Lake inflow dynamics can be affected by the thermal mediation provided by s
hallow littoral regions such as wetlands. In this study, wetland thermal me
diation is evaluated using a linearized dead-zone model. Its impact on lake
inflow dynamics is then assessed by applying the model sequentially to the
river reach, wetland, and lake. Our results suggest that littoral wetlands
can dramatically alter the inflow dynamics of reservoirs located in small
or forested watersheds, for example, by raising the temperature of the infl
ow during the summer and creating surface intrusions when a plunging inflow
would otherwise exist. Consequently, river-borne nutrients, contaminants,
and pathogens enter directly into the epilimnion, where they enhance eutrop
hication and the risk of human exposure. The addition of a littoral wetland
has less significant effects in larger watersheds, where the water has alr
eady equilibrated with the atmosphere upon reaching the wetland and sun sha
ding is less prominent.