Variations in soil moisture conditions and their contributions to stream runoff during the snowmelt season

In a snowy mountain watershed, hillslope soil moisture becomes highest during the snowmelt season because of the continuous water input to the soil from the bottom of the snowpack. We call this water snowpack bottom outflow (SBO). This study evaluates the soil moisture conditions during the snowmelt...

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Veröffentlicht in:	Journal of Japanese Association of Hydrological Sciences 2019/04/26, Vol.49(1), pp.1-17
Hauptverfasser:	YANABA, Daisuke, ISHII, Yoshiyuki
Format:	Artikel
Sprache:	eng ; jpn
Schlagworte:	Basins Components Environmental risk Flooding Moisture content Outflow Ratios Rivers Runoff Seasons Snowmelt snowmelt runoff Snowpack Snowpack Bottom Outflow (SBO) Soil Soil conditions Soil moisture Soil water Soil Water Index (SWI) Storm seepage Stream discharge Subsurface flow Water outflow Watersheds
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