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Sustaining Water, Easing Scarcity: A Second Update

The Case of the Nile River Basin

Perhaps the most vivid example of the interaction of population growth, water scarcity and international conflict is the vast basin of the Nile River in northeastern Africa. The 10 countries with territory in the Nile basin contain 40 percent of Africa's population (not all actually within the basin) and make up 10 percent of its land mass. More than 85 percent of the Nile's water comes from the Blue Nile, which originates in Ethiopia.24 However, the vast majority of the river's flow, estimated at about 85 billion cubic meters annually, is used by Egypt, the last nation on the Nile's path to the Mediterranean Sea.25

For centuries the cultural symbol of Egypt, the Nile provides almost all the fresh water used by more than 60 million Egyptians living along its banks. When few people lived upstream-and modern economic development was a distant dream for the entire basin-Egypt saw no reason to worry about its dependence on the Nile's waters. Its complacency is now ending, however, as the upstream nations begin to harness the Nile's waters to provide economic prosperity for their growing numbers.

Ethiopia, for example, recently emerged from a long period of civil war and famine into a period of accelerated growth and economic development. The government has overseen the construction of more than 200 small dams that will use nearly 500 million cubic meters of the Nile's flow annually. Additional dams are being planned to increase the country's irrigation and hydropower capacity.26 Though Ethiopia's current development plans will require only a small portion of the Nile's water, its potential demands could significantly reduce the river's flow into Egypt. Ethiopia has an estimated 3.7 million hectares of land, an area larger than Belgium, that could be irrigated.27 With a population nearly the size of Egypt's and a faster annual rate of population growth-3.2 percent annually for Ethiopia versus 2 percent for Egypt-Ethiopia will need to develop a large portion of this land for agricultural use.28 Irrigating only half this land area with water from the Nile could reduce the river's flow to Egypt by 15 percent.29 Hydrologists doubt the basin produces enough renewable fresh water to satisfy the irrigation plans of both Ethiopia and Egypt.30

Egypt itself is raising the stakes with ambitious plans for its New Valley land reclamation project. Pressed by population growth within its own borders, the Egyptian government has begun a massive irrigation project in the country's western desert in an attempt to persuade seven million Egyptians to move there from the crowded Nile Valley. When completed, a pipeline will carry up to five billion cubic meters of Nile water from the Lake Nasser reservoir to the New Valley site to facilitate the construction of new cities and provide irrigation to more than 200,000 hectares of desert, an area more than twice the size of New York City.31

Sudan, meanwhile, plans to build its own dam on the Nile north of the capital, Karthoum, where the Blue Nile and the White Nile converge before flowing into Egypt.32 The remaining Nile basin countries currently use only a small portion of the river's water. However, with their cumulative population now numbering over 140 million and projected to grow to more than 340 million by the year 2025, it is inevitable that these countries will soon begin to lay claim to a larger share of the Nile's flow to meet their growing irrigation and development needs.33

The Egyptian government has long recognized upstream development of the Nile's waters as a potential national security threat and has stated its willingness to go to war to preserve its access to fresh water. As the basin's governments come to understand the dynamics of the population-water relationship, however, advance planning and diplomacy may win out over saber rattling and armed conflict. In recent years, representatives of the 10 nations of the Nile watershed have met to review past agreements and consider possible future ones related to their use of this shared natural resource.34

The whole world is watching the Nile and similar international watersheds. At a March 1997 forum on international water issues in Marrakech, Morocco, UN Secretary General Kofi Annan stressed that the projected growth of world population over the next 30 years makes developing cooperative international agreements on shared water resources "one of the most urgent issues on the global agenda."35 And in May, the UN General Assembly approved a convention to establish guidelines for cooperation on sharing the benefits of international watercourses.36 The U.S. State Department and Environmental Protection Agency have opened field offices called environmental hubs to help developing nations negotiate transboundary solutions to regional environmental problems such as freshwater scarcity, deforestation and air pollution, and to raise the profile of environmental issues in global diplomacy. The Eastern Africa hub, which specializes in Nile Basin water resource issues, recently opened in Addis Ababa.37

The growing interest in the region's water issues is encouraging, but the challenge of reconciling competing claims on the Nile will continue to be complicated by political and economic concerns. The scope for water conservation and international cooperation is large, but the competition is unlikely to find permanent resolution until the region's population approaches stabilization.

The Lessons of Water Scarcity Benchmarks

The benchmarks of water stress and water scarcity used in this report are not intended to describe Malthusian limits to growth or strict natural thresholds governing population-environment interactions with consistent and unalterable effects. Rather, they serve as indicators of the likelihood of adverse consequences related to water shortage. As such, these benchmarks can help predict the future urgency of problems related to freshwater availability. Equally important, they can provide insight into how true natural thresholds related to population-environment interactions might operate. In the real world some countries with less than 1,000 cubic meters of renewable fresh water per person per year manage to develop economically, while many countries with abundant water still experience severe problems in supplying water to farms, factories and homes. Despite these apparent inconsistencies, these benchmarks are recognized and used by many hydrologists and by the World Bank and help illustrate important population-water relationships. To understand different responses to water availability, it is important to explain a few of the principles and limitations of the terms and analyses presented in this report.

First, the figures for per capita water availability presented here refer only to renewable fresh water. This is defined as salt free water that is fully replaced in any given year through rain and snow that falls on continents and islands and flows through rivers and streams to the oceans. The figures do not include water that evaporates through the heat of the sun or transpires through plants to the atmosphere, processes known collectively as evapotranspiration. Excluding the amount of water lost to evapotranspiration helps standardize the water availability figures for countries with dry climates and those with wetter climates by counting only that amount of water that is available for human uses-except to the extent that water availability varies by season.

Second, the water availability figures do not include supplies of groundwater that are not replenished by precipitation on human time scales-also called nonrenewable or fossil water. Many countries supplement their renewable water supplies by drawing down their groundwater aquifers. Relying on nonrenewable supplies of groundwater is one way that countries with less than 1,700 cubic meters of renewable fresh water per person per year can avoid, at least temporarily, feeling the constraints of limited supplies of renewable fresh water. However, for most countries this situation cannot be sustained for long, especially as their populations continue to grow, their pumping costs begin to escalate and their development requires greater quantities of water.

In addition, the water availability figures take no account of the timing or seasonality of this availability. Fresh water is often more abundant in some seasons than in others. Throughout the tropics, for example, rainy seasons often produce deluges of renewable fresh water that cause damaging floods and can scarcely be captured for later use. Months later the dry season sets in, drying rivers and streams to a trickle and causing severe, though temporary, freshwater shortages. Under these circumstances, a watershed or country that in theory has sufficient water for its inhabitants can face shortages not accounted for by the annual availability of renewable fresh water. Much more data on seasonal inventories of freshwater availability will be needed before the concept of timing can play a significant role in analyses of population and water relationships.

As previously discussed, the ability of individuals and institutions to adapt to different challenges can obviously vary widely among nations. For this reason, some can naturally manage better than others as the per capita availability of renewable fresh water declines. It would be inappropriate, therefore, to propose any precise levels as absolute thresholds of water scarcity, or insist that they apply equally to all countries. Instead we use the term benchmark to convey that these figures represent approximate levels of freshwater availability-averaged over different climates, soil conditions and economic development levels-below which concern about water shortage tends to rise significantly. By applying these approximate benchmarks, we can establish a framework that helps explain how population dynamics interact with finite resources such as renewable fresh water.

Finally, the benchmarks described here are not meant to imply that countries having more than 1,700 cubic meters of renewable fresh water available to each inhabitant are automatically considered water abundant. This term proved to be misleading when used in Sustaining Water: Population and the Future of Renewable Water Supplies because in many countries-from India to Iran to the United States-the per capita water availability is higher than the 1,700 cubic meter stress benchmark, yet the drier regions of these countries experience significant water shortages at times. In addition, although countries may appear to have a plentiful supply of renewable water, not all of these sources can be exploited at an acceptable cost, given their location relative to population centers. Thus the supply of economically available fresh water is often much lower than the estimates provided here. In this update of Sustaining Water, the term relative water sufficiency conveys the fact that countries with a per capita water availability in excess of the stress and scarcity benchmarks are not guaranteed an abundant freshwater supply in all times and in all places. Even the term "sufficiency" often overstates the reality of freshwater availability in these countries-in the United States the examples of southern California, the Florida Everglades and south Texas come to mind. Nonetheless, it seems the most apt term to describe the condition of renewable water resources in countries with a per capita renewable freshwater supply that exceeds the benchmark levels for water stress or scarcity described in this update.

Next: Table of Population and Annual Renewable Fresh Water Availability

Next Page: Cambodia-Dominican Republic

Next Page: Ecuador-Hungary

Next Page: Iceland-Luxembourg

Next Page: Madagascar-Norway

Next Page: Oman-South Africa

Next Page: South Korea-Uganda

Next Page: Ukraine-Zimbabwe

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