The cross-validated calibration of Hargreaves-Samani evaporation model on lake most
Evaporation is one of the fundamental components of the water cycle in nature and affects almost all aspects of human society. Especially in the context of global climate change, understanding this process is increasingly important. However, the process itself is also very complex and is influenced...
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description | Evaporation is one of the fundamental components of the water cycle in nature and affects almost all aspects of human society. Especially in the context of global climate change, understanding this process is increasingly important. However, the process itself is also very complex and is influenced by many factors, making it very difficult to estimate its magnitude. As a benchmark, the Penman-Monteith equation is generally accepted, which estimates evaporation using air temperature, atmospheric pressure, wind speed, net radiation, changes in heat storage in water and others. Since measurements of these values may not always be available, many simplified methods have been proposed. In this paper, we consider the Hargreaves-Samani method and the calibration of its parameters by optimizing statistical measures against the Penman-Monteith equation. |
doi_str_mv | 10.1063/5.0212304 |
format | Conference Proceeding |
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Especially in the context of global climate change, understanding this process is increasingly important. However, the process itself is also very complex and is influenced by many factors, making it very difficult to estimate its magnitude. As a benchmark, the Penman-Monteith equation is generally accepted, which estimates evaporation using air temperature, atmospheric pressure, wind speed, net radiation, changes in heat storage in water and others. Since measurements of these values may not always be available, many simplified methods have been proposed. In this paper, we consider the Hargreaves-Samani method and the calibration of its parameters by optimizing statistical measures against the Penman-Monteith equation.</description><identifier>ISSN: 0094-243X</identifier><identifier>EISSN: 1551-7616</identifier><identifier>DOI: 10.1063/5.0212304</identifier><identifier>CODEN: APCPCS</identifier><language>eng</language><publisher>Melville: American Institute of Physics</publisher><subject>Air temperature ; Calibration ; Evaporation ; Heat storage ; Wind speed</subject><ispartof>AIP conference proceedings, 2024, Vol.3094 (1)</ispartof><rights>Author(s)</rights><rights>2024 Author(s). 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Especially in the context of global climate change, understanding this process is increasingly important. However, the process itself is also very complex and is influenced by many factors, making it very difficult to estimate its magnitude. As a benchmark, the Penman-Monteith equation is generally accepted, which estimates evaporation using air temperature, atmospheric pressure, wind speed, net radiation, changes in heat storage in water and others. Since measurements of these values may not always be available, many simplified methods have been proposed. In this paper, we consider the Hargreaves-Samani method and the calibration of its parameters by optimizing statistical measures against the Penman-Monteith equation.</description><subject>Air temperature</subject><subject>Calibration</subject><subject>Evaporation</subject><subject>Heat storage</subject><subject>Wind speed</subject><issn>0094-243X</issn><issn>1551-7616</issn><fulltext>true</fulltext><rsrctype>conference_proceeding</rsrctype><creationdate>2024</creationdate><recordtype>conference_proceeding</recordtype><recordid>eNotkM1LAzEQxYMoWD8O_gcL3oTUmXxt9ihFrVDw0ArewiRNdeu2uybbgv-9q-1p3gw_3hseYzcIYwQj7_UYBAoJ6oSNUGvkpUFzykYAleJCyfdzdpHzGkBUZWlHbL74jEVIbc58T029pD4uizAon6iv223RrooppY8UaR8zn9OGtnUR99S1R2DTLmNTDKKhrzhsub9iZytqcrw-zkv29vS4mEz57PX5ZfIw4x0q23Prhbcloa5QSQ2CrFUBCGWw5G1lyYjhAuAjGi8lrGIg8kjehGAwlPKS3R58u9R-72Lu3brdpe0Q6SQYrUylhBiouwOVQ93_v-y6VG8o_TgE91ea0-5YmvwFkmdeNg</recordid><startdate>20240607</startdate><enddate>20240607</enddate><creator>Dubovský, Viktor</creator><creator>Dlouhá, Dagmar</creator><creator>Pospíšil, Lukáš</creator><general>American Institute of Physics</general><scope>8FD</scope><scope>H8D</scope><scope>L7M</scope></search><sort><creationdate>20240607</creationdate><title>The cross-validated calibration of Hargreaves-Samani evaporation model on lake most</title><author>Dubovský, Viktor ; Dlouhá, Dagmar ; Pospíšil, Lukáš</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-p148t-8b2b87a159143502a884c0a13c8ab898a6288400be16b330fecaab1ab6cc61c73</frbrgroupid><rsrctype>conference_proceedings</rsrctype><prefilter>conference_proceedings</prefilter><language>eng</language><creationdate>2024</creationdate><topic>Air temperature</topic><topic>Calibration</topic><topic>Evaporation</topic><topic>Heat storage</topic><topic>Wind speed</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Dubovský, Viktor</creatorcontrib><creatorcontrib>Dlouhá, Dagmar</creatorcontrib><creatorcontrib>Pospíšil, Lukáš</creatorcontrib><collection>Technology Research Database</collection><collection>Aerospace Database</collection><collection>Advanced Technologies Database with Aerospace</collection></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Dubovský, Viktor</au><au>Dlouhá, Dagmar</au><au>Pospíšil, Lukáš</au><au>Tsitouras, Charalambos</au><au>Simos, Theodore</au><format>book</format><genre>proceeding</genre><ristype>CONF</ristype><atitle>The cross-validated calibration of Hargreaves-Samani evaporation model on lake most</atitle><btitle>AIP conference proceedings</btitle><date>2024-06-07</date><risdate>2024</risdate><volume>3094</volume><issue>1</issue><issn>0094-243X</issn><eissn>1551-7616</eissn><coden>APCPCS</coden><abstract>Evaporation is one of the fundamental components of the water cycle in nature and affects almost all aspects of human society. Especially in the context of global climate change, understanding this process is increasingly important. However, the process itself is also very complex and is influenced by many factors, making it very difficult to estimate its magnitude. As a benchmark, the Penman-Monteith equation is generally accepted, which estimates evaporation using air temperature, atmospheric pressure, wind speed, net radiation, changes in heat storage in water and others. Since measurements of these values may not always be available, many simplified methods have been proposed. In this paper, we consider the Hargreaves-Samani method and the calibration of its parameters by optimizing statistical measures against the Penman-Monteith equation.</abstract><cop>Melville</cop><pub>American Institute of Physics</pub><doi>10.1063/5.0212304</doi><tpages>4</tpages></addata></record> |
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subjects | Air temperature Calibration Evaporation Heat storage Wind speed |
title | The cross-validated calibration of Hargreaves-Samani evaporation model on lake most |
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