Too much, too little

The characteristics of water in India

Water availability on the Indian subcontinent is strongly influenced by a number of climatic and geographic factors. Together these combine to provide India with enough freshwater to meet the various demands arising from the agricultural, industrial and domestic sectors. However, the actual distribution of water resources over space and time limits access to certain geographic regions and is confined to only certain months of the year. Government policies and economic incentives have also determined how and how much of India’s water can be used. The following discusses some of the major characteristics of water in India: where it comes from, where it goes and how it is currently being managed.


Climate

The climate in India is dominated by the seasonal monsoon, but regional differences in the micro-climate abound due to the varying topography and the influence of the oceans. Indeed, the presence of the Himalayas and the Indian Ocean lend the country characteristics of both a tropical climate and a continental one. The result is an extreme in temperature and moisture levels from the arid conditions of the Thar Desert to the rainforest climate of the Northeastern States. Similarly, temperatures vary from below freezing in the higher passes of the Himalayas to torrid heat on the Gangetic Plains. It is therefore difficult to generalize about the climate in India as a whole. Nevertheless, India does provide one of the best examples of a monsoon climate due to the distinct division between the wet and dry seasons.

The monsoon in India arises from the reversal of the prevailing wind direction from Southwest to Northeast and results in three distinct seasons during the course of the year. The Southwest monsoon brings heavy rains over most of the country between June and October, and is referred to commonly as the ‘wet’ season. Moisture laden winds sweep in from the Indian Ocean as low-pressure areas develop over the subcontinent and release their moisture in the form of heavy rainfall. Most of the annual rainfall in India comes at this time with the exception of in Tamil Nadu, which receives over half of its rain during the Northeast monsoon from October to November.

The retreating monsoon brings relatively cool and dry weather to most of India as drier air from the Asian interior flows over the subcontinent. From November until February, temperatures remain cool and precipitation low. In northern India it can become quite cold, with snow occurring in the Himalayas as weak cyclonic storms from the west settle over the mountains. Between March and June, the temperature and humidity begin to rise steadily in anticipation of the Southwest monsoon. This pre-monsoonal period is often seen as a third distinct season although the post-monsoon in October also presents unique characteristics in the form of slightly cooler temperatures and occasional light drizzling rain. These transitional periods are also associated with the arrival of cyclonic tropical storms that batter the coastal areas of India with high winds, intense rain and wave activity.

As mentioned, rainfall and temperature vary greatly depending on season and geographic location and even within these, the timing and intensity of the monsoon is notoriously capricious. The result is a vastly unequal and unpredictable distribution over time and space. In general, the northern half of the subcontinent sees greater extremes in temperature and rainfall with the former decreasing towards the north and the latter towards the west. Rainfall in the Thar Desert and areas of Rajasthan can be as low as 200mm per year, whereas on the Shillong Plateau in the Northeast, average annual rainfall can exceed 10,000 mm per year. Similarly, temperatures vary from sub-zero in altitude during the winter months to 48C highs in mid-summer. On average, the mean maximum temperature during the coolest months in northern India is 21C and during the summer months between 38-43C. The extreme southern portion of the country sees less variation in temperature and rainfall. In Kerala, the temperature varies by only 2.5C around the annual mean of 27C and the total annual rainfall is 3,000 mm (CSE, 1995).

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Water Resources

Surface Water / Groundwater / Water Harvesting Systems

Precipitation in the form of rain and snowfall provide over 4000 km3 of fresh water to India, most of which returns to the oceans via the many large rivers which flow across the subcontinent. A portion of this water is absorbed by the soil and is stored in underground aquifers. A much smaller percentage is stored in inland water bodies both natural (lakes and ponds) and man-made (tanks and reservoirs).

Of the 1869 km3 available as annual surface runoff, only an estimated 1122 km3 can be exploited due to topographic constraints and distribution effects. The calculated per capita water availability (from 1997) is 1967 m3, although this value varies from a low of 360 m3 in the Sabarmati basin to 16589 m3 in the Brahmaputra and Barak basins (Ministry of Water Resources, 2001). Already, the potential of most river basins is being exploited beyond 50% and several basins are considered to be water scarce. However, when considered as a whole, India is not a water scarce country and ranks among the top ten water rich countries in the world according to data from World Resources 2000-2001 (World Resources Institute, 2000).

Surface Water

Twelve major river systems drain the subcontinent along with a number of smaller rivers and streams. Of these twelve, the Ganges - Brahmaputra and the Indus systems are the most important in terms of water provision and their impact on Indian society. Together, these systems drain almost half of the country and carry more than 40% of the utilisable surface water from their source in the Himalayas to the ocean.

Over 70% of India’s rivers drain in the Bay of Bengal, mostly as part of the Ganges-Brahmaputra system. The Arabian Sea, on the western side of the country, receives 20% of the total drainage from the Indus system as well as a number of smaller rivers down the western coast. The remaining 10% drains into interior basins and the few natural lakes scattered across the country (Encyclopedia Britannica Online 2000).

The flow regime of India’s rivers is strongly influenced by the monsoon climate. The advent of the monsoon rains results in an annual peak in streamflow in most rivers and streams across the subcontinent. Rivers with sources in the mountains see an additional peak in streamflow during the spring snowmelt. In many cases, water levels increase dramatically and flooding is common. During the dry season, the streamflow diminishes in most large rivers and even disappears entirely in smaller tributaries and streams. To regulate the flow in these rivers and distribute water more evenly throughout the year, a number of large dams have been built on the principal river systems. However, even these measures have been inadequate to control water availability in the country, especially during the dry season.

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Groundwater

Groundwater represents one of the most important water sources in India and accounts for over 400 km3 of the annual utilizable resource in the country. Due to the highly variable nature of the climate, groundwater has become a popular alternative for irrigation and domestic water use across India. Reliance on groundwater resources is particularly strong where dry season surface water levels are low or where wet season flows are too disruptive to be easily tapped. In addition to being accessible, groundwater quality is generally excellent in most areas and presents a relatively safe source of drinking water for Indians in rural and urban centres.

The presence and availability of groundwater varies greatly with changes in topography, subsurface geology and the prevailing climate in the region. In some areas, groundwater exists in deep aquifers while in others the water is stored near the surface. The location of the aquifer also affects its recharge rate and its susceptibility to pollution and overuse.

In general, the mountainous and hilly regions in the north and west do not allow adequate infiltration and as a consequence, groundwater is mostly limited to valleys and other lower lying areas. In the peninsular part of the country, the underlying geology limits the formation of large continuous aquifers. Groundwater is therefore scattered where fissures permit adequate storage or is found in shallow depressions near the surface. As a result, the overall yield potential in this region is low although some areas may see medium to high potential depending on the local hydrogeology. Coastal regions are usually rich in groundwater owing to the largely alluvial terrain, but the aquifers risk being easily contaminated by saltwater ingress due to overpumping. The alluvial tract of the Gangetic plain, which extends over 2000 km across central and northern India has the best potential for groundwater extraction in the country. This large area possesses many favourable characteristics for groundwater storage and recharge, and the yield over most of the region has been estimated at moderate to high.

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Water Harvesting Systems

The unequal distribution of water resources over time and geographic area has necessitated the development of water harvesting systems. These structures are designed to help capture and store rainwater during the monsoon season and serve as a source of drinking and irrigation water during the rest of the year. In India, tanks, ponds and reservoirs cover a total of 5 million hectares, the majority of which lies in the southern portion of the country (MOWR, 2001). Although they do not make a significant contribution to the total freshwater water resource in India, water harvesting systems do have a strong impact in terms of drinking water and irrigation provision on a local scale.

Many of the water harvesting structures used in India are based on ancient models and are therefore highly adapted to the prevailing climatic and hydrologic conditions of the area. The potential of these systems to supply adequate freshwater to all areas and sectors is high. However, since colonial times, these systems have been increasingly abandoned and neglected in favour of large dam and canal irrigation projects. So far, these ‘modern’ structures have been successful in providing water to portions of rural and urban India, yet high economic, social and environmental costs have reduced their overall benefit. As a result, development and civil society organisations have been advocating the return to local water harvesting systems for domestic and irrigation purposes. As awareness and public opinion continue to grow, water harvesting systems will become increasingly more important source of water in India.

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Demands

Agricultural / Industrial / Domestic

Access to adequate water is one of the leading factors limiting development in India. Agricultural, industrial and domestic uses are competing more and more for a limited supply. The agricultural sector continues to dominate water use owing to its continued importance to the Indian economy, while industrial demands are increasing as the sector continues to grow. Domestic needs claim only a small portion of the annual water withdrawals as access to adequate water and sanitation supplies remains low throughout most of the country. Greater access and an improvement in the socio-economic situation in rural India will likely result in higher demand for water from this sector in the coming years.

Agricultural

Agriculture remains central to the Indian economy and it therefore receives the greater share of the annual water allocation. According to the World Resources Institute (2000), 92% of India’s utilisable water is devoted to this sector, mostly in the form of irrigation.

The necessity of irrigation for agricultural production is great due to the unpredictable nature of the monsoon. In regions completely dependent on rainfed agriculture, a weak monsoon season can result in drought conditions that can lead to reduced yields or even total crop failure. Even during normal monsoon seasons, farmers are usually able to produce only one crop per year and yields are generally much lower than in irrigated areas. Indeed, the productivity of irrigated agriculture per unit of land has been estimated at seven times that of rainfed agriculture (World Bank, 1999).

Massive investment in irrigation in the past fifty years has resulted in an expansion of the gross irrigated area from 23 million hectares in 1951 to over 90 million hectares in 1997, and plans exist to continue developing irrigation infrastructure over the coming years (World Bank, 1999). This growth in irrigated area, along with improvements in farming technologies and plant genetics, has been responsible for the incredible growth in crop production over this period. The increase in production has also contributed greatly to the national economy and to India’s food security. However, irrigation expansion has also placed greater demands on surface and groundwater resources. Groundwater alone accounts for 39% of the water used in agriculture and surface water use often comes at the expense of other sectors such as the industrial and domestic supply.

At the other extreme, flood conditions can be equally devastating to the agricultural sector and requires careful planning in terms of drainage and the construction of flood control structures. Development projects such as dam and canal construction were devised to help mitigate the effect of the monsoon on rivers and seasonal streams. For the most part, they have been successful at reducing the impact of flooding in some areas, although their effectiveness is limited in the face of exceptional rainfall events.

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Industrial

In the past several decades, industrial production has increased in India owing to an increasingly open economy and greater emphasis on industrial development and international trade. Water consumption for this sector has consequently risen and will continue growing at a rate of 4.2% per year (World Bank, 1999). According to the World Bank, demand for industrial, energy production and other uses will rise from 67 billion m3 to 228 billion m3 by 2025.

Hydroelectric generation already accounts for a large percentage of the water demand from this sector. The potential in India has been estimated at 84,000 MW, of which only 22,000 MW is currently being harnessed (MOWR, 2001). The large untapped potential, particularly in the northern regions of India, and the growing demands for electricity from a larger population and industrial sector, will ensure that development of this activity continues in the coming years.

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Domestic

Demand from the domestic sector has remained low and accounts for only 5% of the annual freshwater withdrawals in India (World Resources Institute, 2000). Domestic water use will increase as the population continues to grow and access to water is improved. Recent data from the World Bank indicates that demand over the next twenty years will double from 25 billion m3 to 52 billion m3.

Only 85% of the urban and 79% of the rural population has access to safe drinking water and fewer still have access to adequate sanitation facilities (World Resources Institute, 2000). The central government made a commitment to improve access to water in rural and urban areas in the National Water Policy adopted in 1987. The original goal of providing water to 100% of all citizens of India by 1991 had to be revised and now stands at 90% access to urban and 85% access to rural areas, respectively. Drinking water and sanitation nevertheless remain high priorities on the government agenda.

Most urban areas are serviced by a municipal water distribution system. Usually, the municipal water supply originates from local reservoirs or canals, but in some cases water may be imported through inter-basin transfer. Although the major cities in India enjoy access to central water supply systems, these schemes often do not adequately cover the entire urban population and are notoriously inefficient and unreliable. In rural areas, access to water is even more precarious. Over 80% of the rural domestic water comes from groundwater sources since it is more reliable in terms of water quantity and quality. Still, in areas where water is scarce, rural women must travel long distances to wells or streams to fetch water for their daily needs.

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Economics

Operation and Maintenance (O & M) of the water distribution systems, reservoirs, canals and other infrastructure requires financial input from the central and state governments, although in some cases the cost of O & M is also shared by the users. In the past, allocation of funds has been inadequate to properly maintain the existing structures and many have fallen into disrepair with consequent losses in efficiency. Even current construction projects suffer from lack of funding and lengthy delays are not uncommon. With water consumption estimated to double in the next twenty years (World Bank, 1999), greater emphasis will have to be placed on the financial requirements of the water sector.

Due to its important contribution to the Indian economy, the agricultural sector receives greater attention in terms of financing and subsidies. Not surprisingly, irrigation has been the largest recipient of government funds. Over US$ 9 billion was spent in this area during the Eigth Plan and subsidies to this sector accounted for almost 0.3% of the GDP during the 1994-95 fiscal year (World Bank, 1999). The Drinking Water and Sanitation Supply sector in both rural and urban areas has also been subject to subsidies and rate structures that have not reflected the true cost of the resource and discouraged conservation.

For the most part, government spending in all water-related sectors is running at a deficit. Development of new water supply schemes and maintenance of older structures will continue to exhaust government funds while new issues, such as water pollution and scarcity, will require greater investment over the long term.

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Government and Policies

National Water Policy / Acts and Regulations / International Treaties

The management of India’s water resources falls under the jurisdiction of a number of government agencies, although the primary responsibility for the development of water belongs to the individual States. The Central government oversees the implementation of national policy on resource development and exploitation, as well as manages inter-state and international rivers and river valleys. It also provides technical advice to individual States on development, flood control, navigation, coastal erosion, dam safety, navigation and hydropower, if required.

The Ministry of Water Resources (MOWR) is the principal agency responsible for water in India and as such, oversees the planning and development of the resource from policy formulation to infrastructure support. Other central departments working in water are:

Ministry of Agriculture: watershed development and irrigation

Ministry of Power: hydro-power development

Ministry of Environment and Forests: water quality

Ministry of Rural Development: watershed development and drinking water provision

Ministry of Industry: industrial uses of water

Ministry of Urban Development: urban drinking water provision and sanitation

Central Pollution Control Board: water quality monitoring

Indian Council of Agriculture Research: development of water management techniques

National Water Policy

A comprehensive policy on water is necessary in the face of the growing number of social, economic and environmental issues surrounding water resources in India. In 1987, the newly formed National Water Resources Council adopted the National Water Policy (NWP) and submitted the document to Parliament for implementation. The NWP is the primary document stating the position of the Government of India (GOI) on water resource issues ranging from drought and flood management to drinking water provision.

In essence, the policy serves as a guideline to help planners and managers develop the country’s water resources to their maximum potential. But, the adoption of the policy is also a step-forward for the GOI in terms of promoting the sustainable management of the country’s water resources. As stated in the NWP:

"As the country prepares itself to enter the 21st century, efforts to develop, conserve, utilise and manage this important resource have to be guided by national perspectives. The need for a national water policy is thus abundantly clear: water is a scarce and precious national resource to be planned, developed and conserved as such, and on an integrated and environmentally sound basis, keeping in view the needs of the States concerned."

The policy addresses many issues regarding the planning, development and allocation of water, including groundwater and surface water sources. Among the points addressed in the policy are:

§ Development of standardized national information system containing data on water availability and use is essential for appropriate planning;

§ Resource planning should be conducted using a catchment or a watershed as the basic unit;

§ Water development projects should be multi-purpose and address various priorities such as drinking water provision and flood-mitigation;

§ Environmental impact of new projects should be assessed and minimized where possible;

§ Socially disadvantaged groups such as Scheduled Castes and Tribes and other minority groups are to be included in the planning process as much as possible, and farmers must become increasingly involved in irrigation management policies;

§ Groundwater development should be based on the basis of potential and the recharge capabilities of the aquifer;

§ Water allocation should be based on the following priorities: drinking water, irrigation, hydro-power, navigation, industrial and other uses;

§ Irrigation planning should attempt to maximize benefits to farmers and integrate soil and water conservation practices;

§ Water rates should reflect the true cost of water use and encourage economy of the resource;

§ Promotion of conservation through education, regulation and incentives is encouraged;

§ Development of a master plan for flood control and management should be undertaken and include soil conservation, forestry management, zoning and forecasting considerations.

§ Drought-prone areas should be given priority in water development projects and programmes such as soil moisture conservation and water harvesting practices should be encouraged;

§ Additional research in a number of areas such as hydro-meteorology, groundwater hydrology and recharge, water harvesting, crops and cropping systems, sedimentation and reservoirs, river morphology and hydraulics, recycling and re-use, and sea water resources should be pursued.

The National Water Resources Council is the body responsible for reviewing the progress made by the government in implementing the policy. The Council is composed of Secretaries from the various ministries associated with water resources and the Chief Secretaries of States/Union Territories. Through the National Water Board, the Council is able to make recommendations regarding the financing and development of new projects and provide suggestions on further actions to be taken.

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Acts and Regulations

Water in India is governed under three different Acts: the Environmental Protection Act (1986), the River Boards Act (1956) and the Inter-State Water Disputes Act (1956).  Other Acts and Regulations affect water resources in different ways by addressing its importance for agriculture, biodiversity and conservation and drinking water.  These three Acts, however, have the broadest scope in terms of how they impact all aspects of water management.

Environmental Protection Act

The Environmental Protection Act was ratified in 1986 and is based on decisions made at the United Nations Conference on the Human Environment that was held in Stockholm, Sweden in June of 1972. The Act is concerned with the "protection and improvement of the human environment" and as such, does not focus solely on water resource issues. The principal impact of the Environmental Protection Act on water is in terms of protecting water from environmental pollution. In the Act, the government has the power to:

-plan and execute programs related to control and abatement of environmental pollution;

-establish quality standards and maximum allowable limits for emissions and discharges;

-develop standards for the handling of hazardous materials and other substances;

-restrict development in sensitive areas; and

-conduct inspection of facilities as needed to prevent environmental pollution.

Contravention of the Act can result in imprisonment up to five years or a fine up to one lakh Rupees, or both. An additional fine of up to five thousand Rupees per day can be levied if the polluter purposely continues to contravene the regulations.

River Boards Act

The regulation and development of inter-state rivers and river valleys was to be entrusted to various River Boards when this Act was ratified in 1956. The River Boards were designed to advise the central government on development opportunities, co-ordinate activities and resolve disputes. Under their mandate, the Boards were required to provide advice to the government on the following topics:

*conservation with a view to control and optimal use of water resources;

*promotion and operation of schemes related to irrigation, water supply and drainage;

*promotion and opteration of schemes related to hydro-power and flood control;

*promotion and control of naviagation;

*promotion of afforestation and control of soil erosion;

*prevention of pollution; and

*other duties as deemed necessary.

The Indian government has been unable to constitute a River Board since the Act was enacted almost fifty years ago. However, there is recognition that the Act should be revised and amendments are currently underway to strengthen its powers.

Inter-State Water Disputes (ISWD) Act

Since the majority of rivers in India are shared between neighbouring States, the ISWD Act was enacted in 1956 to adjudicate any disputes regarding the distribution or control of the rivers or the river valleys. The Act gives the government the power to constitute Tribunals to serve as intermediaries in the disputes. To date, five Inter-State Water Tribunals have been established:

§ Godavari Water Disputes Tribunal (April 1969)

§ Krishna Water Disputes Tribunal (April 1969)

§ Narmada Water Disputes Tribunal (October 1969)

§ Ravi and Beas Waters Tribunal (April 1986)

§ Cauvery Water Disputes Tribunal (June 1990)

The first three Tribunals have been completed, but a final decision is still pending on the last two matters.

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International Treaties

A number of international disputes regarding the allocation and management of the water in several large transboundary rivers have arisen between India and its neighbours. Fortunately, these differences have been settled through diplomatic channels with the signing of treaties and agreements. The three principal treaties are:

§ The Indus Waters Treaty - India and Pakistan (1960)

§ The Indo Nepal Treaty on the Integrated Development of Mahakali River (1996)

§ The Ganges Water Sharing Treaty with Bangladesh: Sharing of Lean Season Flow of Ganga at Farakka Barrage in India (1996)

All three disputes arose from disagreements on the allocation of water resources between India and the other countries. In the case of both the Indus and Mahakali Rivers, the equitable distribution of irrigation water was under contention. The Farakka Barrage dispute originated when the water level entering Bangladesh from India was reduced to almost nothing during the lean season (January to May) due to the construction of the Farakka Barrage on the Indian side of the border. In 1996, an agreement was reached between the governments of India and Bangladesh to share the flow during the lean season in the ratio of 60% (Bangladesh) and 40% (India).

Although the treaties have been signed, there are still a number of issues which remain to be resolved. However, in general, the treaties have generated a sense of goodwill between India and its neighbours which bodes well for future collaboration.

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