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首页> 外文期刊>The Kasetsart Journal >Estimation of Spatial and Temporal Reference Evapotranspiration in the Chao Phraya River Basin
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Estimation of Spatial and Temporal Reference Evapotranspiration in the Chao Phraya River Basin

机译:湄南河流域的时空参考蒸散量估算

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摘要

In the hydrological cycle and water use, evapotranspiration is one of the most important components because it represents a loss of usable water from the hydrologic supply. The purposes of this research are to calculate spatial and temporal reference evapotranspiration using FAO Penman-Monteith and Kriging methods and to determine the relationship between mean monthly temperature and monthly reference evapotranspiration. To achieve the first purpose, daily reference evapotranspiration from 1971 to 2002 was computed for each weather station using the FAO Penman-Monteith method. The average of monthly reference evapotranspiration in each weather station was figured. Thereafter, monthly reference evapotranspiration, that is point refererce evapotranspiration, was interpolated using the Kriging interpolation. The result of this calculation is spatial reference evapotranspiration or reference evapotranspiration map from January to December (temporal). After spatial and temporal reference evapotranspiration was calculated, the relationship between mean monthly temperature and mean monthly reference evapotranspiration was figured. The result shows that linear regression and polynomial analysis can be used to explain this relationship.
机译:在水文循环和用水中,蒸散量是最重要的组成部分之一,因为它代表了水文供应中可用水的损失。这项研究的目的是使用FAO Penman-Monteith和Kriging方法计算时空参考蒸散量,并确定平均每月温度与月参考蒸散量之间的关系。为了实现第一个目的,使用粮农组织的Penman-Monteith方法计算了每个气象站从1971年到2002年的每日参考蒸散量。计算每个气象站每月参考蒸散量的平均值。此后,使用克里格插值法对月参考蒸散量,即点参考蒸散量进行插值。此计算的结果是1月至12月(时间)的空间参考蒸散量或参考蒸散量图。在计算了时空参考蒸散量后,计算了平均每月温度与平均每月参考蒸散量之间的关系。结果表明,线性回归和多项式分析可以用来解释这种关系。

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