For a large river-type reservoir that is operating for hydroelectric benefits

the impact of its unique water temperature stratification on the water environment cannot be neglected. Most of the previous studies focus on the vertical variation in water temperature and its temporal evolution

lacking an in-depth examination on the hydrodynamic effect during its formation. This study uses mathematical models to simulate and examine the varying process of water temperature structure in the Wudongde reservoir

a typical river-type reservoir in the southwest region. We find that hydrodynamic conditions are the decisive factor in forming certain water temperature structures

and the formation and evolution of the main thermoclines depend on the hydrodynamic mechanism caused by thermal density flow. From February to March

the incoming water plunges into the reservoir bottom

forming a main thermocline at the interface between the two layers

and continuously developing as it advances further downstream at the bottom; From April to June

the inflow plunges down as an intermediate layer

with two thermocline layers formed at its upper and lower edges separately; In July

the inflow stays on the surface as an upward floating flow with a main thermocline below it. In the case of the water intakes

the dynamic suction effect of its orifices causes the main thermoclines to contract locally in certain areas near the dam.