Variación de la evapotranspiración de referencia entre 1968 y 2018 en Córdoba (Argentina)bajo la influencia de la velocidad del viento y la amplitud térmica

Contenido principal del artículo

Antonio de la Casa
Gustavo Gabriel Ovando
Guillermo José Díaz

Resumen

Se analizó la diferencia entre la tasa diaria de evapotranspiración de referencia (ETo), que el método de Penman-Monteith (PM) calcula con el conjunto completo de variables meteorológicas y la obtenida utilizando solo registros térmicos y una velocidad superficial (u2) constante de 2 m s-1 (PMxn), empleando información meteorológica de las estaciones Río Cuarto Aero (RC), Marcos Juárez Aero (MJ), Pilar Observatorio (PI) y Villa Dolores Aero (VD) entre 1968 y 2018. La diferencia entre las tasas de ETo que resultan de PM y PMxn se incrementa de manera lineal con el aumento de u2, de modo que el empleo de PMxn debería estar restringido solo a lugares y días de menor u2. Los valores anuales de ETo obtenidos con ambos procedimientos exhiben una fluctuación entre 1968 y 2018, con valores decrecientes hasta la década de 1990, cuando la lluvia acusa registros máximos en la región; y crecientes desde entonces. Mientras la amplitud térmica (AT) en PI, MJ y RC muestra una fluctuación análoga a ETo, en MJ también u2 exhibe una fluctuación en fase con ETo, y en VD solo u2 presenta la variación de largo plazo concurrente a ETo. Únicamente RC mostró una tendencia lineal creciente de ETo.

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Variación de la evapotranspiración de referencia entre 1968 y 2018 en Córdoba (Argentina)bajo la influencia de la velocidad del viento y la amplitud térmica. (2022). AgriScientia, 39(1), 29-47. https://doi.org/10.31047/1668.298x.v39.n1.34573
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Variación de la evapotranspiración de referencia entre 1968 y 2018 en Córdoba (Argentina)bajo la influencia de la velocidad del viento y la amplitud térmica. (2022). AgriScientia, 39(1), 29-47. https://doi.org/10.31047/1668.298x.v39.n1.34573

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