4.6 Article

Characteristics and Controlling Factors of the Drought Runoff Coefficient

Journal

WATER
Volume 13, Issue 9, Pages -

Publisher

MDPI
DOI: 10.3390/w13091259

Keywords

drought; geology; land use; topography; occurrence probability; water resource management

Funding

  1. JSPS KAKENHI [JP19H02250]

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This study highlights the importance of understanding the relationship between low-flow conditions and controlling factors in order to establish sustainable water resource management based on future drought risk. The research demonstrates the variation in drought runoff coefficient under different severities of drought and identifies the different controlling factors depending on the magnitude of the drought. Effective water resource management requires consideration of precipitation patterns, geology, land use, and topography when estimating the volume of drought runoff.
Increasing water demand due to population growth, economic development, and changes in rainfall patterns due to climate change are likely to alter the duration and magnitude of droughts. Understanding the relationship between low-flow conditions and controlling factors relative to the magnitude of a drought is important for establishing sustainable water resource management based on changes in future drought risk. This study demonstrates the relationship between low-flow and controlling factors under different severities of drought. I calculated the drought runoff coefficient for six types of occurrence probability, using past observation data of annual total discharge and precipitation in the Japanese archipelago, where multiple climate zones exist. Furthermore, I investigated the pattern of change in the drought runoff coefficient in accordance with the probability of occurrence of drought, and relationships among the coefficient and geological, land use, and topographical factors. The drought runoff coefficient for multiple drought magnitudes exhibited three behaviors, corresponding to the pattern of precipitation. Results from a generalized linear model (GLM) revealed that the controlling factors differed depending on the magnitude of the drought. During high-frequency droughts, the drought runoff coefficient was influenced by geological and vegetation factors, whereas land use and topographical factors influenced the drought runoff coefficient during low-frequency droughts. These differences were caused by differences in runoff, which dominated stream discharge, depending on the magnitude of the drought. Therefore, for effective water resource management, estimation of the volume of drought runoff needs to consider the pattern of precipitation, geology, land use, and topography.

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