Climate and terrain factors explaining streamflow response and recession in Australian catchments
A. I. J. M. van Dijk
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Subject: Hillslope hydrology | Techniques and Approaches: Theory developmentSoil moisture: variable in space but redundant in timeAre dissolved organic carbon concentrations in riparian groundwater linked to hydrological pathways in the boreal forest?The influence of diurnal snowmelt and transpiration on hillslope throughflow and stream responseSlope–velocity equilibrium and evolution of surface roughness on a stony hillslope
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