The application of numerical models of free surface flow to fluvial flood p
rediction is currently hampered by the lack of distributed calibration and
validation data. We address this shortcoming by the use of satellite-borne
synthetic aperture radar imagery to map a flood on a 15-km reach of the riv
er Thames, England. A finite element numerical model of shallow water flow
is constructed over the reach, and analysis shows that floodplain friction
is the dominant factor affecting inundation extent when compared to channel
friction, turbulence parameterization, and downstream boundary conditions.
The area of the domain correctly classified by the model is maximized with
the constraint of uniform floodplain friction (77% at maximum), compared w
ith 70% for a simple planar model of the water free surface. A simple distr
ibuted calibration scheme is also tested, with a minor improvement over the
uniform parameterization.