INDUS DELTA, PAKISTAN: Economic Costs of Reduction in Freshwater Flows

Total Page:16

File Type:pdf, Size:1020Kb

INDUS DELTA, PAKISTAN: Economic Costs of Reduction in Freshwater Flows water allocationdecisions. factored intoriverbasinplanning,or benefits of water-basedecosystemsarerarely economic users ofwater.Yettheeconomic schemes, Pakistan’secosystems,too,are hydropower dams, reservoirs,irrigationand as water tolarge-scale,commercialusessuch imperative that favours theallocationof Contrary tothedominantdevelopment economically norecologicallyoptimal. decisions beingmadethatareneither needs has oftenledtowaterallocation Failure torecognisedownstreamecosystem heavily byupstreamwaterabstraction. end of rivers,havebeenimpactedmost the at lie and marineregions,becausethey Coastal ecosystems. needs ofdownstream many cases, left insufficientflowtomeetthe of large volumesofwaterfromrivershas,in particular there isconcernthattheabstraction exacting a heavytollontheenvironment.In This impressive irrigationsystemis,however, world. the irrigated torain-fedlandratioin highest the farmland, affordingPakistan system feedsmorethan15millionhectaresof than 1.65 million km(IRIN2001).The more watercourses witharunninglengthof 89,000 conveyance lengthof57,000km,and head works, 43maincanalswitha or barrages 19 three majorstoragereservoirs, comprises Pakistan’s vastirrigationnetwork Pakistan Water-based developmentsin flows reduction infreshwater economic costsof INDUS DELTA,PAKISTAN: VALUATION #5:May2003 CASE STUDIESINWETLAND Integrating Wetland Economic Values into River Basin Management Managing freshwater flows in the The economic costs and losses arising from Indus River such omissions can be immense, and often The Indus River has a total length of more irreversible, impacting on some of the most than 3,000 km and a drainage area of some fragile ecosystems and the poorest and most 950,000 km2. Almost 90% of the water in the vulnerable human groups. This case study upper portion of the river basin comes from describes the economic costs that have glaciers located in the Himalaya and occurred as a result of inadequate freshwater Karakoram mountain ranges, which border allocation to the Indus Delta in Pakistan. China, Pakistan and India, and the Hindu Especially, it focuses on the crippling Kush, which borders Pakistan and Afghanistan. environmental economic costs that upstream The Indus travels southwards across Punjab water allocation decisions have incurred to and Sindh Provinces in Pakistan before poor local populations, manifested through entering the Arabian Sea through a delta close declining agricultural yields and fisheries to the border with India. production. Figure 1: The Indus Delta The Indus Delta is a typical fan-shaped delta, at this level the amount of freshwater reaching built up by the discharge of large quantities of the Delta was argued to be insufficient to silt washed down from upland and mountain maintain healthy natural ecosystems, and had areas. The present Delta covers an area of resulted in severe saltwater intrusion and about 600,000 hectares and is characterised by salinisation. With the existing reduction in 17 major creeks and innumerable minor creeks, flow, downstream Sindh Province already mud flats and fringing mangroves (Meynell and claims it is short of the minimum 12 billion m3 Qureshi 1993). The mangrove ecosystem of the of water needed to maintain the Delta. Indus Delta is perhaps unique in being the largest area of arid climate mangroves in the The economic significance of the world. As annual rainfall is so low in the region, mangroves are almost wholly Indus Delta dependent upon freshwater discharges from Loss of freshwater flow, and consequent the river, supplemented by a small quantity of saltwater intrusion, has had devastating effects run-off and effluents from Karachi. on the ecology and human economy of the Indus Delta. Land in the area has become The total available freshwater flow in the Indus unsuitable for agriculture, and potable water is about 180 billion m3, carrying with it some sources have become very scarce or have 400 million tonnes of silt (Meynell and Qureshi disappeared altogether. In Thatta, a 1993). Over the last 60 years a series of dams, predominantly agricultural District in Sindh barrages and irrigation schemes have been built Province which is situated where the Indus in upstream parts of the River Indus. Today, it river flows into the Arabian Sea, almost a third is estimated that up to 60% of the Indus water of land has been affected by saltwater is used to feed Pakistan’s irrigation networks, intrusion. It is estimated that up to 0.5 million and that the Indus watershed irrigates up to hectares of fertile land in Thatta and adjoining 80% of Pakistan’s farmland (Iftikhar 2002). areas (IRIN 2001), or about 12% of total There has for some time been a high level of cultivated area in the entire Province controversy surrounding the allocation of the (Government of Pakistan 2001), is now waters of the Indus River, in particular between affected by sea water intrusion. As well as crop competing uses in different Provinces. losses, this has resulted in severe damage to Recurrent disputes over water usage led the livestock through rangeland depletion, shortage government to set in place the Indus Water of fodder, pasture and watering areas, and a Accord in 1991, which apportioned the use of resulting mass migration of both livestock and the river’s water between the four provinces of human populations out of the area. Pakistan. It also recognised − for the first time − the need to allow some freshwater discharge The human population in and around into the delta to safeguard the ecosystem, mangrove forests on the coast of Pakistan is specifying a minimum flow of 12 billion m3. In estimated to total 1.2 million people, nearly 1994, because of drought and water shortages, 900,000 of whom reside in the Indus Delta Punjab Province however demanded and got a (Salman 2002). Of these, a predominantly rural break from the 1991 Water Accord and a population of more than 135,000 depend on subsequent higher reallocation based on mangrove resources for their livelihoods (Shah historical use. 1998). Reductions in freshwater inflows have had tangible impacts on mangrove ecology, and As a result of upstream water abstraction, on the fish populations that rely on them for mainly for irrigation, by the time the Indus breeding and habitat. At least three quarters of reaches the Kotri Barrage (some two thirds of the Delta’s rural population depend, directly or the way into Sindh Province, or 200 km from indirectly, on fishing as their main source of the Arabian Sea), there is inadequate flow to income, and most of Pakistan’s commercial maintain the natural ecosystems of the Indus marine fishery operates in and around the Delta. The annual flow reaching the Delta mangrove creeks on the coast of Sindh before the 1994 break from the Water Accord Province. A large proportion of fish and was less than 43 billion m3, and quantities of crustaceans spend at least part of their life cycle silt discharged estimated to be 100 million in the mangroves, or depend on food webs tonnes/year (Meynell and Qureshi 1993). Even originating there (Meynell and Qureshi 1993). The annual value of catch from mangrove- population of some 155,000 people. This area dependent fish species in the Indus Delta is has been most heavily impacted by seawater estimated at around $20 million. Shrimps are intrusion in the Indus Delta. Valuation relied also particularly important, with a domestic primarily on data collected at the Village, value of $70 million and an export value of Taluka and District levels. Primary data about one and a half times this figure, and the collection, through field visits, involved surveys export of mud crabs contributes an additional of farming and fishing communities, interviews $3 million to the regional economy (Mahmood with government line departments, and and Ali undated). consultations with other public sector and non- governmental organisations. Where data Over 60 percent of the rural population also already existed in the form of statistics from use the Delta’s mangroves as their major Federal and Provincial Government source of domestic fuel, estimated to account publications, these comprised the bulk of for around 18,000 tonnes of firewood (Khalil secondary sources. The study entailed 1999) which is worth up to $460,000 a year collecting data on the ecological impact of sea (Mahmood and Ali undated). Mangroves are intrusion and economic data on agricultural also used by coastal villagers as fodder for and fisheries products, and establishing a link domestic animals. In addition to cattle, sheep between reduced freshwater flows, saltwater and goats kept permanently in the Delta, it has intrusion, and loss of household production. been estimated that at certain times of the year about 16,000 camels are herded into the Using valuation to show the mangroves (Khalil 1999, Meynell and Qureshi 1993). In total, the Indus Delta’s natural economic benefits of allocating ecosystems are thought to contribute about water to ecosystems 67,000 tonnes of leaves and 20,000 tonnes of Analysis of the data collected during the study grasses as livestock pasture and fodder each showed that reduced freshwater flows, and year, together worth up to $1.35 million consequent ecosystem degradation, had (Mahmood and Ali undated). impacted heavily on local livelihoods and economic production in the Indus Delta area. Valuing the economic costs of Both aggregate crop production and fish catch saltwater intrusion had declined steadily as salinity had increased. The three Talukas or 30,000 households The
Recommended publications
  • Estimation of Paleo-Discharge of the Lost Saraswati River, North West India
    EGU2020-21212 https://doi.org/10.5194/egusphere-egu2020-21212 EGU General Assembly 2020 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Estimation of paleo-discharge of the lost Saraswati River, north west India Zafar Beg, Kumar Gaurav, and Sampat Kumar Tandon Indian Institute of Science Education and Research Bhopal, Earth and Environment Sciences, India ([email protected], [email protected], [email protected] ) The lost Saraswati has been described as a large perennial river which was 'lost' in the desert towards the end of the 'Indus-Saraswati civilisation'. It has been suggested that this paleo river flowed in the Sutlej-Yamuna interfluve, parallel to the present-day Indus River. Today, in this interfluve an ephemeral river- the Ghaggar flows along the abandoned course of the ‘lost’ Saraswati River. We examine the hypothesis given by Yashpal et al. (1980) that two Himalayan-fed rivers Sutlej and Yamuna were the tributaries of the lost Saraswati River, and constituted the bulk of its paleo-discharge. Subsequently, the recognition of the occurrence of thick fluvial sand bodies in the subsurface and the presence of a large number of Harappan sites in the interfluve region have been used to suggest that the Saraswati River was a large perennial river. Further, the wider course of about 4-7 km recognised from satellite imagery of Ghaggar-Hakra belt in between Suratgarh and Anupgarh in the Thar strengthens this hypothesis. In this study, we have developed a methodology to estimate the paleo-discharge and paleo- width of the lost Saraswati River.
    [Show full text]
  • National Transport Policy of Pakistan 2017
    National Transport Policy of Pakistan 2017 Ministry of Planning, Development & Reform Government of Pakistan National Transport Policy of Pakistan 2017 Key messages from the Prime Minister, the Minister of Planning, Development and Reform and the Chief Ministers 2 of 40 DRAFT – for concurrence National Transport Policy of Pakistan 2017 Key messages from the Prime Minister, the Minister of Planning, Development and Reform and the Chief Ministers [Brief statements or messages from the Prime Minister, Minister of Planning, Development and Reform and the Chief Ministers to be added.] 3 of 40 DRAFT – for concurrence National Transport Policy of Pakistan 2017 4 of 40 DRAFT – for concurrence National Transport Policy of Pakistan 2017 Contents Introduction messages 2 1 The State of Pakistan’s Transport Sector 4 1.1 Pakistan’s Transport Context: The Current Situation 5 1.2 Business as Usual Scenario 10 2 The Need for a National Transport Policy and Master Plan 14 2.1 Contribution to the Pakistan’s Government Policies and Plans 15 2.2 Relationship with existing policies and transport plans 16 3 National Transport Vision for Pakistan 17 3.1 Vision Statement 17 4 Principles for the Governance of Pakistan’s Transport Sector 18 5 National Transport Policy Objectives 21 6 Policy directions for each of the transport sub-sectors 26 6.1 Road transport 27 6.2 Rail transport 28 6.3 Air transport 29 6.4 Maritime transport 30 6.5 Pipelines 31 6.6 Inland Waterway transport 31 6.7 Urban transport 32 6.8 Multimodal logistics 33 7 Implementation arrangements 34 8 Bibliography 37 5 of 40 DRAFT – for concurrence National Transport Policy of Pakistan 2017 1.
    [Show full text]
  • Power Project at Keti Bundar
    INFORMATION MEMORANDUM 2X660 MW IMPORTED/THAR COAL POWER PROJECTS AT KETI BANDER SINDH COAL AUTHORITY ENERGY DEPARTMENT GOVERNMENT OF SINDH Bungalow No.16 E Street, Zamzama Park, DHA Phase-V, Karachi. Phone: 99251507 1 THE LAND AND THE GOVERNMENT Pakistan, a land of many splendors and opportunities, the repository of a unique blend of history and culture from the East and the west, the cradle of one of the oldest civilizations which developed around the Indus Valley. It is the ninth most popular country of the world with 132.35 million tough, conscientious, hard working people, wishing and striving hard to enter into the 21st century as equal partners in the community of developed nations. It is located between 23 and 37 degrees latitude north and 61 and 76 degrees longitude east. Flanked by Iran and land- locked Afghanistan in the west and the Central Asian Republics and China in the north, Pakistan can rightly boost of having a significant location advantages with a vast only partially tapped market of 200 million people. The affluent Gulf States are just across the Arabian Sea to the south and provide an additional opportunity of a high consumption market. The geographical location, with one of the highest peaks of the world in the north and vast plains in the south, offers an unusual diversity of temperatures ranging from sub-zero levels on the mountains in winter to scorching heat in the plains in summer, providing friendly habitat to exquisite range of flora and fauna and a large variety of agricultural crops used for both foods and raw material for industries.
    [Show full text]
  • 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.
    [Show full text]
  • Water Wars: the Brahmaputra River and Sino-Indian Relations
    U.S. Naval War College U.S. Naval War College Digital Commons CIWAG Case Studies 10-2013 Water Wars: The Brahmaputra River and Sino-Indian Relations Mark Christopher Follow this and additional works at: https://digital-commons.usnwc.edu/ciwag-case-studies Recommended Citation Christopher, Mark, "MIWS_07 - Water Wars: The Brahmaputra River and Sino-Indian Relations" (2013). CIWAG Case Studies. 7. https://digital-commons.usnwc.edu/ciwag-case-studies/7 This Book is brought to you for free and open access by U.S. Naval War College Digital Commons. It has been accepted for inclusion in CIWAG Case Studies by an authorized administrator of U.S. Naval War College Digital Commons. For more information, please contact [email protected]. Draft as of 121916 ARF R W ARE LA a U nd G A E R R M R I E D n o G R R E O T U N P E S C U N E IT EG ED L S OL TA R C TES NAVAL WA Water Wars: The Brahmaputra River and Sino-Indian Relations Mark Christopher United States Naval War College Newport, Rhode Island Water Wars: The Brahmaputra River and Sino-Indian Relations Mark Christopher Center on Irregular Warfare & Armed Groups (CIWAG) US Naval War College, Newport, RI [email protected] CHRISTOPHER: WATER WARS CIWAG Case Studies Bureaucracy Does Its Thing (in Afghanistan) – Todd Greentree Operationalizing Intelligence Dominance – Roy Godson An Operator’s Guide to Human Terrain Teams – Norman Nigh Organizational Learning and the Marine Corps: The Counterinsurgency Campaign in Iraq – Richard Shultz Piracy – Martin Murphy Reading the Tea Leaves: Proto-Insurgency in Honduras – John D.
    [Show full text]
  • Himalaya to the Sea: Geology, Geomorphology and the Quaternary' by John F
    HIMALAYA, the Journal of the Association for Nepal and Himalayan Studies Volume 16 Number 1 Himalayan Research Bulletin No. 1 & Article 17 2 1996 Book review of 'Himalaya to the Sea: Geology, Geomorphology and the Quaternary' by John F. Shroder, Jr. (ed.) Daniel D. Schelling University of Utah Follow this and additional works at: https://digitalcommons.macalester.edu/himalaya Recommended Citation Schelling, Daniel D.. 1996. Book review of 'Himalaya to the Sea: Geology, Geomorphology and the Quaternary' by John F. Shroder, Jr. (ed.). HIMALAYA 16(1). Available at: https://digitalcommons.macalester.edu/himalaya/vol16/iss1/17 This Book Review is brought to you for free and open access by the DigitalCommons@Macalester College at DigitalCommons@Macalester College. It has been accepted for inclusion in HIMALAYA, the Journal of the Association for Nepal and Himalayan Studies by an authorized administrator of DigitalCommons@Macalester College. For more information, please contact [email protected]. William Fisher Harvard University Himalaya to the Sea: Geology, Geomorphology and the Quaternary. Edited by John F. Shroder, Jr. London, Routledge, 1993. Pp. xxvii + 429. $130.00 Located along the northwestern sector of the within the Himalayan region and South Asia (on which Himalayan continental-collision belt, the Kirthar­ many volumes have been published in recent years), and Sulaiman transform plate-boundary, and the eastern therefore the collection of papers in this volume will be sector of the Makran oceanic-subduction zone, Pakistan of interest to earth scientists working in a large number is one of the most tectonically active regions in the of tectonic, sedimentological and geomorphological world.
    [Show full text]
  • Perennial and Non-Perennial River- River Originating from Mountains, They Get Water Throughout the Year, That River Consider As Perennial River
    Perennial and Non-Perennial river- River originating from mountains, they get water throughout the year, that river consider as Perennial river. on the other hand river originating from plateau region called Non-Perennial river. these river do not have enough water for the whole year. Peninsular river- They have a large seasonal fluctuation in volume as they are solely fed from rainfall. These river flow in valley with steep gradients. the river which end in the Bay of Bengal are called 'East flowing' river, If the river empties into the Arabian sea, it is called ' West flowing' river. Inland drainage river- The river which does not empty itself into any sea, and end with any lake or any other water body is known as Inland Drainage river. Classification Indus River Originated from Bokharchu Glacier , near Mansarover. Rivers in India Total length of about 2897 km, it fall into the Arabian sea. Enter in India through Ladakh, flow only in J&K. Ganga River It flow between the Ladakh range and the Zaskar range at Leh. Brahmaputra River Originates as the Bhagirathi from the Gangotri glacier. Originates from Mansaravar Lake. Alaknanda unites with Bhagirathi at Devprayag, Uttarakhand, henceafter know as Ganga. Total length of about 3848 km. It fall into Bay of Bengal. At Bangladesh, Ganga merge with Brahmaputra, mixture known as Padma river. Enter India in Arunachal Pradesh. most of its course lies outside India. Total length of about 2510 km, It fall into the Bay of Bengal. It flow parallel to the Himalayas in the eastward direction. Originate from the Yamunotri glacier, at the Bandarpoonch peak in Uttarakhand.
    [Show full text]
  • “Major World Deltas: a Perspective from Space
    “MAJOR WORLD DELTAS: A PERSPECTIVE FROM SPACE” James M. Coleman Oscar K. Huh Coastal Studies Institute Louisiana State University Baton Rouge, LA TABLE OF CONTENTS Page INTRODUCTION……………………………………………………………………4 Major River Systems and their Subsystem Components……………………..4 Drainage Basin………………………………………………………..7 Alluvial Valley………………………………………………………15 Receiving Basin……………………………………………………..15 Delta Plain…………………………………………………………...22 Deltaic Process-Form Variability: A Brief Summary……………………….29 The Drainage Basin and The Discharge Regime…………………....29 Nearshore Marine Energy Climate And Discharge Effectiveness…..29 River-Mouth Process-Form Variability……………………………..36 DELTA DESCRIPTIONS…………………………………………………………..37 Amu Darya River System………………………………………………...…45 Baram River System………………………………………………………...49 Burdekin River System……………………………………………………...53 Chao Phraya River System……………………………………….…………57 Colville River System………………………………………………….……62 Danube River System…………………………………………………….…66 Dneiper River System………………………………………………….……74 Ebro River System……………………………………………………..……77 Fly River System………………………………………………………...…..79 Ganges-Brahmaputra River System…………………………………………83 Girjalva River System…………………………………………………….…91 Krishna-Godavari River System…………………………………………… 94 Huang He River System………………………………………………..……99 Indus River System…………………………………………………………105 Irrawaddy River System……………………………………………………113 Klang River System……………………………………………………...…117 Lena River System……………………………………………………….…121 MacKenzie River System………………………………………………..…126 Magdelena River System……………………………………………..….…130
    [Show full text]
  • Transboundary River Basin Overview – Indus
    0 [Type here] Irrigation in Africa in figures - AQUASTAT Survey - 2016 Transboundary River Basin Overview – Indus Version 2011 Recommended citation: FAO. 2011. AQUASTAT Transboundary River Basins – Indus River Basin. Food and Agriculture Organization of the United Nations (FAO). Rome, Italy The designations employed and the presentation of material in this information product do not imply the expression of any opinion whatsoever on the part of the Food and Agriculture Organization of the United Nations (FAO) concerning the legal or development status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries. The mention of specific companies or products of manufacturers, whether or not these have been patented, does not imply that these have been endorsed or recommended by FAO in preference to others of a similar nature that are not mentioned. The views expressed in this information product are those of the author(s) and do not necessarily reflect the views or policies of FAO. FAO encourages the use, reproduction and dissemination of material in this information product. Except where otherwise indicated, material may be copied, downloaded and printed for private study, research and teaching purposes, or for use in non-commercial products or services, provided that appropriate acknowledgement of FAO as the source and copyright holder is given and that FAO’s endorsement of users’ views, products or services is not implied in any way. All requests for translation and adaptation rights, and for resale and other commercial use rights should be made via www.fao.org/contact-us/licencerequest or addressed to [email protected].
    [Show full text]
  • Conservation of Gangetic Dolphin in Brahmaputra River System, India
    CONSERVATION OF GANGETIC DOLPHIN IN BRAHMAPUTRA RIVER SYSTEM, INDIA Final Technical Report A. Wakid Project Leader, Gangetic Dolphin Conservation Project Assam, India Email: [email protected] 2 ACKNOWLEDGEMENT There was no comprehensive data on the conservation status of Gangetic dolphin in Brahmaputra river system for last 12 years. Therefore, it was very important to undertake a detail study on the species from the conservation point of view in the entire river system within Assam, based on which site and factor specific conservation actions would be worthwhile. However, getting the sponsorship to conduct this task in a huge geographical area of about 56,000 sq. km. itself was a great problem. The support from the BP Conservation Programme (BPCP) and the Rufford Small Grant for Nature Conservation (RSG) made it possible for me. I am hereby expressing my sincere thanks to both of these Funding Agencies for their great support to save this endangered species. Besides their enormous workload, Marianne Dunn, Dalgen Robyn, Kate Stoke and Jaimye Bartake of BPCP spent a lot of time for my Project and for me through advise, network and capacity building, which helped me in successful completion of this project. I am very much grateful to all of them. Josh Cole, the Programme Manager of RSG encouraged me through his visit to my field area in April, 2005. I am thankful to him for this encouragement. Simon Mickleburgh and Dr. Martin Fisher (Flora & Fauna International), Rosey Travellan (Tropical Biology Association), Gill Braulik (IUCN), Brian Smith (IUCN), Rundall Reeves (IUCN), Dr. A. R. Rahmani (BNHS), Prof.
    [Show full text]
  • Human Impact on the Sediment Loads of Asian Rivers
    Sediment Problems and Sediment Management in Asian River Basins 37 (Proceedings of the Workshop held at Hyderabad, India, September 2009). IAHS Publ. 350, 2011. Human impact on the sediment loads of Asian rivers DES E. WALLING Geography, College of Life and Environmental Sciences, University of Exeter, Exeter EX4 4RJ, UK [email protected] Abstract The suspended sediment load of a river exerts a key influence on its aquatic ecology, its morphology and the exploitation of its water resources. Changes in the sediment loads of rivers can therefore have wide-ranging environmental and social and economic consequences. There is growing evidence that the sediment loads of many Asian rivers have changed significantly in recent years. Some have increased, whereas others have decreased. It is important that such changes should be seen in a longer term context. Although climate change is increasingly seen as a cause of changing sediment loads, human impact is generally recognised to be the key cause. The key drivers of these changes can be grouped into those causing increases and those causing decreases. The former include land clearance, land-use activities and other forms of catchment disturbance. The latter include sediment trapping by dams, soil conservation and sediment control programmes, and sand extraction from river channels. The changes shown by the sediment load of a river will reflect the spatial and temporal integration of the impacts of these drivers. The temporal pattern of change can reflect the contrasting temporal trajectories
    [Show full text]
  • The Marked Reduction of the Indus River Flow
    The marked reduction of the Indus river flow downstream from the Kotry barrage: can the mangrove ecosystems of Pakistan survive in the resulting hypersaline environment? Item Type article Authors Ahmed, S.I. Download date 01/10/2021 19:37:14 Link to Item http://hdl.handle.net/1834/31900 Pakistan Journal of Marine Sciences, Vol.1(2), 145-153, 1992. REVIEW ARTICLE THE MARKED REDUCTION OF THE INDUS RIVER FLOW DOWNSTREAM FROM THE KOTRI BARRAGE: CAN THE MANGROVE ECOSYSTEMS OF PAKISTAN· SURVIVE IN THE RESULTING HYPERSALINE ENVIRONMENT? Saiyed I. Ahmed School of Oceanography, University of Washington, Seattle, WA 98195, U.SA. APPLICATION OF KNOWLEDGE ,OF MANGROVE ECOSYSTEMS FROM AROUND THE WORLD TO THE UNDERSTANDING OF THE PRESENT STATUS OF MANGROVES OF PAKISTAN. The global inventory of obligate mangroves consists of 54 species belonging to 20 genera in 16 families and are estimated to occupy about 23 million hectares of shel­ tered coastal intertidal land (Tomlinson, 1986; Lugo and Snedaker, 1974; Chapman, 1975, 1976). These are regarded as 11 obligate11 mangroves as they are 11 restricted11 to coastal saline intertidal environments compared to 11 facultative 11 mangroves which may develop in non-coastal environments. In a general classification scheme basically two groups of mangroves can be identified: (a) the Eastern Group: mangroves on the coasts of Indian and Western Pacific Oceans, (b) the Western Group: Those on the coasts of the Americas, West Indies and West Africa. Generally speaking, the Eastern Group of mangroves is richer in species diversity with mangroves in India and southeast Asia exhibiting species diversity of > 20 with generally healthy and luxurious plant growth.
    [Show full text]