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SIMULATION OF SUB-DAILY RUNOFF FOR AN
INDIAN WATERSHED USING ArcSWAT MODEL
T. Reshma1, K. venkata Reddy2, Deva Pratap3
2012 INTERNATIONAL SWAT CONFERENCE
NEW DELHI, INDIA
JULY 16-20, 2012
Introduction
 SWAT model is a hydro-dynamic and
physically-based hydrologic model.
 Geographic Information System (GIS)
provides the framework within which
spatially-distributed data are collected and
used to prepare model input files and to
evaluate model results.
2
Literature Review
 Arnold et al. (1999) presented two methods of
simulating excess rainfall on a large basin with
multiple rain gages and compared the
simulations.
 Simic et al. (2009) studied the application of
SWAT in modeling of the rainfall runoff
Process.
 Arnold et al. (2010) presented the development
and testing of a sub-hourly rainfall–runoff
model in SWAT.
3
Objectives
 The objective of the study is to simulate the
sub-daily runoff using ArcSWAT model.
 Harsul watershed has been selected and
relevant hydrological data has been collected.
 Remotely sensed data and GIS have been used
to prepare the thematic maps of the watershed.
4
Methodology
Selection of watershed Remotely sensed data and GIS
Preparation of thematic maps viz.
Land use/Land covers map, soil
map, DEM map and drainage map
of watershed
Hydrological data
collection of a
Watershed
Simulation of
sub- daily runoff
using ArcSWAT
Model
5
Methodology Flowchart
6
Location map and Study area of the Harsul Watershed
Harsul watershed is located in
Nashik district, Maharashtra, India.
The watershed has an area of
10.929 sq. km.
It is situated between East
Longitude of 73º 25´ and 73º 29´
and the North Latitudes of 20º 04´
and 20º 08´.
SWAT Model Description
 The model setup involves the following five
steps:
 Watershed delineation
 HRU definition
 Weather data definition
 Edit SWAT input
 Run SWAT.
7
Menu for Automatic Delineation of Watershed in ArcSWAT model
8
Menu for Hydrologic Response Unit Analysis in ArcSWAT model
9
Menu for Weather Data Definition in ArcSWAT model
10
Menu for Setup and Run SWAT model simulation
11
SWAT Model Application
12
Automatically delineated sub-basins
Harsul watershed
Modified Slope map of
Harsul watershed
Modified Soil map of Harsul Watershed Modified LU/LC map of Harsul
Watershed
13
14
Simulated and Observed hydrographs for the Harsul
watershed ( July 1997)
Results and Discussions
15
Simulated and Observed hydrographs for the Harsul
watershed
(September 1997)
Simulated and Observed hydrographs for the Harsul watershed
( August 1997)
16
17
Rainfall
months
Volume of runoff
(mm)
Peak runoff (m3/sec) Time to peak (Hour)
Observed Simulated Observed Simulated Observed Simulated
July, 1997 307.76 242.21 104.784 12.9 723 730
August,1997 143.24 247.36 4.437 1.67 91 91
September,
1997
16.71447 47.42 5.935 2.37 551 623
Table 1. Simulation results for Harsul watershed
Conclusions
 The model has been applied for the three month’s
rainfall data.
 From the simulations, it is observed that, the
model is able to simulate the volume of runoff
and time to peak runoff. But large variations are
observed in peak runoff.
 This may be because of inexactness in the values
of parameters.
 It is also observed that sensitivity analysis has to
be carried out to improve the simulation results.
 The methodology presented in this study is useful
to simulate hourly runoff in Indian watersheds
using ArcSWAT models.
18
References
 Arnold, J.G., R. Srinivasan, R. Jayakrishnan, and C. Santhi. 2005. Advances in the application of the
SWAT model for water resources management. Hydrological Processes. 19, 749-762.
 Birhanu, B.Z., P.M. Ndomba, and F.W. Mtalo. 2007. Application of SWAT Model for Mountainous
Catchment. Catchment and Lake Research.
 Bijan. D., R. Srinivasan, and G.S. Shimelis. 2008. Hydrological Modelling in the Lake Tana Basin,
Ethiopia Using SWAT Model. The Open Hydrology Journal, 2, 49-62.
 Jeong. J., N. Kannan, J. Arnold, R. Glick, L. Gosselink, and R. Srinivasan.2010. Development and
Integration of Sub-hourly Rainfall–Runoff Modeling Capability Within a Watershed model. Water
Resour Manage. Accepted: 6 May.
 Reshma T., K. Venkata Reddy and Deva Pratap. 2011. Simulation of runoff of a watershed using
ArcSWAT model. In Proc. International Conference on Spatial Technologies for Rural
Development/Watershed Development.
 Srinivasan, R., X. Zhang, and J. Arnold. 2010. SWAT ungauged: hydrological budget and crop yield
predictions in the upper mississippi river basin. American Society of Agricultural and Biological
Engineers. Vol. 53(5): 1533-1546.
 Venkata Reddy. K, Eldho. T. I, Rao. E.P. and Kulkarni, A.T. (2011), FEM-GIS based channel
network model for runoff simulation in agricultural watersheds using remotely sensed data,
International Journal of River Basin Management, 9(1), 17-30.
19
Thank u
20

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g1-3-reshma.pdf

  • 1. SIMULATION OF SUB-DAILY RUNOFF FOR AN INDIAN WATERSHED USING ArcSWAT MODEL T. Reshma1, K. venkata Reddy2, Deva Pratap3 2012 INTERNATIONAL SWAT CONFERENCE NEW DELHI, INDIA JULY 16-20, 2012
  • 2. Introduction  SWAT model is a hydro-dynamic and physically-based hydrologic model.  Geographic Information System (GIS) provides the framework within which spatially-distributed data are collected and used to prepare model input files and to evaluate model results. 2
  • 3. Literature Review  Arnold et al. (1999) presented two methods of simulating excess rainfall on a large basin with multiple rain gages and compared the simulations.  Simic et al. (2009) studied the application of SWAT in modeling of the rainfall runoff Process.  Arnold et al. (2010) presented the development and testing of a sub-hourly rainfall–runoff model in SWAT. 3
  • 4. Objectives  The objective of the study is to simulate the sub-daily runoff using ArcSWAT model.  Harsul watershed has been selected and relevant hydrological data has been collected.  Remotely sensed data and GIS have been used to prepare the thematic maps of the watershed. 4
  • 5. Methodology Selection of watershed Remotely sensed data and GIS Preparation of thematic maps viz. Land use/Land covers map, soil map, DEM map and drainage map of watershed Hydrological data collection of a Watershed Simulation of sub- daily runoff using ArcSWAT Model 5 Methodology Flowchart
  • 6. 6 Location map and Study area of the Harsul Watershed Harsul watershed is located in Nashik district, Maharashtra, India. The watershed has an area of 10.929 sq. km. It is situated between East Longitude of 73º 25´ and 73º 29´ and the North Latitudes of 20º 04´ and 20º 08´.
  • 7. SWAT Model Description  The model setup involves the following five steps:  Watershed delineation  HRU definition  Weather data definition  Edit SWAT input  Run SWAT. 7
  • 8. Menu for Automatic Delineation of Watershed in ArcSWAT model 8
  • 9. Menu for Hydrologic Response Unit Analysis in ArcSWAT model 9
  • 10. Menu for Weather Data Definition in ArcSWAT model 10
  • 11. Menu for Setup and Run SWAT model simulation 11
  • 12. SWAT Model Application 12 Automatically delineated sub-basins Harsul watershed Modified Slope map of Harsul watershed
  • 13. Modified Soil map of Harsul Watershed Modified LU/LC map of Harsul Watershed 13
  • 14. 14 Simulated and Observed hydrographs for the Harsul watershed ( July 1997) Results and Discussions
  • 15. 15 Simulated and Observed hydrographs for the Harsul watershed (September 1997)
  • 16. Simulated and Observed hydrographs for the Harsul watershed ( August 1997) 16
  • 17. 17 Rainfall months Volume of runoff (mm) Peak runoff (m3/sec) Time to peak (Hour) Observed Simulated Observed Simulated Observed Simulated July, 1997 307.76 242.21 104.784 12.9 723 730 August,1997 143.24 247.36 4.437 1.67 91 91 September, 1997 16.71447 47.42 5.935 2.37 551 623 Table 1. Simulation results for Harsul watershed
  • 18. Conclusions  The model has been applied for the three month’s rainfall data.  From the simulations, it is observed that, the model is able to simulate the volume of runoff and time to peak runoff. But large variations are observed in peak runoff.  This may be because of inexactness in the values of parameters.  It is also observed that sensitivity analysis has to be carried out to improve the simulation results.  The methodology presented in this study is useful to simulate hourly runoff in Indian watersheds using ArcSWAT models. 18
  • 19. References  Arnold, J.G., R. Srinivasan, R. Jayakrishnan, and C. Santhi. 2005. Advances in the application of the SWAT model for water resources management. Hydrological Processes. 19, 749-762.  Birhanu, B.Z., P.M. Ndomba, and F.W. Mtalo. 2007. Application of SWAT Model for Mountainous Catchment. Catchment and Lake Research.  Bijan. D., R. Srinivasan, and G.S. Shimelis. 2008. Hydrological Modelling in the Lake Tana Basin, Ethiopia Using SWAT Model. The Open Hydrology Journal, 2, 49-62.  Jeong. J., N. Kannan, J. Arnold, R. Glick, L. Gosselink, and R. Srinivasan.2010. Development and Integration of Sub-hourly Rainfall–Runoff Modeling Capability Within a Watershed model. Water Resour Manage. Accepted: 6 May.  Reshma T., K. Venkata Reddy and Deva Pratap. 2011. Simulation of runoff of a watershed using ArcSWAT model. In Proc. International Conference on Spatial Technologies for Rural Development/Watershed Development.  Srinivasan, R., X. Zhang, and J. Arnold. 2010. SWAT ungauged: hydrological budget and crop yield predictions in the upper mississippi river basin. American Society of Agricultural and Biological Engineers. Vol. 53(5): 1533-1546.  Venkata Reddy. K, Eldho. T. I, Rao. E.P. and Kulkarni, A.T. (2011), FEM-GIS based channel network model for runoff simulation in agricultural watersheds using remotely sensed data, International Journal of River Basin Management, 9(1), 17-30. 19