Charlotta Pers

That is not a error message. HYPE simulated successfully. See for instance the post: https://sourceforge.net/p/hype/discussion/1818967/thread/34111166da/?limit=25#f210 /Lotta

HYPE version 5.35.0

HYPE version 5.35.0. Main changes: three soillayer evapotranspiration, inital soil water options, lake inflow output, concentrations of flow path output.

Hello, No, there is no storage for overflow due to infiltration capacity limit. It is added to the local river the same time step. The ssrcs parameter is only for determining the saturated surface flow. The saturated surface flow does not have a state of its own, but is calculated from the soil water of the uppermost soil layer. The water that become infoverflow on the other hand will not touch the soil water store, but be transfered directly to the river. /Lotta

Yes.

Hello, The unit of the rating curve equation is meter for lake water level (wlm) and threshold (lake_depth), the outflow is in cubic meter per second, and uparea is in square kilometer. In the introduction to HYPE we suggest that these parameters lie in the range gratk=1-100, gratp=1-2 (then grata=0). http://hype.smhi.net/wiki/doku.php?id=start:hype_tutorials:short_intro /Lotta

Hello, uparea refers to the upstream area of the outlet lake. It is total catchment area of all subcatchments upstream of the subcatchment that contains the olake. Parameter grata was first introduced to transfer rating parameters of an outlet lake to lakes in upstream areas when the catchment/lake was divided into several subbasins. /Lotta

HYPE version 5.34.0. Main change: layered lake model. Other changes: loadcrun work with wetlands, landuse dependent OC processes in soil, changed definition of wprodc parameter, OC in manure, additional indatachecks, improved reading of indata files and error messages. T2 bug fixes.