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The influence of elevated atmospheric CO₂ (eCO₂), particularly under future scenarios exceeding 660 ppm, presents a critical uncertainty in modeling the water-food nexus. eCO₂ affects both plant physiology (e.g., stomatal conductance, transpiration, biomass accumulation) and hydrological processes (e.g., evapotranspiration, runoff generation), making its integration into modeling frameworks increasingly important.
I am currently exploring which hydrological and crop growth models are capable of incorporating eCO₂ effects, and to what extent they represent the associated physiological and hydrological mechanisms. Moreover, I am interested in understanding the complexity of these models in terms of how CO₂ response functions are embedded in their algorithms and equations.
Could you recommend hydrologic and crop models that can simulate eCO₂ impacts realistically? How do these models differ in their assumptions, parameterization, and overall representation of CO₂-driven processes?
Your insights, experiences, and any relevant literature would be greatly appreciated.
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Rising atmospheric CO₂ concentrations (eCO₂), particularly in projections forecasting levels exceeding 660 ppm in the coming decades, represent a significant source of uncertainty in modeling the interconnections between water and food systems. eCO₂ directly affects plant physiology—primarily stomatal conductance, transpiration, photosynthesis, and biomass accumulation—and indirectly influences hydrological processes, including evapotranspiration, soil water balance, and surface runoff generation. Therefore, integrating these effects into models is essential for reliable planning under climate change conditions.
Currently available models vary in terms of complexity, the way CO₂ response functions are implemented, and the assumptions on which they are based. Among the models that allow for realistic simulation of eCO₂ effects, the following stand out:
  • APSIM (Agricultural Production Systems sIMulator) – A mechanistic model that simulates crop growth processes in detail under elevated CO₂ conditions, including changes in stomatal behavior and water use efficiency (WUE). It is well-suited for precise plot- and region-scale studies.
  • DSSAT (Decision Support System for Agrotechnology Transfer) – A widely used model that applies empirical functions to simulate the effects of CO₂ on photosynthesis and transpiration. Although somewhat simplified compared to APSIM, it provides valuable insights into crop productivity under various climate scenarios.
  • SWAT (Soil and Water Assessment Tool) – A hydrological model that incorporates CO₂ effects through adjusted coefficients for plant growth and transpiration. However, it relies on fixed, empirical approaches and does not simulate physiological responses of plants dynamically.
  • LPJmL (Lund–Potsdam–Jena managed Land model) – A dynamic global model for land and vegetation management, integrating biogeophysical processes and explicitly simulating the effects of eCO₂ on productivity, evapotranspiration, and water fluxes.
These models differ across key parameters: assumptions (empirical vs. mechanistic functions), parameterization (based on FACE experiment data or localized calibration), and model complexity (number of required inputs, temporal and spatial resolution).
From my research experience and review of relevant literature, I believe the most realistic approaches arise from combining agrometeorological and hydrological models (e.g., APSIM + SWAT), which allow for multiscale analysis—from plant level to watershed scale. However, it is crucial that simulations are always supported by experimental data, particularly from FACE (Free-Air CO₂ Enrichment) studies, to avoid errors arising from over-reliance on unvalidated empirical coefficients.
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I am working on enhancing the SWAT+ model for my PhD research and need to modify its source code. Could anyone suggest:
  1. Tutorials or documentation for understanding and editing the source code?
  2. Tips or tools for compiling and testing changes?
  3. How much knowledge of Fortran is required for this task? Are there any recommended Fortran tutorials tailored to such purposes?
Any guidance would be greatly appreciated. Thank you!
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Finishing last message. If you’re interested in our online version of Svat that can be downloaded. please contact me at tnc@psu.edu. All lowercase.
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My research is on the impact of climate change on soil moisture dynamics in forest and grassland areas using the SWAT model. I need someone grounded in this area to mentor me. I am also open to collaborations and coauthoring. I tried using Hydrus-1D but it was a bit complicated and so I want to explore the SWAT model.
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Thanks for your timely response Prof. Carlson. I shall communicate with you via email.
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I have calibrated my SWAT model with monthly observed flow data, and the NSE coefficient is as high as 0.85 at monthly scale, while when I plot a FDC curve with daily flow data, it does not match well. Generally, the model overestimate the peak flow for a flood process, and the variability of simulated flow is much higher than that of observed, therefore, I want the simulated flow to be more smoother.
I think the SURLAG parameter from the basins.bsn file should be responsible for this.
I have changed the SURLAG from the default value of 4 to 1, 8,22, but it does not result in any difference in FLOW_OUTcms. I wonder why?
Is there any other responsible for this ?
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Hello Wander Araújo Martins , were you able to reduce the flow peaks at the end?
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Actually I am looking for SWAT+ modeling help book/video to understand the basic processes happening in SWAT+ with great details.
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Thank you so much for your kind response.
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at the endpoint of the watershed. The Gaging point is not there.
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Dear Boddepalli Manikanta,
Calibrating and validating hydrological models like SWAT using data from a single subbasin in a larger watershed, known as sub-basin calibration and validation, is a common practice. The rationale is to focus on calibrating the model for a specific area first, to understand and improve its performance, before applying it to the full watershed model. However, the discharge gauge site used for calibration must be at the outlet point for the entire watershed. Using a site partway along the watershed risks missing major tributaries, limiting how representative the calibration is for the overall watershed flows. The best practice is to use the most downstream gauge site encompassing all tributary flows for initial subbasin calibration and validation. This helps ensure the model is properly calibrated before expanding to the full watershed. However, as mentioned, even in the absence of a gauge at the watershed outlet, one can leverage sub-basin streamflow data, particularly when the hydro-climatic and physiographic characteristics of the watershed closely resemble each other. Alternatively, one may consider employing a rating curve established at the outlet by the relevant authorities (Minster of Water) or drawing upon published research specific to that area.
Humble Regards,
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Hi there, I am having an issue delineating the watershed. I am trying to load a .tif file and when I click 'create streams' I get the following error (attached). It's not a problem with QSwat+ software because I was able to follow tutorials online using the software, without issue. Any help would be greatly appreciated.
Edit: the error reads as follows:
*** Problem with TauDEM /Users/user/SWATPlus/TauDEM5Bin/pitremove -z /Users/user/Documents/Masters/Swat+/CGD Pre Harvest/Preharvest5/Preharvest/Watershed/Rasters/DEM/DEM_IRL_ITM.tif -fel /Users/user/Documents/Masters/Swat+/CGD Pre Harvest/Preharvest5/Preharvest/Watershed/Rasters/DEM/DEM_IRL_ITMfel.tif: please examine output above. ***
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Dear Eibhlín Vaughan,
To further diagnose if the issue is with SWAT+ or TauDEM, try running the TauDEM pitremove operation independently outside of SWAT+ using the same input DEM file. This can determine if the issue arises from interaction with SWAT+ or is inherent to TauDEM. Also verify the input DEM raster format is supported by TauDEM, as some formats like GeoTIFF typically work better than others. Start with a very small 10m x 10m subset of the DEM to see if pitremove succeeds on that, then progressively increase the area size to isolate any problems related to data complexity or resource demands. If memory or performance seem insufficient, try decreasing the resolution or computational resources allocated to pitremove. Taking these steps to narrow down the root of the problem can clarify whether the pitremove failure stems from SWAT+ linkage or limitations within TauDEM itself.
Humble Regards,
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Hello friends, I'm trying to run QSWAT and I'm after step 3 on the simulation process , setup my model from 2001 to 2005 with NYSKIP 2. Chose daily because my data prepared like that. Before that I setup my WGEN_user , pcp and tmp data. When I click run SWAT I get the following message - forrtl: severe (24): end-of-file during read, unit 25, file D:\Transffered\N\Z-Zone\BAS\Ogosta_database_model\SWAT_Model_Final\test\Scenarios\Default\TxtInOut\000010000.sub
On step 1 of the model I merged several subbasins because they were very small and I joined them to bigger ones. Could that be the problem?
As you can see from picture 2 file 000010000.sub is empty?
Please share possible solution.
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Hello and have a good time. To change subwatersheds, you cannot manually delete or merge them, and you can adjust this by changing the area threshold of each subwatershed while closing the subwatershed boundary. Maybe the problem is because of this. The things mentioned above related to the implementation of SWAT in ARCGIS are likely to be similar in QGIS as well.
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Dear Community,
I would like a question regarding the use of Partial Least Square Regression Analysis. Basically ,I am confused in units. For example, I have Year 1, Year 2, Year 3 land cover and Water Balance Components. The units of Water Balance Components are "mm", while the units of each landcover type for year 1, 2 and 3 are in square Km. I am confused how the different units will perform the PLSR test.
Either, I have to use the % difference in each Year or % of particular landcover type to the total area of the basin and similarly convert the water balance variables from "mm" to percentage.
Looking for a guidance. Please teach me.
Regards
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In my opinion, Normalizing each component will solve problem!
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I created a QSWAT hydrological model and the simulated daily runoff values in cubic meters per second are extremely higher. Does anyone have an idea what is causing this problem? #QSWAT #Hydrological_model
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Dear Joshua,
Have you calibrated the model for your case study? Are you sure about the calibration and validation process? How about your observation data? you need to recheck your data and modeling stages.
I strongly suggest you consider the "sensitivity analysis stage" in your calculations. it does not only let you know how much each input parameter affects your daily runoff, but you probably be able to infer what is the most impactful parameter in your case study. After sensitivity analysis, you can have a meaningful calibration and the calibrated input parameters will make sense, as well as discharge results.
By the way, I can guess your extremely high values may be related to the soil infiltration rate and your soil data.
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hi
i have calibrated a snow/glacier-fed mountainous watershed.
The calibration results are good with R2 and NSE >0.80 and p factor 0.77 and r factor 0.71, PBIAS 7.5
I have got the following values.
v__SFTMP.bsn                  -1.750000 v__SMTMP.bsn                  -5.850000 v__SMFMX.bsn                  1.100000 v__SMFMN.bsn                  2.100000 v__TIMP.bsn                   0.083333
Is it Ok to have SFTMP < SMTMP and similarly SMFMX < SMFMN for a watershed in the Northern Hemisphere?
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It really depends on how you wish to define "ok".
Regarding the model's functionality, yes, it does not matter very much: even if the calibration process suggested you some parameter values that are physically ridiculous, as long as each value is within its own "functionally acceptable" range, the model can still work and yield discharge result for you.
You can find the reference to this range in the SWAT-CUP interface, "Calibration inputs" >> "Absolute_SWAT_values.txt" (and some of the parameter values can even be outside the given range there).
On the other hand, if you are wondering whether the physical meaning of these calibrated parameters are accetpable, then it is a much more complicated question.
The quick answer to your question would be, no it is not ok.
A suggestion would be to specify the numerical relationship in the initial calibration setting so that this situation can be prevented from the beginning. Assuming you are using SWAT-CUP for calibration, when you add SFTMP and SMTMP in the "Par_inf.txt" of the interface, the third larger column is "Filter condition (optional)", and the last sub-column there is "Conditional filter". Select you desired parameter, and you will see a "..." under this sub-column. Click it and you will open the Conditonal Filter Editor, then include both SFTMP and SMTMP via the "New Parameter", then define their relationship on the right pannel. It is a very simple process, I trust you can understand how to use it once you see it. If not, you may ask me again.
By this way, I think the problem itself can be solved.
However, as I said, it is actually a more complicated question. So I have a longer explanation for you on this issue, you can keep reading if you are interested.
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Before explaining any further, one essential point you need to understand is that an optimization process such as the one that SWAT-CUP use is highly statistics-based. In other words, the calibration process does NOT guarantee the physical meaning of any parameter at all during the calibration process. As a result, even when the NSE, P-bias, or r^2, are all very good after the calibration, it does not necessarily mean the numerical values of the calibrated parameters are physically true to the local reality in your target catchment.
If this notion is the definition of "ok", then theoretically you need to make sure the physical meaning of every calibrated parmater is reasonable and somewhat true to the local reality of your target catchment.
However, you may notice that this notion is rarely realized in most publsihed papers (even from highly ranked journals). This is because without the validation data (not the one to validate discharge result, but to validate the physical meaning of parameters), no one can really prove the numerical values of the calibrated parameters are physically wrong (although at the same time, you cannot prove them correct either). As an alternative solution, the commonly accepted way is to ensure two points:
1. The initial calibration range(s) is physically meaningful (but only in a general sense, not necessarily true to the local reality), so that after the calibration process, the calirated values will still be physically meaningful.
2. The calibrated parmater(s) shows acceptable sensitivity.
Now back to your initial question, if the term "ok" refers to whether the consequent result would be good enough for a thesis or a journal paper, then in most cases, it will be ok as long as you fulfilled these two points and show the evidence in your work.
Hope this helps.
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Hi everyone,
I wanted to know what is the land use classification code used in the lookup table for Mixed Dryland Forest and for Scrub & Shifting Cultivation in the SWAT model.
Thank you all.
Majid.
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Hello Majid Azari, I believe you can find it here in the attached file for the Globeland30 dataset.
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Hi Everyone,
I am going to be carrying out a water quality study for a catchment that has a reservoir at its outlet and its majorly covered by vegetation, with some shifting cultivation and there are a few local villages, so there is some point source and non-point source pollution. So, I wanted to know, can SWAT model the following water quality parameters? And is there any better hydrological model to use for modelling these parameters?
1. Dissolved Oxygen (DO)
2. Biochemical Oxygen Demand
3. Chemical Oxygen Demand 4. Ammonia Nitrogen as N (NH3-N) 5. Total Suspended Solids (TSS)
6. Total Nitrogen as N (TN) 7. Total Phosphorus as P (TP) 8. Percentage of DO Saturation
9. Coliform
10. E. Coli
11. pH
12. Fluoride
13. Chloride
14. Iron
15. Manganese
16. Aluminium
I appreciate the feedbacks.
Thank you all,
Majid.
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  • Some of the water quality parameters that can be modeled by SWAT include : Nitrogen (total nitrogen, nitrate, and ammonium), Phosphorus (total phosphorus and orthophosphate), Sediment (total suspended sediment and sediment yield),Organic matter (total organic carbon),Temperature, Dissolved oxygen, Biochemical oxygen demand (BOD)
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I have a monthly dataset of GLDAS evapotranspiration (version 3.6 a with 3-hourly temporal resolution). The conversions I have come across suggests multiplying the dataset values with 86400*(Number of days in the month) which sounds reasonable however the dataset values are all greater than 1 thus, this conversion will result in unrealistic ET values (>86400 mm at least).
So, I was wondering if the monthly dataset are actually daily ET values averaged over the month, making the actual units of the dataset kg/m2/day (mm/day) which require multiplication only with the number of days in the month.
Please provide your opinion over this.
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Given the density of water, 1000 kg/m^3, the evapotranspiration (ETA) in the units of kg/m2/sec with 3 hours intervals, can be expressed in mm/month as
ETA [mm/month] = ETA [kg/m2/sec] x 10800 [sec/3hr] x 8 [3hr/day] * 30 [days]
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But I have found much HEC HMS better compare to SWAT.
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The HEC-HMS model is a lump-based model, while the SWAT model is a semi-distributed model. Lump-based models consider the total basin as a “single homogeneous element".
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I am currently working on developing a SWAT model for a basin. After I have developed the model and figured out its hydrological components, I need to compare my work with an already published work. Can someone give me suggestions on how to proceed with my paper? or give me links to similar works so that I can get some ideas! Thank You.
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I am familiar with this subject as a practitioner, but do not know of other research/academic work in this space.
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Hello everyone, I am doing calibration of Flow for my watershed. My concern is, I am stuck with the value of NSE, R2 and PBIAS. only the p-factor and r-factor changes into decreasing value.
How to decrease the value of CN2 and ALPHA_BF? These parameters belongs to the most sensitive parameters in my model.
What do I need to check to verify these values?
Thank you!
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Michelle--unfortunately I'm not familiar with Swat Cup software; so I just don't know whether or not Swat Cup can update these two parameters--sorry I can't help you more with this; hopefully someone who works with Swat software will be able to help with your question.
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Hello everyone, I am having a trouble to understand why does my point source located on downstream affected my upper stream data for flow?
Does anyone know any idea why it does?
Thank you!
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Hello James, thank you for your response. As what I understand on your answer above, it would affect only the nearest distance upstream. My concern was, the utmost upper part of the watershed. My point source is located below the discharge site. I attached my area of study. What I did was just edit the point source file.dat and the pOINT SOURCE DISCHARGE at edit swat
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In rainfall-runoff modeling, it is often not possible to find the unique best parameter set, different parameter sets may be given similar good results during calibration. To reduce uncertainty and to define the optimum parameter set, it is a fundamental analysis of model parameters.
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How SWAT model computes the initial soil moisture (SWo) from the general water balance equation SWf = SWo+summation of (P-ET-Q-DP-GW).
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kindly check the reference. Tripathi MP, Raghuwanshi NS, Rao GP (2006) Efect of watershed subdivision on simulation of water balance components. Hydrol
Process 20(5):1137–1156. https:// doi. org/ 10. 1002/ hyp. 5927
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Hi all,
Could you tell me some websites to download temperature data as input to a SWAT model?
Regards.
Brahim.
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Dear All,
 I hope this message finds you well. Actually, I have a problem with the irrigation management in SWAT model and I would appreciate if you can consult me on this issue. In my SWAT model I defined the irrigation manually in mgt files using mgt_op=2 and introduced the values of IRR_AMT for each subbasin and HRU  and the source of the irrigation one by one based on available data. I have three kinds of irrigation sources which are applied in my model: reach or dam or shallow aquifer. For some subbasins and HRUs (for example hru 1 sub1 or hru6 sub1...) the irrigation is defined to be from the reservoir dam but as I checked the OUTPUT.HRU of the SWAT in these regions some parts of irrigation (varied 20% to 80% for some HRUs) are supplied from the shallow aquifer which the value of SA_IRR (irrigated water from the shallow aquifer) shows that in the output file. It is contradictory that in the theoretical manual is also said as follows: For a given irrigation event, SWAT determines the amount of water available in the source. The amount of water available is compared to the amount of water specified in the irrigation operation. If the amount available is less than the amount specified, SWAT will only apply the available water. (ver2009, p 375) Furthermore, I checked the model with different sources added on by one to debug the problem. If all the irrigation source of  a specific subbasin (all HRUs) assumed to be from reach, dam or unlimited source then the  SA_IRR (irrigated water from the shallow aquifer) will be zero but if the shallow aquifer introduced as irrigation source for one or more HRUs of a specific subbasin, the other HRUs can also extract the rest of their irrigation water demand from the shallow aquifer as the SA_IRR will be nonzero. It happened for all the other conditions (IRR_SC=1 or RR_SC=2 or 5  According to the analysis of the irrigation source in my SWAT project, I got the following conclusion: If you define shallow aquifer as an irrigation source in one or some of the HRUs of a specific subbasin, then in all of the HRUs of that subbasin, the SWAT model first supplies the water from the defined source (dam or reach) and then it tries to supply the rest from the shallow aquifer. So I would appreciate if you let me know why the rest of the irrigation demands supplied from the shallow aquifer, whereas the reservoir is defined as source location of the irrigation. The output.hru file for one year of running is attached. Please let me know if you need any further information. Thank you for your kind support in advance. Best Regards,
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Please help me.
SWAT can't simulate my irrigation scheduling input data.
I want to develop irrigation scenarios for my study area. I have done the management operation process in the Mgt. in put file. However, after running the model, the result shows no irrigation input and output information in the mgt.output file.
Please anyone who can help me? thank you,
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Hello Everyone
I am facing an error at the running SWAT model simulation step. Showing that error as  txtInOut/ATOM.ATM.
Screenshot is attached . Please help me in this regard.
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Thank you so much Dudley J Benton
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Working with SWAT modeling in mining regions. The Land Use of the mining region has to be fine enough to understand the impact of change of land disturbance by mining on hydrology.
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The range of spatial resolution you are talking is availble but not free of cost such as Compsat, LISS-IV, Quick bird, Planetscope etc. Free of cost data from Sentinel-2 available at 10 m spatial resolution which could be benficial for you. Please try.
You are most welcome for further queries.
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Hello SWAT users,
I would like to design ponds in the catchment area.  I wonder if in this case it is enough to enter the parameters of the ponds in the .pnd files, or should they also be modificated on the landuse map?
Best regards
Damian
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Thank you very much for your professional reply. In the meantime, I was doing SWAT model analysis with modification of .pnd files and additionally with changes on landuse and soil maps. By modifying the maps, the SWAT model recalculated the HRU areas.
Best regards,
Damian
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The SWAT model didn't report any errors in the previous operations, but when I click "Run SWAT", it runs not successful(fig1). I open the slr.slr as it tells me , but I don't know how to find the error. One more question is that, whether my chooses are correct in the window(fig2). Can anyone tell me how to do? Thank you very much.
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Hi, it says u have a problem with SLR. SLR file, please check the data format in that file, maybe a problem with missing data...
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Hello, honorable forum members. I have a question related to ponds, retention tanks, etc. in the SWAT model. What water balance parameters are affected by adding pond parameters in the .pnd file? I would also like to model an increase in the number of ponds in the catchment area. Is it enough to enter new parameters in the .pnd file for this purpose, or do you also need to draw the joints on the landuse layer? Best regards Damian
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Considering water balance, the quantity and timing of flow may be affected, and evaporation from the ponded water likely to increase. Shallow ponds would evaporate more than deep ones. Deep ponds hold or detain more water. Ponds may have variable leakage rates to groundwater, some of which may emerge downstream. Ponds may be used for irrigation, increasing evapotranspiration rates. Ponds may or may not have downstream discharges, so some sections of streams could dry up, affecting aquatic life. Deep ponds with near bottom discharges may have cooling effect on downstream section, but oxygenation sometimes a problem. Ponds capturing heavy sediment loading may loose capacity with time, and the clean water releases can contribute to downstream erosion. It’s best to evaluate on a case by case basis, and using models that have not been validated to specific area as compared to actually collecting water balance data can cause some major inadequacies in estimates.
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Respected All
The data which is available at https://swat.tamu.edu/data/india-dataset/ , the file named "SOIL_WATERBASE.7z" on this link has only the raster along with "VALUE" and "NAME" of the soil series, which is taken/subsetted from HWSD_FAO,
But the database file require a large number of inputs of different soil properties, for these soil series like, compaction, number of layers, Texture, Bulk density, Available water capacity, Proportion of sand silt and clay, etc, in the dbf file, which has these columns
OBJECTID
MUID
SEQN
SNAM
S5ID
CMPPCT
NLAYERS
HYDGRP
SOL_ZMX
ANION_EXCL
SOL_CRK
TEXTURE
SOL_Z1
SOL_BD1
SOL_AWC1
SOL_K1
SOL_CBN1
CLAY1
SILT1
SAND1
ROCK1
SOL_ALB1
USLE_K1
SOL_EC1
SOL_Z2
SOL_BD2
SOL_AWC2
SOL_K2
SOL_CBN2
CLAY2
SILT2
SAND2
ROCK2
SOL_ALB2
USLE_K2
SOL_EC2
and so on_____________till 10 layers (if available)
The another file named " soil_HWSD_FAO.7z " has its global raster without any information about the soil properties which are used in input database.
I have sub-setted/clipped the indian raster from the global,
although the global raster was missing spatial referencing,
So if someone is sub-setting the same for their area of interest, then you have to manually geo-reference the subsetted image to use it while creating HRU's.
Kindly share if you have any idea about, the source of the soil properties for these soil series.
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Hey! Abhilash plz Share protected password with me
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I faced two errors while I was trying to rewrite SWAT inputs:
SWAT inputs rewriting: 'SPCON' does not belong to table.:RTE file print error on subbasin:1
column 'CO2_X' does not belong to table
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Dear all,
I removed all climate data from wgn except precipitation and temperatures (max and min) and my problem was solved.
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Where can I get future data that can be fed directly into the SWAT model?
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I would like to know the procedure of creating soil database for Australian soil classification types to apply in the SWAT model. Most of the global studies used FAO soil database for SWAT model setup but using Australian soil map will generate more accurate result. Please suggest how can I create a soil database or replace 'usersoil' database schema on SWAT2012. Thanking you in advance.
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Hello again Dear, honestly I'm not an expert in this field. But I read your request and searched for it. Eventually, I found these articles that can be useful:
[ 10.13031/trans.58.10589 (Tile Drainage Simulation in SWAT2012: Parameterization and Evaluation in an Indiana Watershed) ]
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I am selecting an opensource hydrological model to perform a water sustainability assessment at a basin scale, including blue and green water sustainability evaluation and some considerations about water quality. I need an open source, well documented and user friendly open source software. After a first check, I identified two suitable options: SWAT+ and SWIM. I cannot really understand the differences among them. Any suggestion from someone who has already used these models? Thank you for your cooperation.
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I would recommend to use SWAT instead of SWAT+, it is a bit harder to use outside the US, but it's more reliable due to bugs in swat+ (as now, I hope It will change, as swat+ is has more user-friendly interface) - in example swat+ doesn't calculate properly urban CN (uses cn 98 value for permeable areas), overall results differ significantly from swat results using the same input (I didn't look for this bug, just gave up testing swat+).
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I cannot seem to get irrigation depth to be realistic (always underpredicts). I have tried manual and autoirrigation, increasing irrigation depth, changing stress factors, withdrawal source, and heat units/date scheduling. No option gets me close to the ~300 mm/yr for peanut/cotton, or ~400 mm/yr for corn. 
UPDATE: Changing the irrigation method from plant demand to soil moisture demand (WSTRS parameter) causes more realistic irrigation depths for my model, but also causes irrigation to occur all year instead of just during the growing season. Any suggestions?
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This is a good question.
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Hi friends! I ran my project successfully, however there are some reservoirs in my basin. Hence, I have to rewrite data again and set the reservoir parameter up.
Unfortunately, I don't work and the text box show that my reservoir area and volume have to be less than a number (I showed in the picture below). Meanwhile, my real reservoirs are larger than that number.
Does anyone get the same problem with me?
Your answer will be a big help for me. So many thank!
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Alicia Chong So sorry friends, I just read your question now. I suppose that you've already known the answer. However, I write here to help the other persons who have the same question.
You can use the access function of Microsoft to open/edit/save a .dbf file.
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I am using swat model for first time. Now fro usersoil part, i am recording my soil properties by replacing existing data in table. My worry is am i corerct if i use existing codes such as OBJECTID,MUID,SEQN,SNAM and S5ID? By only editin other fields of siol properties. Wuold there be erorr in futuer runing of model?
Thank you,
Abiy
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There shouldn't be any error, but it is better to change other fields (i.e. snam) as well, to remember that there were chenges when you will come back to the project later. If the changes are minor, it is more convenient to do them in swat editor (edit swat input/edit swat databases)
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Good day Sir/Ma'am, I am one of the researchers and here's is our research study for our thesis: "Spur dike installation against soil erosion along mandulog river". And we are currently having a hard time looking for what software will be the fit in our research study and we would like to ask for your advice on where to get the software or what other softwares can we use to analyze the data in our study. Any suggestion will be greatly appreciated. Thank you and have a great day.
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I would like to know at what height from the ground surface the temperature is measured to the weather data for the SWAT model.
Best regards
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Generally, <=2 m above the ground.
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I am facing a challenge with the classification of my soil data in order to help create the usersoil database. My soil data was developed using the USDA classification system but I now have to convert it to the FAO code so as to match those provided in the SWAT2012 database to help generate the usersoil table. Could someone explain to me what the second and last numbers  in the code are and where I can obtain it. E.g Af32-2ab-3, Be49-3c-20
The first letters represents the dominant soils, Ferric Acrisol (Af) or  Eutric Cambisol (Be), the third figure is the soil texture class (1-coarse, 2-medium, 3-fine), the small leters indicate the slope class (a- level to undulating; b- rolling to hilly; c-steeply dissected to mountainous)
What does the second figure of 32 or 49 and the last figure of 3 or 20  represent in the code and where can I obtain them?
Secondly, is there an alternative way to create the usersoil table without using the FAO database, could anyone kindly share any useful resources in this regard?  
Thanks in advance!
Regards,
Brian
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Very interesting question.
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I have a problem with permanent wilting point WP. According to the formula WP = 0.40 * ((% CLAY * Bulk Density) / 100). My data shows that% CLAY = 5%, BulkDensity = 1.55. After converting, I have the result of 31mm per 1000mm of soil. To my knowledge it should be approx. 110 mm per 1000 mm of soil. Can I enter my own WP content data into the input.std file into the SWAT model?
Greetings
Damian
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It is always helpful if the model's example data files are edited to suit our our needs. I hope it is helpful.
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Hello dear user,
when calibrating, I would like to leave the value sol_z (1) - 300mm, sol_z (2) - 1000mm, sol_z (3) - 1500mm (mainly loess soil in the profile), which I used in modeling. Unfortunately, it is difficult to calibrate a model with this parameter. I wonder if there are any parameters that have a lot of dependency on sol_z? When I set the possibility of calibrating the sol_z parameter, the result was satisfactory. Unfortunately, the values of sol_z (1) - 150 mm, sol_z (2) - 300 mm and sol_z (3) -450 mm. This is not satisfactory due to the fact that the research region has a loess thickness of up to 20 meters.
Best regards,
Damian
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Use Soil water assessment tool (SWAT) you can choice by default USGS or change to user requirement and load your local soil to the database and simulate depending on years you desire..
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I have been using the SWAT model, and simulation has been done several times by changing the evapotranspiration calculation method and the rate of hydrological parameters like Soil Evaporation Compensation (ESCO), Groundwater Re-evaporation (GW_REEVAP), Curve Number (CN2), Available water capacity of the soil layer (Sol_Awc), and Slope range of the area.
So, the annual precipitation is 318 mm, the annual surface runoff is 602 mm, but the annual evapotranspiration is based on the Hargraves method (1450 mm) and based on thornthwaite method ( 840 mm). so why runoff and ET are more than precipitation? it can be acceptable in terms of the water balance?
Any solution or recommendation to encounter it, please?
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I don’t know if I could be of help. From what I gather, everything is generated by models. Typically at a minimum, rainfall and runoff are measured, and then the unknowns are estimated with models perhaps. Also, if you try to do the water balance by calendar year, one year may be very wet such as in January or December, and the other month or year may be dry, resulting in some estimation error. The USGS uses the water year approach, with September 30 and October 1 the end and beginning of a water year. But you might in SE USA imagine a hurricane toward end of a September, and much of the flow in a large river showing up in October, for example. Truthfully, your situation is quite unusual, suggesting some errors in assumptions or models. But if your project is in karst terrain, it was shown by using dye studies developed by hydrologist Tom Aley of Missouri, that there were instances of interbasin transfer of water underground. And one might imagine that a watershed with a large karst spring might have more runoff than rainfall. When I worked on the Big Turnaround and other associated wildfires in FL and GA, USA, air became reacquainted with the Suwannee River, which has instances of discharge losses of streamflow due to faults or karst terrain loses underground. Another potential source of error is the rainfall measurement, unless one has a grid of rain gauges. Measuring stream flow professionally even has some error, perhaps plus or minus 20 percent unless very carefully gauged. With the anomalies suggested in your data, I would agree there is something difficult to accept without clarification and perhaps more detailed study, including geology.
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Hello everyone,
I have setup and calibrated the SWAT model with SWAT-CUP, the NSE coefficient is as high as 0.85 both for calibration and validation periods at five gauge sites. But the CN2 parameter for most of the subbasins are as high as 98, I don't think it's reasonable in the physical sense. I wonder how can I decrease CN2 by modifing other parameters?
Would you please give me a suggestion about which other parameter is equivalent or have similiar effect with CN2?
Thanks in advance.
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Hi,
What is your method for changing CN?
I suggest you change it in +-0.3 range (relative change).
Do not use V (replace) for this parameter and soil-related parameters.
Best,
Mamad
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I am trying to add DEM file for watershed delineation in ArcSWAT, but some error occurred. Can anyone help me to solve this issue...
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Try to relocate your dem into C drive and run the process again. If you still face the issue, change the .net framework as suggested by SWAT.
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I am using SWAT 2009 and working on a Godavari basin (India). My main objective is to estimate the monthly runoff. I already ran the model and found monthly runoff but it is overestimating. I used many calibration parameters to calibrate the model i.e. CN2, GWQMIN, GW_REVAP, REVAPMN, GW_DELAY, ALPHA_BF, SL_SOIL, LAT_TIME etc.
I am putting all the values in the parameter range, but I did not find any changes in the simulated runoff. What should I do?
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Hi Sneha, I was not overwriting/saving the new parameter values after any changes in the parameter. After any changes, you have to save the new parameters using the save (do not remember the exact name on the interface) button.
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I wonder how many HRU areas should I do in my catchment area. The catchment area of 30,000 ha is divided into 31 sub-basins. Upland area with a slight slope. 14 landuses. The 3 landuses are separated by the split landuses function into 6 additional landuses. Total landuses there are 20. 32 types of soils. 5 groups of terrain slopes. I used filter by landuse, soil, slope (thresholds) 15% landuses, 15% soils, 10% slope. I received 1,000 HRU areas. Is it correct? Should I accept fewer HRU areas?
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Thank you very much for all the answers.
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Quantifying groundwater recharge in arid and semi-arid areas is a very challenging task because recharge amounts are small in comparison with the resolution of the investigation methods. Additionally, it depends on soil characteristics, geology, topography, land cover characteristics and land use, besides being affected by the temporal variability of precipitation and other hydrometeorological variables under arid and semi-arid climates. Several watershed models used to quantify recharge generally provide recharge estimates as a residual term in the water-budget. Which means that the estimation accuracy of recharge is controlled by the measurement accuracy of the various other parameters in the water budget. Moreover, according to the literature, daily time steps are desirable for estimation of recharge because recharge generally becomes a larger component of the water budget at smaller time scales.
How could we minimize the uncertainties accompanying the estimation of groundwater recharge under semi-arid conditions using SWAT model at small scale (around 350 km2 area)? Should the SWAT use be coupled with any other techniques or models (like Hydrus-1D) to get best results? Are you aware of any studies that have used SWAT to estimate groundwater recharge, or the impact of climate change and/or anthropogenic activities on groundwater recharge under arid or semi-arid conditions?
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Roland Yonaba thank you for this interesting contribution.
Bests,
Mohamed
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Hi
I have a SWAT-CUP calibration question.
When calibration is performed using SWAT-CUP, the correlation coefficient and NS value are decreasing rather than before calibration.
The correlation coefficient before correction was 0.9 or higher, and the NS value was also observed as 0.7.
Through correction, the NS value was increased and correction was carried out.
The Excel graph(figure file name 9) before calibration is based on the \Scenarios\Default\TxtInOut\watout.txt file in the SWAT project folder.
Please advise if I am doing wrong corrections.
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Dear Jinhyuck,
the calibration using SWAT-CUP is based on the parameter selection (parameters and ranges) before run the model. it is better to first run the swat-cup with a combination of a number of parameters to carry out the rank of each parameter based on its sensitivity to the calibrated variable using global sensitivity analysis because one at a time technique can give you only the influence of that unique parameter on the calibrated variable which can be changed when you combine it with other parameters. so it is better to use a such combination of parameters for each iteration compromising a number of simulation which should be at least 500 simulations. best of luck
cheers
Ali
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For my future discharge forecast in the calibrated HEC HMS model, i need the precipitation data of the future.How can i get this data in the daily timescale?
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Interested
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Can anyone explain the steps in SWAT modeling and to proceed ahead.
I am looking for surface and groundwater modeling using SWAT.
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I hope you already explored this website which has lof information and document to use QSAWT.
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Dear Researchers,
I run multiple times my SWAT-CUP SUFI2 but it is contineously giving this problem as attached in picture. Please let me know your expert opinion why I am facing this error and how to fix it.
Thanks in Anticipation.
Kind Regards
Naveed
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how to solve the SWAT_CUP error dispalyed in figure below.
with regards
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Hello and have a good time When running the SWAT model, I encounter the following image error. Is there anyone who can help me solve this problem?
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Please change the destination of your working folder and see
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Of course there is "urban" table, but it isn't enough since I try to model large city. Especially I have problem with green areas such parks, lawns, orchards and courts. BTW, in the table there is a field "urb cn" with value always 98 - does it force CN number in HRU?
If so, is it a good idea to split landuses on urban+grass, depending on %of impervious surface?
I've chosen swat+ because of its popularity, but maybe there is a better software for hydrological modelling of urban areas?
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It depends on how you want to represent the urban. The urbca2 are the default values but if you have your own values you can change them in "SWAT2012" though the name might vary with the version. Usually default value is okay.
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Dear Colleagues
I am using the SWAT model in an irrigated basin where I wanna specify the Irrigation database for major crops (sugarcane, maize, rice, wheat, and cotton) in SWAT model simulations. Does anyone suggest to me "how to address the crop management data including growing, harvesting date, and irrigation amount applied for each crop"?
Your's help will be really appreciated.
Thank you very much.
Kind Regards!
Arshad
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interested
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I set up, run and calibrate SWAT model.
I want to test BMPs scenarios for the next step, but I don't know how to do that.
I have to prepare new input files or I can do on the ArcSWAT interface.
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Dear Miyuru Bandara Gunathilake,
I want to do research with you. I will write you a message soon. Thank you very much.
King regards,
Mirzohid.
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How can download the precipitation data from INDIAN METEOROLOGICAL DEPARTMENT(IMD) or Centre for Climate Change Research (CCCR) of Indian Institute of Tropical Meteorology
(IITM), Pune.
Could you refer to any other web sites?
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Check this link: https://www.ecmwf.int/
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I have a daily flow data at the outlet of my basin. From that data, how can i estimate base flow parameters?I am currently using constant monthly method and i am using a trial and error approach..but i want to explore other possibilities of baseflow methods such as recession baseflow for which i would beed recession constant, initial discharge and ratio to peak.. How can i estimate these parameters?
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Once you have calibrated and validated the hydrological model against the streamflow values at the basin outlet, you can get the baseflow parameters as the actual ones. Another way is to apply the methods of baseflow separation
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Dear all,
I have prepared rainfall datasets for SWAT MODEL using 0.25 degree IMD long term gridded rainfall data,
but as I am using it in the model, it is rounding off the co-ordinates value.
eg:- for the latitude 19.75 and longitude 78.50, the name given to the file is PY1975X7850,
but in the textinout folder, the .pcp file for precipitation is rounding off the coordinates to 19.8 and 78.5.
If it is taking co-ordinate values to 1st decimal place only, then can't we use the 0.25 degree rainfall data in the input?
also it is not displaying the input data in the same format.
Kindly, refer to the attached video to understand the query.
Any valuable suggestions are highly appreciated.
Thanks.
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Try 0.2 or 0.3, more decimals don't accept me either.
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Hi everyone need your help.thank you
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Dear Mahsa,
I think the paper I attached below will help you with your problem
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Hello everyone,
I used the swat model for different land-use scenarios but found that the large land-use change does not impact runoff and evapotranspiration.
If anyone is confronted with the same problem, please help me to solve it.
Thank you.
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Dear Ahmadi Mehamoui,
land use change impacts often balance out if aggregated over space and time. I would therefore recommend to look at changes at the sub-basin or HRU-level as well as to look at dynamic changes. In this respect, the following three papers might help you:
However, if your output at smaller spatial scales is still exactly the same, it is very likely that the change was not correctly implemented. In this case, check your inputs and the model and try again.
Good luck and kind regards,
Paul
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input types and formats...!!!
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Hello dear Melkamu.
I think this video playlist about SWAT model setup can help.
hope you find the solution soon.
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Why the number of weather stations is different between "pcp1.pcp" and input weather data?
I have input 23 stations, but it only 8 stations in the "pcp1.pcp" and "tmp.tmp".
Could you help me? Thank you, very much!
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Sunil Bista,
You are right, I hadn't thought of that. Thanks a lot for your input.
Best,
Konstantinos
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Hi,
I am delineating my watershed for the first time in ArcSWAT 10.3. But when i try to attach my DEM file it gives an error 2147217383 ( failed to copy raster dataset). I have tried to check the permission of folder where DEM is present and everything is fine. DEM coordinates are in Projected UTM.
Can someone guide me through thus error.
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Try moving your folder to Desktop or to another drive. Make sure there is no space in the name of your SWAT project.
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Hello, Has anyone conducted calibration using the SWAT model? If so which method did you use? And was it successful ?
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As part of my PhD research, I am using the SWAT model for hydrological simulations at the watershed scale. Per se, the only calibration method available with SWAT is the manual calibration, which can be accomplished within the ArcSWAT (ArcGIS) interface (or rather QSWAT for QGIS). However, the process can get tedious and you are prone with lots of errors if you are starting with SWAT.
I would rather suggest using the SWAT-CUP alternative. Basically, SWAT-CUP is an automatic calibration program for SWAT model. The workflow is quite simple: you start preparing your model set up with ArcSWAT (or QSWAT), and then you feed this set up to SWAT-CUP. There you can run sensitivity tests on selected parameters, or perform model calibration and validation using many optimization algorithms: SUFI2 (Sequential Uncertainty Fitting), PSO (Particle Swarm Optimisation), GLUE (Generalized Likelihood Uncertainty Estimation), ParaSol (Parameter Solution), MCMC (Markov Chain Monte Carlo). You are not required to know the in-depths or the maths behind such algorithms as the program let you use them in a breeze and produce the necessary graphical outputs to evaluate the simulation runs. The latest version of SWAT-CUp is available for free (https://www.2w2e.com/home/SwatCup). If you buy the license, you can even use parallel processing features.
I can also suggest a swath of papers that might be relevant to evaluate your model calibration.
All the best,
Roland.
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Hi Everyone,
I want to model the inputs of nutrients from septic system (septic tank and pit latrine) into ground water or surface water. could SWAT model this issue?
Any help will be appreciated
Thank you in advance
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Yes you can.
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Hello everyone,
I have a calibration problem. After a few iterations of the model, I get a chart with high flows at the beginning and low flows at the end that do not match the measured flows.  I wonder if I have an error in the flow data somewhere or I am doing some calibration error. I would be very grateful for your help.
Best regards
Damian
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Thank you very much for help.
I was able to calibrate with satisfactory results. But I would like to have an even better NS. I have been standing against the wall for several days.
My calibration facility is located in the upland area in Poland. About 170 to 220 meters above sea level. The area is strongly diversified in terms of height, undulated and cut with deep ravines. Precipitation is about 600 mm per year. PET is a 650 mm per year and eavpotranspiration / transpiration is a 450 mm per year. Advantage of soils with silt loam (SiL). The main landuse is CRDY - 65 percent of the area and FRSD - 10 percent. Slope is 0 - 6 percent - about 75 percent of the area. There is snow cover in winter.
I would like to ask the group for advice on which parameters I can take into account or what to check.
The graph shows the flow in m3 / s. The blue line is observation. Red is a simulation.
Best regards
Damian
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Hi
I am friends I am calibrating stream flow using SWAT-CUP. While altering the parameter ranges to get the best simulated result, how to fix ranges for parameters.
Please help me in this
Regards
Dagani
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SWAT input-outp document provides the details of most of the parameters with ranges. Please choose from there
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I have my watershed file, when i upload the projected Soil Map for HRU analysis, SWAT gives error "there is no overlap with watershed gird" can anyone please answer me how to remove this error.
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I recommend doing all the steps from the beginning with revised projection of input maps.
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Dear All,
SWAT model needs volume of water and spread area when the reservoir is filled to the emergency spillway and principal spillway. In case of reservoir with radial gates the following data are available-
Crest Level of Spillway = 407.51 m
Height of Spillway Gates (Meter) = 15.25
FRL (Full Reservoir Level, m) = 422.76
Maximum level (Meter) = 425.7
Minimum Draw Down Level (MDDL) = 403.6 m
What will be the level for emergency and principal spillway?
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Dr. Abderrahmane Noui
I am very thankful for your kind help. I could get something. An English version will also help for other researchers and me as well if possible for you in future.
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Hi,
Has anyone conducted calibration using the new swat+ model? If so which method did you use? And was it successful?
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Thanks Virendra Kumar Saxena but I'm actually looking for specifically the new SWATPlus model.
Regards,
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Hi All,
I have calibrated my SWAT Project using SWAT-CUP successfully. I now want to incorporate baseline and future climate data into calibrated SWAT Model. As the SWAT CUP gives the best parameter ranges after successful calibration how should I incorporate these ranges in Arch SWAT Project?
If I use SWAT-CUP and copy the tmp and pcp files in the calibrated projected folder what should be the format of pcp and tmp files as they are inserted individually in ArcSWAT for each station but collectively found in pcp and tmp files of SWAT-CUP?
Which out of these two methods s accurate and more reliable?
Also when i use the fitted best parameters into my uncalibrated ArcSWAT folder and run with the same data the results are quite different from those in SWAT-CUP calibrated model , why the results are different in this case ?
TIA
Regards.
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There are some ways, 1) you should generate weather datasets for all observed stations and then add them into ArcSWAT and copy the PCP1.pcp and TMP1.tmp files and run calibrated text files with new pcp and tmp files.
The most important thing here is how to generate precipitation datasets. You should work with multi-station software such as CMHYD or MRD, etc.
2) Use weather adjustment options in SWAT.
Do not use single-site software such as LARS-WG. Because the SWAT model is (semi-) distributed model and could use one to several weather stations. Also, the location of the stations is important.
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Hi everyone!
I am researching the impacts of different PET source on runoff. I want to adjust the SWAT source code to read MODIS PET data. Does anyone have instructions on the SWAT source code and the running structure of the source code? Thanks in advance.
Regards.
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You can add your dataset for PET in ArcSWAT.
Calculate daily PET with your method and add it, like weather datasets.
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Any model output depends on its parameters. SWAT is a conceptual model, it contains an enormous number of physical and process-based parameters to capture real-world behaviour. The physical parameters which we can measure directly and the process-based parameters which cannot measure directly and it has to go through calibration or optimization. While optimizing the model, we will select the influential parameters. But, during the screening of influential parameters itself contains huge uncertainty like:
1. Which parameters have to select?
2. How much range has to take for selected parameters?
3. If we select more parameters, complexity and optimization will increase
4. Which method has to adopt for deriving the parameter value like Absolute, Relative or Replace?
Are any optimal methods available to select parameters and its range?
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Hi guys,
I am trying to calibrate my SWAT model. Every water balance component seems good except for ‘ET’ and ‘GROUNDWATER (SHAL AQ) Q.’ In fact, from experience, ET is 200 mm higher than what it should be, and it needs to transfer to GW-Q.
I have calibrated the model for many different parameters; however, the results are not satisfactory. The ET varies, but it does not go to groundwater, necessarily. I even tried to change the PET calculation method but no difference. In my last try, I calibrated the model for GWQMN.gw, GW_REVAP.gw, EVAMPM.gw, CN2.mgt, SOL_AWC.sol, ESCO.hru, but it seems ‘GROUNDWATER (SHAL AQ) Q’ is not sensitive to any of these parameters.
Any advice and suggestions will be greatly appreciated.
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Try adjusting deep percolation coefficient (RCHRG_DP) manually to keep more water in shallow zone instead of percolating into the deep aquifer and see if there is any change in your shallow flow. Also use a small value for GW_REVAP which makes groundwater available for ET although it's unlikely that such huge discrepancy is resulting from groundwater ET. Still worth a try.
How's you runoff looking? You need to make sure the infiltration method you are using (probably CN) has a reasonable performance before moving to GW. Another approach would be to use Green and Ampt which may show a better performance in simulating infiltration.
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Hi everyone ,
I am master student and I am working in my thesis now in hydrological modelling I will calculate runoff,sediment and infiltration by using swat model but I need some useful references
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Dear saad,
If you want to run SWAT model then first you can read manual of SWAT model and prepare a data as shown in manual. because the data preparation is main task in SWAT model. you should also check the extension of data which you wish to input.
if you have any Problem relate run SWAT Model you can contact me i will help you.
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Solution for Arc SWAT Part-1
Error 73 Floating divide by zero
Severe (64) input conversion error, unit 138 Arc SWAT
Severe (64) input conversion error, unit 137 Arc SWAT
Kindly see the video. It will work..
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Thank you so much for your valuable guidance.
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I need the Globecover2009 landuse information (SWAT Lookup Table and SWAT 2012.mbd) for ArcSWAT model. Does anyone can give any idea about it?
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Search on BHUVAN Land Cover Database
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I have a watershed that has a reservoir (see the picture attached) . I want to model the reservoir as part of my set up. The reservoir takes in water from a stream. Water is withdrawn from the reservoir to feed a power plant.
How can I model the water intake into the reservoir from the stream?
How can I model the water withdrawal of water from the reservoir to the power plant?
Which reservoir modelling method in SWAT should I use?
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You can.
ND Liem
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Dear SWAT users,
I have setup-ed, calibrated and validated the SWAT model for a small catchment, now I want to include reservoir and irrigation practices in SWAT simulations. Please suggest to me.
Thank you for your help.
Rajtantra
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Hi all.
I would like to ask how to include reservoir daily release data into SWAT?
I have tried include the attached txt file but the result doesn't include it.
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I want the daily gridded max min gridded temperature data for running SWAT model that too for the latest current years and within 1 degree x 1 degree.
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IMD
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Can anyone please guide what is the cause of this error in SWAT Run?
forrtl: severe (64): input conversion error, unit 137, file C:\Users\HP\Desktop\swat model final multiple outlets\Scenarios\Default\TxtInOut\slr.slr
I have checked the format of file, all is ok but still this error appears everytime?
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When "forrtl: severe (64): input conversion error" is encountered, all the missing values in the respective files need to be replaced as follows (exactly as mentioned below)
1. pcp1.pcp -------> -99.0
2. tmp1.tmp -------> -99.0
3. slr.slr -------> -099.000
4. wnd.wnd -------> -099.000
5. hmd.hmd -------> -099.000
Save the file and run the ArcSWAT model.
Best Luck!!
Lalit Kumar Gehlot
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Hello everyone,
I have modified the HRU's in my SWAT Model and want to enter weather data yet I cannot!
I found out my problem should be about the weather station database, I don't know who to modify this data? If anyone has a guideline or something it will be very useful. thanks
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Prepare database from weather generatorin in excel and replace that file by importing.
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Hi,
Is it possible to use subdaily timestep precipitation (3 hourly/6 hourly) in SWAT Model? I was able to add them in the weather data definition window. The problem is that in the Run-SWAT window there is no option to define 3 hours(180 minutes) or 6 hours (360 minutes) as Rainfall sub daily timestep. What might be the solution of this issue?
Thanks in advance.
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Hi Nishan Kumar Biswas ,
you can used this format
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How to allot stream order to the streams generated in the SWAT model? It is possible to do it in the SWAT model itself or any other tool? I generated stream line shapefile using the SWAT model but in the attribute table, there is not a field for stream order.
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If you are using ArcGIS, there is a "Stream Order" tool build in ArcGIS, under Spatial Analyst Tool > Hydrology > Stream Order. There are instructions online regarding how to use this tool. Once you generated the stream network with stream order, I believe what you can do is to intersect the stream network generated by SWAT with the stream network that has stream order, then you will get the stream order for SWAT generated streams.
You might be able to find easier ways to accomplish this task, but this is what I can think of by now.
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I need concrete steps.Thanks a lot in advance. 
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Continue with the SWAT & KINEROS tutorial in the AGWA extension
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SWAT Model input data for discharge projection to 2100, RCPs 4.5 and 8.5
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hello, how about your work progress? I also study swat model combining sdsm, but i don't know how to add downcasling data from sdsm into swat?
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The aim is to calibrate SWAT model with soil moisture. How to prepare the remote sensing soil moisture data for the calibration? Is the data has to be converted to mean value of the selected basin or some other way? Secondly, if there is any way to calibrate SWAT model using SWAT-CUP with the remote sensing data?
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1. SWAT reports soil water content (mm) data in the output.hru file. To calibrate SW, you can prepare the SW data of the HRU(s) which you have the SW data available by referring to the example data in the SWAT-CUP.
2. Since you are going to calibrate the data at HRU level, you will need to calculate the mean value of SW for the HRU(s).
3. I guess you need to convert your remote sensing data into numerical values in order to use it for calibration/validation in SWAT-CUP. You can use the intercept function in AcrMap to determine which HRU(s) your data belongs to by intercepting the HRU map with the SW map.
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Hi everyone!
I am modelling runoff using SWAT for the first time. The results indicate that the baseflow is very low. And, simulated runoff peaks in March. How should I adjust parameters?
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I think you can also try to use SWAT-CUP to calibrate your model.
Good luck!
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What is the best model for study effects of Land use change and climate change on Water Resources During the Future Period Except from SWAT model?
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Dear Mohammad, you can use HBV light (available in public domain), it can assess the impacts of climate change and static land cover on the discharge.
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Dear Researchers,
I have calibrated and validated my swat project for a particular Landuse rasyer data set.
Now, I want to develop Landuse change Scenarios in this swat project.
Plz guide me.
Kind Regards
Naveed
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Hi Naveed Ahmed. I normally analyze LU change scenarios as follows. First I calibrate and validate SWAT with the current LU scenario or whatever your baseline scenario is. Next I will re-run the model but modifying the LU input raster according with the scenarios of interest, and using the calibrated parameters that you came up with during the Calibration process. This approach implies that you create your scenarios of interest out of the model according with the problem that you want to analyze. One simple example would be analyzing a deforestation risk map you may identify future scenarios. SWAT also allows you to analyze BMP inside the model.
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Dear Researchers,
I have created the soil user file and now working of LULC file. I have done almost all only remaining are following:
Townland and
Ruralland
Both belongs to urban landcover, so its code must come from Urban database and accordingly code ID will be assigned in the user define Land-use text file. AM I right?
Secondly, Desert, Dryland and Plaindryland I am still struggling how to replace them from the land cover closest category.
Could you please guide me how to fix these problems.
Thanks in anticipation.
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Dear Researchers,
I would like to ask that Is it true that the calibration and validation data period must be same for hydrological modelling of a complex watershed?
For example; we choose 15 years calibration period and we have to choose 15 years for validation...
Or
If someone use 7 years for calibration because the last year of the calibtation duration is the turning point (afte this year there was a significant increase/decrease of flows ) and can he use 20 years for validation.
Thanks
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Hi Naveed,
There is no rule that they must have equal lengths.
For example, if I have a data spanning 1970 to 2010, I would divide it into three parts.
My calibration would be 1975 to 1990, 5 years as warm up, then, my validation will be divided into two independent periods to assess the robustness of your calibration parameters. I would choose 1991 to 2000 as validation period one, 2001 to 2010 as validation period two.
If the model is actually a good one, I should still have relatively good performances for the two validation periods. However, if you do not have long span of data, you may use a validation period.
Having two validation periods is a test of model robustness.
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Hi,
I am evaluating the impacts of riparian buffer (buffer width = 100ft) BMP on sediment output at the subbasin level by using SWAT model. First, I developed and calibrated a SWAT model for the watershed with an original land use map. Then I created another SWAT model with a modified land use map which converted riparian buffer zone to forest land use (forest land use has the lowest SCS curve number among all exiting land use types found in my watershed). And then I incorporated the calibrated parameters in the SWAT model with modified land use map and do the simulation. When comparing the percent change in subbasin sediment output, I found out that several subbasins have shown an increase in sediment output when the riparian buffer was implemented. I can't think of any reason why this would happen. Has anybody encounter the same issue in their research? What are the possible explanation for that? Or is there any problem regarding to my riparian buffer setup?
Thank you very much in advance for answering my questions.
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Unsure, but the practices of land use conversion can sometimes emerge in some models. Changing land use to forestry, may include a practice called site prep, before planting trees. Site prep can include soil scarification or other practices which could temporarily increase sediment. If a road is within buffer zone, it would be decommissioned, smoothed or otherwise stabilized That could cause soil disturbance and erosion temporarily or short term before functionally stable. I dont know SWAT well enough to know what assumptions it might be making when a land conversion is essentually prescribed. At any rate, it is theoretically possible to have some sediment increases as a result of implementing conversion or restoration practices, but these are typically temporary or short term, while in long term, as you and others suggest, sediment should decrease with proper functioning buffers.
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Is it possible to adopt one-year data in the SWAT model, and then compare the results of each year with other years?
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You can take two year and give one year warm-up period and do daily calibration
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Hello Dear SWAT-CUP users / experts
so, to sketch my problem here,
I am working on a SWAT model of a nival/glacier regime Arctic catchment. A big part of a recharge is snow/ice melt. My main goal is to calibrate the discharges (FLOW_OUT). I do not care about sediments/nutrients here.
I finished creating the model, and I started to learn SWAT-CUP.
I already know the basics and with that knowledge I have chosen a set of parameters to calibrate the model. (and method: SUFI)
Here, I would want you to take a look at the parameters as well as on the dotty plots.
I have a little struggle with interpreting dotty plots results. I know that I must look for some trend in the case of parameter sensitivity. no trend = no sensitivity, right?
I am adding 3 screenshots here.
First (1st iteration), with parameter ranges of my own choice.
Second (2nd iteration), with first "new_pars" suggestions from calibration output.
Third (3rd iteration), with second "new_pars" suggestion after running 2nd iteration.
number of simulations = 10.
I know the number should be bigger, I did 100 simulations once and dotty plots looked pretty bad in my opinion...Pretty much structureless graphs with no trend.
Also, I have a question about the calibration and validation periods.
My SWAT model run period is 2004 - 2017 (3 years of warm up).
I have a field discharge data from 2007 - 2012 and from 2017.
Now, I don't really know how to handle the calibration and validation periods.
The screenshots I add here are from the 2007 - 2017 SWAT-CUP run. But now I'm thinking, maybe I should do the calibration period for 2007 - 2012 and validation period for 2017 only?
Please, let me know what you think. Thanks in advance.
list of the parameters I've chosen:
v__SHALLST.gw 0 1500
a__GW_DELAY.gw -10 10
v__ALPHA_BF.gw 0.5 1
v__GWQMN.gw 0 500
v__GW_REVAP.gw 0.02 0.2
v__REVAPMN.gw 0 400
v__CH_L2.rte 5 10
v__CH_D.rte 0.2 3
v__CH_N2.rte 0.05 0.1
v__CH_K2.rte 25 300
v__CH_COV1.rte 0 1
v__CH_COV2.rte 0.5 1
v__ESCO.hru 0.01 1
v__SNO_SUB.sub 0 200
v__SFTMP.bsn -15 1
v__SMTMP.bsn -0.01 0.01
v__SMFMX.bsn 0 20
v__SMFMN.bsn 0 10
v__TIMP.bsn 0 1
v__SNOCOVMX.bsn 0 500
v__SNO50COV.bsn 0.05 0.8
v__LAT_TTIME.hru 0 2
v__CN2.mgt 70 90
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Well,
2/3 for calibration
1/3 for validation
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Hi
I am running SWAT CUP to calibrate stream flow(Observed) in a basin. When I am ran the simulations in SWAT CUP, it is giving single set of parameter values(like one value of: curve number, Ground water recharge.... etc).
As we know SWAT is Semi-distributed model., it should give distributed values. I have 61 sub basins in my study area, Is it possible to get 61 curve number values at every sub basin because every sub basin have different curve number values ? . Why it is not giving curve number for every sub basin.
Is it possible to classify basin according to every individual sub basin curve numbers?
and if we want to give individual curve number for sub basins, how to give that is SWAT model to run the model?
By the way I am calibrating only stream flow at final outlet basin.
Thanks in advance
Best Regards,
D. K . Rao.
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Well,
Before the creat SWAT CUP, click on the sub-basin that you want to simulate
and then create new file in SWATCUP and you change the value of CN2
Good luck
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Hello. I'm preparing the inputs for an SWAT model and am having trouble with solar radiation unit conversion. The data supplied is from a Davis Vantage Pro 2 Solar Sensor and records Solar Radiation in W/m^2 every 5 minutes. In SWAT, solar radiation data must be in MJ/m^2 (daily total). Is it possible to convert the supplied data into the units required by SWAT? If so, may I ask how? Any response will be appreciated. Thank you very much.
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Hi Nick,
It is obvious that J is the unit of Energy while, W is the unit of power (Energy rate) and time duration becomes important. Therefore, it depends on the time scale you want to calculate the power of the sun based on. For example, if you want to calculate the power of the sun during one hour (J/h=J/3600s=1/3600 W), then you must divide the data in J to 3600s to have power in W=J/s. You can extend the time scale even to a day through this method.
Best,
Shiva
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Dear All,
Could you please show me Evapo-transpiration data format to use for swat model in the read-in pet method?
regards,
mesget
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Syntax:
Title ????????????
Year (i4= 4 integers) Date (i3 = 3 integers of day of year) PET (f5.1 = as a float)
Example
PET file for a Random Watershed
2018001001.5
2018002002.3
...