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Storage Routing links model the storage and movement of water through a length of river using a hydrologic routing method. Storage Routing links They can model represent the travel time of water through a reach, the attenuation of flow rates that can occur due to channel shape and roughness and reach processes (such as lateral fluxes). Reach processes include such things as . Examples of lateral fluxes include net evaporation from the water surface and exchanges between groundwater and surface water.
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- linear Muskingum routing,
- non-linear Muskingum routing (using a power function),
- variable parameter Muskingum routing
See the Link storage routing - SRG for a detailed description of storage routing.
Storage Routing links can also be configured to represent lag lagged flow , without attenuation (equivalent to a Lagged Flow link, ) but with the capacity to include lateral fluxes, see /wiki/spaces/SD540/pages/255100492.For detailed information, see Link storage routing - SRG.. See the Links user guide for how to configure the Storage Routing link to achieve this, and the Storage Routing Link SRG for information on the solution procedure.