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Name of the PET station
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Calculating the basin water balance without upland/floodplain routing
Calculating the basin water balance with upland/floodplain routing
All SWAT+ input files are free format and space delimited.
The first line in each input file is reserved for a title. If the files were written using the SWAT+ Editor, the title will specify the name of the file, the version of the SWAT+ Editor, and the date and time the file was written. While this line is required, it is not read in by SWAT+ and may be modified or left blank. The title is limited to 80 spaces.
The second line in all SWAT+ input files except for file.cio is reserved for the header, i.e. the names of the variables listed in the file. Some files will have additional header lines (e.g., print.prt).
Seibert and McDonnell (2002) suggested the use of “hard” and “soft” data for multi-criteria model calibration. Hard data are defined as measured time series, typically at a point (e.g., streamflow, groundwater levels, or soil moisture) that is commonly used in regression-based calibration techniques. Soft data are defined as information on individual processes within a balance that may not be directly measured in the study area, may be an average annual estimate, and may entail considerable uncertainty. Examples of soft data include regional estimates of baseflow ratios or ET, average depths of groundwater tables, average annual runoff coefficients for various land uses, annual rates of denitrification from research plots found in the literature, event mean concentrations, nutrient/sediment export coefficients, sediment deposition from reservoir sedimentation studies, average crop/vegetation LAI, and county crop yields (Arnold et al., 2015).
Seibert and McDonnell (2002) argued that soft data represent a new dimension to the model calibration process that could: (1) enable dialog between experimentalists and modelers, (2) be a formal check on the reasonableness and consistency of internal model structures and simulations, and (3) specify realistic parameter ranges often ignored in today’s automatic calibration routines.
Misrepresented processes (water balance, nutrient balance, sediment source/sinks) within a watershed can cause errors when running management scenarios (Arnold et al., 2015). To ensure proper process representation, a soft calibration routine for water balance was added to SWAT+ code. The processes calibrated are surface runoff, lateral soil flow, percolation, and ET. Tile flow variables are not adjusted, if subsurface tiles are present, tile flow is simulated as the remainder of the water balance when all other processes are calibrated. The processes are input as the ratio to precipitation, thus minimizing the impact of different periods of record or different sources of precipitation. The procedure is a simple, heuristic approach with one variable for each process. The variables, associated process, change type, change limits, and total limits are shown in the table below.
The algorithm uses one variable at a time in the following order: 1) esco, 2) petco, 3) cn3_swf, 4) latq_co, 5) perco, and 6) cn3_swf is calibrated again to ensure surface runoff is accurate. The first iteration with each variable is an initial guess calculated as shown in the table below. In each case, the initial change in each variable is a function of the difference (mm) in the soft ratio multiplied by precipitation minus the modeled process output. For example, if the surface runoff ratio input by the user is 0.2 and the simulated precipitation and surface runoff are 800 mm and 120 mm, respectively, the difference is 0.2*800 – 120 = 40 mm.
After the initial variable change, two additional iterations are performed using linear interpolation between the previous two simulations. Although the process response to the variable change is nonlinear, as the model iterates and approaches the soft data value, the linear interpolation is able it reasonably approximate the soft data. For the surface runoff example, with an initial difference of 40 mm, the next value of cn3_swf used in the calibration would be set to cn3_swf –0.4.
After the soft calibration is complete, the hard calibration of streamflow should only require some adjustments of the peaks and recessions.
Variable
Process
Change Type
Lower Change Limit
Upper Change Limit
Lower Limit
Upper Limit
esco
ET
absolute
-1.
1.
0.
1.
petco
PET
percent
-20.
20.
0.8
1.2
cn3_swf
Surface runoff
absolute
-1.
1.
0.
1.
latq_co
Lateral soil flow
absolute
-1.
1.
0.
1.
perco
Percolation
absolute
-0.7
0.7
0.
1.
Variable
Initial change
esco
(ETsoft – ETsim) / 500.
petco
(ETsoft – ETsim) / ETsoft
cn3_swf
-(SURQsoft – SURQsim) / 100.
latq_co
(LATQsoft – LATQsim) / 400.
perco
(PERCsoft – PERCsim) / 1000.
SWAT+ offers considerable flexibility with regard to the configuration of a watershed. The elements of a watershed are defined as spatial objects:
Landscape Unit
Routing Unit
HRU
Aquifer
Channel
Reservoir
Gravity-based exchange of water between spatial objects is defined in so-called connect files.
Over the past 20 years, the Soil and Water Assessment Tool (SWAT) has become widely used across the globe. Various applications of the model have revealed limitations and identified model development needs. Numerous additions and modifications of the model and its individual components have made the code increasingly difficult to manage and maintain. In response to these issues and in order to face present and future challenges in water resources modeling, the SWAT code has undergone major modifications over the past few years, resulting in SWAT+, a completely restructured version of the model. Even though the basic algorithms used to calculate the processes in the model have not changed, the structure and organization of both the code (object based) and the input files (relational based) have been modified significantly. This is expected to facilitate model maintenance, future code modifications, and foster collaboration with other researchers to integrate new science into SWAT modules. Additionally, SWAT+ provides a more flexible spatial representation of interactions and processes within a watershed.
SWAT was developed by USDA-ARS and Texas A&M scientists.
This file lists the names of all input files used in a simulation run. The files are grouped in different categories and there is one line for each category. The first column lists the names of the categories. The number of columns per line depends on the number of files in a category. Most files are required for all SWAT+ runs, i.e. they have to be listed in file.cio and the corresponding file has to be present in the TxtInOut folder of the SWAT+ project. There are also some optional files that are only required for specific SWAT+ applications. The category names and their files are listed below.
If a file is not being used for a SWAT+ application, 'null' should be entered instead of the filename.
constituents.cs
wind-dir.cli (currently not used)
gwflow.con (a description of the gwflow module and all related input files will be added asap)
aquifer2d.con (currently not used)
channel.con (currently not used)
channel.cha (currently not used)
hydrology.cha (currently not used)
sediment.cha (currently not used)
temperature.cha
rout_unit.dr (currently not used)
exco.exc
exco_om.exc
exco_pest.exc (currently not used)
exco_path.exc (currently not used)
exco_hmet.exc (currently not used)
exco_salt.exc (currently not used)
recall.rec
del_ratio.del (currently not used)
dr_om.del (currently not used)
dr_pest.del (currently not used)
dr_path.del (currently not used)
dr_hmet.del (currently not used)
dr_salt.del (currently not used)
The delivery ratio files will be removed in future versions of SWAT+.
animal.hrd (currently not used)
herd.hrd (currently not used)
ranch.hrd (currently not used)
There are no plans to work on the animal herd module in the foreseeable future unless there is a demand for it in the user community.
water_allocation.wro
The SWAT+ Water Allocation Module is work in progress and not fully functional in the current revision. A description of the general approach as well as input/output files will be added before the release of the next SWAT+ revision.
chan-surf.lin
aqu_cha.lin
pathogens.pth (currently not used)
metals.mtl (currently not used)
salt.slt (currently not used)
The salt routines are work in progress and will be added soon. However, there are no plans to work on the pathogen and metal routines in the foreseeable future unless there is a demand for it in the user community.
cal_parms.cal
calibration.cal
codes.sft
wb_parms.sft
water_balance.sft
ch_sed_budget.sft (currently not used)
ch_sed_parms.sft (currently not used)
plant_parms.sft
plant_gro.sft
om_water.ini
pest_hru.ini
pest_water.ini
path_hru.ini (currently not used)
path_water.ini (currently not used)
hmet_hru.ini (currently not used)
hmet_water.ini (currently not used)
salt_hru.ini (currently not used)
salt_water.ini (currently not used)
soils_lte.sol (currently not used)
res_rel.dtl
scen_lu.dtl
flo_con.dtl
ls_reg.ele
ls_reg.def
ls_cal.reg
ch_catunit.ele
ch_catunit.def
ch_reg.def
aqu_catunit.ele
aqu_catunit.def
aqu_reg.def
res_catunit.ele
res_catunit.def
res_reg.def
rec_catunit.ele
rec_catunit.def
rec_reg.def
The definition of regions in SWAT+ besides the Landscape Units will be revised in the near future and a description of the region files will be added to this documentation as soon as that has happened.
The last five rows in file.cio are used to specify the climate file directories if these are stored in a folder other than the project TxtInOut folder.
If the climate files are stored in the project TxtInOut folder, 'null' should be entered instead of the directory.
Arnold et al. 1998
Bieger et al. 2017
Bieger et al. 2019
Arnold et al. 2018
CARD database
A landscape unit is a collection of HRUs. A landscape units can be equivalent to a subbasin, a floodplain or upland unit, or a grid cell with multiple HRUs. Landscape units are only used for output. The landscape unit output files (water balance, nutrient balance, losses, and plant and weather) are output for HRUs, landscape units, and for the basin. Two input files are required: 1) landscape elements and, 2) landscape define. The elements file includes HRUs and their corresponding LSU fraction and basin fractions. The define file specifies which HRUs are contained in each LSU.
The routing unit is the spatial unit in SWAT+ that allows us to lump outputs and route them to any other spatial object. The routing unit can be configured as a subbasin, then total flow (surface, lateral and tile flow) from the routing unit can be sent to a channel and all recharge from the routing unit sent to an aquifer. This is analogous to the current approach in SWAT. However, SWAT+ gives us much more flexibility in configuring a routing unit. For example, in CEAP, we are routing each HRU (field) through a small channel (gully or grass waterway) before it reaches the main channel. In this case, the routing unit is a collection of flow from the small channels. We also envision simulating multiple representative hillslopes to define a routing unit. Also, we are setting up scenarios that define a routing unit using tile flow from multiple fields and sending that flow to a wetland. Routing units will continue to be a convenient way of spatial lumping until we can simulate individual fields or cells in each basin.
Beginning year of the simulation
If the simulation begins before the first day of the observed climate data, SWAT+ will use simulated climate data for the time period before the start of the observed climate data.
Ending day of the simulation
SWAT+ is able to end a simulation at any day of the year. This option can for example be useful, if the user wishes to simulate hydrological years instead of calendar years.
If day_end = 0, the model will end the simulation on December 31st.
If the simulation begins before the first day of the observed climate data, SWAT+ will use simulated climate data for the time period before the start of the observed climate data.
Beginning day of the simulation
SWAT+ is able to begin a simulation at any day of the year. This option can for example be useful, if the user wishes to simulate hydrological years instead of calendar years.
If day_start = 0, the model will start the simulation on January 1st.
If the simulation begins before the first day of the observed climate data, SWAT+ will use simulated climate data for the time period before the start of the observed climate data.
Ending year of the simulation
If the simulation ends after the last day of the observed climate data, SWAT+ will use simulated climate data for the time period after the end of the observed climate data.
This file specifies the land area and the total area (including ponds and reservoirs) of the watershed and the counts of all spatial objects in a simulation.
Field | Description | Type |
---|
This file controls the simulation time period and time step.
Field | Description | Type |
---|
name | Name of the watershed | string |
ls_area | Land area of the watershed in ha | real |
tot_area | Total area of the watershed in ha | real |
obj | Total number of spatial objects in the simulation | integer |
hru | Number of HRUs in the simulation | integer |
lhru | Number of HRU-ltes in the simulation | integer |
rtu | Number of routing units in the simulation | integer |
gwfl | Number of gwflow river cells | integer |
aqu | Number of aquifers in the simulation | integer |
cha | Currently not used | integer |
res | Number of reservoirs in the simulation | integer |
rec | Number of recalls (point sources/inlets) in the simulation | integer |
exco | Number of export coefficients in the simulation | integer |
dlr | Number of delivery ratios in the simulation | integer |
can | Currently not used | integer |
pmp | Currently not used | integer |
out | Number of outlets in the simulation | integer |
lcha | Number of channels in the simulation | integer |
aqu2d | Currently not used | integer |
hrd | Currently not used | integer |
wro | Currently not used | integer |
Print interval within the period
This parameter specifies the interval within the specified printing period.
Example: If interval = 2, output will be printed for every other day.
Number of years at the beginning of the simulation to not print output
Some simulations will need a warm-up or equilibration period. The use of a warm-up period becomes more important as the simulation period of interest shortens. For 30-year simulations, a warm-up period is optional. For a simulation covering 5 years or less, a warm-up period is recommended.
Examples: If nyskip = 2, the model will skip printing the first two years regardless of the starting year. If nyskip = 0, output for all years of the simulation will be printed. If nyskip equals the number of years in the simulation, no output will be printed.
Number of print intervals for average annual output
If aa_int_cnt = 0, the model will print average annual output for the entire period. If aa_int_cnt > 0, the end years of the print intervals have to be specified by the user by listing them in chronological order in the same line as aa_int_cnt.
Example: If aa_int_cnt = 3 1955 1965 1975, average annual results will be printed for the time periods ending in 1955, 1965, and 1975.
Name of the weather station
The name of the weather station is a primary key referenced by wst in 'object'.con.
Number of the object to print output for
Soil water contents of the soil layers can be printed for all HRUs in the same file by setting obj_typ_no = 0. For all other outputs, a separate object print record with a unique name has to be defined for each object.
Beginning day of the simulation | integer |
Beginning year of the simulation | integer |
Ending day of the simulation | integer |
Ending year of the simulation | integer |
Time step of the simulation | integer |
This file controls which output files will be printed during the simulation.
The print.prt file is formatted differently than most other SWAT+ input files (see figure below). In line three, there are several variables for controlling the time period to be printed. In line five, the user can specify the number of print intervals for average annual output. In line seven, the user can select to have output files printed in a specific file format (in addition to the default *.txt output files). In line 9, the user can control the printing of outputs for soils and management as well as flow duration curves. In lines 11 to 90, there is a list of outputs for different spatial levels and objects that can be printed at daily, monthly, yearly, and average annual time steps. A description of the output files is provided in the SWAT+ Output Files section.
Field | Description | Type |
---|---|---|
This file allows the user to print selected output for individual spatial objects.
The object.prt file is commonly used to:
Print daily channel outflow to compare to observed streamflow a stream gage
Print daily flow to a file that can be read in as a point source from another SWAT+ simulation
The only timestep output can be printed at using this file is daily. A description of the output files is provided in the SWAT+ Output Files section.
Field | Description | Type |
---|---|---|
Objects that output can be printed for at different time steps
The table below lists the objects that are listed in the first column of this section of the print.prt file. For each of these objects, output can be printed at daily, monthly, yearly, and average annual time steps by entering y (=yes) or n (=no) in the following four columns.
The user is advised to print only those outputs that are needed for model evaluation or further analysis. Especially daily printing can result in very large output files that may exceed hard drive storage.
Object | Definition |
---|---|
Type of object to print output for
Output can be printed for the following types of objects:
Object Code | Description |
---|---|
SWAT+ requires daily data for precipitation, maximum and minimum air temperature, solar radiation, relative humidity, and wind speed. The model can read in observed weather data or generate values using the weather generator. Climate data will be generated in two instances: when the user specifies that simulated weather data will be used or when there are missing values in the observed weather data. A Global Weather Generator Database containing weather generator datasets in SWAT+ format for almost 180,000 stations across the globe can be downloaded from the SWAT website: https://swat.tamu.edu/data/.
If observed data is used, one data file has to be provided for each station and variable. The data files for precipitation, temperature, solar radiation, relative humidity, and wind speed should have the file extensions .pcp, .tem, .slr, .hmd, and .wnd, respectively. The names of all available data files for precipitation, temperature, solar radiation, relative humidity, and wind speed will be listed in pcp.cli, tmp.cli, slr.cli, hmd.cli, and wnd.cli, respectively.
If the user wishes to run simulations at a sub-daily time step, precipitation data has to be provided at the simulation time step.
Each spatial object in a SWAT+ setup will be assigned the weather stations that are closest to its centroid. Because the precipitation, temperature, solar radiation, relative humidity, and wind speed stations might be at different locations, several combinations of weather stations might be needed for a SWAT+ setup. These combinations will be listed as a record in weather-sta.cli. Each of them will be given a unique name, which is referenced by the connect files for the different spatial objects. In addition, the name of the closest weather generator station will be specified, which points to weather-wgn.cli. Finally, the user has the option to specify the name of an atmospheric deposition record, which points to atmo.cli.
There is also a field available for specifying the name of a wind direction data file, but the wind direction routines in SWAT+ are currently not functional and there are no plans to work on them in the foreseeable future.
The flowchart below illustrates the relationships between the different SWAT+ climate files.
Type of hydrograph to print
The following hydrographs can be printed:
Hydrograph Code | Description | Object type |
---|---|---|
This file lists the weather stations defined for a SWAT+ setup.
Field | Description | Type |
---|---|---|
Hydrograph connections
This output file is used by the SWAT+ developers for debugging connectivity errors and infinite loops. Its usefulness for SWAT+ users is probably very limited. Accordingly, there is no description of this output file included in the section.
Name of the weather generator station
The name of the weather generator station is a foreign key referencing the primary key in .
Name of the precipitation station
The name of the precipitation station is a foreign key referencing the filenames listed in .
If "sim" is entered instead of a precipitation station name, the model will generate daily precipitation values using the weather generator station specified in column .
Name of the relative humidity station
The name of the relative humidity station is a foreign key referencing the filenames listed in .
If "sim" is entered instead of a relative humidity station name, the model will generate daily relative humidity values using the weather generator station specified in column .
0
day
2
12 hours
24
hour
96
15 minutes
1440
minute
id
ID of the object print record
integer
Type of object to print output for
string
Number of the object to print output for
integer
Type of hydrograph to print
string
filename
User-defined name of output file
string
basin_wb
Basin water balance
basin_nb
Basin nutrient balance
basin_ls
Basin losses
basin_pw
Basin plant and weather
basin_aqu
Basin aquifer
basin_res
Basin reservoir
basin_cha
Currently not used
basin_sd_cha
Basin SWAT-DEG channel
basin_psc
Basin point sources
region_wb
Currently not used
region_nb
Currently not used
region_ls
Currently not used
region_pw
Currently not used
region_aqu
Currently not used
region_res
Currently not used
region_sd_cha
Currently not used
region_psc
Currently not used
water_allo
Water allocation
lsunit_wb
Landscape unit water balance
lsunit_nb
Landscape unit nutrient balance
lsunit_ls
Landscape unit losses
lsunit_pw
Landscape unit plant and weather
hru_wb
HRU water balance
hru_nb
HRU nutrient balance
hru_ls
HRU losses
hru_pw
HRU plant and weather
hru-lte_wb
HRU-lte water balance
hru-lte_nb
Not used (no nutrient processes simulated for HRU-lte objects)
hru-lte_ls
HRU-lte losses
hru-lte_pw
HRU-lte plant and weather
channel
Currently not used
channel_sd
SWAT-DEG channel output
aquifer
Aquifer output
reservoir
Reservoir output
recall
Point source output
hyd
Incoming and outgoing hydrographs
ru
Routing unit output
pest
Pesticide output for all objects and basin
basin_salt
hru_salt
ru_salt
aqu_salt
channel_salt
res_salt
wetland_salt
basin_cs
hru_cs
ru_cs
aqu_cs
channel_cs
res_cs
wetland_cs
hru
HRU
hlt
HRU-lte
ru
Routing Unit
res
Reservoir
sdc
Channel
exc
Export Coefficient
dr
Delivery Ratio
out
Outlet
tot
Total flow
all
rhg
Percolation
hru, ru
sur
Surface runoff
hru, ru
lat
Lateral flow
hru, ru
til
Tiledrain flow
hru, ru
sol_water
Soil moisture
hru
solnut_ly
Soil nutrients (N and P) by layer
hru
solnut_pr
Soil nutrients (N and P) for entire profile
hru
plant
Plant status
hru
cha_fp
Channel and floodplain water balance
hru
Name of the weather station
string
Name of the weather generator station
string
Name of the precipitation station
string
Name of the temperature station
string
Name of the solar radiation station
string
Name of the relative humidity station
string
Name of the wind speed station
string
wnd_dir
Name of the wind direction station (currently not used)
string
Name of the atmospheric deposition station
string
Name of the atmospheric deposition station
The name of the atmospheric deposition station is a foreign key referencing the station names in atmo.cli.
If no atmospheric deposition data are available, "null" should be entered instead of an atmospheric deposition station name.
Name of the weather generator station
The name of the weather generator station is a primary key referenced by wgn in weather-sta.cli.
Name of the solar radiation station
Name of the temperature station
Number of years of maximum monthly 0.5 h rainfall data
This variable is used to calculate values for pcp_hhr.
If no value is specified, the model will set yrs_pcp = 10.
Number of years at the beginning of the simulation to not print output
integer
day_start
Julian day to start printing output (for daily printing only)
integer
yrc_start
Calendar year to start printing output
integer
day_end
Julian day to stop printing output (for daily printing only)
integer
yrc_end
Calendar year to stop printing output
integer
Print interval within the period
integer
Number of print intervals for average annual output
integer
csvout
Code for printing output in CSV format (y=yes, n=no)
string
dbout
Code for printing output in DB format (y=yes, n=no)
string
cdfout
Code for printing output in Net-CDF format (y=yes, n=no)
string
crop_yld
Code for printing yearly and average annual crop yields (y=yes, n=no)
string
mgtout
Code for printing management output (y=yes, n=no)
string
Code for printing hydrograph connection output (y=yes, n=no)
string
fdcout
Code for printing flow duration curve output (y=yes, n=no)
string
Objects that output can be printed for at different time steps
string
daily
Code for printing daily output (y=yes, n=no)
string
monthly
Code for printing monthly output (y=yes, n=no)
string
yearly
Code for printing yearly output (y=yes, n=no)
string
avann
Code for printing average annual output (y=yes, n=no)
string
Standard deviation for daily maximum air temperature in month
This parameter quantifies the variability in maximum temperature for each month. The standard deviation is calculated as
where is the standard deviation for daily maximum temperature in month (ºC), is the daily maximum temperature on day in month (ºC), is the average daily maximum temperature for the month (ºC), and is the total number of daily maximum temperature records for month .
Average or mean daily minimum air temperature for month
This value is calculated by summing the minimum air temperature for every day in the month for all years of record and dividing the sum by the number of days:
where is the mean daily minimum temperature for the month (ºC), is the daily minimum temperature on day in month (ºC), and is the total number of daily minimum temperature records for month .
Average or mean daily maximum air temperature for month
This value is calculated by summing the maximum air temperature for every day in the month for all years of record and dividing the sum by the number of days:
where is the mean daily maximum temperature for the month (ºC), is the daily maximum temperature on day in month (ºC), and is the total number of daily maximum temperature records for month .
Skew coefficient for daily precipitation in month
This parameter quantifies the symmetry of the precipitation distribution around the monthly mean. The skew coefficient is calculated as
where is the skew coefficient for precipitation in the month, is the total number of daily precipitation records for month , is the amount of precipitation for day in month (mm H2O), is the average precipitation for the month (mm H2O), and is the standard deviation for daily precipitation in month (mm H2O). Daily precipitation values of 0 mm are included in the skew coefficient calculation.
Standard deviation for daily precipitation in month
This parameter quantifies the variability in precipitation for each month. The standard deviation is calculated as
where is the standard deviation for daily precipitation in month (mm H2O), is the amount of precipitation for day in month (mm H2O), is the average precipitation for the month (mm H2O), and is the total number of daily precipitation records for month . Daily precipitation values of 0 mm are included in the standard deviation calculation.
This file contains weather generator data to be used for a SWAT+ setup.
The weather generator file contains weather generator data for any number of stations. For each weather generator station, there will be one line specifying the name of the station, its latitude, longitude, and elevation, and the number of years of maximum monthly 0.5 h rainfall data used to define values for . There are no headers for this line. These variables are listed in the first table below. The second line for each weather generator station contains the headers for the following 12 lines, which list the weather generator data for each month of the year. An overview of the weather generator data variables is given in the second table below.
A SWAT+ Global Weather Generator Database containing weather generator datasets for almost 180,000 stations across the globe can be downloaded from the SWAT website: .
If the user wishes to add a new weather generator station, the use of the WGN Parameters Estimation Tool or the WGN Excel macro is recommended. Both can be downloaded from the SWAT website: .
Field | Description | Type | Unit |
---|
Field | Description | Type | Unit | Range |
---|
Probability of a wet day following a wet day in the month
The probability is calculated as
where is the probability of a wet day following a wet day in month , is the number of times a wet day followed a wet day in month for the entire period of record, and is the number of wet days in month during the entire period of record. A wet day is a day with > 0 mm precipitation.
Average or mean total monthly precipitation
The average or mean total monthly precipitation is calculated as
where is the mean monthly precipitation (mm H2O), is the daily precipitation for day in month (mm H2O), is the total number of records in month used to calculate the average, and is the number of years of daily precipitation records used in calculation.
Standard deviation for daily minimum air temperature in month
This parameter quantifies the variability in minimum temperature for each month. The standard deviation is calculated as
where is the standard deviation for daily minimum temperature in month (ºC), is the daily minimum temperature on day in month (ºC), is the average daily minimum temperature for the month (ºC), and is the total number of daily minimum temperature records for month .
Average number of days of precipitation in month
This parameter is calculated as
where is the average number of days of precipitation in month , is the number of wet days in month during the entire period of record, and is the number of years of record.
Probability of a wet day following a dry day in the month
The probability is calculated as
where is the probability of a wet day following a dry day in month , is the number of times a wet day followed a dry day in month for the entire period of record, and is the number of dry days in month during the entire period of record. A dry day is a day with 0 mm of precipitation. A wet day is a day with > 0 mm precipitation.
Average daily dew point temperature for each month (ºC) or relative humidity (fraction)
If all twelve months are < 1.0, the model assumes the data provided is relative humidity. Relative humidity is defined as the amount of water vapor in the air as a fraction of saturation humidity. If any month has a value > 1.0, the model assumes the data provided is dewpoint temperature.
Dew point temperature is the temperature at which the actual vapor pressure present in the atmosphere is equal to the saturation vapor pressure. This value is calculated by summing the dew point temperature for every day in the month for all years of record and dividing the sum by the number of days:
where is the mean daily dew point temperature for the month (ºC), is the dew point temperature for day in month (ºC), and is the total number of daily dew point records for month . Please refer to the SWAT+ Theoretical Documentation for the equations used to convert dew point to relative humidity.
Average daily wind speed in month
This value is calculated by summing the average or mean wind speed values for every day in the month for all years of record and dividing the sum by the number of days:
where is the mean daily wind speed for the month (m/s), is the average wind speed for day in month (ºC), and N is the total number of daily wind speed records for month .
Number of months or years data is available for
For monthly and yearly data, the number of months and number of years of atmospheric deposition data included in the file should be entered, respectively. For average annual data this parameter should be set to 0.
Maximum 0.5-hour rainfall in month
This value represents the most extreme 30-minute rainfall intensity recorded in the entire period of record.
Average daily solar radiation for month
This value is calculated by summing the total solar radiation for every day in the month for all years of record and dividing the sum by the number of days:
where is the mean daily solar radiation for the month (MJ/m2/day), is the total solar radiation reaching the earth’s surface on day in month (MJ/m2/day), and is the total number of daily solar radiation records for month .
Name of weather generator station | string | n/a |
latitude | Latitude of weather generator station | real | Decimal Degrees |
longitude | Longitude of weather generator station | real | Decimal Degrees |
elevation | Elevation of weather generator station | real | m |
Number of years of maximum monthly 0.5 h rainfall data used to define values for pcp_hhr | integer | years |
Average or mean daily maximum air temperature for month | real | °C | -30 - 50 |
Average or mean daily minimum air temperature for month | real | °C | -40 - 40 |
Standard deviation for daily maximum air temperature in month | real | °C | 0.1 - 100 |
Standard deviation for daily minimum air temperature in month | real | °C | 0.1 - 30 |
Average or mean total monthly precipitation | real | mm | 0 - 600 |
Standard deviation for daily precipitation in month | real | mm/day | 0.1 - 50 |
Skew coefficient for daily precipitation in month | real | mm | -50 - 20 |
Probability of a wet day following a dry day in the month | real | n/a | 0 - 0.95 |
Probability of a wet day following a wet day in the month | real | n/a | 0 - 0.95 |
Average number of days of precipitation in month | real | n/a | 0 - 31 |
Maximum 0.5-hour rainfall in month | real | mm | 0 - 125 |
Average daily solar radiation for month | real | MJ/m^2/day | 0 - 750 |
Average daily dew point temperature for each month (ºC) or relative humidity (fraction) | real | °C or fraction | -50 - 25 |
Average daily wind speed in month | real | m/s | 0 - 100 |
These files contain all information needed by the model about observed temperature data.
The temperature data files contain the observed temperature input data. They are named by the user and must have the file ending *.tmp. There must be one file per station used in the simulation. As in all SWAT+ input files, the first line in the temperature data files is reserved for user comments. The second line contains the column headers for the third line, which lists basic information about the station.
Field | Description | Type | Unit |
---|---|---|---|
Starting in the fourth line, the year, Julian day, and the maximum and minimum temperatures are listed. There are no headers for these columns.
Field | Description | Type | Unit |
---|---|---|---|
A negative 99.0 (-99.0) should be inserted for missing data. This value tells SWAT+ to generate minimum and maximum temperatures for that day.
The tmp.cli file lists the names of the temperature data files used in the simulation. The first line is reserved for user comments. The second line is reserved for the column header "filename". The user can list as many temperature data file names as needed for the simulation. Only one file name should be listed per line. All file names listed in weather-sta.cli must be listed here. For every file name listed in tmp.cli, a file with that name must be provided by the user that contains the temperature data measured at the station.
These files contain all information needed by the model about observed precipitation data.
The precipitation data files contain the observed precipitation input data. They are named by the user and must have the file ending *.pcp. There must be one file per station used in the simulation. As in all SWAT+ input files, the first line in the precipitation data files is reserved for user comments. The second line contains the column headers for the third line, which lists basic information about the station.
Field | Description | Type | Unit |
---|---|---|---|
Starting in the fourth line, the year, Julian day, and precipitation amount are listed. There are no headers for these columns.
Field | Description | Type | Unit |
---|---|---|---|
If the user wishes to run simulations at a sub-daily time step, precipitation data has to be provided at the simulation time step. Currently, the model is able to run at an hourly time step. Smaller time steps have not been tested yet. Three additional columns need to be included in the hourly precipitation files:
Field | Description | Type | Unit |
---|---|---|---|
A negative 99.0 (-99.0) should be inserted for missing data. This value tells SWAT+ to generate precipitation for that day.
The pcp.cli file lists the names of the precipitation data files used in the simulation. The first line is reserved for user comments. The second line is reserved for the column header "filename". The user can list as many precipitation data file names as needed for the simulation. Only one file name should be listed per line. All file names listed in weather-sta.cli must be listed here. For every file name listed in pcp.cli, a file with that name must be provided by the user that contains the precipitation data measured at the station.
These files contain all information needed by the model about observed solar radiation data.
The solar radiation data files contain the observed precipitation input data. They are named by the user and must have the file ending *.slr. There must be one file per station used in the simulation. As in all SWAT+ input files, the first line in the solar radiation data files is reserved for user comments. The second line contains the column headers for the third line, which lists basic information about the station.
Field | Description | Type | Unit |
---|---|---|---|
Starting in the fourth line, the year, Julian day, and solar radiation are listed. There are no headers for these columns.
Field | Description | Type | Unit |
---|---|---|---|
A negative 99.0 (-99.0) should be inserted for missing data. This value tells SWAT+ to generate a solar radiation value for that day.
The slr.cli file lists the names of the solar radiation data files used in the simulation. The first line is reserved for user comments. The second line is reserved for the column header "filename". The user can list as many solar radiation data file names as needed for the simulation. Only one file name should be listed per line. All file names listed in weather-sta.cli must be listed here. For every file name listed in slr.cli, a file with that name must be provided by the user that contains the solar radiation data measured at the station.
These files contain all information needed by the model about observed wind speed data.
The wind speed data files contain the observed precipitation input data. They are named by the user and must have the file ending *.wnd. There must be one file per station used in the simulation. As in all SWAT+ input files, the first line in the wind speed data files is reserved for user comments. The second line contains the column headers for the third line, which lists basic information about the station.
Field | Description | Type | Unit |
---|---|---|---|
Starting in the fourth line, the year, Julian day, and wind speed are listed. There are no headers for these columns.
Field | Description | Type | Unit |
---|---|---|---|
A negative 99.0 (-99.0) should be inserted for missing data. This value tells SWAT+ to generate a wind speed value for that day.
The wnd.cli file lists the names of the wind speed data files used in the simulation. The first line is reserved for user comments. The second line is reserved for the column header "filename". The user can list as many wind speed data file names as needed for the simulation. Only one file name should be listed per line. All file names listed in weather-sta.cli must be listed here. For every file name listed in wnd.cli, a file with that name must be provided by the user that contains the wind speed data measured at the station.
Time step of the atmospheric deposition data
Option | Description |
---|---|
Potential evapotranspiration (PET) method
Numerous methods exist to calculate potential evapotranspiration. Three of the most widely-used ones are included in SWAT+, the Priestley-Taylor, Penman/Monteith, and Hargreaves equations. The codes for the three methods are listed in the table below. If a method other than Priestley-Taylor, Penman/Monteith, or Hargreaves is recommended for the area, in which the watershed is located, the user can calculate daily PET values with the recommended method and import them into SWAT+ (using pet in weather-sta.cli).
Code | Option |
---|---|
This file contains control codes for the simulation of basin-level processes.
Field | Description | Type |
---|---|---|
SWIFT input file
Code | Option |
---|---|
Channel water routing method
There are two channel water routing methods available in SWAT+:
Code | Option |
---|---|
The user must be careful to define msk_co1, msk_co2 and msk_x in parameters.bsn when the Muskingum method is chosen.
Plant stress
Code | Option |
---|
General watershed attributes are defined in two basin input files, and . These attributes control a diversity of physical processes at the watershed level. Users can use the default values set by the interfaces or change them to better reflect what is happening in a given watershed.
Even if nutrients are not being studied in a watershed, some attention must be paid to basin nutrient variables, because nutrient cycling impacts plant growth, which in turn affects the hydrologic cycle. Variables governing bacteria or pesticide transport need to be initialized only if these processes are being modeled in the watershed.
Carbon routine
Code | Option |
---|
Papers Xuesong, Armen
Crack flow code
Code | Option |
---|
If crack = 1, the crack volume potential is controlled by in .
Precipitation and temperature lapse rate control
Code | Option |
---|
These files contain all information needed by the model about observed relative humidity data.
The relative humidity data files contain the observed relative humidity input data. They are named by the user and must have the file ending *.hmd. There must be one file per station used in the simulation. As in all SWAT+ input files, the first line in the relative humidity data files is reserved for user comments. The second line contains the column headers for the third line, which lists basic information about the station.
Field | Description | Type | Unit |
---|
Starting in the fourth line, the year, Julian day, and the relative humidity are listed. There are no headers for these columns.
Field | Description | Type | Unit |
---|
A negative 99.0 (-99.0) should be inserted for missing data. This value tells SWAT+ to generate a relative humidity value for that day.
The hmd.cli file lists the names of the relative humidity data files used in the simulation. The first line is reserved for user comments. The second line is reserved for the column header "filename". The user can list as many relative humidity data file names as needed for the simulation. Only one file name should be listed per line. All file names listed in must be listed here. For every file name listed in hmd.cli, a file with that name must be provided by the user that contains the relative humidity data measured at the station.
nbyr
Length of the temperature time series
integer
years
tstep
Time step of the temperature data
integer
n/a
lat
Latitude of the temperature station
real
Decimal Degrees
lon
Longitude of the temperature station
real
Decimal Degrees
elev
Elevation of the temperature station
real
m
year
Year of the observation
integer
n/a
jday
Julian day of the observation
integer
n/a
tmpmax
Observed maximum temperature
real
°C
tmpmin
Observed minimum temperature
real
°C
nbyr
Length of the precipitation time series
integer
years
tstep
Time step of the precipitation data
integer
n/a
lat
Latitude of the precipitation station
real
Decimal Degrees
lon
Longitude of the precipitation station
real
Decimal Degrees
elev
Elevation of the precipitation station
real
m
year
Year of the observation
integer
n/a
jday
Julian day of the observation
integer
n/a
pcp
Observed precipitation
real
mm
year
Year of the observation
integer
n/a
jday
Julian day of the observation
integer
n/a
mon
Month of the observation
integer
n/a
day
Day of the observation
integer
n/a
hr
Time of the observation
integer
n/a
pcp
Observed precipitation
real
mm
nbyr
Length of the solar radiation time series
integer
years
tstep
Time step of the solar radiation data
integer
n/a
lat
Latitude of the solar radiation station
real
Decimal Degrees
lon
Longitude of the solar radiation station
real
Decimal Degrees
elev
Elevation of the solar radiation station
real
m
year
Year of the observation
integer
n/a
jday
Julian day of the observation
integer
n/a
slr
Observed solar radiation
real
MJ/m^2/day
nbyr
Length of the wind speed time series
integer
years
tstep
Time step of the wind speed data
integer
n/a
lat
Latitude of the wind speed station
real
Decimal Degrees
lon
Longitude of the wind speed station
real
Decimal Degrees
elev
Elevation of the wind speed station
real
m
year
Year of the observation
integer
n/a
jday
Julian day of the observation
integer
n/a
wnd
Observed wind speed
real
m/s
mo
Monthly
yr
Yearly
aa
Average annual
0
Priestley-Taylor method
1
Penman/Monteith method
2
Hargreaves method
pet_file
Currently not used
string
wq_file
Currently not used
string
Potential Evapotranspiration (PET) method
integer
event
Currently not used
integer
Crack flow
integer
Writing of input file for SWIFT
integer
sed_det
Currently not used
integer
Channel routing
integer
deg_cha
Currently not used
integer
wq_cha
Currently not used
integer
Turning off of plant stress
integer
cn
Currently not used
integer
c_fact
Currently not used
integer
Carbon routine
integer
Precipitation and temperature lapse rate control
integer
Unit Hydrograph method
integer
sed_cha
Currently not used
integer
Tile drainage equation code
integer
Water table depth algorithms
integer
Soil phosphorus model
integer
Surface runoff method
integer
atmo_dep
Currently not used
string
stor_max
Currently not used
integer
qual2e
Instream nutrient routing method
integer
Flood routing
integer
0
Do not write SWIFT input file
1
Write SWIFT input file (swift_hru.inp)
0
Variable Storage method
1
Muskingum method
0 | All plant stresses applied |
1 | Turn off all plant stress |
2 | Turn off nutrient plant stress only |
0 | Static soil carbon |
1 | C-FARM one carbon pool model |
2 | Century model |
0 | Do not adjust precipitation and temperature for elevation |
1 | Adjust precipitation and temperature for elevation |
0 | Do not compute crack flow in soil |
1 | Compute crack flow in soil |
nbyr | Length of the relative humidity time series | integer | years |
tstep | Time step of the relative humidity data | integer | n/a |
lat | Latitude of the relative humidity station | real | Decimal Degrees |
lon | Longitude of the relative humidity station | real | Decimal Degrees |
elev | Elevation of the relative humidity station | real | m |
year | Year of the observation | integer | n/a |
jday | Julian day of the observation | integer | n/a |
hmd | Observed relative humidity | real | fraction |
Surface runoff lag coefficient
In large routing units with a time of concentration greater than 1 day, only a portion of the surface runoff will reach the main channel on the day it is generated. SWAT+ incorporates a surface runoff storage feature to lag a portion of the surface runoff release to the main channel.
This parameter controls the fraction of the total available water that will be allowed to enter the reach on any one day. For a given time of concentration, as surq_lag decreases in value more water is held in storage. The delay in release of surface runoff will smooth the streamflow hydrograph simulated in the reach.
Initial soil water storage expressed as a fraction of field capacity water content
All soils in the watershed will be initialized to the same fraction. If sw_init = 0.0, the model will calculate it as a function of average annual precipitation.
We recommend using a warm-up period of at least 1 year, i.e. start the simulation at least 1 year prior to the period of interest. This allows the model to get the water cycling properly before any comparisons between measured and simulated data are made. If a warm-up period is incorporated, the value for sw_init will not impact model results.
Rate factor for humus mineralization of active organic nutrients (N and P)
Please refer to the Theoretical Documentation for a description of the use of this parameter in the mineralization calculations.
Nitrate percolation coefficient
This parameter controls the amount of nitrate removed from the surface layer in runoff relative to the amount removed via percolation.
The smaller n_perc, the lower the concentration of nitrate in runoff. If n_perc = 1.0, the surface runoff will have the same nitrate concentration as the percolate.
Peak rate adjustment factor for sediment routing in the subbasin (tributary channels)
Sediment routing is a function of peak flow rate and mean daily flow. Because SWAT originally could not directly calculate the sub-daily hydrograph due to the use of precipitation summarized on a daily basis, this variable was incorporated to allow adjustment for the effect of the peak flow rate on sediment routing. This factor is used in the MUSLE equation and impacts the amount of erosion generated in the HRUs.
Peak rate factor
Sediment routing is a function of peak flow rate and mean daily flow. Because SWAT originally could not directly calculate the sub-daily hydrograph, this variable was incorporated to allow adjustment for the effect of the peak flow rate on sediment routing. This variable impacts channel degradation.
Nitrogen uptake distribution parameter
Root density is greatest near the surface, and plant nitrogen uptake in the upper portion of the soil will be greater than in the lower portion. The depth distribution of nitrogen uptake is controlled by n_uptake, the nitrogen uptake distribution parameter.
The importance of the nitrogen uptake distribution parameter lies in its control over the maximum amount of nitrate removed from the upper layers. Because the top 10 mm of the soil profile interacts with surface runoff, the nitrogen uptake distribution parameter will influence the amount of nitrate available for transport in surface runoff. The model allows lower layers in the root zone to fully compensate for lack of nitrate in the upper layers, so there should not be significant changes in nitrogen stress with variation in the value used for n_uptake.
Residue decomposition coefficient
The fraction of residue that will decompose in a day assuming optimal moisture, temperature, C:N ratio, and C:P ratio.
Pesticide percolation coefficient
This parameter controls the amount of pesticide removed from the surface layer in runoff and lateral flow relative to the amount removed via percolation. This parameter is only important if pesticide transport is simulated.
The lower pest_perc, the lower the concentration of the pesticide in runoff. If pest_perc = 1.0, the surface runoff will have the same pesticide concentration as the percolate.
Phosphorus percolation coefficient
The phosphorus percolation coefficient is the ratio of the solution phosphorus concentration in the top 10 mm of soil to the concentration of phosphorus in the percolate.
Nitrogen concentration coefficient for tile flow and leaching from bottom layer
Weighting factor control relative importance of inflow rate and outflow rate in determining storage on reach
The weighting factor is a function of the wedge storage. This parameter is only important if channel routing is simulated using the Muskingum routing method.
For reservoir-type storage, there is no wedge and msk_x should be 0.0. For a full-wedge, msk_x should be 0.5. For rivers, msk_x will fall between 0.0 and 0.3 with a mean value near 0.2.
Instream nutrient routing method
Code | Option |
---|---|
Unit Hydrograph method
Code | Option |
---|---|
The Unit Hydrograph method is only relevant when simulating at a sub-daily timestep and gampt = 0.
Surface runoff method
Code | Option |
---|---|
Water table depth algorithm code
Code | Option |
---|---|
This file contains basin-level parameters.
Field | Description | Type | Unit | Default | Range |
---|---|---|---|---|---|
Tile drainage equation code
Code | Option |
---|---|
Papers Daniel, Tássia
Soil phosphorus model
Code | Option |
---|
Vadas & White (2010)
Phosphorus uptake distribution parameter
This parameter controls plant uptake of phosphorus from the different soil horizons in the same way that controls nitrogen uptake.
Phosphorus removed from the soil by plants is taken from the solution phosphorus pool. The importance of the phosphorus uptake distribution parameter lies in its control over the maximum amount of solution P removed from the upper layers. Because the top 10 mm of the soil profile interacts with surface runoff, the phosphorus uptake distribution parameter will influence the amount of labile phosphorus available for transport in surface runoff. The model allows lower layers in the root zone to fully compensate for lack of solution P in the upper layers, so there should not be significant changes in phosphorus stress with variation in the value used for p_uptake.
Flood routing
Code | Option |
---|
Phosphorus availability index
Many studies have shown that after an application of soluble P fertilizer, solution P concentration decreases rapidly with time due to reaction with the soil. This initial "fast" reaction is followed by a much slower decrease in solution P that may continue for several years (Barrow and Shaw, 1975; Munns and Fox, 1976; Rajan and Fox, 1972; Sharpley, 1982). In order to account for the initial rapid decrease in solution P, SWAT+ assumes a rapid equilibrium exists between solution P and an "active" mineral pool. The subsequent slow reaction is simulated by the slow equilibrium assumed to exist between the "active" and "stable" mineral pools. The algorithms governing movement of inorganic phosphorus between these three pools are taken from Jones et al. (1984).
Equilibration between the solution and active mineral pool is governed by the phosphorus availability index. This index specifies the fraction of fertilizer P which is in solution after an incubation period, i.e. after the rapid reaction period.
A number of methods have been developed to measure the phosphorus availability index. Jones et al. (1984) recommends a method outlined by Sharpley et al. (1984) in which various amounts of phosphorus are added in solution to the soil as K2HPO4. The soil is wetted to field capacity and then dried slowly at 25°C. When dry, the soil is rewetted with deionized water. The soil is exposed to several wetting and drying cycles over a 6-month incubation period. At the end of the incubation period, solution phosphorus is determined by extraction with anion exchange resin.
The P availability index is then calculated as:
where pai is the phosphorus availability index, is the amount of phosphorus in solution after fertilization and incubation, is the amount of phosphorus in solution before fertilization, and is the amount of soluble P fertilizer added to the sample.
Barrow, N.J. and T.C. Shaw. 1975. The slow reactions between soil and anions. 2. Effect of time and temperature on the decrease in phosphate concentration in soil solution. Soil Science 119(2): 167-177.
Jones et al. 1984
Munns and Fox. 1976
Rajan and Fox. 1972
Sharpley. 1982
Sharpley et al. 1984
0
Instream nutrient routing using QUAL2E
1
Instream nutrient routing using QUAL2E with simplified nutrient transformations
0
Triangular Unit Hydrograph
1
Gamma Function Unit Hydrograph
0
Curve Number
1
Green & Ampt
0
Simulate shallow water table using original water table depth routine (fill to upper limit)
1
Simulate shallow water table using DRAINMOD water table depth routine
lai_noevap
Currently not used
real
Initial soil water storage expressed as a fraction of field capacity water content
real
0
0-1
Surface runoff lag coefficient
real
4
1-24
Peak rate adjustment factor for sediment routing in the subbasin (tributary channels)
real
1
0.5-2
Peak rate adjustment factor for sediment routing in the main channel
real
1
0-2
lin_sed
Currently not used
real
exp_sed
Currently not used
real
Rate factor for humus mineralization of active organic nutrients (N and P)
real
0.0003
0.001-0.003
Nitrogen uptake distribution parameter
real
20
0-100
Phosphorus uptake distribution parameter
real
20
0-100
Nitrate percolation coefficient
real
0.2
0-1
Phosphorus percolation coefficient
real
10m^3/M
10
10-17.5
Phosphorus soil partitioning coefficient
real
m^3/Mg
175
100-200
Phosphorus availability index
real
0.4
0.01-0.7
Residue decomposition coefficient
real
0.05
0.02-0.1
Pesticide percolation coefficient
real
0.5
0-1
Coefficient to control the impact of the storage time constant for normal flow on the overall storage time constant for the channel
real
0.75
0-10
Coefficient to control the impact of the storage time constant for low flow on the overall storage time constant for the channel
real
0.25
0-10
Weighting factor control relative importance of inflow rate and outflow rate in determining storage on reach
real
0.2
0-0.3
Nitrogen concentration coefficient for tile flow and leaching from bottom layer
real
0
0-1
Reach evaporation adjustment factor
real
0.6
0.5-1
scoef
Currently not used
real
Denitrification exponential rate coefficient
real
1.4
0-3
Denitrification threshold water content
real
1.3
0-1
man_bact
Currently not used
real
Adjustment factor for subdaily unit hydrograph basetime
real
0
0-1
Parameter for frozen soil adjustment on infiltration/runoff
real
0.000862
0-0
Time threshold used to define dormancy
real
hrs
0
0-24
Precipitation lapse rate
real
mm/km
Temperature lapse rate
real
deg C/km
Maximum daily nitrogen fixation
real
kg/ha
20
1-20
Minimum daily residue decay
real
fraction
0.01
0-0.05
rsd_cover
Currently not used
real
Maximum initial abstraction for urban areas
real
5
0-10
petco_pmpt
Currently not used
real
Alpha coefficient for gamma function unit hydrograph
real
5
0.5-10
Splash erosion coefficient
real
1
0.9-3.1
Rill erosion coefficient
real
0.7
0.5-2
Exponential coefficient for overland flow
real
1.2
1-3
Scaling parameter for cover and management factor for overland flow erosion
real
0.03
0.001-0.45
cha_d50
Currently not used
real
CO2 concentration at start of simulation
real
ppm
1.57
1-5
day_lag_max
Currently not used
real
igen
Currently not used
integer
0
Simulate tile flow using drawdown days equation
1
Simulate tile flow using DRAINMOD equations
0 |
Original soil phosphorus model |
1 | New soil phosphorus model |
0 | GWFlow module not active |
1 | GWFlow module active |
Coefficient to control the impact of the storage time constant for low flow on the overall storage time constant for the channel
Normal flow is defined as the streamflow when the channel is at 0.1*bankfull depth. This parameter is only important if channel routing is simulated using the Muskingum routing method.
Phosphorus soil partitioning coefficient
The phosphorus soil partitioning coefficient p_soil is the ratio of the soluble phosphorus concentration in the top 10 mm of soil to the concentration of soluble phosphorus in surface runoff.
The primary mechanism of phosphorus movement in the soil is by diffusion. Diffusion is the migration of ions over small distances (1-2 mm) in the soil solution in response to a concentration gradient. Due to the low mobility of solution phosphorus, surface runoff will only partially interact with the solution P stored in the top 10 mm of soil.
Coefficient to control the impact of the storage time constant for normal flow on the overall storage time constant for the channel
Normal flow is defined as the streamflow when the channel is at bankfull depth. This parameter is only important if channel routing is simulated using the Muskingum routing method.
There are three files that control the settings for a simulation run:
object.cnt specifies the land area and the total area (including ponds and reservoirs) of the watershed and the counts of all spatial objects in a simulation,
time.sim controls the simulation time period and time step, and
print.prt controls which output files will be printed for a simulation.
An additional, optional file, object.prt, allows the user to print selected output for individual spatial objects.
This file contains observed atmospheric deposition data.
SWAT+ is able to read in monthly, yearly, and average annual atmospheric deposition values. Reading in daily values is currently not an option in SWAT+. The time step of the atmospheric deposition data has to be specified by the user in codes.bsn and the time step of the data in atmo.cli has to match the specified time step.
The structure of the file atmo.cli varies slightly depending on the time step of the data. As in all SWAT+ input files, the first line is reserved for user comments. The second line contains the column headers for the third line, which lists basic information about the atmospheric deposition stations.
Field | Description | Type |
---|---|---|
Below, there will be 5 lines for each station included in the atmospheric deposition file. In the first of these, the name of the station will be specified. It is followed by 4 lines of data:
Wet deposition of ammonia nitrogen
Wet deposition of nitrate nitrogen
Dry deposition of ammonia nitrogen
Dry deposition of nitrate nitrogen
The number of values listed in the data lines depends on the number of months or years data is available for.
num_sta
Number of stations included in the file
integer
Time step of the atmospheric deposition data
integer
mo_init
First month data is available for (0 for yearly and average annual data)
integer
yr_init
First year data is available for (0 for average annual data)
integer
Number of months or years data is available for
integer