Comparison of evapotranspiration variations between the Yellow River and Pearl River basin, China
Abstract Based on daily meteorological data at 43 gauging stations in the Pearl River basin and 65 gauging stations in the Yellow River basin, we analyze changing properties of actual evapotranspiration ($ ET_{a} $), reference evapotranspiration ($ ET_{ref} $) and precipitation in these two river ba...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Zhang, Qiang [verfasserIn] Xu, Chong-Yu [verfasserIn] Chen, Yongqin David [verfasserIn] Ren, Liliang [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2010 |
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| Schlagwörter: |
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| Übergeordnetes Werk: |
Enthalten in: Stochastic environmental research and risk assessment - Berlin : Springer, 1987, 25(2010), 2 vom: 08. Juli, Seite 139-150 |
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| Übergeordnetes Werk: |
volume:25 ; year:2010 ; number:2 ; day:08 ; month:07 ; pages:139-150 |
| Links: |
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| DOI / URN: |
10.1007/s00477-010-0428-6 |
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| Katalog-ID: |
SPR006400663 |
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| 520 | |a Abstract Based on daily meteorological data at 43 gauging stations in the Pearl River basin and 65 gauging stations in the Yellow River basin, we analyze changing properties of actual evapotranspiration ($ ET_{a} $), reference evapotranspiration ($ ET_{ref} $) and precipitation in these two river basins. In our study, Pearl River basin is taken as the ‘energy-limited’ system and the Yellow River basin as the ‘water-limited’ system. The results indicate decreasing $ ET_{a} $ in the Pearl River and Yellow River basin. However, different changing properties are detected for $ ET_{ref} $ when compared to $ ET_{a} $. The middle and upper Yellow River basin are characterized by increasing $ ET_{ref} $ values, whereas the Pearl River basin is dominated by decreasing $ ET_{ref} $ values. This result demonstrates enhancing drying force in the Yellow River basin. $ ET_{a} $ depends mainly on the changes of precipitation amount in the Yellow River basin. In the Pearl River basin, however, $ ET_{a} $ changes are similar to those of $ ET_{ref} $, i.e. both are in decreasing trend and which may imply weakening hydrological cycle in the Pearl River basin. Different influencing factors are identified behind the $ ET_{a} $ and $ ET_{ref} $ in the Pearl River and Yellow River basin: In the Pearl River basin, intensifying urbanization and increasing aerosol may contribute much to the evapotranspiration changes. Variations of precipitation amount may largely impact the spatial and temporal patterns of $ ET_{a} $ in the Yellow River basin. The current study is practically and scientifically significant for regional assessment of water resource in the arid and humid regions of China under the changing climate. | ||
| 650 | 4 | |a Reference evapotranspiration |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Actual evapotranspiration |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a The humid and arid regions |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Hydrological cycle |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a China |7 (dpeaa)DE-He213 | |
| 700 | 1 | |a Xu, Chong-Yu |e verfasserin |4 aut | |
| 700 | 1 | |a Chen, Yongqin David |e verfasserin |4 aut | |
| 700 | 1 | |a Ren, Liliang |e verfasserin |4 aut | |
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10.1007/s00477-010-0428-6 doi (DE-627)SPR006400663 (SPR)s00477-010-0428-6-e DE-627 ger DE-627 rakwb eng 550 ASE 43.03 bkl 58.50 bkl Zhang, Qiang verfasserin aut Comparison of evapotranspiration variations between the Yellow River and Pearl River basin, China 2010 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Based on daily meteorological data at 43 gauging stations in the Pearl River basin and 65 gauging stations in the Yellow River basin, we analyze changing properties of actual evapotranspiration ($ ET_{a} $), reference evapotranspiration ($ ET_{ref} $) and precipitation in these two river basins. In our study, Pearl River basin is taken as the ‘energy-limited’ system and the Yellow River basin as the ‘water-limited’ system. The results indicate decreasing $ ET_{a} $ in the Pearl River and Yellow River basin. However, different changing properties are detected for $ ET_{ref} $ when compared to $ ET_{a} $. The middle and upper Yellow River basin are characterized by increasing $ ET_{ref} $ values, whereas the Pearl River basin is dominated by decreasing $ ET_{ref} $ values. This result demonstrates enhancing drying force in the Yellow River basin. $ ET_{a} $ depends mainly on the changes of precipitation amount in the Yellow River basin. In the Pearl River basin, however, $ ET_{a} $ changes are similar to those of $ ET_{ref} $, i.e. both are in decreasing trend and which may imply weakening hydrological cycle in the Pearl River basin. Different influencing factors are identified behind the $ ET_{a} $ and $ ET_{ref} $ in the Pearl River and Yellow River basin: In the Pearl River basin, intensifying urbanization and increasing aerosol may contribute much to the evapotranspiration changes. Variations of precipitation amount may largely impact the spatial and temporal patterns of $ ET_{a} $ in the Yellow River basin. The current study is practically and scientifically significant for regional assessment of water resource in the arid and humid regions of China under the changing climate. Reference evapotranspiration (dpeaa)DE-He213 Actual evapotranspiration (dpeaa)DE-He213 The humid and arid regions (dpeaa)DE-He213 Hydrological cycle (dpeaa)DE-He213 China (dpeaa)DE-He213 Xu, Chong-Yu verfasserin aut Chen, Yongqin David verfasserin aut Ren, Liliang verfasserin aut Enthalten in Stochastic environmental research and risk assessment Berlin : Springer, 1987 25(2010), 2 vom: 08. Juli, Seite 139-150 (DE-627)27160235X (DE-600)1481263-0 1436-3259 nnns volume:25 year:2010 number:2 day:08 month:07 pages:139-150 https://dx.doi.org/10.1007/s00477-010-0428-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE 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_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_267 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_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_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4277 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 43.03 ASE 58.50 ASE AR 25 2010 2 08 07 139-150 |
| spelling |
10.1007/s00477-010-0428-6 doi (DE-627)SPR006400663 (SPR)s00477-010-0428-6-e DE-627 ger DE-627 rakwb eng 550 ASE 43.03 bkl 58.50 bkl Zhang, Qiang verfasserin aut Comparison of evapotranspiration variations between the Yellow River and Pearl River basin, China 2010 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Based on daily meteorological data at 43 gauging stations in the Pearl River basin and 65 gauging stations in the Yellow River basin, we analyze changing properties of actual evapotranspiration ($ ET_{a} $), reference evapotranspiration ($ ET_{ref} $) and precipitation in these two river basins. In our study, Pearl River basin is taken as the ‘energy-limited’ system and the Yellow River basin as the ‘water-limited’ system. The results indicate decreasing $ ET_{a} $ in the Pearl River and Yellow River basin. However, different changing properties are detected for $ ET_{ref} $ when compared to $ ET_{a} $. The middle and upper Yellow River basin are characterized by increasing $ ET_{ref} $ values, whereas the Pearl River basin is dominated by decreasing $ ET_{ref} $ values. This result demonstrates enhancing drying force in the Yellow River basin. $ ET_{a} $ depends mainly on the changes of precipitation amount in the Yellow River basin. In the Pearl River basin, however, $ ET_{a} $ changes are similar to those of $ ET_{ref} $, i.e. both are in decreasing trend and which may imply weakening hydrological cycle in the Pearl River basin. Different influencing factors are identified behind the $ ET_{a} $ and $ ET_{ref} $ in the Pearl River and Yellow River basin: In the Pearl River basin, intensifying urbanization and increasing aerosol may contribute much to the evapotranspiration changes. Variations of precipitation amount may largely impact the spatial and temporal patterns of $ ET_{a} $ in the Yellow River basin. The current study is practically and scientifically significant for regional assessment of water resource in the arid and humid regions of China under the changing climate. Reference evapotranspiration (dpeaa)DE-He213 Actual evapotranspiration (dpeaa)DE-He213 The humid and arid regions (dpeaa)DE-He213 Hydrological cycle (dpeaa)DE-He213 China (dpeaa)DE-He213 Xu, Chong-Yu verfasserin aut Chen, Yongqin David verfasserin aut Ren, Liliang verfasserin aut Enthalten in Stochastic environmental research and risk assessment Berlin : Springer, 1987 25(2010), 2 vom: 08. Juli, Seite 139-150 (DE-627)27160235X (DE-600)1481263-0 1436-3259 nnns volume:25 year:2010 number:2 day:08 month:07 pages:139-150 https://dx.doi.org/10.1007/s00477-010-0428-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE 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_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_267 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_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_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4277 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 43.03 ASE 58.50 ASE AR 25 2010 2 08 07 139-150 |
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10.1007/s00477-010-0428-6 doi (DE-627)SPR006400663 (SPR)s00477-010-0428-6-e DE-627 ger DE-627 rakwb eng 550 ASE 43.03 bkl 58.50 bkl Zhang, Qiang verfasserin aut Comparison of evapotranspiration variations between the Yellow River and Pearl River basin, China 2010 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Based on daily meteorological data at 43 gauging stations in the Pearl River basin and 65 gauging stations in the Yellow River basin, we analyze changing properties of actual evapotranspiration ($ ET_{a} $), reference evapotranspiration ($ ET_{ref} $) and precipitation in these two river basins. In our study, Pearl River basin is taken as the ‘energy-limited’ system and the Yellow River basin as the ‘water-limited’ system. The results indicate decreasing $ ET_{a} $ in the Pearl River and Yellow River basin. However, different changing properties are detected for $ ET_{ref} $ when compared to $ ET_{a} $. The middle and upper Yellow River basin are characterized by increasing $ ET_{ref} $ values, whereas the Pearl River basin is dominated by decreasing $ ET_{ref} $ values. This result demonstrates enhancing drying force in the Yellow River basin. $ ET_{a} $ depends mainly on the changes of precipitation amount in the Yellow River basin. In the Pearl River basin, however, $ ET_{a} $ changes are similar to those of $ ET_{ref} $, i.e. both are in decreasing trend and which may imply weakening hydrological cycle in the Pearl River basin. Different influencing factors are identified behind the $ ET_{a} $ and $ ET_{ref} $ in the Pearl River and Yellow River basin: In the Pearl River basin, intensifying urbanization and increasing aerosol may contribute much to the evapotranspiration changes. Variations of precipitation amount may largely impact the spatial and temporal patterns of $ ET_{a} $ in the Yellow River basin. The current study is practically and scientifically significant for regional assessment of water resource in the arid and humid regions of China under the changing climate. Reference evapotranspiration (dpeaa)DE-He213 Actual evapotranspiration (dpeaa)DE-He213 The humid and arid regions (dpeaa)DE-He213 Hydrological cycle (dpeaa)DE-He213 China (dpeaa)DE-He213 Xu, Chong-Yu verfasserin aut Chen, Yongqin David verfasserin aut Ren, Liliang verfasserin aut Enthalten in Stochastic environmental research and risk assessment Berlin : Springer, 1987 25(2010), 2 vom: 08. Juli, Seite 139-150 (DE-627)27160235X (DE-600)1481263-0 1436-3259 nnns volume:25 year:2010 number:2 day:08 month:07 pages:139-150 https://dx.doi.org/10.1007/s00477-010-0428-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE 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_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_267 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_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_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4277 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 43.03 ASE 58.50 ASE AR 25 2010 2 08 07 139-150 |
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10.1007/s00477-010-0428-6 doi (DE-627)SPR006400663 (SPR)s00477-010-0428-6-e DE-627 ger DE-627 rakwb eng 550 ASE 43.03 bkl 58.50 bkl Zhang, Qiang verfasserin aut Comparison of evapotranspiration variations between the Yellow River and Pearl River basin, China 2010 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Based on daily meteorological data at 43 gauging stations in the Pearl River basin and 65 gauging stations in the Yellow River basin, we analyze changing properties of actual evapotranspiration ($ ET_{a} $), reference evapotranspiration ($ ET_{ref} $) and precipitation in these two river basins. In our study, Pearl River basin is taken as the ‘energy-limited’ system and the Yellow River basin as the ‘water-limited’ system. The results indicate decreasing $ ET_{a} $ in the Pearl River and Yellow River basin. However, different changing properties are detected for $ ET_{ref} $ when compared to $ ET_{a} $. The middle and upper Yellow River basin are characterized by increasing $ ET_{ref} $ values, whereas the Pearl River basin is dominated by decreasing $ ET_{ref} $ values. This result demonstrates enhancing drying force in the Yellow River basin. $ ET_{a} $ depends mainly on the changes of precipitation amount in the Yellow River basin. In the Pearl River basin, however, $ ET_{a} $ changes are similar to those of $ ET_{ref} $, i.e. both are in decreasing trend and which may imply weakening hydrological cycle in the Pearl River basin. Different influencing factors are identified behind the $ ET_{a} $ and $ ET_{ref} $ in the Pearl River and Yellow River basin: In the Pearl River basin, intensifying urbanization and increasing aerosol may contribute much to the evapotranspiration changes. Variations of precipitation amount may largely impact the spatial and temporal patterns of $ ET_{a} $ in the Yellow River basin. The current study is practically and scientifically significant for regional assessment of water resource in the arid and humid regions of China under the changing climate. Reference evapotranspiration (dpeaa)DE-He213 Actual evapotranspiration (dpeaa)DE-He213 The humid and arid regions (dpeaa)DE-He213 Hydrological cycle (dpeaa)DE-He213 China (dpeaa)DE-He213 Xu, Chong-Yu verfasserin aut Chen, Yongqin David verfasserin aut Ren, Liliang verfasserin aut Enthalten in Stochastic environmental research and risk assessment Berlin : Springer, 1987 25(2010), 2 vom: 08. Juli, Seite 139-150 (DE-627)27160235X (DE-600)1481263-0 1436-3259 nnns volume:25 year:2010 number:2 day:08 month:07 pages:139-150 https://dx.doi.org/10.1007/s00477-010-0428-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE 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_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_267 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_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_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4277 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 43.03 ASE 58.50 ASE AR 25 2010 2 08 07 139-150 |
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10.1007/s00477-010-0428-6 doi (DE-627)SPR006400663 (SPR)s00477-010-0428-6-e DE-627 ger DE-627 rakwb eng 550 ASE 43.03 bkl 58.50 bkl Zhang, Qiang verfasserin aut Comparison of evapotranspiration variations between the Yellow River and Pearl River basin, China 2010 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Based on daily meteorological data at 43 gauging stations in the Pearl River basin and 65 gauging stations in the Yellow River basin, we analyze changing properties of actual evapotranspiration ($ ET_{a} $), reference evapotranspiration ($ ET_{ref} $) and precipitation in these two river basins. In our study, Pearl River basin is taken as the ‘energy-limited’ system and the Yellow River basin as the ‘water-limited’ system. The results indicate decreasing $ ET_{a} $ in the Pearl River and Yellow River basin. However, different changing properties are detected for $ ET_{ref} $ when compared to $ ET_{a} $. The middle and upper Yellow River basin are characterized by increasing $ ET_{ref} $ values, whereas the Pearl River basin is dominated by decreasing $ ET_{ref} $ values. This result demonstrates enhancing drying force in the Yellow River basin. $ ET_{a} $ depends mainly on the changes of precipitation amount in the Yellow River basin. In the Pearl River basin, however, $ ET_{a} $ changes are similar to those of $ ET_{ref} $, i.e. both are in decreasing trend and which may imply weakening hydrological cycle in the Pearl River basin. Different influencing factors are identified behind the $ ET_{a} $ and $ ET_{ref} $ in the Pearl River and Yellow River basin: In the Pearl River basin, intensifying urbanization and increasing aerosol may contribute much to the evapotranspiration changes. Variations of precipitation amount may largely impact the spatial and temporal patterns of $ ET_{a} $ in the Yellow River basin. The current study is practically and scientifically significant for regional assessment of water resource in the arid and humid regions of China under the changing climate. Reference evapotranspiration (dpeaa)DE-He213 Actual evapotranspiration (dpeaa)DE-He213 The humid and arid regions (dpeaa)DE-He213 Hydrological cycle (dpeaa)DE-He213 China (dpeaa)DE-He213 Xu, Chong-Yu verfasserin aut Chen, Yongqin David verfasserin aut Ren, Liliang verfasserin aut Enthalten in Stochastic environmental research and risk assessment Berlin : Springer, 1987 25(2010), 2 vom: 08. Juli, Seite 139-150 (DE-627)27160235X (DE-600)1481263-0 1436-3259 nnns volume:25 year:2010 number:2 day:08 month:07 pages:139-150 https://dx.doi.org/10.1007/s00477-010-0428-6 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE 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_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_267 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_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_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4277 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 43.03 ASE 58.50 ASE AR 25 2010 2 08 07 139-150 |
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Enthalten in Stochastic environmental research and risk assessment 25(2010), 2 vom: 08. Juli, Seite 139-150 volume:25 year:2010 number:2 day:08 month:07 pages:139-150 |
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Enthalten in Stochastic environmental research and risk assessment 25(2010), 2 vom: 08. Juli, Seite 139-150 volume:25 year:2010 number:2 day:08 month:07 pages:139-150 |
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Reference evapotranspiration Actual evapotranspiration The humid and arid regions Hydrological cycle China |
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Stochastic environmental research and risk assessment |
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Zhang, Qiang @@aut@@ Xu, Chong-Yu @@aut@@ Chen, Yongqin David @@aut@@ Ren, Liliang @@aut@@ |
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2010-07-08T00:00:00Z |
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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">SPR006400663</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20220110190415.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">201005s2010 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s00477-010-0428-6</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)SPR006400663</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(SPR)s00477-010-0428-6-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="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">ASE</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">43.03</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">58.50</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Zhang, Qiang</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Comparison of evapotranspiration variations between the Yellow River and Pearl River basin, China</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2010</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="520" ind1=" " ind2=" "><subfield code="a">Abstract Based on daily meteorological data at 43 gauging stations in the Pearl River basin and 65 gauging stations in the Yellow River basin, we analyze changing properties of actual evapotranspiration ($ ET_{a} $), reference evapotranspiration ($ ET_{ref} $) and precipitation in these two river basins. In our study, Pearl River basin is taken as the ‘energy-limited’ system and the Yellow River basin as the ‘water-limited’ system. The results indicate decreasing $ ET_{a} $ in the Pearl River and Yellow River basin. However, different changing properties are detected for $ ET_{ref} $ when compared to $ ET_{a} $. The middle and upper Yellow River basin are characterized by increasing $ ET_{ref} $ values, whereas the Pearl River basin is dominated by decreasing $ ET_{ref} $ values. This result demonstrates enhancing drying force in the Yellow River basin. $ ET_{a} $ depends mainly on the changes of precipitation amount in the Yellow River basin. In the Pearl River basin, however, $ ET_{a} $ changes are similar to those of $ ET_{ref} $, i.e. both are in decreasing trend and which may imply weakening hydrological cycle in the Pearl River basin. Different influencing factors are identified behind the $ ET_{a} $ and $ ET_{ref} $ in the Pearl River and Yellow River basin: In the Pearl River basin, intensifying urbanization and increasing aerosol may contribute much to the evapotranspiration changes. Variations of precipitation amount may largely impact the spatial and temporal patterns of $ ET_{a} $ in the Yellow River basin. The current study is practically and scientifically significant for regional assessment of water resource in the arid and humid regions of China under the changing climate.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Reference evapotranspiration</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Actual evapotranspiration</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">The humid and arid regions</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Hydrological cycle</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">China</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Xu, Chong-Yu</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Chen, Yongqin David</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Ren, Liliang</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Stochastic environmental research and risk assessment</subfield><subfield code="d">Berlin : Springer, 1987</subfield><subfield code="g">25(2010), 2 vom: 08. 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Zhang, Qiang |
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Zhang, Qiang ddc 550 bkl 43.03 bkl 58.50 misc Reference evapotranspiration misc Actual evapotranspiration misc The humid and arid regions misc Hydrological cycle misc China Comparison of evapotranspiration variations between the Yellow River and Pearl River basin, China |
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550 ASE 43.03 bkl 58.50 bkl Comparison of evapotranspiration variations between the Yellow River and Pearl River basin, China Reference evapotranspiration (dpeaa)DE-He213 Actual evapotranspiration (dpeaa)DE-He213 The humid and arid regions (dpeaa)DE-He213 Hydrological cycle (dpeaa)DE-He213 China (dpeaa)DE-He213 |
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ddc 550 bkl 43.03 bkl 58.50 misc Reference evapotranspiration misc Actual evapotranspiration misc The humid and arid regions misc Hydrological cycle misc China |
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comparison of evapotranspiration variations between the yellow river and pearl river basin, china |
| title_auth |
Comparison of evapotranspiration variations between the Yellow River and Pearl River basin, China |
| abstract |
Abstract Based on daily meteorological data at 43 gauging stations in the Pearl River basin and 65 gauging stations in the Yellow River basin, we analyze changing properties of actual evapotranspiration ($ ET_{a} $), reference evapotranspiration ($ ET_{ref} $) and precipitation in these two river basins. In our study, Pearl River basin is taken as the ‘energy-limited’ system and the Yellow River basin as the ‘water-limited’ system. The results indicate decreasing $ ET_{a} $ in the Pearl River and Yellow River basin. However, different changing properties are detected for $ ET_{ref} $ when compared to $ ET_{a} $. The middle and upper Yellow River basin are characterized by increasing $ ET_{ref} $ values, whereas the Pearl River basin is dominated by decreasing $ ET_{ref} $ values. This result demonstrates enhancing drying force in the Yellow River basin. $ ET_{a} $ depends mainly on the changes of precipitation amount in the Yellow River basin. In the Pearl River basin, however, $ ET_{a} $ changes are similar to those of $ ET_{ref} $, i.e. both are in decreasing trend and which may imply weakening hydrological cycle in the Pearl River basin. Different influencing factors are identified behind the $ ET_{a} $ and $ ET_{ref} $ in the Pearl River and Yellow River basin: In the Pearl River basin, intensifying urbanization and increasing aerosol may contribute much to the evapotranspiration changes. Variations of precipitation amount may largely impact the spatial and temporal patterns of $ ET_{a} $ in the Yellow River basin. The current study is practically and scientifically significant for regional assessment of water resource in the arid and humid regions of China under the changing climate. |
| abstractGer |
Abstract Based on daily meteorological data at 43 gauging stations in the Pearl River basin and 65 gauging stations in the Yellow River basin, we analyze changing properties of actual evapotranspiration ($ ET_{a} $), reference evapotranspiration ($ ET_{ref} $) and precipitation in these two river basins. In our study, Pearl River basin is taken as the ‘energy-limited’ system and the Yellow River basin as the ‘water-limited’ system. The results indicate decreasing $ ET_{a} $ in the Pearl River and Yellow River basin. However, different changing properties are detected for $ ET_{ref} $ when compared to $ ET_{a} $. The middle and upper Yellow River basin are characterized by increasing $ ET_{ref} $ values, whereas the Pearl River basin is dominated by decreasing $ ET_{ref} $ values. This result demonstrates enhancing drying force in the Yellow River basin. $ ET_{a} $ depends mainly on the changes of precipitation amount in the Yellow River basin. In the Pearl River basin, however, $ ET_{a} $ changes are similar to those of $ ET_{ref} $, i.e. both are in decreasing trend and which may imply weakening hydrological cycle in the Pearl River basin. Different influencing factors are identified behind the $ ET_{a} $ and $ ET_{ref} $ in the Pearl River and Yellow River basin: In the Pearl River basin, intensifying urbanization and increasing aerosol may contribute much to the evapotranspiration changes. Variations of precipitation amount may largely impact the spatial and temporal patterns of $ ET_{a} $ in the Yellow River basin. The current study is practically and scientifically significant for regional assessment of water resource in the arid and humid regions of China under the changing climate. |
| abstract_unstemmed |
Abstract Based on daily meteorological data at 43 gauging stations in the Pearl River basin and 65 gauging stations in the Yellow River basin, we analyze changing properties of actual evapotranspiration ($ ET_{a} $), reference evapotranspiration ($ ET_{ref} $) and precipitation in these two river basins. In our study, Pearl River basin is taken as the ‘energy-limited’ system and the Yellow River basin as the ‘water-limited’ system. The results indicate decreasing $ ET_{a} $ in the Pearl River and Yellow River basin. However, different changing properties are detected for $ ET_{ref} $ when compared to $ ET_{a} $. The middle and upper Yellow River basin are characterized by increasing $ ET_{ref} $ values, whereas the Pearl River basin is dominated by decreasing $ ET_{ref} $ values. This result demonstrates enhancing drying force in the Yellow River basin. $ ET_{a} $ depends mainly on the changes of precipitation amount in the Yellow River basin. In the Pearl River basin, however, $ ET_{a} $ changes are similar to those of $ ET_{ref} $, i.e. both are in decreasing trend and which may imply weakening hydrological cycle in the Pearl River basin. Different influencing factors are identified behind the $ ET_{a} $ and $ ET_{ref} $ in the Pearl River and Yellow River basin: In the Pearl River basin, intensifying urbanization and increasing aerosol may contribute much to the evapotranspiration changes. Variations of precipitation amount may largely impact the spatial and temporal patterns of $ ET_{a} $ in the Yellow River basin. The current study is practically and scientifically significant for regional assessment of water resource in the arid and humid regions of China under the changing climate. |
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| title_short |
Comparison of evapotranspiration variations between the Yellow River and Pearl River basin, China |
| url |
https://dx.doi.org/10.1007/s00477-010-0428-6 |
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Xu, Chong-Yu Chen, Yongqin David Ren, Liliang |
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2024-07-03T22:49:44.203Z |
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| score |
7.4011345 |