Riparian Rights: a Case Study of India and Pakistan
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Identification of Glacial Flood Hazards in Karakoram Range Using Remote Sensing Technique and Risk Analysis
IDENTIFICATION OF GLACIAL FLOOD HAZARDS IN Arshad Ashraf*† , Rakhshan Roohi*, Rozina Naz* KARAKORAM RANGE USING REMOTE SENSING and Naveed Mustafa* TECHNIQUEAND RISK ANALYSIS ABSTRACT importance of this situation has magnified over the past decades due to increase in numbers of glacial Glacial Lake Outburst Floods (GLOFs) are great lakes that are formed at the glacier terminus. Thirty- hazard for the downstream communities in context of five destructive out-burst floods have been recorded changing climatic conditions in the glaciated region of for the Karakoram Range during the past two hundred Pakistan. The remote sensing data of Landsat ETM+ years (Hewitt, 1982). Some of the ice dams may have was utilized for the identification of glacial lakes been the result of glacier surges. There is susceptible to posing GLOF hazard in Karakoram unambiguous evidence of large reservoirs ponded by Range. Overall, 887 glacial lakes are identified in 18 glaciers. Kelly (1988) outlines the historical different river-basins of Karakoram Range, out of development and disappearance of Virjerab lake in which 16 lakes are characterized as potentially Hunza due to glacial motion. There occurred a series dangerous in terms of GLOF. The analysis of of GLOF events in upper Hunza valley, central community’s response to GLOF events of 2008 in the Karakoram Range, within short time periods during central Karakoram Range indicated gaps in 2008 that had a devastating effect on the nearby coordination and capacity of the local communities to communities (Roohi, Ashraf, Mustafa and Mustafa, cope with such natural hazards. A regular monitoring 2008). The people residing at considerable distances of hot spots and potential GLOF lakes along with downstream from the unstable lakes are facing a capacity-building of local communities and institutions serious threat to their lives and property. -
Distributors of World Bank Publications
(4?m 1:13q WORLDBANK TECHNICAL PAPER NUMBER173 Water Users Associations in World Public Disclosure Authorized Bank-Assisted Irrigation Projects in Pakistan LE COPY0 Kerry J. Byrnes Public Disclosure Authorized ALtOCATON ~~~~~~~~~~ )_ 0151.10.1~0z Public Disclosure Authorized rSiI~~~~~~~~~~~~~~~~~~~~0NG _ L ¢5 >'3~~~~~~~~~~~~~~~~~~~~~C~TTa >~~~~~~~~~~~~~~~~~~~~~~E" 07"O I-j ~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~.1To$MCTR ACTWIT Public Disclosure Authorized RECENT WORLD BANK TECHNICAL PAPERS No. 110 Dixon, Talbot, and Le Moigne, Damsand the Environment:Considerations in WorldBank Projects No. 111 Jeffcoateand Pond, Large WaterMeters: Guidelinesfor Selection, Testing, and Maintenance No. 112 Cook and Grut, Agroforestryin Sub-SaharanAfrica: A Farmer'sPerspective No. 113 Vergara and Babelon, The PetrechemicalIndustry in DevelopingAsia: A Reviewvof the Current Situationand Prospectsfor Developmentin the 1990s No. 114 McGuire and Popkins, HelpingWomen Improve Nutrition in the DevelopingWorld: Beating the Zero Sum Game No. 115 Le Moigne, Plusquellec, and Barghouti, Dam Safetyand the Environment No. 116 Nelson, DrylandManagement: The 'Desertification"Problem No. 117 Barghouti, Timmer, and Siegel,.Rural Diversification:Lessons from East Asia No. 118 Pritchard, Lendingby the WorldBankfor AgriculturalResearch: A Review of the Years1981 through 1987 No. 119 Asia Region Technical Department, FloodControl in Bangladesh:A Planfor Action No. 120 Plusquellec, The GeziraIrrigation Scheme in Sudan:Objectives, Design, and Performance No. 121 Listorti, EnvironmentalHealth Components for WaterSupply, Sanitation,and UrbanProjects No. 122 Dessing, Supportfor Microenterprises:Lessons for Sub-SaharanAfrica No. 123 Barghouti and Le Moigne, Irrigationin Sub-SaharanAfrica: The Developmentof Public and PrivateSystems No. 124 Zymelman, Science,Education, and Developmentin Sub-SaharanAfrica No.125 van de Walle and Foster, FertilityDecline in Africa:Assessment and Prospects No. 126 Davis, MacKnight, IMO Staff, and Others, EnvironmentalConsiderationsfor Port and Harbor Developments No. -
Negotiating the Indus Waters Treaty: an Historical Assessment
Journal of the Research Society of Pakistan Volume No. 57, Issue No. 1 (January – June, 2020) Muhammad Nawaz Bhatti* Farzad Ahmad ** Asia Saif Alvi *** Muhammad Kashif Ali **** Nabila Akhtar ***** Negotiating the Indus Waters Treaty: An Historical Assessment Abstract International watercourses are the only supplementary sources of water for the many states having arid or semi-arid climatic conditions that could economically be developed to bridge the rapidly increasing gap between demand and supply. In absence of any international law to deal with uses of international watercourses other than navigational purposes, agreements among co-riparian states are very important for the development of an entire basin. Although the U. N. Convention on the Uses of International Rivers for non-navigational purposes was adopted by the U. N. General Assembly in 1997 and after the rectification of 35 Member States, it has been functioning since 2014, but the importance of the negotiation processes that resulted in numerous successful agreements on water resource management can never be denied. This document provides an historical analysis of the negotiating process which culminated into the Indus Waters Treaty. Keywords: Partition of India, Pakistan, India, Water dispute, Negotiations, Indus waters Treaty Introduction In arid and semi-arid climatic regions, water is considered one of the most important factors of development. The availability of sufficient water in those areas in terms of quantity and quality, suitable for all purposes, has already become a serious issue. All tendencies show that difficulties emerging due to this critical issue would increase significantly in coming years. Starting in the 1990s and beyond, the management and development of international watercourses would become an increasingly critical problem. -
Mehbooba Mufti Can End the Power Crisis in J&K
3 Days’ Forecast Jammu www.thenorthlines.com www.epaper.northlines.com Date Min Temp Max Temp Weather July 26 25.0 34.0 Generally cloudy sky July 27 25.0 34.0 Generally cloudy sky July 28 26.0 35.0 Generally cloudy sky Srinagar July 26 19.0 31.0 Thunderstorm with rain July 27 20.0 31.0 Thunderstorm with rain July 28 20.0 32.0 Thunderstorm with rain Vol No: XXIII Issuethe No. 178 29.07.2018 (Sunday)northlines Daily Jammu Tawi Price 3/- Pages-12 Regd. No. JK|306|2017-19 Alliance with BJP was like 'drinking Tapping of 111.05 GWp of Solar energy a cup of poison': Mehbooba Mufti can end the power crisis in J&K No government without 28 PDP MLAs can be formed: Altaf NL CORRESPONDENT requirement around 70% of provide a strong impetus sufficient in power SRINAGAR, JUL 28 power is imported / for the growth of its generation has failed to Muzaffar Baig back to centre stage, purchased from outside," economy. "Optimal harness even a bit in the Though Jammu and sources maintained. exploitation of available same. sparks row with 'partition' remarks Kashmir has a potential to Quoting official figures, hydel resources in the Sources said National generate 111.05 GWp of one of the former officials State would not only meet Institute of Solar Energy hydel energy, the state still of the PDD told that, in the internal demand but (NISE), in its study has SRINAGAR, JULY 28 purchases energy worth 2004-05, the state had a will also supply power to said that Jammu and crores annually to meet demand of 1706 MW and the Northern grid to boost Kashmir has solar power PDP president Mehbooba Mufti on Saturday brought the demand. -
Most Important Mcqs (Set III) for CSS, PMS, PCS, NTS
Pakistan Studies/Affairs: Most Important MCQs (Set III) for CSS, PMS, PCS, NTS Jinnah Barrage is located near: (a) Kalabagh (b) Tarbela Dam (c) Warsak Dam (d) None of these Answer: a The largest desert of Pakistan is: (a) Thal (b) Thar (c) Sehan (d) Cholistan Answer: b The total height of Peshawar from sea level is: (a) 1160 ft (b) 1164 ft (c) 1164 ft (d) 1178 ft Answer: b How high is Quetta from sea level? (a) 5000 ft (b) 5500 ft (c) 6000 ft Answer: b Taunsa Barrage was completed in: (a) 1953 (b) 1955 (c) 1956 (d) 1958 Answer: d Check Also: Important and Most Wanted MCQs about Current Federal Cabinet of Pakistan Sindh Sagar Doab is between the rivers of: (a) Indus and Jhelum Downloaded from www.csstimes.pk | 1 Pakistan Studies/Affairs: Most Important MCQs (Set III) for CSS, PMS, PCS, NTS (b) Indus and Chenab (c) Sutluj and Ravi (d) Ravi and Chenab Answer: a Ganji Bar is between the rivers of: (a) Ravi and Chenab (b) Ravi and Satluj (c) Jhelum and Chenab (d) Indus and Jhelum Answer: b The city has maximum height from sea level is: (a) Ziarat (b) Murree (c) Khanpur (d) Loralai Answer: b Chaj Doab is located between the rivers: (a) Ravi and Chenab (b) Jhelum and Chenab (c) Indus and Ravi (d) Ravi and Jhelum Answer: b Jinnah Barrage was completed in: (a) 1970 (b) 1946 (c) 1965 (d) None of these Answer: b The first canal built by British in the subcontinent is: (a) Sohag Canal (b) Upper Bari Doab (c) Chenab Canal (d) Lower Bari Doab Answer: b Downloaded from www.csstimes.pk | 2 Pakistan Studies/Affairs: Most Important MCQs (Set III) for CSS, -
Indus Waters Treaty
Title: Indus Waters Treaty 1960 between the Government of India, the Government of Pakistan and the International Bank for reconstruction and development Parties: India, Pakistan Basin: Indus Date: 9/19/1960 INDIA, PAKISTAN and INTERNATIONAL BANK FOR RECONSTRUCTION AND DEVELOPMENT The Indus Waters Treaty 1960 (with annexes). Signed at Karachi on 19 September 1960 Protocol to the above-mentioned Treaty. Signed on 27 November, 2 and 23 December 1960 Official text: English. Registered by India on 16 January 1962. No. 6032. THE INDUS WATERS TREATY 1960 1 BETWEEN THE GOVERNMENT OF INDIA, THE GOVERNMENT OF PAKISTAN AND THE INTERNATIONAL BANK FOR RECONSTRUCTION AND DEVELOPMENT. SIGNED KARACHI, ON 19 SEPTEMBER 1960 PREAMBLE The Government of India and the Government of Pakistan, being equally desirous of attaining the most complete and satisfactory utilisation of the waters of the Indus system of rivers and recognizing the need, therefore, of fixing and delimiting, in a spirit of goodwill and friendship, the rights and obligations of each in relation to the other concerning the use of these waters and of making provision for the settlement, in a cooperative spirit, of all such questions as may hereafter arise in regard to the interpretation or application of the provisions agreed upon herein, have resolved to conclude a Treaty in furtherance of these objectives, and for this purpose named as their plenipotentiaries: The Government of India: Shri Jawaharlal Neliru, Prime Minister of India, and The Government of Pakistan: Field Marshal Mohammad Ayub Khan, H.P., H.J., President of Pakistan who, having communicated to each other their respective Full Powers and found them in good and due form, have agreed upon the following Articles and Annexures: Article I DEFINITIONS As used in this Treaty: (1) The terms "Article" and "Arinexure" mean respectively an Article of, an Annexure to, this Treaty. -
NW-49 Final FSR Jhelum Report
FEASIBILITY REPORT ON DETAILED HYDROGRAPHIC SURVEY IN JHELUM RIVER (110.27 KM) FROM WULAR LAKE TO DANGPORA VILLAGE (REGION-I, NW- 49) Submitted To INLAND WATERWAYS AUTHORITY OF INDIA A-13, Sector-1, NOIDA DIST-Gautam Buddha Nagar UTTAR PRADESH PIN- 201 301(UP) Email: [email protected] Web: www.iwai.nic.in Submitted By TOJO VIKAS INTERNATIONAL PVT LTD Plot No.4, 1st Floor, Mehrauli Road New Delhi-110074, Tel: +91-11-46739200/217 Fax: +91-11-26852633 Email: [email protected] Web: www.tojovikas.com VOLUME – I MAIN REPORT First Survey: 9 Jan to 5 May 2017 Revised Survey: 2 Dec 2017 to 25 Dec 2017 ACKNOWLEDGEMENT Tojo Vikas International Pvt. Ltd. (TVIPL) express their gratitude to Mrs. Nutan Guha Biswas, IAS, Chairperson, for sparing their valuable time and guidance for completing this Project of "Detailed Hydrographic Survey in Ravi River." We would also like to thanks Shri Pravir Pandey, Vice-Chairman (IA&AS), Shri Alok Ranjan, Member (Finance) and Shri S.K.Gangwar, Member (Technical). TVIPL would also like to thank Irrigation & Flood control Department of Srinagar for providing the data utilised in this report. TVIPL wishes to express their gratitude to Shri S.V.K. Reddy Chief Engineer-I, Cdr. P.K. Srivastava, Ex-Hydrographic Chief, IWAI for his guidance and inspiration for this project. We would also like to thank Shri Rajiv Singhal, A.H.S. for invaluable support and suggestions provided throughout the survey period. TVIPL is pleased to place on record their sincere thanks to other staff and officers of IWAI for their excellent support and co-operation through out the survey period. -
The Geographic, Geological and Oceanographic Setting of the Indus River
16 The Geographic, Geological and Oceanographic Setting of the Indus River Asif Inam1, Peter D. Clift2, Liviu Giosan3, Ali Rashid Tabrez1, Muhammad Tahir4, Muhammad Moazam Rabbani1 and Muhammad Danish1 1National Institute of Oceanography, ST. 47 Clifton Block 1, Karachi, Pakistan 2School of Geosciences, University of Aberdeen, Aberdeen AB24 3UE, UK 3Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA 4Fugro Geodetic Limited, 28-B, KDA Scheme #1, Karachi 75350, Pakistan 16.1 INTRODUCTION glaciers (Tarar, 1982). The Indus, Jhelum and Chenab Rivers are the major sources of water for the Indus Basin The 3000 km long Indus is one of the world’s larger rivers Irrigation System (IBIS). that has exerted a long lasting fascination on scholars Seasonal and annual river fl ows both are highly variable since Alexander the Great’s expedition in the region in (Ahmad, 1993; Asianics, 2000). Annual peak fl ow occurs 325 BC. The discovery of an early advanced civilization between June and late September, during the southwest in the Indus Valley (Meadows and Meadows, 1999 and monsoon. The high fl ows of the summer monsoon are references therein) further increased this interest in the augmented by snowmelt in the north that also conveys a history of the river. Its source lies in Tibet, close to sacred large volume of sediment from the mountains. Mount Kailas and part of its upper course runs through The 970 000 km2 drainage basin of the Indus ranks the India, but its channel and drainage basin are mostly in twelfth largest in the world. Its 30 000 km2 delta ranks Pakiistan. -
Soil Erosion and Sediment Load Management Strategies for Sustainable Irrigation in Arid Regions
sustainability Article Soil Erosion and Sediment Load Management Strategies for Sustainable Irrigation in Arid Regions Muhammad Tousif Bhatti 1,* , Muhammad Ashraf 2,* and Arif A. Anwar 1 1 International Water Management Institute, Lahore 53700, Pakistan; [email protected] 2 Department of Agricultural Engineering, Khwaja Fareed University of Engineering & Information Technology, Rahim Yar Khan 64200, Pakistan * Correspondence: [email protected] (M.T.B.); [email protected] (M.A.) Abstract: Soil erosion is a serious environmental issue in the Gomal River catchment shared by Pakistan and Afghanistan. The river segment between the Gomal Zam dam and a diversion barrage (~40 km) brings a huge load of sediments that negatively affects the downstream irrigation system, but the sediment sources have not been explored in detail in this sub-catchment. The analysis of flow and sediment data shows that the significant sediment yield is still contributing to the diversion barrage despite the Gomal Zam dam construction. However, the sediment share at the diversion barrage from the sub-catchment is much larger than its relative size. A spatial assessment of erosion rates in the sub-catchment with the revised universal soil loss equation (RUSLE) shows that most of −1 −1 the sub-catchment falls into very severe and catastrophic erosion rate categories (>100 t h y ). The sediment entry into the irrigation system can be managed both by limiting erosion in the catchment Citation: Bhatti, M.T.; Ashraf, M.; and trapping sediments into a hydraulic structure. The authors tested a scenario by improving Anwar, A.A. Soil Erosion and the crop management factor in RUSLE as a catchment management option. -
Watershed Atlas Part IV
PART IV 99 DESCRIPTION PART IV OF WATERSHEDS I. MAP AND STATISTICS BY WATERSHED II. AMU DARYA RIVER BASIN III. NORTHERN RIVER BASIN IV. HARIROD-MURGHAB RIVER BASIN V. HILMAND RIVER BASIN VI. KABUL (INDUS) RIVER BASIN VII. NON-DRAINAGE AREAS PICTURE 84 Aerial view of Panjshir Valley in Spring 2003. Parwan, 25 March 2003 100 I. MAP AND STATISTICS BY WATERSHED Part IV of the Watershed Atlas describes the 41 watersheds Graphs 21-32 illustrate the main characteristics on area, popu- defined in Afghanistan, which includes five non-drainage areas lation and landcover of each watershed. Graph 21 shows that (Map 10 and 11). For each watershed, statistics on landcover the Upper Hilmand is the largest watershed in Afghanistan, are presented. These statistics were calculated based on the covering 46,882 sq. km, while the smallest watershed is the FAO 1990/93 landcover maps (Shapefiles), using Arc-View 3.2 Dasht-i Nawur, which covers 1,618 sq. km. Graph 22 shows that software. Graphs on monthly average river discharge curve the largest number of settlements is found in the Upper (long-term average and 1978) are also presented. The data Hilmand watershed. However, Graph 23 shows that the largest source for the hydrological graph is the Hydrological Year Books number of people is found in the Kabul, Sardih wa Ghazni, of the Government of Afghanistan – Ministry of Irrigation, Ghorband wa Panjshir (Shomali plain) and Balkhab watersheds. Water Resources and Environment (MIWRE). The data have Graph 24 shows that the highest population density by far is in been entered by Asian Development Bank and kindly made Kabul watershed, with 276 inhabitants/sq. -
India-Pakistan Conflicts – Brief Timeline
India-Pakistan Conflicts – Brief timeline Added to the above list, are Siachin glacier dispute (1984 beginning – 2003 ceasefire agreement), 2016- 17 Uri, Pathankot terror attacks, Balakot surginal strikes by India Indo-Pakistani War of 1947 The war, also called the First Kashmir War, started in October 1947 when Pakistan feared that the Maharaja of the princely state of Kashmir and Jammu would accede to India. Following partition, princely states were left to choose whether to join India or Pakistan or to remain independent. Jammu and Kashmir, the largest of the princely states, had a majority Muslim population and significant fraction of Hindu population, all ruled by the Hindu Maharaja Hari Singh. Tribal Islamic forces with support from the army of Pakistan attacked and occupied parts of the princely state forcing the Maharaja Pragnya IAS Academy +91 9880487071 www.pragnyaias.com Delhi, Hyderabad, Bangalore, Tirupati & Pune +91 9880486671 www.upsccivilservices.com to sign the Instrument of Accession of the princely state to the Dominion of India to receive Indian military aid. The UN Security Council passed Resolution 47 on 22 April 1948. The fronts solidified gradually along what came to be known as the Line of Control. A formal cease-fire was declared at 23:59 on the night of 1 January 1949. India gained control of about two-thirds of the state (Kashmir valley, Jammu and Ladakh) whereas Pakistan gained roughly a third of Kashmir (Azad Kashmir, and Gilgit–Baltistan). The Pakistan controlled areas are collectively referred to as Pakistan administered Kashmir. Pragnya IAS Academy +91 9880487071 www.pragnyaias.com Delhi, Hyderabad, Bangalore, Tirupati & Pune +91 9880486671 www.upsccivilservices.com Indo-Pakistani War of 1965: This war started following Pakistan's Operation Gibraltar, which was designed to infiltrate forces into Jammu and Kashmir to precipitate an insurgency against rule by India. -
Pak Geogrophy. 6
Gather and Edited By Yasir Shahzad( Gujrat) Mcq OF Pak Geography Best Of Luck You Can Not Help Every one But Every One Can Help Someoone Pakistan is located in tropic zone of South North East West Pakistan is divided into how many divisions? 5 9 8 7 Which one is the highest peak of Hindukush range? Tirch Mir K2 Mount Everest Nanga Parbat What is height of K-2 in metres? 8611 8650 8600 8645 What is the height of Nanga Parbat in metres? 8126 8150 8148 8179 Which one is the highest peak of Sulaiman Range? Takht-e-Sulaimat K-2 Nanga Parbat Tirch Mir Which is the hottest place in Pakistan? Jaccobabad Sibbi Murree Multan Which is the coldest place in Pakistan? Ziarat Islamabad Skardu Murree Pakistan comes at which number in world with respect to area? 34th 35th 40th 32nd What is the total area of Punjab province in sq. km.? 205,444 205,698 504,669 304,897 What is the total area of Sindh in sq. km? 140914 150478 169807 144589 What is total area of Balochistan in sq. km? 347192 395973 450299 502497 Choose the correct total length of coast line of Pakistan. 700 km 500 km 600 km 980 km What is total length of Pak-India border in km? 1610 1846 1652 1489 What is total length of Pak-Iran border in km? 805 850 845 758 What is Durand line? Boundary between Pakistan and Afghanistan Boundary between Pakistan and Iran Boundary between Pakistan and India Boundary between Pakistan and China Total length of Durand Line is 2252 km 1205 km 2065 km 2564 km Area of highest rainfall is Murree.