Climate Change Impact on Water Resources of Upper
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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. -
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. -
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). -
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. -
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 . -
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~). -
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. -
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. -
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. -
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. -
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). -
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.