grd.S: grd.S
In nexModeling/dddGroundwater: Groundwater in the hydrological model ddd

The function grd.S() computes the deficit S for all sub surface layers (not the overland flow layer)

1	grd.S(ddistx, X, ddist)

`ddistx`	distance distribution of each saturation level
`X`	excess water, scalar
`ddist`	states (in mm) of each saturation level

It follows the expression dS/dt = -dD/dt from Skaugen,Peerebom and Nilsson(2015)

The output is a scalar

## Not run: 
grd.S()

## End(Not run)

nexModeling/dddGroundwater documentation built on May 23, 2019, 4:28 p.m.

nexModeling/dddGroundwater index

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