Hydrometeorological data, i.e. meteorological, water discharge and moisture
content data have been collected over the past 10 years in the Tone area o
f central Japan. By analyzing soil moisture data and by making inferences f
rom field studies, possible factors influencing stream discharge are explor
ed. The soil moisture data obtained from 40-cm depth carry the integrated e
ffect of the upstream catchment area and are important for estimating strea
m discharge. Vertical infiltration is important in the upper 2D-cm, due to
the high hydraulic conductivity of this part of forested soil. However, lat
eral flow through this layer becomes dominant during very high rainfall and
/or following a long succession of rainfall events, resulting in rapid thro
ughflow. A new type of artificial neural network (ANN) model based on a bac
k propagation algorithm is formulated using the analyses. The formulated AN
N model makes use of soil moisture data in estimating stream runoff and may
be considered useful as an aid to catchment monitoring. (C) 2000 Elsevier
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