Evapotranspiration estimation methods in hydrological models
Abstract Actual evapotranspiration is a key process of hydrological cycle and a sole term that links land surface water balance and land surface energy balance. Evapotranspiration plays a key role in simulating hydrological effect of climate change, and a review of evapotranspiration estimation meth...
Ausführliche Beschreibung
Autor*in: |
Zhao, Lingling [verfasserIn] |
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Format: |
Artikel |
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Sprache: |
Englisch |
Erschienen: |
2013 |
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Schlagwörter: |
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Anmerkung: |
© Science Press and Springer-Verlag Berlin Heidelberg 2013 |
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Übergeordnetes Werk: |
Enthalten in: Journal of geographical sciences - SP Science Press, 2001, 23(2013), 2 vom: 30. Jan., Seite 359-369 |
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Übergeordnetes Werk: |
volume:23 ; year:2013 ; number:2 ; day:30 ; month:01 ; pages:359-369 |
Links: |
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DOI / URN: |
10.1007/s11442-013-1015-9 |
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Katalog-ID: |
OLC2051260613 |
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520 | |a Abstract Actual evapotranspiration is a key process of hydrological cycle and a sole term that links land surface water balance and land surface energy balance. Evapotranspiration plays a key role in simulating hydrological effect of climate change, and a review of evapotranspiration estimation methods in hydrological models is of vital importance. This paper firstly summarizes the evapotranspiration estimation methods applied in hydrological models and then classifies them into the integrated converting methods and the classification gathering methods by their mechanism. Integrated converting methods are usually used in hydrological models and two differences exist among them: one is in the potential evaporation estimation methods, while the other in the function for defining relationship between potential evaporation and actual evapotranspiration. Due to the higher information requirements of the Penman-Monteith method and the existing data uncertainty, simplified empirical methods for calculating potential and actual evapotranspiration are widely used in hydrological models. Different evapotranspiration calculation methods are used depending on the complexity of the hydrological model, and importance and difficulty in the selection of the most suitable evapotranspiration methods is discussed. Finally, this paper points out the prospective development trends of the evapotranspiration estimating methods in hydrological modeling. | ||
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10.1007/s11442-013-1015-9 doi (DE-627)OLC2051260613 (DE-He213)s11442-013-1015-9-p DE-627 ger DE-627 rakwb eng 910 VZ 14 ssgn 74.00$jGeographie$jAnthropogeographie: Allgemeines bkl Zhao, Lingling verfasserin aut Evapotranspiration estimation methods in hydrological models 2013 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Science Press and Springer-Verlag Berlin Heidelberg 2013 Abstract Actual evapotranspiration is a key process of hydrological cycle and a sole term that links land surface water balance and land surface energy balance. Evapotranspiration plays a key role in simulating hydrological effect of climate change, and a review of evapotranspiration estimation methods in hydrological models is of vital importance. This paper firstly summarizes the evapotranspiration estimation methods applied in hydrological models and then classifies them into the integrated converting methods and the classification gathering methods by their mechanism. Integrated converting methods are usually used in hydrological models and two differences exist among them: one is in the potential evaporation estimation methods, while the other in the function for defining relationship between potential evaporation and actual evapotranspiration. Due to the higher information requirements of the Penman-Monteith method and the existing data uncertainty, simplified empirical methods for calculating potential and actual evapotranspiration are widely used in hydrological models. Different evapotranspiration calculation methods are used depending on the complexity of the hydrological model, and importance and difficulty in the selection of the most suitable evapotranspiration methods is discussed. Finally, this paper points out the prospective development trends of the evapotranspiration estimating methods in hydrological modeling. hydrological model actual evaporation potential evaporation function of soil moisture Xia, Jun aut Xu, Chong-yu aut Wang, Zhonggen aut Sobkowiak, Leszek aut Long, Cangrui aut Enthalten in Journal of geographical sciences SP Science Press, 2001 23(2013), 2 vom: 30. Jan., Seite 359-369 (DE-627)33352800X (DE-600)2055945-8 (DE-576)094642230 1009-637X nnns volume:23 year:2013 number:2 day:30 month:01 pages:359-369 https://doi.org/10.1007/s11442-013-1015-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-OAS SSG-OLC-MFO SSG-OPC-GGO GBV_ILN_40 GBV_ILN_4314 74.00$jGeographie$jAnthropogeographie: Allgemeines VZ 106417150 (DE-625)106417150 AR 23 2013 2 30 01 359-369 |
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Evapotranspiration estimation methods in hydrological models |
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Evapotranspiration estimation methods in hydrological models |
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Journal of geographical sciences |
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Zhao, Lingling Xia, Jun Xu, Chong-yu Wang, Zhonggen Sobkowiak, Leszek Long, Cangrui |
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evapotranspiration estimation methods in hydrological models |
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Evapotranspiration estimation methods in hydrological models |
abstract |
Abstract Actual evapotranspiration is a key process of hydrological cycle and a sole term that links land surface water balance and land surface energy balance. Evapotranspiration plays a key role in simulating hydrological effect of climate change, and a review of evapotranspiration estimation methods in hydrological models is of vital importance. This paper firstly summarizes the evapotranspiration estimation methods applied in hydrological models and then classifies them into the integrated converting methods and the classification gathering methods by their mechanism. Integrated converting methods are usually used in hydrological models and two differences exist among them: one is in the potential evaporation estimation methods, while the other in the function for defining relationship between potential evaporation and actual evapotranspiration. Due to the higher information requirements of the Penman-Monteith method and the existing data uncertainty, simplified empirical methods for calculating potential and actual evapotranspiration are widely used in hydrological models. Different evapotranspiration calculation methods are used depending on the complexity of the hydrological model, and importance and difficulty in the selection of the most suitable evapotranspiration methods is discussed. Finally, this paper points out the prospective development trends of the evapotranspiration estimating methods in hydrological modeling. © Science Press and Springer-Verlag Berlin Heidelberg 2013 |
abstractGer |
Abstract Actual evapotranspiration is a key process of hydrological cycle and a sole term that links land surface water balance and land surface energy balance. Evapotranspiration plays a key role in simulating hydrological effect of climate change, and a review of evapotranspiration estimation methods in hydrological models is of vital importance. This paper firstly summarizes the evapotranspiration estimation methods applied in hydrological models and then classifies them into the integrated converting methods and the classification gathering methods by their mechanism. Integrated converting methods are usually used in hydrological models and two differences exist among them: one is in the potential evaporation estimation methods, while the other in the function for defining relationship between potential evaporation and actual evapotranspiration. Due to the higher information requirements of the Penman-Monteith method and the existing data uncertainty, simplified empirical methods for calculating potential and actual evapotranspiration are widely used in hydrological models. Different evapotranspiration calculation methods are used depending on the complexity of the hydrological model, and importance and difficulty in the selection of the most suitable evapotranspiration methods is discussed. Finally, this paper points out the prospective development trends of the evapotranspiration estimating methods in hydrological modeling. © Science Press and Springer-Verlag Berlin Heidelberg 2013 |
abstract_unstemmed |
Abstract Actual evapotranspiration is a key process of hydrological cycle and a sole term that links land surface water balance and land surface energy balance. Evapotranspiration plays a key role in simulating hydrological effect of climate change, and a review of evapotranspiration estimation methods in hydrological models is of vital importance. This paper firstly summarizes the evapotranspiration estimation methods applied in hydrological models and then classifies them into the integrated converting methods and the classification gathering methods by their mechanism. Integrated converting methods are usually used in hydrological models and two differences exist among them: one is in the potential evaporation estimation methods, while the other in the function for defining relationship between potential evaporation and actual evapotranspiration. Due to the higher information requirements of the Penman-Monteith method and the existing data uncertainty, simplified empirical methods for calculating potential and actual evapotranspiration are widely used in hydrological models. Different evapotranspiration calculation methods are used depending on the complexity of the hydrological model, and importance and difficulty in the selection of the most suitable evapotranspiration methods is discussed. Finally, this paper points out the prospective development trends of the evapotranspiration estimating methods in hydrological modeling. © Science Press and Springer-Verlag Berlin Heidelberg 2013 |
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Evapotranspiration estimation methods in hydrological models |
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Xia, Jun Xu, Chong-yu Wang, Zhonggen Sobkowiak, Leszek Long, Cangrui |
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