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...e integer divisible into the groundwater model time-step. During rainfall events, the groundwater model time-step is temporarily changed to the overall mode :* ''Relaxation'' – The relaxation coefficient is used to project the current solution out into the future in an attempt to speed up convergence. A valu

...the stream, especially in ephemeral streams near the beginning of rainfall events, the flow direction is determined around each node and the locally upstream ...he channel, channel routing is halted during periods outside precipitation events. Fluxes between the stream and the groundwater are still computed and adju

...e top cell is equal to the depth of ponded water. The typical sequence of events is described below. ...flux, then all the water cannot infiltrate into the soil column during the current time step. In this case, water ponds on the soil surface and the upper bou

where ''z'' is the height to the cloud-base (km), fixed in the current formulation at 1.5 km. The molecular scattering coefficient, ''a'', is def The standard reference level, ''z'', is taken as 2 m. The current formulation does not explicitly calculate the leaf temperature of the veget

...tains the time in minutes since the beginning of the simulation for single events, the time in decimal years for continuous simulations, or the strict Julian A list of all the current overland point output capability is listed below:

...must be set up in order to run the basic model. GSSHAâ„¢ can run multiple events in long-term mode only, so for now we will set up a single rainfall event. ...HAâ„¢ Precipitation dialog is used to set up both uniform events and gaged events.]] <br>

...t the very bottom of page. We strongly suggest that users start using the current release version 7.13. ...hum, thanks David! This version has all the latest snow advancements, the current version of the permafrost modeling, cell blocking, depth varying overland r

...e top cell is equal to the depth of ponded water. The typical sequence of events is described below. ...flux, then all the water cannot infiltrate into the soil column during the current time step. In this case, water ponds on the soil surface and the upper bou

...e top cell is equal to the depth of ponded water. The typical sequence of events is described below. ...flux, then all the water cannot infiltrate into the soil column during the current time step. In this case, water ponds on the soil surface and the upper bou