Abstract:
he researchers used hydro-informatics methods to model and map flood risks in the Kafu
River catchment area. To improve flood preparedness, mitigation planning, and sustainable
watershed management, the study focused on identifying and analysing the main causes of
flooding, developing a comprehensive flood risk model, and ensuring its accuracy and
reliability. A multidisciplinary approach was adopted to accomplish these goals. Historical
river flow and rainfall data spanning 30 years (1993–2023) were collected and analysed to
assess rainfall trends and flood recurrence intervals. The research integrated modelling
techniques, geographic information systems, community surveys, and field-based data
collection in a mixed-method approach. Hydrological modelling was performed using HECHMS
software,
with
rainfall-runoff
relationships
developed
through
the
SCS
Unit
Hydrograph
method
for
direct
runoff
transformation
and
the
SCS
Curve
Number
method
for
loss
estimation.
Peak
flows
and
related
flood
depths
for
five
return
periods
were
simulated
by
calibrating
both
the
hydraulic model (HEC-RAS) and the hydrological model (HEC-HMS). Estimated peak
discharges for the 10-, 50-, 100-, 200-, and 500-year return periods were 203.26 m³/s, 281.02
m³/s, 313.90 m³/s, 346.66 m³/s, and 389.87 m³/s, respectively, based on the Gumbel
distribution. The maximum flood depths at the Kimengo cross-section near Kafu Bridge were
5.13 m, 6.34 m, 6.67 m, 7.13 m, and 7.46 m when these discharges were input into the HECRAS
model.
Statistical
analyses,
including
the
Chi-square
test
of
independence
and
flood
depth
comparisons,
confirmed
the
significant
relationship
between
flood
frequency
and
proximity
to
river
channels.
The
model's
ability
to
predict
flood
depths
was
validated
by
a
strong
correlation
(R²
> 0.90) between field data and simulated results. The study identified key factors
contributing to flooding as land use changes—particularly deforestation and wetland
encroachment—as well as heavy rainfall events and insufficient drainage infrastructure. Flood
risk maps highlighted the areas surrounding the main Kafu River channel and its primary
tributaries as most vulnerable to flooding. The findings demonstrated that combining GIS tools
with hydrological and hydraulic models offers a strong framework for flood risk assessment
and zoning. Overall, the developed model proved to be a valuable and reliable tool for flood
risk management within the Kafu catchment area. To reduce flood impacts, it was
recommended that local authorities and water resource managers prioritise flood-prone zones
in future land use and infrastructure planning, employ GIS-based flood risk frameworks, and
enhance community awareness.