Storm flows and Stream Morphology
Storm flows and Stream Morphology
Storm flows and Stream Morphology
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Non-l<strong>and</strong>use Factors Controlling <strong>Storm</strong>flow Response<br />
Shallower soils:<br />
These soils have lower water holding capacity<br />
<strong>and</strong> thus more discharge <strong>and</strong> higher peak<br />
<strong>flows</strong>.<br />
–Less water stored by soils, less water moved<br />
as baseflow, <strong>and</strong> more subsurface or surface<br />
as soils is saturated (Flashy).
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