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• W1546800960 abstract "[1] In this study, the results of intensive soil moisture monitoring and analysis are reported in order to highlight the seasonal differences in hydrological processes on a hillslope scale. A soil monitoring system for a steep hillslope was designed and installed to monitor the temporal features of soil moisture with respect to the terrain attributes. Comparison of soil moisture analyses for two different periods, one during late autumn and the other during late spring, yielded different soil moisture characteristics, even though both seasons were subject to similar rainfall and saturation conditions. Comparative analyses indicated that soil moisture response patterns can be characterized and classified into three different zones. A substantial portion of the rainfall contributed to recharge of the water storage in autumn, while soil moisture responses were less variable during spring. Infiltration patterns between the two seasons were significantly different, hence the different distribution of soil moisture and hydrological responses. Vertical flux and recharge were the requirements for lateral redistribution of soil moisture in the study area. The seasonal impact of the vegetation, such as transpiration, fine root density, and interception, is apparent on the soil moisture distribution on the hillslope scale as well as runoff features in the mountainous forest catchment." @default.
• W1546800960 created "2016-06-24" @default.
• W1546800960 creator A5005487766 @default.
• W1546800960 date "2009-09-01" @default.
• W1546800960 modified "2023-09-27" @default.
• W1546800960 title "Characterization of soil moisture responses on a hillslope to sequential rainfall events during late autumn and spring" @default.
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• W1546800960 doi "https://doi.org/10.1029/2008wr007239" @default.
• W1546800960 hasPublicationYear "2009" @default.
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