Climate Change Impact on Water Resources of Upper

Total Page:16

File Type:pdf, Size:1020Kb

Climate Change Impact on Water Resources of Upper OPTIMAL CONTROL OF MULTIPLE RESERVOIRS SYSTEM UNDER WATER SCARCITY By Iftikhar Ahmad M.Sc (Geology) M.Phil (Hydrology) A thesis submitted in the fulfillment of requirements for the degree of Doctor of Philosophy INSTITUTE OF GEOLOGY UNIVERSITY OF THE PUNJAB, LAHORE-PAKISTAN 2009 OPTIMAL CONTROL OF MULTIPLE RESERVOIRS SYSTEM UNDER WATER SCARCITY By Iftikhar Ahmad M.Sc (Geology) M.Phil (Hydrology) Under the Supervision of Prof. Dr. Nasir Ahmad Ph.D. (U.K), M.Sc. (Pb) A thesis submitted to the Punjab University in the fulfillment of requirements for the degree of Doctor of Philosophy INSTITUTE OF GEOLOGY UNIVERSITY OF THE PUNJAB, LAHORE-PAKISTAN 2009 Dedicated to my family and brother CERTIFICATE It is hereby certified that this thesis is based on the results of modeling work carried out by Iftikhar Ahmad under our supervision. We have personally gone through all the data/results/materials reported in the manuscript and certify their correctness/ authenticity. We further certify that the materials included in this thesis have not been used in part or full in a manuscript already submitted or in the process of submission in partial/complete fulfillment for the award of any other degree from any other institution. Iftikhar Ahmad has fulfilled all conditions established by the University for the submission of this dissertation and we endorse its evaluation for the award of PhD degree through the official procedures of the University. SUPERVISOR SUPERVISOR Prof. Dr. Nasir Ahmad Prof. Dr. Zulfiqar Ahmad Director Institute of Geology Chairman Department of Earth Sciences University of the Punjab Quad-i-Azam University Lahore, Pakistan Islamabad, Pakistan i ABSTRACT The use of mathematical programming for short term (10-day) operation of Indus River System under uncertainty was investigated. A two stage mix optimization procedure was proposed for the stochastic optimization of the Indus River System. The first stage of the proposed procedure cycles through three main programs, a transition probability matrix (tmp) computation algorithm, a DDP-SDP (Deterministic-Stochastic Dynamic Programming) model and a simulation program. In DDP-SDP program, four model types and three objective types were investigated for multiresevoir system. These non-linear objectives were calibrated for the large scale complex system to minimize the irrigation shortfalls, to maximize the hydropower generation and to optimize the flood storage benefits. Simulation program was used for the validation of each policy derived through this cycle. The accumulation of these programs is called 10 day reservoir operation model of the multireservoir Indus River System. Various model types in SDP/DDP formulation may produce different results in different reservoir conditions and different hydrologic regimes. The model types are therefore system specific. For the Indus Reservoir System best fit SDP model type was identified, alternate multi objective functions were proposed and analysed. Taking one or two objectives and ignoring other or considering all the objectives to optimize, produced different results in different model types. Especially the results were significantly different in terms of storage contents of the reservoir during simulation. The proposed procedure identifies the best stochastic operational policies for the system under uncertainty. The second stage of proposed procedure uses advantages of the stochastic optimal policies derived in the first stage of the optimization with a Network Flow programming (NFP) model developed for the Indus River System for 10 day operation. The whole system was represented by a capacitated network in which nodes are reservoirs, system inflow locations or canal diversion locations. The nodes are connected with the arcs which represent rivers, canal reaches or syphons in the system. The maximum and minimum flow conditions were defined from the physical data. The NFP model was solved with the help of two main programs, the out of kilter algorithm and on line reservoir operation model with stochastic operating policies. The accumulation of these programs is called 10 day stochastic network flow programming (SNFP) model of the multireservoir Indus River System. The proposed SNFP model provides two main benefits. First, the incorporation of the stochastic operating policies at reservoir nodes controls the uncertainty and improves the system operation performance. The stochastic behaviour of the inputs and non-linear objectives in the linear programming model is incorporated in this way. Second, the complete system is under control and presents acomplete physical picture of the system. The results obtained from the above two stage procedure were verified with help of simulating the system with forecasted inflows and comparing these results with actual historic data record. For this purpose, 10 day forecasting models were investigated, calibrated and verified. The results also proved the methodology effective for the test case. The reservoir operation model is characterized as generalised and flexible model, and can be used for any other reservoir. The SNFP model is system (the Indus River System) specific to and needs minor modifications to be used for other water resource systems. ii The proposed optimization procedure presents the optimum operation of reservoirs for irrigation water supplies, hydropower production and flood protection, optimal allocation of water resources in the canal network of Indus River System and identifies the resource limitations at various locations in the system. While comparing with the historic data records, the model performance was found to be better than the historic data at all locations in the system during simulation. The complete model may be used as a guiding tool for the optimum 10 day operation of the Indus River System. A two stage frame work consisting of a steady state SDP 10 day reservoir operation model followed by a Network Flow model appears to be promising for the optimization of Indus River System. The model has also been used for future planning of water resources in Pakistan. The methodology developed provides a viable way of applying stochastic optimization into deterministic optimization procedure under multireservoir, multiobjective water resource system with 10 day operation under uncertainty. iii ACKNOWLEDGEMENTS I would like to extend my sincere thanks to my research supervisors, Prof. Dr. Nasir Ahmad (Director, Institute of Geology) and Prof. Dr. Zulfiqar Ahmad (Chairman, Department of Earth Sciences, Quid-e-Azam University, Islambad) for their keen interest, proficient guidance, valuable suggestions, and encouraging attitude during the course of this research work. Special recognitions go to Dr. S. M. Saeed Shah (Head of hydrology division, Centre of Excellence in Water Resources Engineering, University of Engineering and Technology Lahore) for his insightful suggestions while writing up this thesis. I am extremely grateful to Prof. Dr. Iftikhar Hussain Baloch (Principal, College of Earth and Environmental Sciences, University of The Punjab) for his cooperation and encouragement. I wish to thank many professional colleagues, specially Dr. Ashraf Malik, ex.Chief Hydrology, NESPAK, Dr. Muhammad Younas Khan, ex General Manager, Tarbela Dam WAPDA, and Dr. Maboob Alam, Director IWASRY WAPDA for their wise comments on the script. I thank to my University fellows, Mr. Muhammad Akhtar and Mr. Khursheed Alam for their co-operation. Finally, I would like to express my heartiest gratitude to my wife and children whose cooperation, prayers and well wishes strengthened my confidence to endure hardships faced during this study. iv LIST OF TABLES Table 4.1 Details of Indus Basin Rivers 124 Table 4.2 Hydraulic characteristics of Indus River and its tributaries 126 Table 4.3 Salient features of Jhelum river and its tributaries 128 Table 4.4 Hydraulic characteristics of tributaries of Ravi joining within Pakistan 132 Table 4.5 Hydraulic characteristics of important tributaries of Sutlej 132 Table 4.6 Water and Power benefits from Tarbela dam 139 Table 4.7 Water and Power benefits from Mangla dam 145 Table 4.8 Water benefits from Chasma reservoir 148 Table 4.9 Loss of reservoir capacities in MAF 149 Table 4.10 Summary of the basic Information of the Barrages located in the Indus Basin 153 Table 4.11 Indus zone and Jhelum Chenab Zone 154 Table 4.12 Average gains and losses of the 46 years of data 156 Table 5.1 Statistics of Annual Flows (Time series Oct-Sep) 161 Data Statistics, Consistency and Outliers in 10 Daily Inflows 1922-2004 Oct- Table 5.2 169 Sep, Jhelum at Mangla Data Statistics, Consistency and Outliers in 10 Daily Inflows 1961-2004 Oct- Table 5.3 170 Sep, Indus at Tarbela Table 5.4 Serial Correlation Coefficients 173 Table 5.5 Correlation Coefficients between 10 daily flows 174 Table 5.6 Transition Probability Matrix of Period August 1, Indus at Tarbela 176 Table 5.7 Variation of Rescale Range and Hurst Exponent 177 Table 5.8 Results of Gould transitional probability matrix method 179 v Table 5.9 Summary result from Rippl mass curve analysis 182 Table 5.10 Summary results of Sequent Peak Analysis 183 Table 5.11 Selected Regression Models for 10 day forecasting in Indus Rivers 199 Summary results for calibration of stochastic network flow programming model, Table 7.1 254 simulation period 1985-95. Sample result of calibration of SNFP model 10 day time period 10 year Table 7.2 255 simulation for 1985-1995 (values in 1000 x cfs) Summary results for validation of stochastic network
Recommended publications
  • Khyber Pakhtunkhwa - Daily Flood Report Date (29 09 2011)
    Khyber Pakhtunkhwa - Daily Flood Report Date (29 09 2011) SWAT RIVER Boundary 14000 Out Flow (Cusecs) 12000 International 10000 8000 1 3 5 Provincial/FATA 6000 2 1 0 8 7 0 4000 7 2 4 0 0 2 0 3 6 2000 5 District/Agency 4 4 Chitral 0 Gilgit-Baltistan )" Gauge Location r ive Swat River l R itra Ch Kabul River Indus River KABUL RIVER 12000 Khyber Pakhtunkhwa Kurram River 10000 Out Flow (Cusecs) Kohistan 8000 Swat 0 Dir Upper Nelam River 0 0 Afghanistan 6000 r 2 0 e 0 v 0 i 1 9 4000 4 6 0 R # 9 9 5 2 2 3 6 a Dam r 3 1 3 7 0 7 3 2000 o 0 0 4 3 7 3 1 1 1 k j n ") $1 0 a Headworks P r e iv Shangla Dir L")ower R t a ¥ Barrage w Battagram S " Man")sehra Lake ") r $1 Amandara e v Palai i R Malakand # r r i e a n Buner iv h J a R n ") i p n Munda n l a u Disputed Areas a r d i S K i K ") K INDUS RIVER $1 h Mardan ia ") ") 100000 li ") Warsak Adezai ") Tarbela Out Flow (Cusecs) ") 80000 ") C")harsada # ") # Map Doc Name: 0 Naguman ") ") Swabi Abbottabad 60000 0 0 Budni ") Haripur iMMAP_PAK_KP Daily Flood Report_v01_29092011 0 0 ") 2 #Ghazi 1 40000 3 Peshawar Kabal River 9 ") r 5 wa 0 0 7 4 7 Kh 6 7 1 6 a 20000 ar Nowshera ") Khanpur r Creation Date: 29-09-2011 6 4 5 4 5 B e Riv AJK ro Projection/Datum: GCS_WGS_1984/ D_WGS_1984 0 Ghazi 2 ") #Ha # Web Resources: http://www.immap.org Isamabad Nominal Scale at A4 paper size: 1:3,500,000 #") FATA r 0 25 50 100 Kilometers Tanda e iv Kohat Kohat Toi R s Hangu u d ") In K ai Map data source(s): tu Riv ") er Punjab Hydrology Irrigation Division Peshawar Gov: KP Kurram Garhi Karak Flood Cell , UNOCHA RIVER $1") Baran " Disclaimers: KURRAM RIVER G a m ") The designations employed and the presentation of b e ¥ Kalabagh 600 Bannu la material on this map do not imply the expression of any R K Out Flow (Cusecs) iv u e r opinion whatsoever on the part of the NDMA, PDMA or r ra m iMMAP concerning the legal status of any country, R ") iv ") e K territory, city or area or of its authorities, or concerning 400 r h ") ia the delimitation of its frontiers or boundaries.
    [Show full text]
  • Hydrological Modeling of Haro River Watershed, Pakistan
    IJRRAS 30 (1) ● January 2017 www.arpapress.com/Volumes/Vol30Issue1/IJRRAS_30_1_02.pdf HYDROLOGICAL MODELING OF HARO RIVER WATERSHED, PAKISTAN Mona A. Hagras 1 & Rasikh Habib 2 1 Faculty of Engineering, Ain Shamas University, Cairo, Egypt 2 National University of Sciences and Technology (NUST), Islamabad, Pakistan ABSTRACT Geographical Information System based semi distributed model, Soil and Water Assessment Tool (SWAT) is used to model the hydrology of Haro river watershed 40 kilometer North West Islamabad, Pakistan. Thus, it aims to simulate the stream flow, establish the water balance and estimate the monthly volume inflow to Khanpur dam located at the basin outlet. SWAT model was calibrated for a ten years period from 1994 to 2003 and validated for a seven years period from 2004 to 2010. Statistical indicators; Pearson Correlation, Coefficient of Determination and Nash-Sutcliffe Efficiency were used to verify the simulation abilities of the model. Results illustrate a good performance for both calibration and validation periods and acceptable agreement between measured and simulated values of both annual and monthly discharge. The water balance components were estimated and presented here for the studied watershed. Finally, it is concluded that SWAT model can be used in semi-arid regions for the water resources management of the studied watershed. Key words: Hydrological modeling, Soil and Water Assessment Tool, Haro River, Khanpur Dam. 1. INTRODUCTION Pakistan is classified as one of the extremely high level water stress country in the world (Tianyi Luo et al., 2015). Agriculture in Pakistan uses well over 95% of the freshwater resources in addition to the high losses in the sprawling irrigation system.
    [Show full text]
  • Geology of the Southern Gandghar Range and Kherimar Hills, Northern Pakistan
    AN ABSTRACT OF THE THESIS OF Michael D. Hylland for the degree of Master of Science in Geology presented on May 3. 1990 Title: Geology of the Southern Gandghar Range and Kherimar Hills. Northern Pakistan Abstract approved: RobeS. Yeats The Gandghar Range and Kherimar Hills, located in the Hill Ranges of northern Pakistan, contain rocks that are transitional between unmetarnorphosed foreland-basin strata to the south and high-grade metamorphic and plutonic rocks to the north. The southern Gandghar Range is composed of a succession of marine strata of probable Proterozoic age, consisting of a thick basal argillaceous sequence (Manki Formation) overlain by algal limestone and shale (Shahkot, Utch Khattak, and Shekhai formations). These strata are intruded by diabase dikes and sills that may correlate with the Panjal Volcanics. Southern Gandghar Range strata occur in two structural blocks juxtaposed along the Baghdarra fault. The hanging wall consists entirely of isoclinally-folded Manki Formation, whereas the footwall consists of the complete Manki-Shekhai succession which has been deformed into tight, northeast-plunging, generally southeast (foreland) verging disharmonic folds. Phyllite near the Baghdarra fault displays kink bands, a poorly-developed S-C fabric, and asymmetric deformation of foliation around garnet porphyroblasts. These features are consistent with conditions of dextral shear, indicating reverse-slip displacement along the fault. South of the Gandghar Range, the Panjal fault brings the Gandghar Range succession over the Kherimar Hills succession, which is composed of a basal Precambrian arenaceous sequence (Hazara Formation) unconformably overlain by Jurassic limestone (Samana Suk Formation) which in turn is unconformably overlain by Paleogene marine strata (Lockhart Limestone and Patala Formation).
    [Show full text]
  • Irrigation System, Arid Piedmont Plains of Southern Khyber-Paktunkhwa (NWFP), Pakistan; Issues & Solutions
    Irrigation System, Arid Piedmont Plains of Southern Khyber-Paktunkhwa (NWFP), Pakistan; Issues & Solutions Muhammad Nasim Golra Javairia Naseem Golra Department of Irrigation, AGES Consultants, Government of Khyber-Paktunkhwa, Peshawar Peshawar IRRIGATION POTENTIAL Khyber-Paktunkhwa (Million (NWFP) Acres) Total Area (NWFP+FATA) 25.4 Cultivable Area 6.72 Irrigated Area Govt. Canals 1.2467 Civil Canals 0.82 Lift Irrigation Schemes 0.1095 Tube Wells/Dug Wells 0.1008 Total 2.277 Potential Area for Irrigation 4.443 Lakki Marwat 0.588 D.I. Khan 1.472 Tank 0.436 Total 2.496 Rest of Province 1.947 Upper Siran Canal Kunhar River Siran River Lower Siran Canal Icher Canal Haro River Irrigation System , KP (NWFP) Indus River Daur River Khan Pur Dam Sarai Saleh Channel L.B.C R.B.C Mingora 130 miles 40 miles 96 miles Swat River Tarbela Dam P.H.L.C Ghazi Brotha Barrage Topi Bazi Irrigation Scheme Pehur Main Swabi Swan River Amandara H/W Indus River Chashma Barrage Machai Branch U.S.C Taunsa Barrage Lower Swat Kalabagh Barrage Kabul River Mardan Nowshera D.I.Khan Kohat Toi CRBC Kohat Munda H/W Panj Kora River Peshawar Main Canal L.B. Canal CRBC 1st Lift 64 Feet Tanda Dam K.R.C CRBC 2nd Lift 120 Feet Warsak Canal Bannu CRBC 3rd Lift 170 Feet Warsak Lift Canal Tank Civil Canal Kurram Ghari H/W Kurram Tangi Dam Marwat Canal Baran Dam Gomal River Kurram River Tochi Baran Link D.I. Khan-Tank Gomal Zam Dam Area Kaitu River Tochi River Flood Irrigation Vs Canal Irrigation Command D.
    [Show full text]
  • Of Indus River at Darband
    RESTRICTED For official use only Not for . UNN42 Vol. 6 Public Disclosure Authorized REPORT TO THE PRESIDENT OF THF, INTERNATIONAL BANK FOR RECONSTRUCTION AND DEVELOPMENT AS ADMINISTRATOR OF THE INDUS BASIN DEVELOPMENT FUND STUDY OF THIE WATER AND POWER RESOURCES OF WEST PAKISI AN Public Disclosure Authorized VOLUME III Program for the Development of Surface Water Storage Public Disclosure Authorized Prepared by a Group of the World Barnk Staff Headed by Dr. P. Lieftinck July 28, 1967 Public Disclosure Authorized i R0C FPU-F ClJRRENCY EQUIVALENTS 4.76 rupees = U.S. $1.00 1 rupee = U.S. $0. 21 1 millior rupees = U. S. $210, 000 TABLE OF CONTENTS Page No. I, INTRODUCTION 11..........- II-.. SURFACE. WATER HYDROLOGY. .3 .. .. , 3 Meteorological and GeographicalI Factors, .................... 3 Discharge- Measurement and River. F-lows- ... ....... .. ,44... Sediment-.Movement ..... v...............8....... 8. Floods-.JO,:,. ,10: III.. HISTORICAL. USE OF SURFACE WATER, . 12 Development of- the. System ....... ... 12 IV.. THE IACA APPROACH ..... 17 Method- of Analysis. ........... v.. 17 Surface. Water Re.quirements;. ........ r19. Integration, of.Surface and Groundwater Supplies' .. 22 Storable. Water. 23 Balancng- of Irrigation and Power..-Requi:rements.. 25 Future. River Regime ... .. 27 Accuracy- of Basic. Data . ....................... , ,,.. 27 Vt., IDENTIFICATION OF DAM'SITES AND, COMPARISON OF. PROJECTS' 29: S'cope of-the Studies ... 29. A. The Valley of the Indus,.......... 31 Suitability of the- Valley, for: Reservoir' Storagel 31 A(l.) The Middle Indus-. ...........-.. 31 Tarbela.Projject- . .. 32 Side Valley- ProjS'ectsi Associatedt w-ith Tar.bela ... 36 The Gariala' Site......... 36 The. Dhok Pathan S.te . ... ... 39 The Sanjwal-Akhori S'ites -.- , ... 40- The Attock Site .
    [Show full text]
  • The Panjab, North-West Frontier Province, and Kashmir
    1 Chapter XVII CHAPTER I CHAPTER II CHAPTER III CHAPTER IV CHAPTER V CHAPTER VI CHAPTER VII CHAPTER VIII CHAPTER IX CHAPTER X CHAPTER XI CHAPTER XII CHAPTER XIII CHAPTER XIV CHAPTER XV CHAPTER XVI CHAPTER XVII CHAPTER XVIII CHAPTER XIX CHAPTER XX CHAPTER XXI CHAPTER XXII CHAPTER XXIII CHAPTER XXIV CHAPTER XXV Chapter XXX. CHAPTER XXVI CHAPTER XXVII CHAPTER XXVIII The Panjab, North-West Frontier Province, and by Sir James McCrone Douie 2 CHAPTER XXIX CHAPTER XXX The Panjab, North-West Frontier Province, and by Sir James McCrone Douie The Project Gutenberg eBook, The Panjab, North-West Frontier Province, and Kashmir, by Sir James McCrone Douie This eBook is for the use of anyone anywhere at no cost and with almost no restrictions whatsoever. You may copy it, give it away or re-use it under the terms of the Project Gutenberg License included with this eBook or online at www.gutenberg.org Title: The Panjab, North-West Frontier Province, and Kashmir Author: Sir James McCrone Douie Release Date: February 10, 2008 [eBook #24562] Language: English Character set encoding: ISO-8859-1 ***START OF THE PROJECT GUTENBERG EBOOK THE PANJAB, NORTH-WEST FRONTIER PROVINCE, AND KASHMIR*** E-text prepared by Suzanne Lybarger, Asad Razzaki, and the Project Gutenberg Online Distributed Proofreading Team (http://www.pgdp.net) Note: Project Gutenberg also has an HTML version of this file which includes the original illustrations and maps. See 24562-h.htm or 24562-h.zip: (http://www.gutenberg.net/dirs/2/4/5/6/24562/24562-h/24562-h.htm) or (http://www.gutenberg.net/dirs/2/4/5/6/24562/24562-h.zip) Transcriber's note: Text enclosed between tilde characters was in bold face in the original book (~this text is bold~).
    [Show full text]
  • Hydrologic Evaluation of Salinity Control and Reclamation Projects in the Indus Plain, Pakistan a Summary
    Hydrologic Evaluation of Salinity Control and Reclamation Projects in the Indus Plain, Pakistan A Summary GEOLOGICAL SURVEY WATER-SUPPLY PAPER 1608-Q Prepared in cooperation with the West Pakistan Water and Powt > Dei'elofunent Authority under the auspices of the United States Agency for International Development Hydrologic Evaluation of Salinity Control and Reclamation Projects in the Indus Plain, Pakistan A Summary By M. ]. MUNDORFF, P. H. CARRIGAN, JR., T. D. STEELE, and A. D. RANDALL CONTRIBUTIONS TO THE HYDROLOGY OF ASIA AND OCEANIA GEOLOGICAL SURVEY WATER-SUPPLY PAPER 1608-Q Prepared in cooperation with the West Pakistan Water and Power Development Authority under the auspices of the United States Agency for International Development UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1976 UNITED STATES DEPARTMENT OF THE INTERIOR THOMAS S. KLEPPE, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress Cataloging in Publication Data Main entry under title: Hydrologic evaluation of salinity control and reclamation projects in the Indus Plain, Pakistan. (Contributions to the hydrology of Asia and Oceania) (Geological Survey water-supply paper; 1608-Q) Bibliography: p. Includes index. Supt. of Docs, no.: I 19.13:1608-Q 1., Reclamation of land Pakistan Indus Valley. 2. Salinity Pakistan Indus Valley. 3. Irrigation Pakistan Indus Valley. 4. Hydrology Pakistan Indus Valley. I. Mundorff, Maurice John, 1910- II. West Pakistan. Water and Power Development Authority. III. Series. IV. Series: United States. Geological Survey.
    [Show full text]
  • West Pakistan Fisheries Rules, 1965
    WEST PAKISTAN FISHERIES RULES, 1965 CONTENTS RULES Preamble. PART I – PRELIMINARY 1. Short title and commencement. 2. Definitions. PART II – LICENCES 3. Licences to be issued by the Directors. 4. Duration of validity of a licence. 5. Area to which a licence extends. 6. Kinds of fishing gears. 7. Fees for the licences. 8. Free licences. 9. Duplicate licence. 10. Refund of licence. 12. Licence not transferable. No adult to be engaged as helper. 13. Method of payments of fees. 14. No erection of fixed engines. 15. Seizures. 16. Cancelling of licences. 17. Restriction on Size and number of fish to be caught. PART III – LEASES 18. Auction of fishing rights. 19. Departmental operation. 20. Units for auction. 21. Payment of lease money. 22. Refund of lease money. 23. Report of breach of rules. 24. Cancellation of lease due to no-payment of installments. 25. Appeal. PART IV – DEPARTMENTAL OPERATIONS 26. Licences for reserved waters. 27. Validity of licences. 28. Sale of fish. 29. Share of licences. 30. Confiscation. PART V – TROUT WATERS 31. Division Kunhar River and its tributaries. 32. Licences for trout waters. 33. Number of licences to be granted by Extra Assistant Director. 34. Fee. 35. Fees for condition of licences not to be refunded or altered. 36. Licences not to be transferred or shared. 37. Duplicate licences. 38. Kinds of lures to be used. 39. No fish to be killed during the closed season. 40. Seizures. PART VI – PROVINCIAL ANGLING LICENCE 41. Grant of Angling Licence. 42. Application for Angling Licences. 43. Validity etc. of licences.
    [Show full text]
  • Demonstration River Basins in Pakistan
    Demonstration River Basins in Pakistan Dr. Bashir AHMAD Water Resources Research Institute National Agriculture Research Center Islamabad, Pakistan Indus River Length:3200 km Indus basin area: 566,000 km2 Total watershed area:944,000 km Major tributaries = 14 Upper Indus China UU Afghanistan II BB Pakistan Iran Nepal India Indus Basin International Areas Country/Regio Area (sq. km) Area (%) ¾ 80 to 90% of the UIB becomes snow- n covered during most of winter season China 92,981 10 ¾ In UIB, seasonally snow covered areas are India 67,340 7 typically between 1500 m and 5000 m Kashmir 179,486 19 ¾ Snowline retreats to elevation about 4500 - Afghanistan 75628 8 5000 m during July and August Pakistan 529,135 56 Total Area 944,569 100 UIB: Upper Indus Basin INDUS IRRIGATION SYSTEM IN PAKISTA KEY FACTS 3 No. of major Reservoirs: No. of Barrages: 16 No. of Headworks: 2 No. of Inter-link Canals: 12 No. of Canal Systems: 44 No. of Watercourses: 107,000 Length of Canals: 56,073 km 1.6 million Length of Watercourses: km Average Canal Water Diversions: 104.7 MAF Groundwater Abstractions: 41.6 MAF No. of Tubewells: > 550,000 36 million Irrigated Area: acres Average Escapage to the Sea: 39.4 MAF Source of fresh water is rainfall, snowmelt and glacier melt ¾More than 70% of water resources are contributed by snowmelt and glacier melt Source of fresh water is rainfall, snowmelt and glacier melt ¾70 % rainfall is from summer monsoons and rest is from westerly disturbances Water resources issues • Water logging • Salinity • Water quality • Floods • Landslide • Sediment flow • Water scarcity • Monitoring (especially in remote and difficult approach area Pakistan Meteorological Department (PMD) Pakistan Meteorological Department (PMD) is a federal agency with a mandate to monitor and analyze meteorological data.
    [Show full text]
  • Provincial Geographies of India
    िव�ा �सारक मंडळ, ठाणे Title : The Panjab North West Frontier Province and Kashmir Author : Douie, Sir James Publisher : Cambridge : Cambridge University Press Publication Year : 1916 Pages : 393 गणपुस्त �व�ा �सारत मंडळाच्ा “�ंथाल्” �तल्पा्गर् िनिमर्त गणपुस्क िन�म्ी वषर : 2014 गणपुस्क �मांक : 052 The PANJARNORTfrWE FRONTIER PROVINCE AND KASHMIR WJAMESDOUIE,MA.KGS'I. PROVINCIAL GEOGRAPHIES OF INDIA L Provincial Geographies of India General Editor Sir T. H. HOLLAND, K.C.I.E., D.Sc, F.R.S. THE PANJAB, NORTH-WEST FRONTIER PROVINCE ' AND KASHMIR CAMBRIDGE UNIVERSITY PRESS C. F. CLAY, Manager ILottiJOn: FETTER LANE, E.G. IBUinburgf) : 100 PRINCES STREET £cfo lorfe: G. P. PUTNAM'S SONS 33ombao, (Calcutta atrti fflaDras: MACMILI.AN AND CO., Ltd. Toronto: J. M. DENT AND SONS, Ltd. aTofep.o: THE MARUZEN-KABUSHIKI-KAISHA All tights reserz'ed AX" THE PANJAB, NORTH-WEST FRONTIER PROVINCE AND KASHMIR BY SIR JAMES DOUIE, M.A., K.C.S.I. Cambridge : at the University Press 19 1 6 EDITOR'S PREFACE T N his opening chapter Sir James Douie refers to the -*- fact that the area treated in this volume—just one quarter of a million square miles—is comparable to that of The be Austria-Hungary. comparison might extended ; for on ethnographical, linguistic and physical grounds, the geographical unit now treated is just as homogeneous in composition as the Dual Monarchy. It is only in the political sense and by force of the ruling classes, temporarily united in one monarch, that the term Osterreichisch could be used to include the Poles of Galicia, the Czechs of Bohemia and Moravia, the Szeklers, Saxons and more numerous Rumanians of Transylvania, the Croats, Slovenes and Italians of "Illyria," with the Magyars of the Hungarian plain.
    [Show full text]
  • Sediment Management of Tarbela Reservoir
    17 Paper No. 733 SEDIMENT MANAGEMENT OF TARBELA RESERVOIR DR. IZHAR UL HAQ 18 Dr. Izhar ul Haq 72nd Annual Session of Pakistan Engineering Congress 19 SEDIMENT MANAGEMENT OF TARBELA RESERVOIR By Dr. Izhar ul Haq1 ABSTRACT Sedimentation of Tarbela Reservoir was discussed in its 2nd and 5th periodic Inspections of the dam. Sediment Management studies of Tarbela (SMST) reservoir were carried out by M/s Tams and Wellingford in 1998. Investigation of sediments were carried out by bore holes in 1987 and 1989 about 20 Km u/s of the dam on topset of delta. In 2008 boreholes were done at 24 and 26 Km u/s of dam. Shallow hand driven boreholes were done in 2012 on exposed delta. Standard Penetration Tests were carried out in bore holes. Samples were tested for gradation and shear tests. A comprehensive study comprising of bathymetric survey, delta exploration by drilling boreholes in bottom set and foreset slope of the delta, testing of the sediments samples and the effects of the sediment on the d/s structures when flushed from Tarbela reservoir was carried out by Mot MacDonald in 2011-13. Sediment Management: Mathematical Model studies of Tarbela reservoir were carried out by H R Wallingford and Mot MacDonald for Wapda in 2013. The feasibility and impact of the following sediment management approaches were studied:- The management of the minimum operating level at the reservoir (option 0). The release of sediment from the reservoir during hydraulic flushing (option 1). The reduction of sediment inflow into reservoir due to future construction of dams u/s Tarbela (option 2).
    [Show full text]
  • Impact Assessment of Future Climate Change on Streamflows Upstream
    water Article Impact Assessment of Future Climate Change on Streamflows Upstream of Khanpur Dam, Pakistan using Soil and Water Assessment Tool Saima Nauman *, Zed Zulkafli , Abdul Halim Bin Ghazali and Badronnisa Yusuf Department of Civil Engineering, Faculty of Engineering, Universiti Putra Malaysia, Selangor Darul Ehsan 43400, Malaysia; [email protected] (Z.Z.); [email protected] (A.H.B.G.); [email protected] (B.Y.) * Correspondence: [email protected] Received: 6 February 2019; Accepted: 9 April 2019; Published: 24 May 2019 Abstract: The study aims to evaluate the long-term changes in meteorological parameters and to quantify their impacts on water resources of the Haro River watershed located on the upstream side of Khanpur Dam in Pakistan. The climate data was obtained from the NASA Earth Exchange Global Daily Downscaled Projection (NEX-GDDP) for MIROC-ESM model under two Representative Concentration Pathway (RCP) scenarios. The model data was bias corrected and the performance of the bias correction was assessed statistically. Soil and Water Assessment Tool was used for the hydrological simulation of watershed followed by model calibration using Sequential Uncertainty Fitting version-2. The study is useful for devising strategies for future management of Khanpur Dam. The study indicated that in the future, at Murree station (P-1), the maximum temperature, minimum temperature and precipitation were anticipated to increase from 3.1 ◦C (RCP 4.5) to 4.0 ◦C (RCP 8.5), 3.2 ◦C (RCP 4.5) to 4.3 ◦C (RCP 8.5) and 8.6% to 13.5% respectively, in comparison to the baseline period.
    [Show full text]