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Distribución espacial del índice de concentración de precipitación diaria en los Andes centrales peruanos: valle del rio Mantaro

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High percentages of the yearly total precipitation concentration in a few very rainy days can increase the potential of erosion, slope instability and risks of floods, these problems are common in Peru. So it is important to know about the daily precipitation. In this paper, an investigation of the...

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Detalles Bibliográficos
Autor: Zubieta y Cols., Ricardo
Formato: artículo
Fecha de Publicación:2019
Institución:Centro de Preparación para la Ciencia y Tecnología
Repositorio:ECIPERÚ
Lenguaje:español
OAI Identifier:oai:revistas.eciperu.net:article/181
Enlace del recurso:https://revistas.eciperu.net/index.php/ECIPERU/article/view/181
Nivel de acceso:acceso abierto
Materia:índice de concentración, precipitación diaria; curva exponencial; valle del rio Mantaro.
concentration index; daily precipitation; exponential curves; Mantaro river valley.
Descripción
Sumario:High percentages of the yearly total precipitation concentration in a few very rainy days can increase the potential of erosion, slope instability and risks of floods, these problems are common in Peru. So it is important to know about the daily precipitation. In this paper, an investigation of the spatial and temporal patterns of daily precipitation concentration, in central Andes of Perú, by Concentration index (CI) that evaluates the varying weight of daily precipitation, the contribution of the days of greatest rainfall to the total amount, is presented. The index is applied to exponential curves such as Y = aX exp(bX), which adjust the accumulated percentages of precipitation Y contributed by the accumulated percentage of days X on which it took place, in the period 1964-2004, with which it is possible to generate concentration surfaces daily pluviometric. The highest concentrations recorded in the Mantaro river valley, may be associated with the dynamics of the winds as the jet stream in South America, leading into the valley from the north and south, where 25% of rainy days account for 60% or more of the total number of days with rain.  
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