Wednesday, July 4, 2012

Pakistan India international water in perspective of Remote sensing


The water emergency prevailing in the country both due to recurring cycle of floods and drought and the unsustainable and inefficient use of most water resources has brought home the urgent need for developing a strategy for the conservation of every drop of water and its sustainable and equitable use. Water is the most important renewable and finite natural resources since it is required for agriculture, industry and domestic purposes.

Surface and ground water that cross international boundaries present increased challenges to regional stability because hydrologic needs can often be overwhelmed by political considerations. While the potential for paralyzing disputes is especially high in these basins, history shows that water can catalyze dialogue and cooperation, even between especially contentious riparian. There are 263 rivers around the world that cross the boundaries of two or more nations, and an untold number of international ground water aquifers. 


 Water dispute between Pakistan India  

Water disputes between India and Pakistan emerged immediately after the partition of the sub-continent into two independent and sovereign states.  This partition unfortunately cut across the already established and well functioning networks of irrigation canals and numerous hydraulic structures with control structures of the Eastern Rivers falling within the domain of India and canal network extending into West Punjab and irrigating some 5 million acres of fertile land.

Soon after the partition, India communicated to Pakistan of its intention to diver t the waters of Eastern Rivers for its own uses. As the control structures were in the Indian Territory, India could do it easily. This meant that the single and only economic base of Pakistan, i.e., irrigated agriculture would be left high and dry. This act of India was tantamount to strangulatin Pakistan' agro-based economy and igniting the fuse for a major war. The sensitivities of this issue were realized by international communities as well and with the good offices of the World Bank and over a decade of negotiations, the Indus Waters Treaty was signed in 1960 between India and Pakistan with World Bank as a guarantor and also signatory to the Treaty. This treaty sets out the legal framework for the sharing of the waters of six rivers

The Indus River: originates in Chinese-controlled Tibet and flows through Jammu & Kashmir.
The Chenab originates in India’s Himachal Pradesh state, travels through Jammu & Kashmir.
The Jhelum rises in Jammu & Kashmir and flows into Pakistan, finally joining Chenab.

The Treaty affords India use of the following three rivers:

The Sutlej originates in Tibet, flows through Himachal Pradesh and Punjab before joining the Chenab.
The Beas and the Ravi originates in Himachal Pradesh state and flow into Pakistan, emptying into the Chenab.


Indian violation of Indus water treaty

India is currently constructing three hydropower projects on River Indus. These include Chutak Dam with 59- meter height, Nimoo Bazgo with 57-metre height and Dumkhar of 42-meter height. These projects are at initial or middle stages of construction.

Other violations are: India is irrigating about 800,000 acres in Chenab area which is not permissible; it has built five more canals in the past 10 years to increase the irrigated area in the region. Pakistan has also asked India to provide details of its agricultural acreage, crops and other projects in Kashmir to enable it to make plans in advance. Low inflows are in evidence in the Rivers Chenab and Jhelum for the past several months. In particular, the flow of the Chenab has become very low after the construction of Baglihar Hydropower project. 


Construction of diamer bhasha dam on Indus River
The expediency of Remote sensing and GIS for water management


By using high-resolution SAR (synthetic aperture radar) satellite imagery to estimate discharge in remote, braided, glacial rivers that may be sensitive to changing regional or global climate. The sensors used in these and other river studies may be classified into two types:

(1)   Passive, in which the sensor receives energy naturally reflected by or emitted from the earth's surface.
(2)   Active, in which the sensor provides its own illumination and records the amount of incident energy returned from the imaged surface.

Passive sensors include all of the visible and infrared instruments such as the Landsat Thematic Mapper (TM) and Multi-Spectral Scanner (MSS), the Advanced Very High Resolution Radiometer (AVHRR), the Satellite (SPOT) and the anticipated Advanced Spaceborne Thermal Emission and Refraction Radiometer (ASTER), Moderate-Resolution Imaging Spectroradiometer (MODIS) and Landsat-7 sensors.
Passive microwave radiometers such as the Special Sensor Microwave/ Imager (SSM/I) measure the amount of microwave energy naturally emitted from the Earth's surface.

More recently, improvements in satellite orbital precision and the increasing availability of multi-temporal satellite data have enabled the estimation of river stage and discharge from space. While these techniques are largely in their infancy and not yet used operationally, three general approaches have emerged:


(1)   Direct measurement of water surface level from radar altimeter waveform data.
(2)   Determination of water surface elevations at their point of contact with the land surface using high-resolution satellite imagery and topographic data.
(3)   Correlation of satellite-derived water surface areas with ground measurements of stage or discharge.

Conclusion

Through the use of RS and GIS, both the countries can surveillance their main rivers and related tributaries. High-resolution visible/infrared sensors such as Landsat imagery provide good delineation of flood extent where Clouds, trees or floating vegetation do not obscure the water surface. Passive microwave radiometers show promise for acquiring estimates of inundation area over very large rivers or wetlands, but sensor resolution is coarse and the land-water boundary cannot be located accurately. Spaces borne synthetic aperture radars (SARs) are not limited by weather conditions or darkness. So these technologies not only help these countries to resolve their water dispute but also established a solid foundation to resolve other conflicts.


       
PREPARED BY
                              Hafiz Ali Imran
                              M.phil (space science)    
                              Session 2011-2013
Email:                   hfz_ali_imran@hotmail.com
Contact No:          0334-4096620




Tuesday, July 3, 2012

Pakistan Forests - A Remote Sensing Perspective


A forest referred to as a wood or the woods in an area with a high density of trees.

The forestry sector of Pakistan is a main source of lumber, paper, fuelwood, medicine as well as food and provide ecotourism and wildlife conservation purposes.

Overall Pakistan forest resources are limited, covering only 2.5percent of total land area, which is far below the standard of 25%,Less than five per cent of the country`s total area is under forests forest cover which is very poor as compared with other Asian countries. For example, in India, Japan, Sri-Lanka, Philippines, Korea, Bhutan and Brunei, natural forest area is 24.2, 36.4, 42.1, 43.6, 49.8, 50.4 and 90.4 per cent respectively of the total land area. Contrary to this, total forest area of Pakistan is around four million hectares including 0.51, 1.33, 0.84 and 1.36 million hectares in Punjab, NWFP, Sindh and Balochistan, respectively. However, forests of Pakistan are very rich in terms of biodiversity and present a unique blend of tree, shrub, grass and animal species, living across various ecological (climatic) zones. Most of the natural forest resources of Pakistan are concentrated in the mountainous regions of the north covering Himalaya, Hindukush and Karakoram ranges, where more than 60% of the country natural forest resources are found. The rest of forestry resource is distributed among the south-western mountains of Baluchistan, plains of Punjab and Sindh and the coastal areas of Arabian Sea in the south.
Forest covers distribution in Pakistan
Ecologically is distributed into nine ecological zones depending mainly on moisture availability, temperature, elevation and soil conditions .Each ecological zone offers specific environmental, topographic and climatic conditions required to support particular trees and plants species. Based on these specific ecological conditions the forests of Pakistan are classified into nine major forest types for the sake of simplicity, it can be clustered into some broader groups, as described below

Alpine forests of Pakistan are found at very high elevations in the mountainous regions of Himalaya, Karakoram and Hidukush. These forests are subdivided into Sub Alpine forests, Alpine scrub and Alpine pastures. The Sub Alpine forests grow to the tree limit and due to harsh climatic conditions tree density is low. Alpine scrubs include shrub 150 m or more above the sub-alpine forests. Alpine pastures are situated above the tree line of 4000 meters, where growing season is very short and vegetation mainly consists of perennial, herbaceous plants. These high altitude pastures are found mostly in the northern districts of Gilgit, Diamer, Chitral and Skardu.                                                              

Temperate forests of Pakistan are sub-divided into moist and dry temperate, depending on the rainfall. In moist temperate zone high summer rainfall occurs where mountain masses stand exposed to the moist southwest winds. Moist temperate forests of Pakistan are concentrated in the northern districts of Muree, Kaghan valley, Kashmir region, and Swat Valley etc. On the other hand Dry temperate forests grow at the same altitude, as the moist temperate, but receive little of no summer rains.These forests are mostly found in the northern districts of Dir, Chitral, Kohistan, Diamer and Gilgit etc.



Sub-tropical forests are found in the lower reaches of Himalya, Hindukush and Sulaiman Ranges between 600-1700 m above sea level. These forests are subdivided into sub tropical broad-leaved forest and sub tropical pine forests. Broad leaved forests grow in the lower most reaches between 600-1000 m, and consists of drought resistant species. These sub tropical broad leaved forests cover fairly large area of about 1,191,000 ha. On the other hand Sub-tropical pine forests are found at little higher altitude1000-1700 m, meeting the temperate forests at the upper end.Chir pine is the major specie found.

Dry Tropical Forests fairly large areas of Pakistan fall under the dry tropical zone consisting of Indus plains in Punjab and Sindh and low hills in southern and western Balochistan. The climatic conditions varies from semi-arid (250-750 mm rainfall) to arid (<250 mm rainfall). The summer temperature in zone goes up to as high as 50oC. Dry Tropical Forests of Pakistan can be categorized into two group’s i.e. tropical thorn forests and tropical dry deciduous forests. Tropical thorn forests mainly consist of low and scanty trees and shrubs of thorny species. On the other hand Tropical dry deciduous forests consist of almost entirely of deciduous species. These forests do not occur extensively in Pakistan but are limited to the Rawalpindi foothills.

Main forest types are:

The coniferous forests occur from 1,000 to 4,000 m altitudes. Chitral, Swat, ranges of the Himalayas and Hindu Kush and Abbottabad districts of Pakhtunkhwa, Northern Areas and Islamabad district of the Punjab are the main areas covered with coniferous forests. Silver fir, deodar, blue pine, chir pine are the most common varieties. The Coniferous forests also occur in Balochistan hills. Chilghoza pine and juniper are the two most common species of Balochistan.
They supply people with lumber, fuel wood, fodder and medicinal plants.

The riverine forests mostly grow on the banks and dry bed of the River Indus in the flood plains of Sindh and Punjab. Their existence depends on annual flooding in the Indus basin. These forests are of high economic value yielding timber, fuel wood and latex. These forests also form a protective line barrier between river and the embankments against floods.

The mangrove forests are located in the Indus River Delta.Mangrove forests are the natural shield for heightened waves, cyclone and tsunami. Their roots and stems absorb shocks of the tides and transform them to a gentle stage. Mangrove forests also provide the breeding ground for fish, birds and livelihood to fishermen. Different organizations using remote sensing data for monitoring the health of newly planted mangroves forests in the coastal region. Satellite images can show the distribution of mangrove forests along coast of Pakistan and can depict mangrove forest in Indus delta

Irrigated forest is spread over the plains of Punjab and Sindh.The canal water is used for development and growth of this plantation.A typical example is Chhanga Manga irrigated forest plantation.
The irrigated plantations were first developed in 1866 at Changa Manga in Lahore. Today they occupy about 226,000 ha. Sheesham, mulberry and species of Populus are the common tree species grown in the irrigated plantations.The Irrigated forests were raised to meet demand for fuel wood.

            Deforestation

Pakistan has few forests to begin with, and they’re vanishing fast. The country has lost a quarter of its natural forest cover over the past two decades and is currently experiencing a deforestation rate of 2.1 percent a year. Pakistan is having the world's second highest rate of deforestation.

The causes of the deforestation are multiple i.e.increase in temperature and decrease in rainfall, illegal cutting and clearing of forested lands for agriculture and for expanding urban areas are only the main ones.

Effects of deforestation are erosion of soil, disruption of the water cycle, flooding and drought, climate change.

A province-wise breakdown of forest land converted to other uses shows that Punjab tops the list with conversion of 99,711 acres, followed by Sindh with 27,874 acres, Balochistan with 13,693 acres, Khyber Pakhtunkhwa with 9,692 acres, and Azad Jammu and Kashmir with only 577 acres. This way the forest land conversion becomes 151,548 acres.


The highest rate of deforestation has been found in the Indus delta mangroves, which has depleted at a rate of around 2.3 percent, while the coniferous forest depleted at 1.99 percent and ravine forests at 0.23 percent.
  Over 4.242 million hectares in the country were forest land in 1992. However, it declined to 3.44 million hectares by 2001.
Between 1990 and 2010, Pakistan lost an average of 42,000 ha or 1.66% per year. In total, between 1990 and 2010, Pakistan lost 33.2% of its forest cover or around 840,000 ha.

TOTAL FOREST COVER (1000 ha)
1990                2000             2005               2010
2527                 2116           1902                1687  
ANNUAL CHANGE RATE (percent) 
1990-2000     2000-2005       2005-2010
-1.76               -2.11               -2.37                          
Negative number represents deforestation

Afforestation of Sindh coastline was made to save Thatta and its adjoining areas from destruction   caused by sea intrusion, the provincial government has decided to plant trees on the coastline of the district. Sea intrusion and destruction of mangrove forests has exposed these coastline districts to other disasters such as cyclones and tsunamis. Mangroves, coconuts and other trees should be planted in these areas as they can survive the damp and salty climate of the ocean.                        

 REFERENCES

http://www.wildlifeofpakistan.com/IntroductiontoPakistan/forestsofPakistan.htm
http://www.suparco.gov.pk/downloadables/10-Role-of-Satellite-Remote-Sensing.pdf

This article was compiled by:

Arsheen Nasir
Department of Space Sciences,
Uinversity of the Punjab,
Quaid-e-Azam campus,Lahore

Marine/Coastal Resources of Pakistan


I. Introduction

The oceans provide modern society with numerous resources. These resources include mineral deposits, oil and gas, electrical energy, food from marine animals and plants, transportation, and recreation. Unfortunately, many types of marine resources have been mismanaged and over-exploited, and their future sustainability is uncertain.

The Pakistan coast is about 1000 km long extending from the Indian border on the east to the Iranian border in the west. The Exclusive Economic Zone (EEZ) of Pakistan is about240,000 sq. km with an additional continental shelf area of about50,000 sq. km.



The pakistan coastal area is not only rich in living resources but it is also characterized by distinctive oceanic phenomena that could produce abundant mineral, renewable energy and hydrocarbon resource. According to a preliminary survey conducted by the National Institute of Oceanography, it is estimated that about 1100 MW power can be produced from the Indus Deltaic Creek areas (Qurashee 1986).

Living resources:




  • Vegetation

Mangrove forests are extremely important coastal resources, which are vital to our socio‐economic development. A vast majority of human population lives in coastal area, and most communities depend on local resources for their livelihood. The mangroves are sources of highly valued commercial products and fishery resources and also as sites for developing a burgeoning eco‐tourism (Kathiresan and Bingham, 2001).







  • Animal Life

The coastal/marine areas of Pakistan support large fisheries. Fishing grounds for large pelagic species, tuna, mackerel, sharks etc. are located in our offshore waters. Species such as mullet, silver wittings and other small sized demersal fishes, especially juveniles of large commercially important estuarine fish, are harvested from shallow waters in the creek area of the Indus and other small rivers and also in enclosed and semi-enclosed bays throughout the coastal waters (UN-ESCAP 1996).





Non-Living Resources:


  • Fresh Water

A huge quantity of fresh water resource is available in the form of seawater. This resource can be utilized economically with the development of desalination technology (Khan 1999). It will become increasingly essential to develop this resource as the cost of sweet water increases and Pakistan becomes a water short country. 




  • Energy

Renewable Ocean Energy: Tides, Currents, and Waves
Coastal marine areas have significant potential for energy/ fuel generation from marine plants and other organic materials, hydrogen generated from a variety of ocean renewables and marine geothermal power (Quraishee 1986 & Zaigham 2004).

Wave Energy Converter systems extract the power of ocean waves and convert it into electricity.

Tidal/Current systems capture the energy of ocean currents below the wave surface and convert them into electricity. 

Ocean Thermal Energy Conversion (OTEC) generates electricity through the temperature differential in warmer surface water and colder deep water.

Offshore Wind generates electricity by taking advantage of the vast wind resources available across oceans and large water bodies. Out at sea, winds blow freely, unobstructed by buildings or other structures. 

Bio-fuel (next-generation fuel) Marine microalgae, a simple rootless plant accumulates high levels of natural oils and has promising potential as an alternative energy source, it is expected to yield significant energy security and environmental advantage.

Oil and Gas Offshore regions of Pakistan have thick marine sedimentary reservoir rocks with potential traps both structural and stratigraphic. These are a positive indication of the occurrence of hydrocarbon resources in the offshore regions. 

  • Industrial chemicals
Marine flora and fauna and seawater have always been sources of chemicals for industries that include leather, paper, textile, cosmetics, food, and pharmaceuticals.
  • Mineral Potential
The origin and nature of the geological features and processes along the coast suggest that the Pakistan marine geological environment is favorable for the formation of mineral resources. 

  • Placer Minerals
Deposits of coarse-grained placer minerals occur in shallow coastal regions .Placer mineral studies undertaken by the National Institute of Oceanography, Pakistan show concentration of these minerals along the coast (Memon & Ikramuddin 1995). 
  • Building Material

The reserves of gravel and sand in the coastal area drained by the rivers have been heavily exploited during the past decades for construction purposes. In coastal areas, deposits of shells and calcareous sand have been in use for construction and making lime. In shallow waters, the mechanical action of waves and currents concentrates sand and gravel.




Men harvest sea salt at a salt field in Sandspit

  • Sea Salts

Presently sea salt of about 60,000 m tons/year is being extracted from the seawater along the Sindh and Balochsitan coasts. Soda ash and other salts are also being extracted on a small scale by the traditional methodology of creating saltpans in enclosed water.




Coastal resource management issues
Managing ocean resources requires accurate information, extensive survey, data collection and research to understand the processes and features which have direct bearings on locating living and nonliving resources and their sustainable exploitation and conservation. Constraints on marine resources management are as follows:
  • Lack of coordination among stakeholders
  • Uncontrolled exploration of marine resources leading to environmental hazards and/or use conflicts
  • Lack of political commitment and low harmonization of national management plans and legislation related to marine resources
  •  Natural disasters such as rising sea level, flooding, forest fires etc.
The following recommendations are made to expedite resource development of the Pakistan coastal area:

  • Promote education and research in marine science and technology.
  •  Development, management and sustainable utilization of all coastal marine resources.
  •  More funding for ocean/marine education, research and technology development
  •  Substantial ocean resources should be mapped and studied.
  •  Incentives should be provided for private investments for promotion of ocean technologies.
  •  Economic management of coastal marine areas and sustainable use of marine resources
  • Improved institutional capacity and effectiveness in coastal marine resources
  • management along the coast.



References:
Photo credits: GIS Laboratory WWF-Pakistan

Harms, J C.,  Cappel H. N. and Francis D. C., (1984),  “Geology of the Makran Cost annd offshorte Petroleum Potential”. Proceedings Marine Geology and Oceanography of Arabian Sea and Coastal Pakistan” edited by: Bilal U. Haq and John D Milliman.


MARINE RESOURCES IN PAKISTAN: A TENTATIVE INVENTORY by Nuzhat Khan


This article was compiled by:


Wasif Yousaf,
Department of Space Sciences,
Uinversity of the Punjab,
Quaid-e-Azam campus,Lahore



Groundwater prospecting in Pakistan


Groundwater has emerged as an exceedingly important freshwater resource and its everincreasing
demand for agriculture, domestic and industrial uses ranks it as of strategic importance. Global estimates show that groundwater comprises one sixth of the total freshwater
resources available in the world.

Where does underground water come from?

Precipitation that soaks in the ground and trickles downward. Water underground trickles down
between particles of sol and through cracks and spaces in layers of rock.

Pakistan’s major groundwater resource is in the irrigated areas of the Indus Basin, while the
second source lies in the areas outside the Indus Basin.
Canal irrigation was introduced in the Indus Basin about a century ago. Before the irrigation
system the groundwater table was 100 feet below the ground surface in most of the Basin. With
the introduction of the irrigation system, groundwater is now in a range of 5 to 30 feet below
ground surface.

Groundwater Quality

A number of the activities of man pose threats to water quality. Some of these
activities include:

Landfill solid waste disposal, Liquid waste disposal basins, Septic waste infiltration systems,
Highway deicing with chemicals ,Gasoline service stations, Petroleum bulk storage facilities,
Underground storage tanks, Many industrial activities, Livestock feed lots, Urban storm water
infiltration.


An arid country, Pakistan depends heavily on annual glacier melts and monsoon rains. Water from these sources flows down the rivers and out to the sea. En route, there are seepages into the ground, where water-bearing rocks or aquifers absorb and store this water. Many of Pakistan’s glaciers are retreating as a result of climate change. This retreat impacts water supplies to millions of
people. Most parts of the country receive scant rainfall and have little or no access to surface water. Pakistan Water Partnership (PWP) states that in Pakistan the total available surface water is about 153 million acre feet (MAF) and the total ground water reserves are approximately 24 MAF, of which a substantial part has been mined without allowing for natural recharge. Currently estimated at 160 million, the population of Pakistan is set to double in 2.5 decades. This means that the per capita availability of water will decrease. There is likely to be a net decrease, rather than an increase in the country’s water resources, due to a number of factors including population growth, climate change, and exploitation of water. Because of the absence of groundwater management in the private sector, anyone can install a tube well anywhere in his land and can extract whatever amount of water he wants any time without consideration of the detrimental effect of his action on the resource. If the pumping is equal to recharge rate for a sufficient period of time, the water table depth will stabilize somewhere below the ground surface.







Our water resource base continues to be degraded because of pollution, atrophy, verse of surface water and over-exploitation of groundwater. The Indus delta has been reduced to one partially active creek and there is no water flowing downstream of the Kotri Barrage for almost the entire year. Pakistan is dependent on a single river system and we cannot afford to take any more chances with the water/sediment/salt balance of the Indus Basin. The rivers and reservoirs in Pakistan are running dry, the underground water table is receding fast and there is widespread talk of massive water shortages in the country.




RECOMMENDATIONS

A groundwater regulatory framework should be introduced and implemented for the sustainability of groundwater use.

There is need to manage the demand of water.

Low water delta crops should be preferred to high delta crops.

Efficient irrigation methods should be used to irrigate crops.

Recharge of groundwater should be increased by increasing canal diversions, rainwater harvesting and check dams.

Saline water can be used for saline agro-forestry or for alternative agricultural crops.

Energy charges should be proportional to the use of energy for tube wells.

Research on groundwater recharge is urgently required.






References


http://www.huffingtonpost.com/bill-chameides/where-has-all-the-water-g_b_778491.html
http://earthsci.org/processes/geopro/ugwater/ugwater.html
http://www.tbl.com.pk/pakistans-water-problems/
http://www.tbl.com.pk/indus-basin-irrigation-system-of-pakistan/
Sind Univ. Res. Jour. (Sci. Ser.) Vol. 41 (1) 47-54 (2009)
The Lahore Journal of Economics 15: SE (September 2010): pp. 187-211
http://cms.waterinfo.net.pk/pdf/wr.pdf





This article was compiled by:



ZAFAR IQBAL ZAFAR
Department of space science
University of the Punjab Lahore
Email: zafarziz@hotmail.com
Phon: 0345-4776066