xiehela hydrological station increased slightly, while the indexes at the other five stations (Shanliguilank, Kaqun, Yuzmenlek, Tongguzlek and Wuluwati) showed decreasing trends. (3) The CDIs of runoff in the mountain headstreams had significant periods of 3–8 years, which were similar to those of air temperature during high- and low-flow periods, but differed from those of precipitation. (4) Both climate change and human activities had significant effects on the total runoff of oasis headstreams during the period of 1993–2007, and climate change was a leading factor driving runoff evolution of oasis headstreams during high-flow periods. Overall, the results of this study provide a scientific basis for realizing reasonable allocation of water resources in the Tarim River Basin. |
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