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{\bf Figure captions}

\ni
{\sl Note:} If publishing in color is not possible we can make
color versions of figures available at:

\ni
{\sl http://www2.gis.uiuc.edu/papers/unesco99.html}


\bsn
{\sl Fig. 1 Monte Carlo solution of sediment transport equation
using increasing number of walkers: (a) sediment flow rate, (b) 
net erosion and deposition.

\bsn
Fig. 2 Terrain model with (a) traditional land use and
observed rills and gullies, (b) simulated sediment flow,
(c) erosion/deposition pattern for 70 mm/hr rainfall excess 
and bare soil in the agricultural field.

\bsn
Fig. 3 Terrain model with (a) observed depths of colluvial deposits,
(b) simulated sediment flow,
(c) erosion/deposition pattern for 20 mm/hr rainfall excess and
vegetative cover in the agricultural field.

\bsn
Fig. 4 Univariate and bivariate computation of net erosion and deposition
for transport capacity limiting case: (a) erosion/deposition as a change
 of 1D sediment flow along flow line:$ d |{\bf q_s}| / ds$, 
(b) erosion/deposition as a divergence of 2D vector field 
representing sediment flow:$ div {\bf q_s}$.

\bsn
Fig. 5 Terrain model with (a) computer designed land use,
(b) simulated sediment flow,
(c) erosion/deposition pattern for 70 mm/hr rainfall excess
and bare soil in the agricultural field.

\bsn
Fig. 6 Multi-scale simulation of steady state water depth:
(a)water depth at combined 10m and 2m resolution for the entire
study area, (b) targeted subarea at 10m resolution, (c) targeted
subarea at 2m resolution.}

\bye


