Currently infered hydrogeological parameters can be negative because depending on the data of streambed elevation and groundwater elevation, the difference between both can be positiv, which results in a negative parameter h_m and hence in a negative kf_value
Currently infered hydrogeological parameters can be negative because depending on the data of streambed elevation and groundwater elevation, the difference between both can be positiv, which results in a negative parameter
h_mand hence in a negativekf_value