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Flood Simulation Using Weather Forecast & Hydrological Models. PDF

68 Pages·2015·5.14 MB·English
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Flood Simulation using Weather Forecasting and Hydrological Models Thesis submitted to the Andhra University, Visakhapatnam in partial fulfilment of the requirement for the award of Master of Technology in Remote Sensing and GIS. Submitted By: Mr. Pratiman Patel Supervised By: Dr. Shiv Prasad Aggarwal Dr. Praveen Kumar Thakur Head Scientist/ Engineer ‘SE’ Water Resources Department, Water Resources Department, Indian Institute of Remote Sensing Indian Institute of Remote Sensing Dehradun Dehradun Indian Institute of Remote Sensing, Indian Space Research Organnization, Dept. of Space, Govt. of India, Dehradun – 248001 Uttarakhand, India June, 2015 ACKNOWLEDGEMENT I would first and foremost like to express my deepest sense of gratitude to our respected director, Dr. A. Senthil Kumar, for his continuous encouraging suggestions and support during the research which from time to time has led us to rethink and establish our goals and objectives in a defined way. I would also like to thank Dr. Y.V.N. Krishna Murthy, former Director, IIRS for his valuable suggestions at the time of synopsis too. I would like to express my special thanks of gratitude to my supervisors Dr. Shiv Prasad Aggarwal, Head, Water Resources Department and Dr. Praveen Kumar Thakur, Scientist/Engineer ‘SE’, Water Resources Department, IIRS, who gave me the golden opportunity to do this project on the topic “Flood Simulation using Weather forecasting and Hydrological Models”, which also helped me in doing a lot of Research and I came to know about so many new things. I am really thankful to them. I would like to thank to Dr. Bhaskar R. Nikam, Dr. Vaibhav Garg and Mr. Arpit Chouksey who helped in understanding various subjects during the course work. They have provided support in various forms. Their suggestions always have been very important to me. I would like to thank Andhra University for providing Master of Technology Degree in Remote Sensing and GIS. Along with this, I would also like to thank Dr. S.P.S. Kushwaha, Dean (Academics), Dr. S.K. Saha former Dean (Academics) and Ms. Shefali Agarwal, M.Tech Course Director, Indian Institute of Remote Sensing, Dehradun for providing an opportunity to do this research. I would like to thank Hydrologic Engineering Center (HEC) and WRF community for providing the HEC-HMS, HEC-GeoHMS and source code of WRF-ARW, WRF-Hydro, MET and NCL scripts respectively. Special thanks to Central Water Commission (CWC) for providing the discharge data of Joshimath and Uttarkashi for model calibration and validation. I would not be withstanding the course without the help of my friends Vikrant, Surya, Ram, Raja, Abhishek Saikia, Prakit, Sanjay, Neeraj, K.D., Sukant, Sakshi, Richa, Raunak, Rohit sir and all others. Their friendship supported me a lot and the time with them can never be forgotten. Lastly my moral supporters my family, grandparents, mom, dad & prateek for their utmost care and concern. They are real motivation to me, without them I would have never thought of completing this project. Date: 16 June 2015 Pratiman Patel II CERTIFICATE This is to certify that Mr. Pratiman Patel has carried out the dissertation entitled “Flood simulation using weather forecasting and hydrological model” in partial fulfilment of the requirements for the award of Master of Technology in Remote Sensing and GIS. This work has been carried out under the supervision of Dr. Shiv Prasad Aggarwal, Head, Water Resources Department and Dr. Praveen Kumar Thakur, Scientist/Engineer ‘SE’, Water Resources Department, Indian Institute of Remote Sensing, Indian Space Research Organisation, Dehradun, Uttarakhand, India. Dr. Shiv Prasad Aggarwal Dr. Praveen Kumar Thakur Head Scientist/ Engineer ‘SE’ Water Resources Department, Water Resources Department, Indian Institute of Remote Sensing, Indian Institute of Remote Sensing, Dehradun Dehradun Dr. S.P.S. Kushwaha Dr. A. Senthil Kumar Dean (Academics) Director Indian Institute of Remote Sensing, Indian Institute of Remote Sensing, Dehradun Dehradun III DECLARATION I, Pratiman Patel hereby declare that this dissertation entitled “Flood Simulation using Weather forecasting and Hydrological Models” submitted to Andhra University, Visakhapatnam in partial fulfilment of the requirements for the award of Master of Technology in Remote Sensing & GIS, is my own work and that do the best of my knowledge and belief. It is a record of original research carried out by me under the guidance and supervision of Dr. Shiv Prasad Aggarwal, Head, Water Resources Department and Dr. Praveen Kumar Thakur, Scientist/Engineer ‘SE’, Water Resources Department, Indian Institute of Remote Sensing, Indian Space Research Organisation, Dehradun. It contains no material previously published or written by another person nor material which to a substantial extent has been accepted for the award of any other degree or diploma of the university or other institute of higher learning, except where due acknowledgement has been made in the text. Place: Dehradun Mr. Pratiman Patel Date: 16 June 2015 IV DEDICATED TO MY FAMILY V ABSTRACT Floods are among one of the most common disaster that happen all around the world, every year. In mountainous areas flash floods are very common phenomenon due to heavy precipitation, cloud burst, landslide, or glacier lake outburst. In this research project, flash floods prediction due to heavy precipitation is being simulated using a weather forecasting model (WRF-ARW) for precipitation prediction and uncoupled hydrological model for rainfall-runoff (HEC-HMS) and hydrodynamic (MIKE 11) modelling. Weather forecasting model (WRF) is parameterized for land use/ land cover, topographical data and six microphysics and cumulus schemes combinations. These parameters are used for simulating three past events of cloud bursts i.e. 01 Aug 2012, 13 September 2012 and 13 June 2013. These parameters are validated for accuracy, probability of detection and false alarm ratio using IMD grids of rainfall and TRMM (3B42 v7 3 hourly product). The most suitable parameters are MODIS land use/ land cover and WRF Double Moment 6 Class Scheme with Grell 3D as microphysics and cumulus schemes respectively. The best output of WRF is selected for hydrological modelling. Hydrological is performed for uncoupled and coupled models (WRF-Hydro). HEC-HMS is calibrated and validated before using it for results obtained from WRF. The results of HEC-HMS model for WRF outputs are compared with TRMM 3B42 v7 3-hourly product. There is a clear under prediction and time shift of WRF outputs with the TRMM product. This effect is also observed in the hydrodynamic model. For coupled model, the results are not satisfactory for the current version of WRF-Hydro. The results obtained are very promising for uncoupled mode but there is further improvement required for precipitation prediction. Keywords: Flood forecasting, WRF, rainfall-runoff modelling, hydrodynamic modelling, uncoupled modelling, coupled modelling. VI TABLE OF CONTENTS Sr. No. Title Page No. 1. Introduction 1 1.1 Research questions 2 1.2 Objective 2 2. Literature Review 3 2.1 Numerical Weather Prediction (NWP) 3 2.2 GIS based Hydrologic and Hydrodynamic Modelling 6 2.3 Digital Elevation Models 7 2.4 Flood 8 3. Study area and data used 10 4. Methodology 16 4.1 Model Overview 16 4.2 Overall Methodology 26 5. Results and Discussions 40 6. Conclusion and Recommendation 52 7. References 53 8. Appendix 1 56 VII LIST OF FIGURE AND TABLES List of figures: Figure 3.1: Map showing the study area with major rivers and important 12 locations. 12 Figure 3.2: FCC of Landsat 8 for the study area. 13 Figure 3.3: Land Use/ Land Cover of the study area. 13 Figure 3.4: Soil map of the study area. 14 Figure 3.5: CartoDEM of the study area. 14 Figure 3.6: AWiFS land use/ land cover for domain 03 of WRF. 15 Figure 3.7: MODIS land use/ land cover for domain 03 of WRF. 15 Figure 3.8: USGS land use/land cover of domain 03 for WRF. 16 Figure 4.1: ARW n coordinate Figure 4.2: Flow diagram for WRF. 17 Figure 4.3: SCS unit hydrograph. 20 Figure 4.4: Calculation of cross-sectional area for relative roughness not equal to 1.0. a) Highest water level above maximum specified elevation b) 23 Highest water level below maximum specified elevation Figure 4.5 Channel section with computational grid 25 26 Figure 4.6: WRF Hydro architecture showing various components. 26 Figure 4.7: Calling structure of WRF-Hydro 27 Figure 4.8: Flowchart showing overall methodology. 28 Figure 4.9: Domain Configuration of WRF. Figure 4.10: Geogrid description in namelist.wps for use of MODIS 29 LULC. 30 Figure 4.11: GEOGRID.TBL for SRTM DEM. Figure 4.12: A. CARTOSAT DEM of the area. B. CN Map generated from 32 LULC & soil Map. C. Impervious Map generated from ISAT-tool. D. Initial Abstraction Map generated from LULC & soil map. VIII Figure 4.13: Watershed and River network delineated from HEC- 33 GeoHMS. 33 Figure 4.14: HEC-HMS model setup. 34 Figure 4.15: Flowchart showing MIKE 11 Methodology. 35 Figure 4.16: Network File of MIKE 11. 35 Figure 4.17: Cross-section file of MIKE 11. 36 Figure 4.18: Channel grid for WRF-Hydro. 37 Figure 4.19: Flow direction grid for WRF-Hydro. 37 Figure 4.20: Land use/ Land Cover for WRF-Hydro. 38 Figure 4.21: Latitude grid for WRF-Hydro. 38 Figure 4.22: Longitude grid for WRF-Hydro. 39 Figure 4.23: Stream order grid for WRF-Hydro. 39 Figure 4.24: Topographic grid for WRF-Hydro. Figure 5.1: USGS LULC comparison with different microphysics and 40 cumulus schemes for 17 June 2013. Figure 5.2: MODIS LULC comparison with different microphysics and 40 cumulus schemes for 17 June 2013. Figure 5.3: Difference image of TRMM and WRF results for USGS & 41 MODIS LULC with different microphysics and cumulus schemes for 13- 17 June 2013. Figure 5.4: WRF model comparison for different microphysics and 42 cumulus schemes for 15 June 2013. Figure 5.5: IMD and WRF grid difference of different microphysics and 42 cumulus schemes for 17 June 2013. Figure 5.6: Difference images of TRMM and WRF for different 43 microphysics and cumulus schemes (1-3 Aug 2012). Figure 5.7: Difference images of TRMM and WRF for different 43 microphysics and cumulus schemes (13-15 Sep 2012). Figure 5.8: WRF model comparison for different microphysics and 44 cumulus schemes for 03 August 2012. Figure 5.9: WRF model comparison for different microphysics and 44 cumulus schemes for 15 September 2012. Figure 5.10: Hydrograph comparison of simulated and observed runoff at 45 Uttarkashi and Joshimath for year 2005. Figure 5.11: Hydrograph comparison of simulated and observed runoff at 45 Uttarkashi and Joshimath for year 2006. Figure 5.12: Hydrograph comparison of simulated and observed runoff at 46 Uttarkashi and Joshimath for year 2007. IX 46 Figure 5.13: Hydrograph comparison of TRMM & WRF at Uttarkashi. 47 Figure 5.14: Hydrograph comparison of TRMM & WRF at Devprayag. 47 Figure 5.15: Hydrograph comparison of TRMM & WRF at Joshimath. 48 Figure 5.16: Hydrograph comparison of TRMM & WRF at Rudraprayag. 48 Figure 5.17: Hydrograph comparison of TRMM & WRF at Haridwar. 49 Figure 5.18: Hydrograph comparison for different Curve Number Values. Figure 5.19: Stage comparison of WRF and TRMM at Uttarkashi and 50 Devprayag stations. 51 Figure 5.20: Hydrograph at Haridwar for WRF-Hydro. List of tables: Table 2.1: Scale definitions of some important atmospheric events. 3 Table 2.2: Major cloud bursts events in Uttarakhand in 2012 8 Table 3.1: Bands in Landsat 8. 11 Table 4.1: Combination for USGS & MODIS land use land cover 28 parameterization simulations. Table 4.2: Combinations for full parameterization. 29 Table 5.1: Curve Number Values for sub-watershed. 49 Table A1.1: Geogrid configuration for domain. 57 Table A1.2: Time information 57 Table A1.3: Domain configuration for namelist.input 57 Table A1.4: Common physics options for all full parameter simulations. 58 Table A1.5: Common physics options for land use land cover 58 simulations. X

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work has been carried out under the supervision of Dr. Shiv Prasad Aggarwal, Head, Water. Resources Department Resources Department, Indian Institute of Remote Sensing, Indian Space Research .. phenomena. For example, planetary waves travel at speed of 10 m/s and gravity waves at 300.
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