TECHNICAL PAPERS
Nov 1, 2007

Storm Event and Continuous Hydrologic Modeling for Comprehensive and Efficient Watershed Simulations

Publication: Journal of Hydrologic Engineering
Volume 12, Issue 6

Abstract

Based on recent reviews of 11 physically based watershed models, the long-term continuous model soil and water assessment tool (SWAT) and the storm event dynamic watershed simulation model (DWSM) were selected to examine their hydrologic formulations, calibrate, and validate them on the 620km2 watershed of the upper Little Wabash River at Effingham, Ill., and examine their compatibility and benefits of combining them into a more comprehensive and efficient model. Calibration and validation of the SWAT by comparing monthly simulated and observed flows and adjusting the model-assigned resulted in coefficients of determination and Nash–Sutcliffe coefficients for individual years and cumulatively for the calibration period (1995–1999) and for the entire simulation period (1995–2002) mostly above or near 0.50 with an exception of 0.05 and 0.27 , respectively, in 2001, relatively a dry year. Visual comparisons of the hydrographs showed SWAT’s weakness in predicting monthly peak flows (mostly underpredictions.) Therefore, SWAT needs enhancements in storm event simulations for improving its high and peak flow predictions. Calibration of DWSM was not necessary; its three physically based parameters were taken from SWAT. Validation of DWSM on three intense storms in May 1995, March 1995, and May 2002 resulted 1, 29 , and 16% errors in peak flows and 0, 11 , and 0% errors in times to peak flows, respectively. Comparisons of DWSM’s 15-min flow hydrographs with SWAT’s daily flow hydrographs along with the 15-min and daily observed flow hydrographs during the above three storms confirmed that DWSM predicted more accurate high and peak flows and precise arrival times than SWAT. DWSM’s robust routing scheme using analytical and approximate shock-fitting solutions of the kinematic wave equations was responsible for the better predictions, the addition of which along with its unique combination with the popular runoff curve number method for rainfall excess computation to SWAT would be a significant enhancement. Parameters and data of both the models are interchangeable and, therefore, are compatible and their combination will result in a more comprehensive and efficient model.

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Acknowledgments

This paper is based on research supported by the Midwest Technology Assistance Cent (MTAC) and the Illinois State Water Survey (ISWS). Any opinions, findings, and conclusions recommendations expressed in this paper are those of the authors and do not necessarily reflect the views of ASCE, MTAC, or ISWS. Mention of products or commercial services does not reflect endorsement by the authors, ASCE, MTAC, or ISWS.

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Go to Journal of Hydrologic Engineering
Journal of Hydrologic Engineering
Volume 12Issue 6November 2007
Pages: 605 - 616

History

Received: Jan 24, 2006
Accepted: Nov 27, 2006
Published online: Nov 1, 2007
Published in print: Nov 2007

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Authors

Affiliations

Deva K. Borah, M.ASCE
Senior Project Manager, Woolpert Inc., 415 Port Centre Parkway, Suite 101, Portsmouth, VA 23704-4924 (corresponding author). E-mail: [email protected]
Jeffrey G. Arnold
Agricultural Engineer and Research Hydraulic Engineer, USDA-ARS Grassland Soil and Water Research Laboratory, 808 East Blackland Rd., Temple, TX 76502. E-mail: [email protected]
Maitreyee Bera
Senior Modeler, Borah Hydro-Environmental Modeling, 2812 Valley Brook Drive, Champaign, IL 61822-7621. E-mail: [email protected]
Edward C. Krug
Biogeochemist, Office of the Chief, Illinois State Water Survey, IDNR & UIUC, 2204 Griffith Dr., Champaign, IL 61820-7495. E-mail: [email protected]
Xin-Zhong Liang
Professional Scientist, Center for Atmospheric Science, Illinois State Water Survey, IDNR and UIUC, 2204 Griffith Dr., Champaign, IL 61820-7495. E-mail: [email protected]

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