Dear Peter,
we have to define in FeFlow the dimensionsless storativity S [-] which is defined as the depth integrated specific storativity SS, which has usually the unit [1/m].
What was the asumption not to define the specific storativity SS to the groundwater model ?
My question is therefore:
What must we assign to the Storativity:
The specific storativity multiplicated with the total depth of the groundwater body S = SS * M or
the specific storativity multiplicated SS with the depth of each layer representing the aquifer, because we assign the storativity for each model layer ?
Best regards Tubaheni
