start:hype_file_reference:info.txt
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start:hype_file_reference:info.txt [2023/11/22 18:19] cpers |
start:hype_file_reference:info.txt [2024/02/21 08:47] (current) cpers |
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| |''deepground''|//0/1/2//|defines which model to use for regional groundwater flow and aquifers. Default is none (0), alternative is a regional groundwater flow model without dedicated aquifer volumes (subsurface transfer between subcatchments) (1) and an aquifer model with dedicated regional aquifer volumes (2) (requires aquifer definition in input file [[start:hype_file_reference:AquiferData.txt|AquiferData.txt]]).| | |''deepground''|//0/1/2//|defines which model to use for regional groundwater flow and aquifers. Default is none (0), alternative is a regional groundwater flow model without dedicated aquifer volumes (subsurface transfer between subcatchments) (1) and an aquifer model with dedicated regional aquifer volumes (2) (requires aquifer definition in input file [[start:hype_file_reference:AquiferData.txt|AquiferData.txt]]).| | ||
| |''diffusesource''|//0/1//|defines how rural household diffuse source should be added to the soil. (0) as a flow (the locsoil part) with concentration, (1) as a load. See [[start:hype_file_reference:GeoData.txt|GeoData.txt]]| | |''diffusesource''|//0/1//|defines how rural household diffuse source should be added to the soil. (0) as a flow (the locsoil part) with concentration, (1) as a load. See [[start:hype_file_reference:GeoData.txt|GeoData.txt]]| | ||
| - | |''erosionmodel''|//0/1//|defines which soil erosion model to be used for simulation of suspended sediments. Default (0) is similar to erosion of PP (uses CropData), alternative (1) is based on HBV-sed.| | + | |''erosionmodel''|//0/1//|defines which soil erosion model to be used for simulation of sediments and phosphorus. Default (0) is based on MMF , alternative (1) is based on HBV-sed.| |
| |''floodmodel''|//0/1/2/3//|defines which model to use for floodplains. Default is none (0), alternatives are a simple model (1) and a model with soilroutines (2). A fourth option (3) is to use the model with soil routines and connecting floodplains. All requires floodplain information in input file [[start:hype_file_reference:FloodData.txt|FloodData.txt]]).| | |''floodmodel''|//0/1/2/3//|defines which model to use for floodplains. Default is none (0), alternatives are a simple model (1) and a model with soilroutines (2). A fourth option (3) is to use the model with soil routines and connecting floodplains. All requires floodplain information in input file [[start:hype_file_reference:FloodData.txt|FloodData.txt]]).| | ||
| |''frozensoil''|//0/1/2//|defines which frozen soil model to use. Default is none (0), the alternatives calculates frozen volume as a function of temperature with (1) one temperature per soil layer (2) temperature distribution within soil layer. Frozen soil model uses parameters 'logsatmp', 'bcosby' and 'fzsexpand'.| | |''frozensoil''|//0/1/2//|defines which frozen soil model to use. Default is none (0), the alternatives calculates frozen volume as a function of temperature with (1) one temperature per soil layer (2) temperature distribution within soil layer. Frozen soil model uses parameters 'logsatmp', 'bcosby' and 'fzsexpand'.| | ||
| |''glacierini''|//0/1//|defines if initialization from SLC+parameters overrides saved state of glacier volume (1). Default is to use saved state (0).| | |''glacierini''|//0/1//|defines if initialization from SLC+parameters overrides saved state of glacier volume (1). Default is to use saved state (0).| | ||
| - | |''growthstartmodel''|//0/1/2/3//|defines if varying start of the growth season should be used. Default (0) is no variation, then [[start:hype_file_reference:CropData.txt|CropData.txt]] constant parameter bd2 is used for nutrient uptake and plantday for irrigation. The alternatives are (1) to used varying growth season start for nutrient uptake, (2) to use varying growth season start for irrigation but not for nutrient uptake, and (3) to use varying growth season start for irrigation and nutrient uptake. For the alternatives the season start is calculated based on degreedays (equation defined by parameters in [[start:hype_file_reference:CropData.txt|CropData.txt]]).| | + | |''growthstartmodel''|//0/1/2/3/4//|defines if varying start of the growth season should be used. Default (0) is no variation, then [[start:hype_file_reference:CropData.txt|CropData.txt]] constant parameter //bd2// is used for nutrient uptake and plantday for irrigation. The alternatives are (1) to used varying growth season start (degree day method) for nutrient uptake, (2) to use varying growth season (degree day method) start for irrigation but not for nutrient uptake, (3) to use varying growth season start (degree day method) for irrigation and nutrient uptake, and (4) use varying growth season start (temperature threshold method) for irrigation and nutrient uptake. For all methods the season start is calculated based on parameters in [[start:hype_file_reference:CropData.txt|CropData.txt]].| |
| |''infiltration''|//0/1/2/3//|defines which infiltration model should be used. Default is the basic infiltration model of HYPE. For infiltration model 1 infiltration is limited by frozen soils. Infiltration model 2 is an alternative model where infiltration and percolation is added after runoff and evaporation is calculated. Model 3 is a combination of model 2 and 1.| | |''infiltration''|//0/1/2/3//|defines which infiltration model should be used. Default is the basic infiltration model of HYPE. For infiltration model 1 infiltration is limited by frozen soils. Infiltration model 2 is an alternative model where infiltration and percolation is added after runoff and evaporation is calculated. Model 3 is a combination of model 2 and 1.| | ||
| |''lakeriverice''|//0/1/2//|defines if ice on lakes and rivers should be simulated. Default is no (0), while a positive number means yes. The alternative models are (1) with temperature transfer between air and water and (2) with water surface heat balance. The ice calculations require that //substance// T2 (water temperature) is simulated.| | |''lakeriverice''|//0/1/2//|defines if ice on lakes and rivers should be simulated. Default is no (0), while a positive number means yes. The alternative models are (1) with temperature transfer between air and water and (2) with water surface heat balance. The ice calculations require that //substance// T2 (water temperature) is simulated.| | ||
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| |''snowdensity''|//0/1//|defines which snowdensity model to use. Default is snow age dependent snowdensity (0), and alternative is snow compactation snow density model (1).| | |''snowdensity''|//0/1//|defines which snowdensity model to use. Default is snow age dependent snowdensity (0), and alternative is snow compactation snow density model (1).| | ||
| |''snowevaporation''|//0/1//|defines if evaporation (sublimation) from snow and glaciers should be calculated. Default is off (0), and alternative is on (1). Snow and glacier evaporation is governed by the general parameters ‘fepotsnow’, ‘fepotglac’, and ‘fsceff’ in [[start:hype_file_reference:par.txt|par.txt]].| | |''snowevaporation''|//0/1//|defines if evaporation (sublimation) from snow and glaciers should be calculated. Default is off (0), and alternative is on (1). Snow and glacier evaporation is governed by the general parameters ‘fepotsnow’, ‘fepotglac’, and ‘fsceff’ in [[start:hype_file_reference:par.txt|par.txt]].| | ||
| - | |''snowfalldist''|//0/1/2//|defines which snowfall distribution model to use. Default is none (0), alternatives are scaling using linear (1) or log-linear (2) Winstrals coefficients (WSF). (3) snowfall distribution between subbasin as well as within (loglin WSF).| | + | |''snowfalldist''|//0/1/2/3/4//|defines which snowfall distribution model to use. Default is none (0), alternatives are scaling using linear (1) or log-linear (2) equation with Winstrals coefficients (WSF). (3) snowfall distribution to nearest downwind subbasin as well as within the subbasin (log-lin WSF). (4) snowfall distribution between subbasins within a distance range (log-lin WSF). | |
| |''snowfallmodel''|//0/1//|defines if an alternative snowfall model should be used. Default is threshold temperature (0), alternative is snowfall fraction from [[start:hype_file_reference:SFobs.txt|SFobs.txt]] (1).| | |''snowfallmodel''|//0/1//|defines if an alternative snowfall model should be used. Default is threshold temperature (0), alternative is snowfall fraction from [[start:hype_file_reference:SFobs.txt|SFobs.txt]] (1).| | ||
| |''snowheat''|//0/1//|defines if snow heat shall be calculated and used to limit snow melt. Default is no (0), and alternative is yes (1). Snow heat model uses parameters 'sdnsnew' and 'snkika'.| | |''snowheat''|//0/1//|defines if snow heat shall be calculated and used to limit snow melt. Default is no (0), and alternative is yes (1). Snow heat model uses parameters 'sdnsnew' and 'snkika'.| | ||
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| |''crit n''|''parameter''|//numeric//|parameter value used for RA-criteria coefficient value. See coefficient ''a'' in [[start:hype_file_reference:info.txt:criteria_equations#criteria_equations_for_a_time_series_of_a_station| RA equation definition]].| | |''crit n''|''parameter''|//numeric//|parameter value used for RA-criteria coefficient value. See coefficient ''a'' in [[start:hype_file_reference:info.txt:criteria_equations#criteria_equations_for_a_time_series_of_a_station| RA equation definition]].| | ||
| |''crit n''|''conditional''|//numeric//|parameter value. Only used for DEMC-calibration. The parameter value is the threshold for the criterion.| | |''crit n''|''conditional''|//numeric//|parameter value. Only used for DEMC-calibration. The parameter value is the threshold for the criterion.| | ||
| - | |''crit n''|''cgroup''|//name//|name of the classgroup for which the simulated variable to calculate criterion with is to be taken. Note observed variables can not be specified on classgroup level. Suitable variable can be defined as e.g. xom1.| | + | |''crit n''|''cgroup''|//name//|name of the classgroup for which the simulated and recorded variable represent.| |
| + | |''crit n''|''cgroupcomp''|//name//|name of the classgroup for which the simulated variable represent. The observed variables is specified separately.| | ||
| + | |''crit n''|''cgrouprec''|//name//|name of the classgroup for which the recorded variable represent. Note that if cgrouprec (or cgroup) is not given the basinwide variable will be used. In this cas, suitable variable can be defined as e.g. xom1.| | ||
| </sortable> | </sortable> | ||
start/hype_file_reference/info.txt.1700673595.txt.gz · Last modified: 2023/11/22 18:19 by cpers
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