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sheet flow

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sheet flow [′shēt‚flō]
(hydrology)
An overland flow or downslope movement of water taking the form of a thin, continuous film over relatively smooth soil or rock surfaces and not concentrated into channels larger than rills.


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In small depressions and upslope of rocks and plants, the soil moisture would linger longer than in areas where sheet flow went unchecked.
Anything that reduces friction between the ice and the ground, such as adding water, makes the ice sheet flow faster.
The objectives One of the earliest goals of CERP and one that dramatically exhibits the complications of the project, is to increase the overall sheet flow of the watershed into Florida Bay.
 
 
 
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