Himalayan Water Security: The Challenges for South and Southeast Asia

The scramble for control of natural resources to support economic and population growth, combined with the uncertain effects of climate change on the Tibetan Plateau, is raising tensions in Asia over Himalayan water resources.

Ten of the region’s largest and longest rivers (the Amu Darya, Brahmaputra, Ganges, Indus, Irrawaddy, Mekong, Salween, Tarim, Yangtze, and Yellow) originate in the Himalayas. These rivers help provide water, food, and energy for nearly 4 billion people in China and across South and Southeast Asia—nearly half of the world’s population. However, depletion and diversion of these transborder resources to meet growing industrial, agricultural, and urban demands have the potential to trigger far-reaching economic, social, and environmental challenges.

The lack of comprehensive and effective regional frameworks for cooperation hinders sustainable management of these waterways. China, which controls the headwaters of these rivers, has an enormous need for Himalayan water to satisfy economic and energy demands but has little incentive to participate in formal water-sharing and water-management agreements with its neighbors. China’s dam-building and water-diversion projects are a source of major concern to the countries downstream, which often complain about Beijing’s lack of transparency and reluctance to share information. Although managing water-sharing relations with China might be the most prominent challenge, cooperation is not much easier at the middle and lower reaches of the rivers. Collaboration in South and Southeast Asia is frequently frustrated by competing national interests, economic priorities, political disputes, and weak regional organizations. In addition to the environmental impacts of man-made diversion projects and unsustainable freshwater usage, there is also inadequate cooperation on scientific research to understand and prepare for the effects of climate change on the region’s water supplies.

This Asia Policy roundtable contains seven essays that discuss the challenges and implications of water security in Asia and recommend steps that both upstream and downstream countries could take to better manage the region’s shared water resources.

Asia’s Unstable Water Tower: The Politics, Economics, and Ecology of Himalayan Water Projects
Kenneth Pomeranz

China’s Upstream Advantage in the Great Himalayan Watershed
Jennifer L. Turner, Susan Chan Shifflett, and Robert Batten

Melting the Geopolitical Ice in South Asia
Robert G. Wirsing

Himalayan Water Security: A South Asian Perspective
Tushaar Shah and Mark Giordano

Hydropower Dams on the Mekong: Old Dreams, New Dangers
Richard P. Cronin

Climate Change and Water Security in the Himalayan Region
Richard Matthew

Securing the Himalayas as the Water Tower of Asia: An Environmental Perspective
Jayanta Bandyopadhyay

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As I have been arguing for a number of years South Asia needs to re-negotiate the Indus Water Treaty to encompass Afghainstan, Bangladesh, Bhutan, China, India, Nepal and Pakistan before the region starts to suffer from water insecurity and the effects of climate change. Editor

 

 

 

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Rains Failing Over India:

Feeble 2014 Monsoon Heightens Concerns That Climate Change is Turning A Once-Green Land into Desert

El Nino has yet to be declared. Though signs of the Pacific Ocean warming event abound, they are still in the early stages. But for all the impact on the current Indian Monsoon — the rains this vast sub-continent depends on each year for a majority of its crops — the current pre-El Nino may as well be a monster event comparable to 1998.

For the rains that have come so far have been feeble. By June 18, precipitation totals were more than 50% below the typical amount by this time of year for northern and central India and 45% below average for the country as a whole. A stunted Monsoon that many are saying is about as weak as the devastatingly feeble 2009 summer rains. And with Pacific Ocean conditions continuing to trend toward El Nino, there is concern that this year’s already diminished rains will snuff out entirely by mid-to-late summer, leaving an already drought-wracked India with even less water than before.

Through June 25th, the trend of abnormally frail monsoonal rains continued unabated:

India cloud cover on June 25, 2013 [Left Lower image] compared to India cloud cover on June 25 of 2014 [right upper image].

Note the almost complete lack of storms over India for this year compared to 2013 when almost the entire country was blanketed by rains. Image source: LANCE-MODIS.)

India’s Rain Pattern Has Changed

It’s not just that 2014 is a bad year for India. It’s that the current weakened monsoon comes at the tail end of a long period in which the rains have increasingly failed. Where in the past it took a strong El Nino to stall the rains, ever-increasing human atmospheric and ocean warming have pushed the threshold for Monsoonal failure ever lower. Now even the hint of El Nino is enough to set off a dry spell. A growing trend of moisture loss that is bound to have more and more severe consequences.

A new study by Stanford University bears out these observations in stark detail. For the yearly monsoon that delivers fully 80 percent of India’s rains has fallen in intensity by more than 10% since 1951. And though a 10% loss may seem relatively minor, year on year, the effects are cumulative. Overall, the prevalence of dry years increased from 1981 to 2011 by 27% and the number of years experiencing 3 or more dry spells doubled.

Meanwhile, though a general drying trend has taken hold, rain that does occur happens in more intense bursts, with more rain falling over shorter periods. These newly intensified storms are more damaging to lands and homes, resulting in both increasing destruction of property while also greatly degrading the land through more intense erosion.

25 Percent of India’s Land is Turning to Desert

Loss of annual monsoonal rains is coming along with a dwindling of water flows from the melting Himalayan glaciers. These two climate change induced drying effects are already having stark impacts.

For according to the Indian Government’s Fifth National Report on Desertification, Land Degradation and Drought, a quarter of India’s land mass is now experiencing desertification even as 32 percent is suffering significant degradation due to heightening dryness and erosion. This amounts to more than 80 million hectares of land facing desertification while more than 100 million hectares are steadily degrading. The report also noted that areas vulnerable to drought had expanded to cover 68% of the Indian subcontinent.

From the report: (India Monsoon.)

Desertification and loss of biological potential will restrict the transformation of dry lands into productive ecosystems. Climate change will further challenge the livelihood of those living in these sensitive ecosystems and may result in higher levels of resource scarcity.

Monsoonal Delay, Weakening Continues

By today, June 26, the long disrupted and weakened monsoon continues to sputter. Moisture flow remains delayed by 1-2 weeks even as the overall volume of rainfall is greatly reduced.

Though storms have exploded over some provinces, resulting in flash flooding, much of the country remained abnormally dry.

Overall, preliminary negative rainfall departures remained at greater than 40% below average for most of the nation with only five provinces receiving normal rainfall and the remaining 31 receiving either deficient or scant totals. More

 

 

 

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Pakistan has only 30 days of water reserves - researchers

ISLAMABAD, Pakistan (Thomson Reuters Foundation) – Inadequate planning is exposing Pakistan to water-related threats from climate change and putting the country’s agriculture, industry and hydropower at risk, water experts say.

Speaking at a water summit in Pakistan recently, they said the country desperately needs more reservoirs to increase its water storage capacity, and they called for conservation awareness campaigns, the introduction of drought-tolerant crop varieties and more economical irrigation.

“The country is gravely vulnerable to water-related (effects) of the changing weather patterns,” said Pakistan’s minister for planning, development and reform, Ahsan Iqbal, in a keynote address at the summit in the nation’s capital.

In December, the World Resources Institute ranked Pakistan among the 36 most water-stressed countries in the world.

Iqbal said that Pakistan needs a minimum storage capacity of 40 percent of the around 115 million acre-feet of water available in the Indus river system throughout the year. But the country’s storage capacity is only 7 percent and is decreasing due to sediment build-up in reservoirs.

This gives Pakistan a stored water supply, adequate to meet its needs, of just 30 days. By contrast, “carryover capacity” in other countries ranges from 200 days in India to 1,000 days in Egypt, he said.

“In Pakistan, planners and policy makers across different sectors, including agriculture and industry, energy and health now have ... a daunting challenge before them of increasing the country’s water storage capacity,” Iqbal said.

The minister urged the finance ministry to explore funding avenues for new water storage projects to boost storage capacity. Many of these are hydroelectric dams, which would also produce power.

THREATS TO HYDROPOWER, AGRICULTURE

But Pakistan Water Partnership’s country director, Pervaiz Amir, warned that if climate change leads to lower water flows in the northwest of the country, it would cut the amount of hydroelectricity that can be produced.

More variable rainfall and glacier melt in the face of climate change also means that agriculture, which he said accounts for over 96 percent of the country’s water consumption, will be affected, Amir said.

Without more facilities to divert and store water, heavy rainfall and flooding in some parts of the country will continue to damage crops, increase soil erosion and delay planting and harvesting, he said.

Pakistan ranks ninth among countries most affected by floods, according to UN-Water’s World Water Development Report.

Arun Shrestha, a senior climate change specialist at the International Centre for Integrated Mountain Development (ICIMOD), said that many South Asian countries lack preparedness for water-related hazards, including flood, droughts and glacial lake outburst floods, and instead focus mainly on post-disaster relief.

What is “more appalling,” he said, is that climate change is dealt with as a separate problem rather than integrated into planning for water-related areas of the government and economy including agriculture, industry, health and energy.

Shrestha urged South Asian countries to include disasters attributable to climate change in their respective water-related planning and policies.

He called for them to analyse their vulnerabilities to increasingly frequent flooding, droughts and glacial lake outburst floods, and to share the findings with each other to develop a regional action plan for dealing with climate-related disasters.

Shrestha underlined the need for regional coordination between government agencies so that river basins can be managed more efficiently, for example by sharing data about river flows.

Stephen Davies, a senior research fellow at the International Food Policy Research Institute, said that water, food and energy are closely interconnected, yet energy models do not properly address water constraints in South Asia and other regions.

Industrial growth and accelerating urbanisation are creating greater demand for energy, he said, but efforts to expand hydropower generation are being hampered by the shrinking availability of water.

Limitations on water availability also are impacting food production to meet the country’s galloping population growth, he added.

Chief executive of LEAD Pakistan and climate policy expert Tauqeer Ali Sheikh urged policymakers to incorporate the interdependence of water, food and energy into their planning.

In South Asia, “energy planning is often made without taking into account possible changes in water availability due to climate change or other water competing uses,” he pointed out. More

Saleem Shaikh and Sughra Tunio are climate change and development reporters based in Islamabad, Pakistan.

 

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How NASA Can Save Us Billions of Gallons of Water

Here’s something to add to your doomsday list of natural resources that people need to survive but are threatened by climate change: snow.

It’s a key source of freshwater for more than 1 billion people across the globe, slaking thirst, irrigating croplands, and driving turbines that generate electricity. Conveniently, in much of the world, snow also acts as a natural reservoir, storing water during wet seasons, then rationing it out slowly during drier summer months. But today, growing populations, warming temperatures, and changing weather patterns are straining that supply like never before. “June is the new July,” says Auden Schendler, vice president of sustainability at Aspen Skiing Company in Colorado. “Snowmelt comes earlier than it used to, and it all happens in one big flood.”

Which means that knowing exactly how much snow is in the highlands—and when it’s coming down to lower elevations to feed rivers, aqueducts, and irrigation channels—is ever more important. But how do you measure something that’s spread over thousands of miles of steep, rugged, alpine terrain?

Tom Painter, a research scientist at NASA’s Jet Propulsion Laboratory, has an answer: by measuring snow from thousands of feet in the air. Using sophisticated, aircraft-borne sensors that gauge snow’s depth and the amount of light it reflects, Painter and his team are assembling the most accurate measurement ever made of just how much water the mountains hold.

This is welcome news in California, where the water content of accumulated snow is at historically low levels. Runoff from the Sierra Nevada mountains provides about a third of the entire state’s water, and up to 80 percent in some areas, supplying tens of millions of people and almost 1 million acres of farmland.

Painter can’t make it snow, but he can provide more and better data to water managers, who need to plan how to most efficiently fill their reservoirs; farmers deciding which crops to plant and when; and cities trying to figure out if they’ll have enough water to supply their residents—or will need to start rationing. “The demand for knowledge about water resources is at an all-time high,” says Painter, a gregarious, athletically built 46-year-old.

For decades, state water officials have estimated the snowpack’s water content by a straightforward method that will appeal to steampunk aficionados: They clamber into the mountains on snowshoes and stick aluminum tubes into the snow. The tubes indicate depth while collecting a sample revealing water volume. More recently, California has added a network of tabletop-size scales scattered through the mountains that electronically transmit the weight of snow that has fallen on them.

Both systems yield reliable measurements but only of the snow where the measurement is taken; extrapolating out from that to a whole basin, or a whole mountain range, is better than guesswork but less than precise. What’s more, both the scales and the human surveyors are concentrated at lower elevations, leaving scientists to wonder what lies farther uphill. “The old system worked OK historically because there was always enough water,” says Painter. “But now it’s all been allocated out, and demand is starting to exceed supply.” More

 

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‘China a concern for South and Central Asia’s water security’

New Delhi: With China building a “cascade of dams” in the upper reaches of rivers that flow into Central and South Asia and drawing large amounts of water to sustain its economy and people, there is a need to engage the Asian giant at bilateral and multilateral fora on the issue of water that is fast becoming a scarce and contentious commodity, said diplomats and experts here.

Himalayas - Source of S. Asia's water

Addressing a round table on “Regional Water Security and Riverine Disputes: Issues Common to Central and South Asia” here Thursday, speakers, including ambassadors from Central Asian countries and other domain experts, also said that there is a need for Track II dialogue between civil society activists of countries and for transparency in sharing of hydro information in order to resolve the issues concerning sharing of water.

Leading strategic expert Brahma Chellaney said Central and South Asia share common water security issues. He said China is “happily placed” as it is home to the largest number of trans-border rivers, which all originate from the Tibetan Plateau and the Xinjiang region. Chellaney said China’s “annexation” of Tibetan Plateau and Xinjiang “changed the water discourse” for the people of South and Central Asia.

Chellaney, who is professor of strategic studies at the Centre for Policy Research, said China “is an issue of concern in South Asia and Central Asia… China is building a cascade of dams just before the rivers flow out of its territory.”

Ajay Bisaria, joint secretary in the Eurasia division of the external affairs ministry, said that India stands to benefit from the Central Asia South Asia Electricity Transmission and Trade Project, better known as CASA-1000, a new electricity transmission system to connect the countries of hydropower producing countries of Kyrgyzstan and Tajikistan with Afghanistan and Pakistan.

Ashok Sajjanhar, former ambassador to Kazakhstan, said the Aral Sea from being a lake of plenty with fish, birds and wildlife, has turned into an “ecological disaster” with very high salinity and water level shrunk massively. The Aral Sea is a lake lying between Kazakhstan and Uzbekistan. Sajjanhar said the issue of water distribution and water management between countries sharing water bodies is very crucial.

Rajiv Dogra, former ambassador, said the Central Asian water bodies were once clear blue and pristine, but have shrunk due to overuse.

“A drop of water is a grain of gold”, is the value placed on water in Turkmenistan, said the country’s Ambassador Parakhat Hommadovich Durdyev at the seminar held at the India International Centre and organised by the think tank Society for Policy Studies in collaboration with Asia News Agency.

William Young, Lead Resource, South Asian Water Initiative, World Bank, said the Ganga plains is inhabited by 600 million people, which shows the dependency on the river. He said the World Bank was looking to establish dialogues for the Ganga and Brahmaputra basin river countries.

Sanjoy Hazarika, director of Centre for North East Studies at Jamia Millia Islamia, said the run of river dams that China was building on the Brahmaputra removes the fertile silt from the river water when it is released downstream into India, thereby harming agriculture and leading to climate change.

Hazarika also slammed the idea of interlinking of rivers being proposed in India, terming it a disastrous idea. More

 

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World’s largest hydropower project planned for Tibetan Plateau

This is part of a special report produced by on the future of the Brahmaputra river – one of the world’s great transboundary rivers – which starts on the Tibetan Plateau before passing through India and Bangladesh.

Also read:
- It’s time for a new era of cooperation on the Brahmaputra
- Why India and China should leave the Brahmaputra alone
- Brahmaputra river is a living ecosytem, not just a source of hydropower

The Tibetan Plateau, the world’s third pole, gives birth to many of Asia’s major rivers. As the key for maintaining the continent’s ecology, and one of the world’s most important ecosystems in its own right, it is of huge strategic significance.

The Yarlung Tsangpo (known as the Brahamputra in India), which runs alongside the majesty of the Himalayas, is the world’s highest river. It runs west to east along the rift created by the impact of the Eurasian Plate, cutting through the Tibetan Plateau until it meets the point where the Himalayas, the Nyenchen Tanglha and Hengduan mountains join. Here it forces its way between the Gyala Peri and Namcha Barwa peaks to form the world’s deepest gorge, then makes its way to South Asia where it joins the Ganga and flows to the Indian Ocean.

The Yarlung Tsangpo rises at a high altitude, in a geologically complex area. The river’s powerful flow, long course and large drop in altitude give it great potential for hydropower development. But the scale of dam building planned by China and India could have disastrous ecological consequences.

China’s plans date back to the early 1990s, when it carried out a series of hydropower development surveys of the river, with the Yarlung Tsangpo Gorge the focus of interest.

In the late 20th century, this gorge was recognised as the world’s deepest. In the 400 kilometres from the top of the gorge, the river twists around the mountain of Namcha Barwa (known as the Great Bend) and loses more than 2,000 metres in altitude, forming several waterfalls and giving up huge energy potential as it goes. Hydropower experts say a tunnel that cuts the river’s natural loop could carry 2,000 cubic metres of water a second, with a drop in altitude of 2,800 metres – enough to power a 50-gigawatt hydropower station that could provide 300 billion kilowatt hours of electricity a year. It would be the largest hydropower project in human history – about three times the size of the Three Gorges Dam.

The world’s largest dam

Eleven hydropower stations are planned on the river, three along the middle reaches from Sangri to Gyaca, and nine on the gorge up to the Great Bend, with total generating capacity of 60 gigawatts.

Work started on the Zangmu Dam – one of the three planned on the Sangri-Gyaca section – in 2010 and this is expected to be generating electricity this year. There are also plans for about 65 gigawatts of hydropower development on the major tributaries of the Yarlung Tsangpo.

India has also been planning hydropower development along the Yarlung Tsangpo and its tributaries on a huge scale; public and private companies have proposed 168 massive dams, to produce 57 gigawatts of hydropower in the country’s north-east.

Floods, landslides and extinction

The Yarlung Tsangpo Gorge is a young and still active geological formation, any interference could have disastrous knock-on effects, from which the ecosystem may not be able to recover.

There are powerful geological stresses here, and seismic activity and landslides are common. The gorge is still taking shape, and I have found more than 100 active landslips or mudslides which any future earthquakes could worsen.

In the early 1950s, an earthquake of magnitude 8 on the Richter scale caused many secondary landslides, which resulted in sustained flooding downstream. In April 2000, I personally witnessed a huge landslide at Yi’ong, which created a four billion cubic metre barrier lake. Sixty days later the barrier failed. The resulting floods affected millions of people and paralysed transportation. Natural disasters of this type are common here.

We still don’t know what the long-term impact of climate change will be on the Tibetan Plateau, but the glaciers and snowlines of the Himalayas are retreating, depriving the rivers of a source of water. If this continues, the plateau’s waterways will be cut off, or even dry up and the land will become a desert.

Today, the ecosystem of the gorge region is already in decline. The primary forests made up of tall trees are now over-mature and swathes of forest over 2,500 metres in altitude are dying. Secondary growth is mono-cultural – the forests are failing to regenerate. Meanwhile, the Monpa and Luopa people who live deep in the gorge continue slash-and-burn methods of farming – the forests on many steep slopes have been torched to provide farmland, resulting in the rapid spread of soil erosion and landslides.

Much of the area’s wildlife – it is one of the most biodiverse regions of the world – is also facing extinction. The ecosystem of the gorge and surrounding areas have become fragmented, meaning animals have smaller areas in which to roam. This leads to imbalances in the food chain, while the mono-cultural secondary forests prevent populations growing and surviving.

The importance of the Tibetan Plateau’s environment to the health of the Yarlung Tsangpo and other rivers should not be ignored. Its worsening environment is a major factor in the degradation of the ecologies of the Yarlung Tsangpo and other rivers; interference from human development and hydropower projects will only add insult to injury. More

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Full Planet, Empty Plates: The New Geopolitics of Food Scarcity - Lester Brown

Peak Water and Food Scarcity

Although many analysts are concerned about the depletion of oil resources, the depletion of underground water resources poses a far greater threat to our future. While there are substitutes for oil, there are none for water. Indeed, modern humans lived a long time without oil, but we would live for only a matter of days without water.

Not only are there no substitutes for water, but the world needs vast amounts of it to produce food. As adults, each of us drinks nearly 4 liters of water a day in one form or another. But it takes 2,000 liters of water—500 times as much—to produce the food we consume each day. 1

Since food is such an extraordinarily water-intensive product, it comes as no surprise that 70 percent of world water use is for irrigation. Although it is now widely accepted that the world is facing severe water shortages, not everyone realizes that a future of water shortages will also be a future of food shortages. 2

The use of irrigation to expand food production goes back some 6,000 years. Indeed, the development of irrigation using water from the Tigris and Euphrates Rivers set the stage for the emergence of the Sumerian civilization, and it was the Nile that gave birth to ancient Egypt. 3

Throughout most of history, irrigation spread rather slowly. But in the latter half of the twentieth century it underwent a rapid expansion. In 1950, there were some 250 million acres of irrigated land in the world. By 2000, the figure had nearly tripled to roughly 700 million acres. After these several decades of rapid increase, however, the growth in irrigated area has slowed dramatically since the turn of the century, expanding only 9 percent from 2000 to 2009. Given that governments are much more likely to report increases than decreases, the recent net growth in irrigated area may be even smaller. This dramatic loss of momentum in irrigation expansion, coupled with the aquifer depletion that is already reducing irrigated area in some countries, suggests that peak water may now be on our doorstep. 4

The trend in irrigated land area per person is even less promising. For the last half-century, the irrigated area has been expanding—but not as fast as population. As a result, the irrigated area per person today is 10 percent less than it was in 1960. With so many aquifers being depleted and more and more irrigation wells going dry, this shrinkage in irrigated area per person is likely not only to continue but to accelerate in the years ahead. 5

Roughly 40 percent of the world grain harvest is grown on irrigated land. The rest is rainfed. Among the big three grain producers—China, India, and the United States—the role of irrigation varies widely. In China, four fifths of the grain harvest comes from irrigated land. For India it is three fifths, and for the United States, only one fifth. Asia, where rice is the staple food, totally dominates the world irrigated area. 6

Farmers use both surface and underground water for irrigation. Surface water is typically stored behind dams on rivers and then channeled onto the land through a network of irrigation canals. Historically, and notably from 1950 until 1975, when most of the world’s large dams were built, this was the main source of growth in world irrigated area. During the 1970s, however, as the sites for new dams diminished, attention shifted from building dams to drilling wells for access to underground water. 7

Most underground water comes from aquifers that are regularly replenished with rainfall; these can be pumped indefinitely as long as water extraction does not exceed recharge. A small minority of aquifers are fossil aquifers, however, containing water put there eons ago. Since these do not recharge, irrigation ends once they are pumped dry. Among the more prominent fossil aquifers are the Ogallala underlying the U.S. Great Plains, the deep aquifer under the North China Plain, and the Saudi aquifers. 8

Given a choice, farmers generally prefer having their own wells because it enables them to control the timing and amount of water delivered with a precision that is not possible with large, centrally managed canal irrigation systems. Pumps let them apply water precisely when the crop needs it, thus achieving higher yields than with large-scale, river-based irrigation systems. Forty percent of world irrigated area is now dependent on underground water. As world demand for grain has climbed, farmers have drilled more and more irrigation wells with little concern for how many the local aquifers could support. As a result, water tables are falling and millions of irrigation wells are either going dry or are on the verge of doing so. 9

As groundwater use for irrigation expands, so does the grain harvest. But if the pumping surpasses the sustainable yield of the aquifer, aquifers are depleted. When this happens, the rate of irrigation pumping is necessarily reduced to the aquifer’s natural rate of recharge. At this point, grain production declines too.

The resulting water-based “food bubbles,” which create a short-term false sense of security, can now be found in some 18 countries that contain more than half the world’s people. In these countries, food is being produced by drawing down water reserves. This group includes China, India, and the United States. 10 (See Table 6–1.) More

 

Pakistan tackles water crisis with rainwater harvesting

MORRY-JE-WANDH, Pakistan (AlertNet) – Wearing colourful traditional dresses with silver jewellery and bangles on their arms, the women of Tharparkar district look festive. But the empty earthen pots they carry tell a different story.

Women of Tharparkar district

“Walking for three miles and (hoisting) a ... bucket filled with water through a wooden pulley from a 130-feet-deep well twice a day is toilsome work,” says Marvi Bheel, who lives in isolated Morry-je-Wandh village in this arid district of Sindh province, some 450 km (280 miles) south-east of Karachi.

Increasing temperatures and lower rainfalls, believed to be associated with climate change, are creating intense water shortages in much of Pakistan, a situation which is likely to worsen if the country’s 170 million population doubles as projected in the next 25 years.

In response, non-governmental organizations are trying to improve water harvesting in rural areas. A pilot project in Morry-je-Wandh has seen the construction of a large covered pond with the capacity to supply the domestic and drinking water needs of 20 families (135 villagers) for more than eight months.

“The new rainwater harvesting facilities have transformed the lives of people, as we have now a safe source of clean water,” said Sobho Bheel, a farmer unrelated to Marvi Bheel.

The effects of having a good supply of drinking water at hand are far-reaching, he added: diseases have diminished, children can go to school and women have more time to spend on other economic activities.

IMPROVING LIFE FOR WOMEN

Women in Tharparker district, as in many places around the world, are charged with the task of gathering water. But as water becomes scarcer, travelling long distances to collect it can be arduous.

“Women fall unconscious on their way to these dug wells, while others develop pregnancy related complications due to being malnourished,” Marvi Bheel said. On summer days temperatures hover around 48 to 50 degrees Celsius (118 to 122 degrees Fahrenheit), and the falling water table means that water sometimes has to be hauled from a depth of 200 to 250 feet (62 to 77 metres).

Dug wells are the major source of water for over 90 percent of the approximately 1.4 million people living in Tharparkar, Pakistan’s largest arid district, which spreads over nearly 20,000 square kilometres (7,600 square miles) and comprises some 2,350 villages.

Water is taken from the wells for domestic, agriculture and livestock needs. But because of the inadequate number of wells in the district and demand for water exceeding supply, wells often produce too little water or dry up within several months of being recharged by rain.

Bharumal Armani of Chelhar village recalls that during August 2010, rains in the Thar Desert recharged parched shallow wells, raised the water table in deep wells and filled household cisterns.

But after four months, local people were without sufficient water even for drinking. Many villagers had to walk miles to fetch supplies, while herdsmen were forced to take their livestock to reservoirs to water them.

According to a study by the Pakistan Council for Research on Water Resources (PCRWR), a government body, the entire Thar Desert receives between 260 and 280 mm (1.0-1.1 inches) of rainfall annually. The scanty precipitation, however, could suffice to meet the domestic water needs of the locals and their livestock for three years, according to the PCRWR.

95 PERCENT OF RAINFALL LOST

But because of inadequate storage and rainwater harvesting facilities, more than 95 percent of the water is lost under sand dunes or evaporates in the summer heat.

“Hardly 0.06 percent of the total annual rainwater is harvested by the locals in their household cisterns or in other indigenous ways,” said A.D. Khan, director for groundwater management at the water council. Khan believes the water shortage problem can be addressed by scaling up rainwater harvesting to at least 0.25 percent of the annual rainfall.

In Morry-je-Wandh, a water storage pond with a cover to curb evaporation is part of that effort. The pond, constructed by the Sukkar Foundation, a non-governmental organisation, cost Rs. 125,000 (about $1,400) and relied on financial and technical support from WaterAid-UK’s Pakistan chapter.

“We lay a geo-membrane sheet under the floor of these (ponds) to check seepage, and cover them with roofs that help check evaporation of stored rainwater during the sizzling summer days,” said Abdul Hafeez, WaterAid’s national programme manager.

Using hand pumps connected to the storage ponds through pipes, women can fill their pitchers with water without any difficulty.

According to Qamar uz Zaman Chaudhry, Pakistan’s advisor on climate change affairs, the country is one of the world’s most arid. Most areas have little or no access to surface water. By international standards, Pakistan was already considered a water-scarce country in 1992 with an annual per capita availability of 1,700 cubic metres. This has now declined to fewer than 1,100 cubic metres, according to the government.

“The situation will grow tenser as rains are becoming more erratic and scarce due to climate change,” said Chaudhry, who is author of Pakistan’s national climate change policy.

Climate change and overuse of limited water is expected to create severe problems for the country in coming years, according to Simi Kamal, chairperson of the Hisar Foundation for Water, Food and Livelihood Security, promotes water conservation and management practices in Pakistan.

Annual per capita availability of water may fall to half its current level by 2020 if the depletion of water resources goes unchecked, she said. She believes much of the solution to growing water stress lies in planning and implementing workable rainwater harvesting programmes at medium and small levels.

Chaudhry agrees.

“More than adequate water can be made available for domestic, agriculture, industrial, livestock and other miscellaneous needs, provided that viable strategic plans are drawn up and implemented for rainwater harvesting at all levels,” he said. More

Saleem Shaikh and Sughra Tunio are development reporters based in Karachi, Pakistan.