The RIVMOD hydrodynamic model was used to route upstream flows through
a 115 km section of the Carson River and Lahontan Reservoir, Nevada.
RIVMOD results will later be used to predict sediment movement and ult
imately to determine mercury transport within the river/reservoir syst
em. Significant modifications to the model computer code were necessar
y to represent the narrow, steeply sloping rectangular channel and rel
atively shallow sloping floodplain of the Carson River and its conflue
nce with the Lahontan Reservoir, These changes include expansion of th
e continuity and momentum equations to account for rapidly changing ch
annel widths along with the characterization of a complex cross-sectio
nal shape. This modified version of the RIVMOD model can handle shallo
wer side slopes and much more severe flood flow simulations than the o
riginal version. A 0.25 km spatial increment was required in the zone
of confluence between the river and reservoir. Model predictions show
excellent agreement with observed downstream flow and reservoir stage
for the entire 1986 water year, which includes one of the most severe
flood events of recent record.