Abstract. Gully-type debris flow induced by high-intensity and short-duration rainfall
frequently causes great loss of properties and causalities in mountainous
regions of southwest China. In order to reduce the risk by geohazards, early
warning systems have been provided. A triggering index can be detected in an
early stage by the monitoring of rainfall and the changes in physical
properties of the deposited materials along debris flow channels. Based on the
method of critical pore pressure for slope stability analysis, this study
presents critical pore pressure threshold in combination with rainfall
factors for gully-type debris flow early warning. The Wenjia gully, which
contains an enormous amount of loose material, was selected as a case study
to reveal the relationship between the rainfall and pore pressure by field
monitoring data. A three-level early warning system (zero, attention, and
warning) is adopted and the corresponding judgement conditions are defined in
real time. Based on this threshold, there are several rainfall events in
recent years have been validated in Wenjia gully, which prove that such a
combined threshold may be a reliable approach for the early warning of
gully-type debris flow to safeguard the population in the mountainous areas.