Characteristic of the water temperature lag in Three Gorges Reservoir and its effect on the water temperature structure of tributaries
Abstract The water temperature regimes of the Yangtze River has changed a lot since the impoundment of the Three Gorges Reservoir (TGR), which lead to a significant effect on the water environment in the TGR. This paper focuses on the analysis of characteristics of water temperature regimes of the m...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Long, Liang-Hong [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2016 |
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| Schlagwörter: |
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| Anmerkung: |
© Springer-Verlag Berlin Heidelberg 2016 |
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| Übergeordnetes Werk: |
Enthalten in: Environmental earth sciences - Berlin : Springer, 2009, 75(2016), 22 vom: 22. Nov. |
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| Übergeordnetes Werk: |
volume:75 ; year:2016 ; number:22 ; day:22 ; month:11 |
| Links: |
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| DOI / URN: |
10.1007/s12665-016-6266-1 |
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| Katalog-ID: |
SPR02672409X |
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| 100 | 1 | |a Long, Liang-Hong |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a Characteristic of the water temperature lag in Three Gorges Reservoir and its effect on the water temperature structure of tributaries |
| 264 | 1 | |c 2016 | |
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| 520 | |a Abstract The water temperature regimes of the Yangtze River has changed a lot since the impoundment of the Three Gorges Reservoir (TGR), which lead to a significant effect on the water environment in the TGR. This paper focuses on the analysis of characteristics of water temperature regimes of the main stream in the TGR and the lagging effect of water temperature on temperature structure differences in six typical tributaries. The results showed that water temperature gradually decreased along the main stream and stratified position of water temperature was about 5–10 m arisen in estuaries of six tributaries in heating period. However, water temperature gradually increased along the main stream, and water temperature stratification of the six estuaries disappeared in cooling period. Annual vertical water temperature showed little change. After the impoundment of the TGR, the impact of water temperature is mainly reflected in lag characteristics. The monthly mean temperature difference significantly doubled, and the whole process of water temperature had been put off one month. Through further analyses, water temperature profile tends to be stable with the success of the TGR impounding to 175 m and contributes to water temperature differences in tributary, which is the main reason for water temperature structure changed from three layer to two layer gradually. | ||
| 650 | 4 | |a Three Gorges Reservoir |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Cumulative effect |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Hydrodynamic |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Water temperature |7 (dpeaa)DE-He213 | |
| 700 | 1 | |a Xu, Hui |4 aut | |
| 700 | 1 | |a Ji, Dao-Bin |4 aut | |
| 700 | 1 | |a Cui, Yu-Jie |4 aut | |
| 700 | 1 | |a Liu, De-Fu |4 aut | |
| 700 | 1 | |a Song, Lin-Xu |4 aut | |
| 773 | 0 | 8 | |i Enthalten in |t Environmental earth sciences |d Berlin : Springer, 2009 |g 75(2016), 22 vom: 22. Nov. |w (DE-627)599673451 |w (DE-600)2493699-6 |x 1866-6299 |7 nnns |
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10.1007/s12665-016-6266-1 doi (DE-627)SPR02672409X (SPR)s12665-016-6266-1-e DE-627 ger DE-627 rakwb eng Long, Liang-Hong verfasserin aut Characteristic of the water temperature lag in Three Gorges Reservoir and its effect on the water temperature structure of tributaries 2016 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag Berlin Heidelberg 2016 Abstract The water temperature regimes of the Yangtze River has changed a lot since the impoundment of the Three Gorges Reservoir (TGR), which lead to a significant effect on the water environment in the TGR. This paper focuses on the analysis of characteristics of water temperature regimes of the main stream in the TGR and the lagging effect of water temperature on temperature structure differences in six typical tributaries. The results showed that water temperature gradually decreased along the main stream and stratified position of water temperature was about 5–10 m arisen in estuaries of six tributaries in heating period. However, water temperature gradually increased along the main stream, and water temperature stratification of the six estuaries disappeared in cooling period. Annual vertical water temperature showed little change. After the impoundment of the TGR, the impact of water temperature is mainly reflected in lag characteristics. The monthly mean temperature difference significantly doubled, and the whole process of water temperature had been put off one month. Through further analyses, water temperature profile tends to be stable with the success of the TGR impounding to 175 m and contributes to water temperature differences in tributary, which is the main reason for water temperature structure changed from three layer to two layer gradually. Three Gorges Reservoir (dpeaa)DE-He213 Cumulative effect (dpeaa)DE-He213 Hydrodynamic (dpeaa)DE-He213 Water temperature (dpeaa)DE-He213 Xu, Hui aut Ji, Dao-Bin aut Cui, Yu-Jie aut Liu, De-Fu aut Song, Lin-Xu aut Enthalten in Environmental earth sciences Berlin : Springer, 2009 75(2016), 22 vom: 22. Nov. (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:75 year:2016 number:22 day:22 month:11 https://dx.doi.org/10.1007/s12665-016-6266-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 75 2016 22 22 11 |
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10.1007/s12665-016-6266-1 doi (DE-627)SPR02672409X (SPR)s12665-016-6266-1-e DE-627 ger DE-627 rakwb eng Long, Liang-Hong verfasserin aut Characteristic of the water temperature lag in Three Gorges Reservoir and its effect on the water temperature structure of tributaries 2016 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag Berlin Heidelberg 2016 Abstract The water temperature regimes of the Yangtze River has changed a lot since the impoundment of the Three Gorges Reservoir (TGR), which lead to a significant effect on the water environment in the TGR. This paper focuses on the analysis of characteristics of water temperature regimes of the main stream in the TGR and the lagging effect of water temperature on temperature structure differences in six typical tributaries. The results showed that water temperature gradually decreased along the main stream and stratified position of water temperature was about 5–10 m arisen in estuaries of six tributaries in heating period. However, water temperature gradually increased along the main stream, and water temperature stratification of the six estuaries disappeared in cooling period. Annual vertical water temperature showed little change. After the impoundment of the TGR, the impact of water temperature is mainly reflected in lag characteristics. The monthly mean temperature difference significantly doubled, and the whole process of water temperature had been put off one month. Through further analyses, water temperature profile tends to be stable with the success of the TGR impounding to 175 m and contributes to water temperature differences in tributary, which is the main reason for water temperature structure changed from three layer to two layer gradually. Three Gorges Reservoir (dpeaa)DE-He213 Cumulative effect (dpeaa)DE-He213 Hydrodynamic (dpeaa)DE-He213 Water temperature (dpeaa)DE-He213 Xu, Hui aut Ji, Dao-Bin aut Cui, Yu-Jie aut Liu, De-Fu aut Song, Lin-Xu aut Enthalten in Environmental earth sciences Berlin : Springer, 2009 75(2016), 22 vom: 22. Nov. (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:75 year:2016 number:22 day:22 month:11 https://dx.doi.org/10.1007/s12665-016-6266-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 75 2016 22 22 11 |
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10.1007/s12665-016-6266-1 doi (DE-627)SPR02672409X (SPR)s12665-016-6266-1-e DE-627 ger DE-627 rakwb eng Long, Liang-Hong verfasserin aut Characteristic of the water temperature lag in Three Gorges Reservoir and its effect on the water temperature structure of tributaries 2016 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag Berlin Heidelberg 2016 Abstract The water temperature regimes of the Yangtze River has changed a lot since the impoundment of the Three Gorges Reservoir (TGR), which lead to a significant effect on the water environment in the TGR. This paper focuses on the analysis of characteristics of water temperature regimes of the main stream in the TGR and the lagging effect of water temperature on temperature structure differences in six typical tributaries. The results showed that water temperature gradually decreased along the main stream and stratified position of water temperature was about 5–10 m arisen in estuaries of six tributaries in heating period. However, water temperature gradually increased along the main stream, and water temperature stratification of the six estuaries disappeared in cooling period. Annual vertical water temperature showed little change. After the impoundment of the TGR, the impact of water temperature is mainly reflected in lag characteristics. The monthly mean temperature difference significantly doubled, and the whole process of water temperature had been put off one month. Through further analyses, water temperature profile tends to be stable with the success of the TGR impounding to 175 m and contributes to water temperature differences in tributary, which is the main reason for water temperature structure changed from three layer to two layer gradually. Three Gorges Reservoir (dpeaa)DE-He213 Cumulative effect (dpeaa)DE-He213 Hydrodynamic (dpeaa)DE-He213 Water temperature (dpeaa)DE-He213 Xu, Hui aut Ji, Dao-Bin aut Cui, Yu-Jie aut Liu, De-Fu aut Song, Lin-Xu aut Enthalten in Environmental earth sciences Berlin : Springer, 2009 75(2016), 22 vom: 22. Nov. (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:75 year:2016 number:22 day:22 month:11 https://dx.doi.org/10.1007/s12665-016-6266-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 75 2016 22 22 11 |
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10.1007/s12665-016-6266-1 doi (DE-627)SPR02672409X (SPR)s12665-016-6266-1-e DE-627 ger DE-627 rakwb eng Long, Liang-Hong verfasserin aut Characteristic of the water temperature lag in Three Gorges Reservoir and its effect on the water temperature structure of tributaries 2016 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag Berlin Heidelberg 2016 Abstract The water temperature regimes of the Yangtze River has changed a lot since the impoundment of the Three Gorges Reservoir (TGR), which lead to a significant effect on the water environment in the TGR. This paper focuses on the analysis of characteristics of water temperature regimes of the main stream in the TGR and the lagging effect of water temperature on temperature structure differences in six typical tributaries. The results showed that water temperature gradually decreased along the main stream and stratified position of water temperature was about 5–10 m arisen in estuaries of six tributaries in heating period. However, water temperature gradually increased along the main stream, and water temperature stratification of the six estuaries disappeared in cooling period. Annual vertical water temperature showed little change. After the impoundment of the TGR, the impact of water temperature is mainly reflected in lag characteristics. The monthly mean temperature difference significantly doubled, and the whole process of water temperature had been put off one month. Through further analyses, water temperature profile tends to be stable with the success of the TGR impounding to 175 m and contributes to water temperature differences in tributary, which is the main reason for water temperature structure changed from three layer to two layer gradually. Three Gorges Reservoir (dpeaa)DE-He213 Cumulative effect (dpeaa)DE-He213 Hydrodynamic (dpeaa)DE-He213 Water temperature (dpeaa)DE-He213 Xu, Hui aut Ji, Dao-Bin aut Cui, Yu-Jie aut Liu, De-Fu aut Song, Lin-Xu aut Enthalten in Environmental earth sciences Berlin : Springer, 2009 75(2016), 22 vom: 22. Nov. (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:75 year:2016 number:22 day:22 month:11 https://dx.doi.org/10.1007/s12665-016-6266-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 75 2016 22 22 11 |
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10.1007/s12665-016-6266-1 doi (DE-627)SPR02672409X (SPR)s12665-016-6266-1-e DE-627 ger DE-627 rakwb eng Long, Liang-Hong verfasserin aut Characteristic of the water temperature lag in Three Gorges Reservoir and its effect on the water temperature structure of tributaries 2016 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Springer-Verlag Berlin Heidelberg 2016 Abstract The water temperature regimes of the Yangtze River has changed a lot since the impoundment of the Three Gorges Reservoir (TGR), which lead to a significant effect on the water environment in the TGR. This paper focuses on the analysis of characteristics of water temperature regimes of the main stream in the TGR and the lagging effect of water temperature on temperature structure differences in six typical tributaries. The results showed that water temperature gradually decreased along the main stream and stratified position of water temperature was about 5–10 m arisen in estuaries of six tributaries in heating period. However, water temperature gradually increased along the main stream, and water temperature stratification of the six estuaries disappeared in cooling period. Annual vertical water temperature showed little change. After the impoundment of the TGR, the impact of water temperature is mainly reflected in lag characteristics. The monthly mean temperature difference significantly doubled, and the whole process of water temperature had been put off one month. Through further analyses, water temperature profile tends to be stable with the success of the TGR impounding to 175 m and contributes to water temperature differences in tributary, which is the main reason for water temperature structure changed from three layer to two layer gradually. Three Gorges Reservoir (dpeaa)DE-He213 Cumulative effect (dpeaa)DE-He213 Hydrodynamic (dpeaa)DE-He213 Water temperature (dpeaa)DE-He213 Xu, Hui aut Ji, Dao-Bin aut Cui, Yu-Jie aut Liu, De-Fu aut Song, Lin-Xu aut Enthalten in Environmental earth sciences Berlin : Springer, 2009 75(2016), 22 vom: 22. Nov. (DE-627)599673451 (DE-600)2493699-6 1866-6299 nnns volume:75 year:2016 number:22 day:22 month:11 https://dx.doi.org/10.1007/s12665-016-6266-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 75 2016 22 22 11 |
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Long, Liang-Hong @@aut@@ Xu, Hui @@aut@@ Ji, Dao-Bin @@aut@@ Cui, Yu-Jie @@aut@@ Liu, De-Fu @@aut@@ Song, Lin-Xu @@aut@@ |
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<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">SPR02672409X</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230401020202.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">201007s2016 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s12665-016-6266-1</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)SPR02672409X</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(SPR)s12665-016-6266-1-e</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Long, Liang-Hong</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Characteristic of the water temperature lag in Three Gorges Reservoir and its effect on the water temperature structure of tributaries</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2016</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© Springer-Verlag Berlin Heidelberg 2016</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract The water temperature regimes of the Yangtze River has changed a lot since the impoundment of the Three Gorges Reservoir (TGR), which lead to a significant effect on the water environment in the TGR. This paper focuses on the analysis of characteristics of water temperature regimes of the main stream in the TGR and the lagging effect of water temperature on temperature structure differences in six typical tributaries. The results showed that water temperature gradually decreased along the main stream and stratified position of water temperature was about 5–10 m arisen in estuaries of six tributaries in heating period. However, water temperature gradually increased along the main stream, and water temperature stratification of the six estuaries disappeared in cooling period. Annual vertical water temperature showed little change. After the impoundment of the TGR, the impact of water temperature is mainly reflected in lag characteristics. The monthly mean temperature difference significantly doubled, and the whole process of water temperature had been put off one month. 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Long, Liang-Hong |
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Long, Liang-Hong misc Three Gorges Reservoir misc Cumulative effect misc Hydrodynamic misc Water temperature Characteristic of the water temperature lag in Three Gorges Reservoir and its effect on the water temperature structure of tributaries |
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Characteristic of the water temperature lag in Three Gorges Reservoir and its effect on the water temperature structure of tributaries Three Gorges Reservoir (dpeaa)DE-He213 Cumulative effect (dpeaa)DE-He213 Hydrodynamic (dpeaa)DE-He213 Water temperature (dpeaa)DE-He213 |
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Characteristic of the water temperature lag in Three Gorges Reservoir and its effect on the water temperature structure of tributaries |
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characteristic of the water temperature lag in three gorges reservoir and its effect on the water temperature structure of tributaries |
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Characteristic of the water temperature lag in Three Gorges Reservoir and its effect on the water temperature structure of tributaries |
| abstract |
Abstract The water temperature regimes of the Yangtze River has changed a lot since the impoundment of the Three Gorges Reservoir (TGR), which lead to a significant effect on the water environment in the TGR. This paper focuses on the analysis of characteristics of water temperature regimes of the main stream in the TGR and the lagging effect of water temperature on temperature structure differences in six typical tributaries. The results showed that water temperature gradually decreased along the main stream and stratified position of water temperature was about 5–10 m arisen in estuaries of six tributaries in heating period. However, water temperature gradually increased along the main stream, and water temperature stratification of the six estuaries disappeared in cooling period. Annual vertical water temperature showed little change. After the impoundment of the TGR, the impact of water temperature is mainly reflected in lag characteristics. The monthly mean temperature difference significantly doubled, and the whole process of water temperature had been put off one month. Through further analyses, water temperature profile tends to be stable with the success of the TGR impounding to 175 m and contributes to water temperature differences in tributary, which is the main reason for water temperature structure changed from three layer to two layer gradually. © Springer-Verlag Berlin Heidelberg 2016 |
| abstractGer |
Abstract The water temperature regimes of the Yangtze River has changed a lot since the impoundment of the Three Gorges Reservoir (TGR), which lead to a significant effect on the water environment in the TGR. This paper focuses on the analysis of characteristics of water temperature regimes of the main stream in the TGR and the lagging effect of water temperature on temperature structure differences in six typical tributaries. The results showed that water temperature gradually decreased along the main stream and stratified position of water temperature was about 5–10 m arisen in estuaries of six tributaries in heating period. However, water temperature gradually increased along the main stream, and water temperature stratification of the six estuaries disappeared in cooling period. Annual vertical water temperature showed little change. After the impoundment of the TGR, the impact of water temperature is mainly reflected in lag characteristics. The monthly mean temperature difference significantly doubled, and the whole process of water temperature had been put off one month. Through further analyses, water temperature profile tends to be stable with the success of the TGR impounding to 175 m and contributes to water temperature differences in tributary, which is the main reason for water temperature structure changed from three layer to two layer gradually. © Springer-Verlag Berlin Heidelberg 2016 |
| abstract_unstemmed |
Abstract The water temperature regimes of the Yangtze River has changed a lot since the impoundment of the Three Gorges Reservoir (TGR), which lead to a significant effect on the water environment in the TGR. This paper focuses on the analysis of characteristics of water temperature regimes of the main stream in the TGR and the lagging effect of water temperature on temperature structure differences in six typical tributaries. The results showed that water temperature gradually decreased along the main stream and stratified position of water temperature was about 5–10 m arisen in estuaries of six tributaries in heating period. However, water temperature gradually increased along the main stream, and water temperature stratification of the six estuaries disappeared in cooling period. Annual vertical water temperature showed little change. After the impoundment of the TGR, the impact of water temperature is mainly reflected in lag characteristics. The monthly mean temperature difference significantly doubled, and the whole process of water temperature had been put off one month. Through further analyses, water temperature profile tends to be stable with the success of the TGR impounding to 175 m and contributes to water temperature differences in tributary, which is the main reason for water temperature structure changed from three layer to two layer gradually. © Springer-Verlag Berlin Heidelberg 2016 |
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| title_short |
Characteristic of the water temperature lag in Three Gorges Reservoir and its effect on the water temperature structure of tributaries |
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https://dx.doi.org/10.1007/s12665-016-6266-1 |
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Xu, Hui Ji, Dao-Bin Cui, Yu-Jie Liu, De-Fu Song, Lin-Xu |
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|
| score |
7.401865 |