This shows you the differences between two versions of the page.
Both sides previous revision Previous revision Next revision | Previous revision | ||
start:hype_model_description:hype_tracer [2023/04/27 10:09] cpers [Processes] |
start:hype_model_description:hype_tracer [2024/01/25 11:37] (current) |
||
---|---|---|---|
Line 229: | Line 229: | ||
==== Surface water processes ==== | ==== Surface water processes ==== | ||
- | River model option (add first) | + | === River model option === |
- | ----------------- | + | |
- | Temperature T2 of a river is not affected by point sources which not have T2 (''ps_t2'') set in PointSourceData. In this case the recieving main river flow will keep the temperature it had before adding of the point sources. | + | As default, temperature of the main river flow is affected by the temperature of water added to the river. Temperature T2 of a river is not affected by point sources which not have T2 (''ps_t2'') set in PointSourceData though. In this case the recieving main river flow will keep the temperature it had before adding of the point sources. |
- | In earlier HYPE versions, temperature T2 of a river was not affected by irrigation withdrawal, abstractions, rural households or point source additions, constructed wetlands, or water returning from aquifers. To get this old function of HYPE, there is a modeloption to use (modeloption rivert2model 1). | + | |
+ | In earlier HYPE versions, the temperature of the river was not affected by irrigation withdrawal, abstractions, rural households or point source additions, constructed wetlands, or water returning from aquifers. To get this older function of T2 in HYPE, there is a modeloption that can be set (modeloption rivert2model 1). | ||