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A Comparison of a SWAT A Comparison of a SWAT model for the model for the
Cannonsville Watershed Cannonsville Watershed with and without Variable with and without Variable
Source Area HydrologySource Area HydrologyJosh WoodburyJosh Woodbury
Christine A. ShoemakerChristine A. ShoemakerDillon CowanDillon Cowan
Zachary EastonZachary Easton
OutlineOutline
SWAT2005 vs SWAT-VSASWAT2005 vs SWAT-VSA Calibration Calibration Corn analysisCorn analysis ConclusionConclusion Questions ?Questions ?
SWAT2005 and SWAT-SWAT2005 and SWAT-VSAVSA
The current SWAT2005 version is a replication of the The current SWAT2005 version is a replication of the SWAT 2000 model developed by Bryan TolsonSWAT 2000 model developed by Bryan Tolson
Dillon Cowan replicated the SWAT 2000 files as Dillon Cowan replicated the SWAT 2000 files as closely as possible to create the current SWAT2005 closely as possible to create the current SWAT2005 versionversion This included creating the same number of subbasins with This included creating the same number of subbasins with
similar HRUssimilar HRUs Much time was spent insuring that the corn and pasture areas Much time was spent insuring that the corn and pasture areas
in each model are identicalin each model are identical Although corn is only a small percentage of the watershed, it Although corn is only a small percentage of the watershed, it
accounts for a significant percentage of the phosphorous loading accounts for a significant percentage of the phosphorous loading to the reservoirto the reservoir
Meticulous attention to corn area is important in order to create Meticulous attention to corn area is important in order to create an accurate model replicationan accurate model replication
Very time consuming since the watershed delineation did not Very time consuming since the watershed delineation did not create the correct amount of corn area because of the small create the correct amount of corn area because of the small percentagepercentage
SWAT2005 and SWAT-VSA
Source code changes done in the 2000 version (Tolson and Shoemaker, 2007, Jn of Hydrology) were also done in the 2005 source code Includes modifications to manure
spreading, plant growth, flow in/on frozen soils, and monthly subbasin temperatures
Tolson showed that these changes produce a better model
SWAT-VSA model
The SWAT-VSA model incorporates the model and file changes in the SWAT2005 model, as well as Variable Source Area Hydrology VSA hydrology is incorporated into the model
using the same techniques used to create the Town Brook VSA model
Meticulously accounted for corn and pasture areas between the SWAT2005 and SWAT-VSA models
SWAT-VSA uses 10 different wetness classes
Why bother with VSA hydrology?
The VSA model will make different predictions concerning the spatial distribution of the nutrient transport than a non-VSA model
If we know where the runoff is coming from, we can make judgments about the best nutrient placement
Apply management practices to the model and see how this changes future predictions
We can compare the future predictions of SWAT2005 and SWAT-VSA to see if careful placement of nutrients changes nutrient loading to the reservoir
OutlineOutline
SWAT2005 vs SWAT-VSASWAT2005 vs SWAT-VSA CalibrationCalibration Corn analysisCorn analysis ConclusionConclusion Questions ?Questions ?
CalibrationCalibration
Both of the models are calibrated first for Both of the models are calibrated first for flow, then sediment and finally flow, then sediment and finally phosphorousphosphorous
The calibration period is from Jan. 1994 The calibration period is from Jan. 1994 to Dec. 1999to Dec. 1999
Auto-calibration and manual calibration Auto-calibration and manual calibration techniques are used to get the best fittechniques are used to get the best fit
Parameters used are based upon a Parameters used are based upon a sensitivity analysis done by Ryan Flemingsensitivity analysis done by Ryan Fleming
CalibrationCalibration
Firstly the models are calibrated using an Firstly the models are calibrated using an algorithm called DDSalgorithm called DDS DDS is a simple stochastic single-solution based DDS is a simple stochastic single-solution based
heuristic global search algorithm designed for heuristic global search algorithm designed for automatic calibration of watershed models automatic calibration of watershed models (Tolson and Shoemaker, WRR, 2007)(Tolson and Shoemaker, WRR, 2007)
DDS is used with a weighted Sum of DDS is used with a weighted Sum of Squared Error objective functionSquared Error objective function
SedSedFlow SSESSEOF
Sed
FlowSed SSE
SSE
CalibrationCalibration
Once flow and sediment are calibrated, Once flow and sediment are calibrated, Total Dissolved Phosphorous (TDP) and Total Dissolved Phosphorous (TDP) and Particulate Phosphorous (PP) are Particulate Phosphorous (PP) are calibrated using DDScalibrated using DDS
PPTDP SSESSEOF
Manual calibration techniques are then Manual calibration techniques are then used to slightly improve the modelsused to slightly improve the models
Calibration Many different attempts where made in
order to find the best way to calibrate for more than one output at a time The problem is that the SSE values for each of
the outputs vary by orders of magnitude By simply summing all the outputs, some of the
outputs are weighted more heavily than others This problem has plagued users trying to auto-
calibrate SWAT Most papers addressing the subject suggest using some
type of weighting scheme, either simple weighting factors, or complicated statistical weighting schemes
Calibration
Initially tried to calibrate for Flow, Sediment, PP and TDP at once Tried using weighting values, taking the natural
log of the data, and weighting the natural logs of the data in order to decrease the differences in magnitude
Eventually gave up on calibrating all four outputs at once and adopted the calibration method previously presented
This is still not the best way to auto-calibrate, as it still requires some manual calibration at the end
Results – Calibration Results – Calibration PeriodPeriod
SWAT2005 (Monthly)
Flow
Sediment
TDP PP
R – Squared 0.85 0.73 0.7 0.72
% Diff. 0.34 -3.3 -4.18 -6.22
SWAT-VSA (Monthly)
Flow
Sediment
TDP PP
R – Squared 0.84 0.73 0.72 0.53
% Diff. 0.44 -1.9 -4.77 -0.85
Calibration period: January 1994 to December 1999 Both models do well simulating the measured data Discrepancy in PP phosphorous results
SWAT model does better although both models do well with sediment
Results – Flow and Results – Flow and SedimentSediment
0
500
1000
1500
2000
2500
Jan-94
Apr-94
Jul-94
Oct-94
Jan-95
Apr-95
Jul-95
Oct-95
Jan-96
Apr-96
Jul-96
Oct-96
Jan-97
Apr-97
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Oct-97
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Apr-98
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Oct-98
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Apr-99
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Oct-99
cms
Measured
SWAT
VSA
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4000
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12000
Jan-94
Apr-94
Jul-94
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Apr-97
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Apr-99
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tonnes
Measured
SWAT
VSA
Flow Calibrations are quite good, both models capture trends
Models tend to over predict high flows and under predict low flows
Sediment Models do well with average loads, but tend to under predict high loadings
Some of this error can be attributed to flow error
Flow
Sediment
Results – Phosphorous Results – Phosphorous
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1000
2000
3000
4000
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6000
7000
8000
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10000
Jan-94
Mar-94
May-94
Jul-94
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Nov-94
Jan-95
Mar-95
May-95
Jul-95
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Nov-95
Jan-96
Mar-96
May-96
Jul-96
Sep-96
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Jan-97
Mar-97
May-97
Jul-97
Sep-97
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Jan-98
Mar-98
May-98
Jul-98
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Nov-98
Jan-99
Mar-99
May-99
Jul-99
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Nov-99
kg
Measured
SWAT
VSA
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5000
10000
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20000
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30000
Jan-94
Apr-94
Jul-94
Oct-94
Jan-95
Apr-95
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Jul-96
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Apr-97
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Apr-98
Jul-98
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Apr-99
Jul-99
Oct-99
kg
Measured
SWAT
VSA
TDP Both models do well with average loads, but tend to under predict high loads
Part of this error can be attributed to flow under predictionPP
SWAT2005 model does better than SWAT-VSA model
Interesting since PP is largely impacted by sediment, which is captured well by both models
TDP
PP
OutlineOutline
SWAT2005 vs SWAT-VSASWAT2005 vs SWAT-VSA Calibration Calibration Corn analysisCorn analysis ConclusionConclusion Questions ?Questions ?
Land Use Management Analysis
Since SWAT-VSA uses a combination of land use and wetness class to determine HRUs, we can look into the impact of moving different land uses
In this analysis, we looked at the impact of moving corn to low runoff generating areas, i.e. low wetness classes
Corn Analysis - Setup SWAT-VSA
All corn HRUs are changed to either wetness class 1 or 2
Turned corn wetness classes of 3 – 10 into hay or pasture
In order to keep total corn area constant, some hay and pasture wetness classes 1 and 2 were turned into corn
Meticulously kept track of each wetness class area as well as land use area
SWAT2005 All corn was turned into either hay or pasture of
the same soil type Only thing that can really be done with SWAT in
terms of land use
SWAT2005 Model without Corn
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Jan-94
Apr-94
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Model
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Jan-94
Apr-94
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Jul-95
Oct-95
Jan-96
Apr-96
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Apr-97
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tonnes
Model
Min
Flow % Difference = 0.23
There is no difference because overall CN did not change
Sediment % Difference = -33.5
Peak sediment loads are nearly cut in half, shows the impact of corn on the sediment loading
SWAT2005 Model without Corn
TDP % Difference = -38.4
Shows the large impact that corn has on TDP loading
PP % Difference = -71
large impact on PP is due to removal of corn as a direct source as well as the decrease in sediment loading
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1000
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7000
Jan-94
Apr-94
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Apr-95
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Apr-96
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Model
Min
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Jan-94
Apr-94
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Apr-95
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Jul-98
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kg
Model
Min
SWAT-VSA Model Corn Analysis
Flow % Difference = -0.07
Does not change because overall wetness class areas do not change
Sediment % Difference = -0.23
Does not change because decrease in sediment loading from corn is balanced by the increase in sediment loading from hay and pasture
0
200
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600
800
1000
1200
1400
1600
34335
34425
34516
34608
34700
34790
34881
34973
35065
35156
35247
35339
35431
35521
35612
35704
35796
35886
35977
36069
36161
36251
36342
36434
cms
Model
Min
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2000
3000
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6000
7000
Jan-94
Apr-94
Jul-94
Oct-94
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Apr-95
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Oct-95
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kg
Model
Min
SWAT-VSA Model Corn Analysis
TDP % Difference = -27.5
substantial decrease in peak loadings shows the impact of moving corn to areas of lower runoff
PP % Difference = -49
Since the overall sediment loadings do not change, this change in PP is directly due to moving corn areas
0
1000
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4000
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7000
Jan-94
Apr-94
Jul-94
Oct-94
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Apr-95
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Oct-95
Jan-96
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Jan-97
Apr-97
Jul-97
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Oct-99
kg
Model
Min
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10000
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14000
Jan-94
Apr-94
Jul-94
Oct-94
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Apr-95
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kg
Model
Min
Corn Analysis - conclusion
From the previous analysis, it is apparent that the location of corn areas has a significant impact on Phosphorous runoff
Analysis results make physical sense This type of nutrient reduction would occur in the
watershed if all corn is moved to low-runoff areas Although this is a best case scenario in terms of
nutrient reduction, it may not be entirely practical Moving corn to low-runoff areas may also reduce corn
yeild Need to find some trade-off point
OutlineOutline
SWAT vs SWAT-VSASWAT vs SWAT-VSA Calibration Calibration Corn analysisCorn analysis ConclusionConclusion Questions ?Questions ?
ConclusionConclusion SWAT-VSA and SWAT 2005 Models produce SWAT-VSA and SWAT 2005 Models produce
similar results based on available calibration data similar results based on available calibration data for the large 1200 kmfor the large 1200 km22 Cannonsville watershed. Cannonsville watershed.
Flow distributions can have important Flow distributions can have important implications for nutrient managementimplications for nutrient management
Management scenarios in SWAT-VSA can include Management scenarios in SWAT-VSA can include specific nutrient placement based on flow specific nutrient placement based on flow distributionsdistributions
SWAT-VSA will predict decreases in phosphorous SWAT-VSA will predict decreases in phosphorous transport when corn is placed mostly in dry areas.transport when corn is placed mostly in dry areas.
OutlineOutline
SWAT vs SWAT-VSASWAT vs SWAT-VSA Calibration Calibration Corn analysisCorn analysis ConclusionConclusion Questions ?Questions ?