Abstract

The Yom River is subjected to flooding and drought for six months each year. Several studies suggested storing water during the rainy season for use in the dry season. None of them, however, quantified the precise amounts of storage needed along the river with acceptable risks. In an attempt to quantify the required storage, we performed frequency analyses to learn the severity of streamflow droughts along the river. A deficit volume, defined as when the amount of flow is less than a selected threshold level, was used to characterize a drought event. The Weibull distribution model was chosen for analysis after comparison of log normal and Pareto models with an empirical distribution. Results showed a more severe drought condition exists towards the downstream section of the river where paddy fields are larger. A large deep groundwater irrigation project located near the mid-section of the river mitigates drought along this section. Drought is more severe further downstream from the project. One reason for this is that the baseflow is cut off by groundwater abstraction. This method presented can help to quantify the severity of hydrological drought along any river so that drought management measures can be undertaken.

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