Environmental and agricultural studies require spatial information on
the soil water table level. Data collection based on dip-well measurem
ents requires frequent measurements and a high number of dip-wells as
the soil water table depth is varying strongly within short distances
and time intervals. This paper presents a model based method, requirin
g a limited number of dip-wells and related mapped soil information, t
o describe water table depth fluctuations in time and space. A dip-wel
l specific, regressive model was developed with meteorological data as
input. This model described the fluctuations in time at the dip-well
locations successfully. Based on the relationship between model parame
ters and mapped soil data, spatially extended models were created.