Modelación de la dinámica térmica de embalses mediterráneos. El caso del embalse de Amadorio (Alicante, España)

[EN] Water quality in lakes and reservoirs is influenced by several physical, chemical and biological processes. Among them, the thermal stratification cycle is one of the most influential factors. Increased water temperature leads to less solubility of oxygen and an increase in microbial activity....

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Detalles Bibliográficos
Autores: Paredes Arquiola, Javier|||0000-0003-3198-2169, Solera Solera, Abel|||0000-0001-7464-3963, Andreu Álvarez, Joaquín|||0000-0001-5087-5014, Rubio, Carolina
Tipo de recurso: artículo
Fecha de publicación:2013
País:España
Institución:Universitat Politècnica de València (UPV)
Repositorio:RiuNet. Repositorio Institucional de la Universitat Politécnica de Valéncia
Idioma:español
OAI Identifier:oai:riunet.upv.es:10251/59090
Acceso en línea:https://riunet.upv.es/handle/10251/59090
Access Level:acceso abierto
Palabra clave:Modelación de la calidad del agua
Embalses
Hidrodinámica
Temperatura del agua
Embalse Amadorio
INGENIERIA HIDRAULICA
Descripción
Sumario:[EN] Water quality in lakes and reservoirs is influenced by several physical, chemical and biological processes. Among them, the thermal stratification cycle is one of the most influential factors. Increased water temperature leads to less solubility of oxygen and an increase in microbial activity. Therefore, modeling is highly important to the study of water quality in lake and reservoirs. This study presents the use of the DYRESM hydrodynamic reservoir model to simulate the thermal structure of the Amadorio reservoir during a six-year period. The Amadorio reservoir is a typical Mediterranean reservoir with high summer releases. The calibration and sensitivity analyses developed demonstrate the importance of the method to calculate cloud cover and the extinction coefficient in the results of the model. Otherwise, in this case and considering what is usual, wind velocity is not one of the determinant factors. Finally it is demonstrated that turbulence processes generated by high summer releases lead to hypolimnion temperatures, which are difficult to model using this tool.