Effects of a Proposed Hydraulic Project on the Hydrodynamics in the Poyang Lake Floodplain System, China.

Model simulations indicated that the resulting increase in water surface temperature was observed in the range of ~0.5 to ~1.5 °C for the majority of the lake regions, while a decreasing trend can be found in the catchment river inlets adjacent to the lake shoreline, with a maximum of around −2.0 °C ( Figure 10 a).

also in 47,180 other papers