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Harper's Magazine
July, 2000
RUNNING DRY.(water
scarcity )
Author/s: Jacques
Leslie
What happens when the
world no longer has enough freshwater?
In the world there is
nothing more submissive and weak than water. Yet for attacking that
which is hard and strong nothing can surpass it.
--Lao-tzu (sixth
century B.C.)
When I was a war
correspondent twenty-five years ago, I paid more attention to blood
than to water. Carnage transfixed and terrified me; water seemed to
flow inconsequentially through the embattled landscape before me.
The Mekong River, in its multifingered brownness, and the
reverse-flowing, hugely contracting and expanding great Cambodian
lung-lake, the Tonle Sap, barely registered on my psyche, except as
obstacles: my thoughts on water consisted chiefly of military
observations, such as that the onset of the rainy season slowed down
Khmer Rouge advances more effectively than the regime's hapless
human enemies did. I can't say when the pendulum began to
swing--probably about the time I stopped thinking about the war, a
decade or two later. More recently, I started to notice how many
news stories involved water. The subjects weren't just hurricanes,
droughts, and floods but less predictable phenomena, such as the
accelerating destruction of U.S. watersheds caused by urban sprawl,
violent protests in Bolivia prompted by a water-utility-rate
increase, and a death sentence handed down to a Chinese
administrator who embezzled nearly $2 million set aside for the
resettlement of people displaced by Three Gorges Dam. I began
reading every water text I could find, and in March I attended an
international water conference in The Hague at which water ministers
from 115 countries declined to agree on how to address the problem
of water scarcity. Now when I envision the globe, I try to see
beyond political boundaries to the world as it really is: a
collection of watersheds, lakes, rivers, and aquifers that together
maintain the earth's biota--which is to say, us. Now the world's
quotidian skirmishes and conflagrations are mere background noise.
Now it is water that scares me.
We face an
unassailable fact: we are running out of freshwater. In the last
century we humans have so vastly expanded our use of water to meet
the needs of industry, agriculture, and a burgeoning population that
now, after thousands of years in which water has been plentiful and
virtually free, its scarcity threatens the supply of food, human
health, and global ecosystems. With global population hurtling
toward roughly 9 billion people by 2050, projections suggest that if
we continue consuming water with our habitual disregard all those
needs cannot be met at once.
The world's supply of
freshwater remains roughly constant, at about 2 1/2 percent of all
water, and of that, almost two thirds is stored in ice caps and
glaciers, inaccessible to humans; what must change is how we use the
available supply. Humans have grown so numerous that the usual
response to anticipated water scarcity--to increase supply with
dams, aqueducts, canals, and wells--is beginning to push against an
absolute limit.
In the developed
world widespread water shortages are projected but not yet broadly
experienced. In the developing world the crisis has already arrived.
As many as 1.2 billion people--one out of five on the globe--lack
access to clean drinking water. Nearly 3 billion live without
sanitation: no underground sewage, toilets, or even latrines. More
than 5 million people a year die of easily preventable waterborne
diseases such as diarrhea, dysentery, and cholera; in fact, most
disease in the developing world is water-related. As Peter Gleick
writes in The World's Water 1998-1999, "For nearly three billion
people, access to a sanitation system comparable to that of ancient
Rome would be a significant improvement in their quality of
life."
To be sure, the water
shortages that give rise to these conditions so far are regional,
not global, and often involve inequality of distribution and high
pollution levels as much as absolute scarcity. Thus one water basin
experiences a shortage while neighboring basins enjoy ample
supplies. Water doesn't ship well, except in unusual circumstances,
such as the provisioning of some Greek and Caribbean islands by tanker or barge: water is
far too cheap and unwieldy to justify long-distance transport. This
tends to keep shortages confined to specific areas, but it also
means that they can't easily be alleviated with water from another
region.
In one way, however,
the impact of water shortages has already registered globally,
thanks to water's role in agricultural production. Indeed, water
experts refer to grain as "virtual water," since many countries
facing water shortages respond by importing grain. It takes roughly
a thousand tons of water to produce a ton of grain, so importing
grain has an obvious shipping advantage. As a result, stockpiling
grain is one way to counter water shortages. The billion-dollar
question among water and agriculture experts, in fact, is whether,
owing in part to water scarcity, the human race in the twenty-first
century will lose the capacity to feed itself. For now, the answer
is unknowable, since predictions inevitably rest on highly
speculative assumptions. One forecaster, Lester Brown of the
Washington, D.C.-based Worldwatch Institute, has advanced a dire
scenario in which China's water shortage
forces it to import so much grain that poorer nations are priced out
of the international grain market, inducing widespread starvation.
More plausibly, others argue that in many developing countries water
scarcity is the most significant component of environmental
degradation, which in turn is an underlying cause of mass migration,
peasant revolt, and urban insurrection. Such notions have not
escaped the attention of U.S. policymakers, as
evidenced by meetings of officials from the Department of Defense,
the CIA, the State Department, and the White House last September to
consider the global implications of water conflicts. At a time when
the First World is obsessed with computer technology, genetics, and
the froth of media entertainments, we would be well advised to
remember our relationship to the two atoms of hydrogen and one of
oxygen that, bound in nature, support all life.
IRRIGATION AND ITS
DISCONTENTS
In the
Tigris-Euphrates, Indus, and Yellow
river basins, ancient civilizations flourished when they
devised ways to grow crops with irrigated water and foundered when
the systems collapsed, either because sediment clogged their canals
or waterborne salt poisoned their soils. We like to think that we've
mastered irrigation--indeed, in the last two centuries humans have
increased land under irrigation thirtyfold. Yet the daunting
obstacles we face in maintaining irrigation systems are not so
different from those that brought down the Sumerian and Indus civilizations. "The overriding lesson
from history is that most irrigation-based civilizations fail,"
writes Sandra Postel in her compelling survey of the global water
crisis, Pillar of Sand: Can the Irrigation Miracle Last? "As we
enter the third millennium A.D., the question is: Will ours be any
different?"
Now, more than ever,
humans depend on irrigation: less than a fifth of the world's
cropland is irrigated, but because irrigation typically enables
higher yields and two or three crops a year, irrigated land produces
two fifths of the world's food. Even so, the planet's reliance on
irrigated crops undoubtedly will intensify in the coming decades.
The world's food supply comes from three major sources: cropland,
rangeland, and fisheries. Livestock have already grown so numerous
that 20 percent of the earth's rangeland has lost productivity
because of overgrazing, and most of the world's fisheries have been
decimated by overfishing. By default, the likely source of food for
the roughly 3 billion additional humans expected in the next fifty
years will be cropland. Yet the amount of cropland is not likely to
grow much: newly cultivated land probably will barely surpass the
amount of land lost to agriculture because of erosion, urbanization,
and salination. Moreover, the best cropland is already in use; much
of the land still awaiting cultivation has the potential to be only
marginally productive. The result is that population growth is
already outstripping growth of irrigated land. In fact, the area of
global per capita irrigated land peaked in 1978 and has dropped 5
percent since then. Projections by international agencies suggest
that by 2020, per capita irrigated land will have dropped 17-28
percent from the 1978 peak. Success in feeding all the people who
will populate the earth in the mid-twenty-first century therefore
depends largely on increasing the productivity of existing cropland.
"The difference between the Malthusian pessimists and the
cornucopian optimists," says Postel, "comes down to little more than
an assumption about grainland productivity over the next several
decades--specifically, whether yields will grow at closer to the 1
percent rate of the 1990s or the 2 percent rate of the previous four
decades."
There's reason to
worry. The 2 percent rate occurred as farmers applied Green
Revolution techniques to land irrigated by groundwater or
reservoirs, but those techniques have largely fulfilled their
promise, and yields in recent years have either stagnated or
declined. One reason may be irrigation itself: some scientists
believe that soils become depleted when repeatedly subjected to the
two or three annual crops that irrigation enables. In addition,
Green Revolution agriculture depends on copious applications not
just of pesticides and fertilizer but of water: between 1950 and
1995 grainland productivity increased 240 percent while water use
for irrigation increased 220 percent. With global depletion of
groundwater and increasing diversions of agricultural water for
industrial, urban, and environmental needs, the scarcity of water is
likely to become the most important factor in limiting agricultural
production. That means that more people may hunger for relatively
less food.
UNSEEN
LAKES, PUMPED
DRY
Compared with the
earth's visible freshwater--in lakes, ponds, and rivers--the amount
of water stored in underground aquifers is sixty times as large. A
stock that immense might seem beyond our capacity to exhaust, yet in
many parts of the world groundwater is being depleted at an
unsustainable rate. The Ogallala Aquifer, one of the world's largest
stores of groundwater, covers 225,000 square miles beneath parts of
eight U.S.
states, from Texas to South Dakota,
and feeds a fifth of the nation's irrigated lands. Although its
stock is "fossil water"--water locked underground for thousands of
years, with few sources of replenishment--it is being depleted so
rapidly that many farmers who once depended on it now must rely on
rainwater, significantly lowering yield. The amount of acreage
supported by the Ogallala in six states fell from its peak in 1978
by nearly 20 percent in less than a decade; despite efforts to limit
use of Ogallala water, substantial withdrawals continue.
Of course, unlike the
Ogallala, most aquifers are naturally "recharged"--replenished by
rain and runoff--but even these are being depleted dramatically, as
the rate of withdrawal easily surpasses the recharged amount.
India's volume of annual
groundwater overdraft is higher than any other nation's. Almost
everywhere in the country, water withdrawals are proceeding at
double the rate of recharge, causing a drop in aquifers of three to
ten feet per year; in the state of Tamil Nadu, groundwater levels
have dropped as much as ninety-nine feet since the 1970s, and some
aquifers there have become useless. The cost of land subsidence
caused by aquifer depletion in the United States is about $400
million per year, with incidents occurring in Houston, New Orleans,
and California's Santa Clara County and San Joaquin valley; Beijing
is sinking at an annual rate of about four inches a year; and
certain Mexico City barrios sink as much as a foot a year. In both
Florida and the Indian state of
Gujarat, the water table has
dropped so low that seawater has invaded the aquifers, limiting
their usefulness for drinking or irrigation. In Palestine's Gaza Strip, which relies almost
entirely on groundwater, saltwater intrusion from the Mediterranean has been detected as far as a
mile inland, and some experts predict that the aquifer will become
totally salinized. Groundwater depletion, says the International
Water Management Institute, a World Bank-supported group in
Sri
Lanka, is "the single most serious
problem in the entire field of water resources management.... Many
of the most populous countries of the world--China, India, Pakistan,
Mexico and nearly all of the countries of the Middle East and North
Africa--have literally been having a free ride over the past two or
three decades by depleting their groundwater resources. The penalty
of mismanagement of this valuable resource is now coming due, and it
is no exaggeration to say that the results could be catastrophic for
these countries, and, given their importance, for the world as a
whole."
Humans alone cannot
deplete aquifers: we lack the strength to draw that much water or
dig wells that deep. Rather, groundwater depletion is a phenomenon
of the late twentieth century, made possible by the availability of
electricity and cheap pumps. IWMI calls the spread of small pump
sets throughout the world "one of the most dramatic yet generally
unappreciated revolutions in water resource technology." In some
ways pump irrigation is ideal: the water is stored underground and
shielded from evaporation, so it can be used during the dry season,
when crops need water most. In many Asian countries pump irrigation
alone deserves much of the credit for high Green Revolution
yields.
Yet in many countries
the new technology shattered traditional water-sharing arrangements
that had worked for centuries. John Briscoe, a senior water adviser
at the World Bank, cites the example of Yemen, which once had
"very sophisticated ancient water management techniques" that
handled everything from floods to water allocation. "Then you come
to the post-Second World War, with deep wells and electricity and
diesel pumps for groundwater, and people pump like there's no
tomorrow. You have a lot of food production as a result of this, but
in the basin around San'a, the capital, for instance, four times
more water is being pumped out than is being recharged, and the
aquifer is dropping three meters a year."
Often the new
technology combines catastrophically with government policies.(1)
Until the early 1990s, individual farmers in Mexico used powerful
pumps, concluding, "If I don't pump fast, my neighbor will, so I
might as well pump faster than he does." On top of this, the
government subsidized everything from fertilizer to energy costs and
imposed tariffs on competing foreign crops, accelerating the waste
of water. "The whole thing was a total disaster," Briscoe says. The
government finally phased out tariffs and created subsidies to
encourage sustainable water use. The reforms forced thousands of
Mexican farmers off the land, yet, Briscoe says, there are "very
clear signs" that the remaining farmers have begun to manage their
water use.
In places such as
Punjab and Haryana, India's breadbasket
states, the new technology also widened the gap between rich and
poor. As water tables dropped, farmers had to drill deeper wells and
buy more powerful pumps, but only rich farmers could afford the new
equipment. Poor farmers, whose shallow pumps became useless, were
forced to rent their land to richer farmers, for whom they became
laborers. The IWMI report lists the consequences if this trend is
not reversed: "Lakes and rivers dry up as the aquifer recedes. ...
The costs of pumping become so high that the pumps are shut down and
the whole house of cards collapses. It is not difficult to believe
that India could lose 25% or
more of its total crop production under such a scenario."
From the earth's
surface, groundwater is invisible: farmers don't realize they've
used up an aquifer until it s too late. Even in countries where
limits on withdrawals exist, enforcement is virtually impossible, so
no governments have established regulations for sustainable
groundwater use. Yet reliance on groundwater in agriculture causes
food to be grossly undervalued. Postel estimates the global annual
groundwater overdraft in the mid-1990s at about 163 million
acre-feet, or roughly enough water to grow about 198 million tons of
grain, a tenth of the global harvest. Agricultural prices are now at
their lowest point in two decades and have forced some American
farmers out of work, but if overpumping were to cease, grain prices
probably would rise significantly. Instead, the mounting cost of
pumping groundwater from deeper and deeper levels may eventually
produce the same result.
FOREVER DAMMED
What aquifers are
belowground, dams create aboveground. Many environmentalists will
tell you, however, that the very concept is faulty, that anything as
destructive as a dam cannot be an uncomplicated good. Even by their
reckoning, however, the best dam--the one that is the closest to the
ideal--surely is Hoover Dam, the first of the modern water era.
Hoover is America's Great Pyramid,
whose face was designed without adornment to emphasize its power, to
focus the eye on its smooth, arcing, awe-inspiring bulk. Yet the dam
nods to beauty with a grace that seems more precious year by year:
its suave Art Deco railings, fluted brass fixtures, and three miles
of polished terrazzo granite walkways are the sort of features
missing from the purely utilitarian public-works projects of more
recent decades. Hoover is a miraculous giant
thumbnail that happens to have transformed the American West. Take
it away, and you take away water and power from more than 20 million
people. Take it away, and you remove a slice of American history,
including a piece of the recovery from the Depression, when news of
each step in the dam's construction--the drilling of the diversion
tunnels, the building of the earth-and-rock cofferdams, the digging
to bedrock, the first pouring of foundation, the accretion of
five-foot-high cement terraces that eventually formed the
face--heartened hungry and dejected people across the land.
The dam and Las Vegas more or less vivified each other; if
Hoover evokes glory, Las Vegas,
only thirty miles away, is its malignant twin. Even now, Hoover provides 85 percent of Las Vegas's water, turning a desert outpost
into the fastest-growing metropolis in the country--so, by all
means, take away Las
Vegas. Take away Hoover, and you might also have to take away
the Allied victory in World War II, which partly depended on
warplanes and ships built in southern California with Hoover's hydroelectric current. And
take away modern Los Angeles,
San Diego, and Phoenix: you
reverse the twentieth-century shift of American economic power from
East Coast to West. Take away Hoover and the dams it spawned on the
Colorado--Glen Canyon, Davis, Parker, Headgate Rock, Palo Verde, all
the way to Morelos across the Mexican border--and you restore much
of the American Southwest's landscape, including a portion of its
abundant agricultural land, to shrub and cactus desert. Above all,
take away Hoover, and you take away the
American belief in technology, now on a millennial crest of
enthusiasm. At Hoover's September 30, 1935,
dedication, Interior Secretary Harold Ickes reflected the common
understanding when he declared, "Pridefully, man acclaims his
conquest of nature." After Hoover every country wanted dams,
and every major country, regardless of ideology, built them. (Even
now, the ubiquitousness of dams is one of their most striking
features: the world's highest dam is in Tadzhikistan, the largest reservoir
is in Uganda, and the dam with
the biggest hydroelectric capacity is on the Brazil-Paraguay
border.) At its completion Hoover
towered 280 feet above the world's second-highest dam, the Arrowrock
in Idaho, and was the planet's
largest source of electricity, but its current ranking, sixteenth in
height and lower than twentieth in hydroelectric capacity, reflects
the momentum that the dam movement eventually gathered. Take away
Hoover Dam, and you take away a bearing, a confidence, a sense of
what nations are for.
Yet in a sense that's
what's happening. Even if Hoover lasts another 1,100 years (when
Bureau of Reclamation officials say Lake Mead will be filled with
sediment, turning the dam into an expensive waterfall), its
teleological edifice is crumbling. In sixty-five years we have
learned that if you take away Hoover,
you also take away millions of tons of salt that the Colorado once
carried to the sea but which have instead been strewn across the
irrigated landscape, slowly poisoning the soil. Take away the
Colorado River dams, and you return the silt gathering behind them
to a free-flowing river, allowing it again to enrich the wetlands
downstream and the once fantastically abundant, now often caked,
arid, and refuse-fouled delta. Take away the dams, and the Cocopa
Indians, whose ancestors fished and farmed the delta for more than a
millennium, might again have a chance of avoiding cultural
extinction. Take away the dams, and the Colorado would again bring its nutrients to
the Gulf of California, helping
that depleted fishery to recover the status it held a half-century
ago as an unparalleled repository of marine life. Take away the
dams, finally, and the Colorado
River returns to its virgin state: tempestuous, fickle,
in some stretches astonishing.
What we have learned
is that we have overestimated dams and underestimated the water that
runs through them. In the era of big dams that has at last peaked
and started to decline, river water that reached the sea was
considered wasted because it had not been turned to human ends. Only
recently have we noticed that the human good is not served by the
depleted rivers and wetlands that the diversions create. We would
have been wise to listen to Aldo Leopold, the celebrated naturalist,
who wrote in 1933, two years before Hoover Dam's dedication: "We
build storage reservoirs or power dams to store water, and mortgage
our irrigated valleys and our industries to pay for them, but every
year they store a little less water and a little more mud.
Reclamation, which should be for all time, thus becomes in part the
source of a merely temporary prosperity."
The prosperity is
evident, but so, increasingly, is its transience. Dams have
lifetimes as surely as any natural thing. The rate at which a
reservoir fills depends on its size and the amount of sediment
flowing into it. Sediment has filled more than half the storage
capacity of some dams within a decade. Other dams, like Hoover, have a projected lifetime of more than
a thousand years--though Hoover is deceptive because the
Glen Canyon Dam upstream traps most of the sediment that would
otherwise reach it. On average, sediment annually reduces by 1
percent the storage capacity of the world's reservoirs. In
China, where soil erodes
easily, reservoirs fill at a rate of 2.3 percent a year. One dam on
the silty Yellow River, the
Yangouxia, lost almost a third of its storage capacity even before
it was commissioned.
Radiating outward
from any dam, irrigated water slowly poisons the land with salt.
Salinity has affected a fifth of the world's agricultural land; each
year it forces farmers to abandon a million hectares and affects an
additional 2 million hectares. If in the course of a year a farmer
applies the unremarkable sum of 10,000 tons of water to a single
hectare, the land will collect two to five tons of salt. It's
precisely the process by which ancient Mesopotamia turned into the
barren desert of contemporary southern Iraq. Salt problems are
severe in China,
India,
Pakistan, Central
Asia, and the Colorado and
San Joaquin river basins of the
American West. In many arid areas the soil is naturally saline. As
rainwater and snowmelt flow through a saline watershed to a river,
they collect salt throughout their path. A few billion years ago the
oceans were full of freshwater, then were gradually turned saline by
riverborne salt. Now, in the modern water era, dams divert both the
water and the salt. Because reservoirs expose so much water to the
sun, those in hot climates lose a huge quantity to evaporation: for
example, a full third of the Colorado's flow evaporates from
reservoirs. In the remaining water, salt concentrations increase.
Some water is distributed to surrounding croplands, where the salt
collects. As the water permeates the soil, it accumulates more salt,
then returns to the river with a more concentrated share; on a
single trip down the Colorado, the same water may be
used for irrigation eighteen times. Human use of the Colorado has
approximately doubled its salinity. Neither the environment nor
urban areas are spared salt's effects: it kills aquatic organisms in
the lower river and corrodes pipes in Los
Angeles, San Diego, and
Phoenix.
The world's most
spectacular saline catastrophe is Central Asia's Aral Sea. Decades ago Soviet planners diverted
two major rivers that feed the Aral in order to turn the surrounding
desert into a cotton cornucopia. As cotton bloomed, however, the sea
wilted: it now contains a third of its former volume and may
disappear.
All twenty-four
native fish species in the Aral have already vanished, and the fish
catch has dropped from 48,000 tons to none. The regional climate has
declined, producing less rainfall and greater temperature extremes.
Each year windstorms pick up 44 million tons of salt and dust from
the dried seabed and scatter them over the river basin. Cotton
output is dropping. The drinking water is contaminated with high
concentrations of salt and agricultural chemicals. Inhabitants
suffer plagues of cancer, respiratory illnesses, and waterborne
diseases such as hepatitis and typhoid fever.
All dams cause
environmental damage: they fragment the riverine ecosystem,
isolating upstream and downstream populations, and, by preventing
floods, cut off the river from its floodplain. Within the reservoir
lake, water temperature changes dramatically. Deep reservoir water
is usually colder in summer and warmer in winter than river water.
Thus water leaving Glen Canyon Dam never varies more than a few
degrees from its 46 degree average. For 240 miles below the dam the
water is too cold for native fish to reproduce.(2)
The reservoir lake
traps not just sediment but nutrients. Algae thrive on the nutrients
and end up consuming the lake's oxygen, turning the water acidic. It
comes out of the dam "hungry," more energetic after shedding its
sediment load, ready to capture new sediment from the riverbed and
-bank. As it scours the downstream river, the bed deepens, losing
its gravel habitats for spawning fish and the tiny invertebrates
they feed on. Within nine years after Hoover Dam was sealed, hungry
water took 89,000 acre-feet of material from the first 87-mile
stretch of riverbed beneath. In places the riverbed dropped by more
than thirteen feet, and it sometimes took floodplain water tables
down with it. In addition, riverbank erosion has undermined some
embankments and flood-control levees.
"A dammed river,"
Wallace Stegner wrote, "is not only stoppered like a bathtub, but it
is turned on and off like a tap." Instead of varying with snowmelt
and rainfall, its flow is regulated to meet the requirements of
power generation and human recreation. Most fluctuations reflect
electricity demand: the river level changes hour by hour and is
lower on Sundays and holidays. These quick fluctuations intensify
erosion, eventually washing away riverbank trees, shrubs, and
grasses as well as riverine nesting areas. Riverside creatures lose
needed food and shelter.
The changes are
registered all the way to the river's mouth and beyond. Because of
dams, many major rivers--including the Colorado, the Yellow, and the Nile--flow to the sea only intermittently.
Without its customary allotment of sediment, the coastline is
subject to erosion. By one estimate, dams have reduced by four
fifths the sediment reaching the southern California
Coast, causing
once wide beaches to disappear and cliffs to fall into the ocean.
Estuaries, where riverine freshwater mixes with ocean saltwater, are
crucial in the development of plankton, which in turn supports a
huge abundance of marine life; deprived of large portions of
freshwater and nutrients, the estuaries decline, and with them so do
fisheries. Migrating fish such as salmon and steelhead trout find
their paths obstructed, both as juveniles swimming downstream to
mature and as adults going upstream to spawn. For this reason, the
Columbia River, where 2 million
fish returned annually to spawn just before the dam era began, has
hosted half that number in recent years, and most remaining stocks
in the upper river are in danger of extinction.
Only by multiplying
all these effects by the number of the world's river basins studded
with dams--an overwhelming majority--can the full environmental
impact of dams be appreciated. The numbers are stunning. The planet
accommodates 40,000 large dams--dams more than four stories
high--and some 800,000 small ones. They have shifted so much weight
that geophysicists believe they have slightly altered the speed of
the earth's rotation, the tilt of its axis, and the shape of its
gravitational field. Together they blot out a terrain bigger than
California.
The most obvious
beneficiaries of dams are politicians, bureaucrats, and builders,
all of whom profit from the dams' huge price tags. Think of the
towering political leaders of the twentieth century--Roosevelt, Stalin, Mao, Nehru. They all loved
dams. Dams provide jobs and a generous amount of money to
constituents, some of whom don't mind donating a portion back to the
politicians. Bureaucrats like dams because that's where the action
is: the expense of dams ensures power to its overseers. The
constituents include dam builders, road builders, engineers,
electricians, carpenters, cooks, plus every sort of professional
boomtowns attract, from developers to prostitutes. In fact, dams,
which provide nearly a fifth of the world's electricity, are also
among the world's costliest public-works projects; by the time
China's Three Gorges Dam is completed (in about 2009), it will have
become the world's largest and most expensive, with an estimated
cost of up to $75 billion.
The attraction of
dams to farmers is obvious. Supported by funding from central
governments and international agencies, farmers rarely pay more than
20 percent of the real cost of the irrigated water. The subsidies
distort the farmers' economic outlook: instead of planting crops
that match the hydrology of their fields, farmers take advantage of
abundant cheap water to plant crops that guzzle water, even if the
crops bring a low return. In the San Joaquin valley of
California, the
richest irrigated land in the world, some farmers grow
water-guzzling cotton, or, worse (because it is fed to cows, the
most notorious guzzlers of all), alfalfa. It takes at least 15,000
tons of water to produce a ton of beef and nearly that much to
produce a ton of cotton; comparatively, a ton of grain requires
1,000 tons of water.
Still, many farmers
founder. For one thing, canal maintenance is often underfunded and
neglected, particularly in developing countries. Planners often
overestimate the amount of water available to the system and
underestimate leakage, evaporation, and waste. Farmers near a canal
head--the "head-enders"--almost invariably receive much more water
than those far down the canal--the "tailenders." The head-enders may
have bought their position with bribes; they are often wealthy
enough to afford the new equipment, seeds, fertilizers, and
pesticides that irrigation farming promotes. At the other end, the
tail-enders may be forced to borrow money at high rates; deeply
indebted, they often end up as tenants on their own land.
The biggest losers
are people displaced by dams. They're usually minorities, often
uneducated and powerless, and therefore hard to count or even
notice, particularly by a government's ruling elite. If the
government bothers to relocate them, it's usually to inferior land,
where settled residents resent them. Rates of illness and death
usually increase after relocation. One estimate puts the worldwide
total of people displaced by dams at 30 to 60 million. As startling
as that sum is, it omits another huge group, the floodplain
residents living downstream from dams whose livelihoods are
jeopardized by the sudden loss of regular nutrient-bearing floods or
other hydrological changes.
If dams are so
destructive in so many ways, why don't we tear them down? The most
obvious answer is that we can't afford to; dismantling dams is
nearly as expensive as building them. Some dams may be
decommissioned and drained, but in the foreseeable future even those
will be few, for the world's reliance on dams for electric power and
irrigation has grown too great to do without them: a world abruptly
deprived of a fifth of its electricity and a significant portion of
its food supply would not remain tranquil for long. Boxed in by the
size of our population, we have approached a natural limit, damned
if we do dam and damned if we don't dam.
The result is a kind
of standoff. While dam building has largely stopped in the
United States and
northern Europe, companies based in North America, Europe, and
Japan continue to lead
construction efforts in developing nations. But even Third World governments increasingly must
finance dams themselves or look for support from private investors.
The World Bank once enthusiastically financed dams throughout the
Third World, until a series of embarrassments, culminating in
militant opposition to a project to build 30 large dams, 135
medium-sized ones, and 3,000 small ones in the Narmada valley of
India caused it
to reconsider. "We now build very few dams," says Briscoe, the World
Bank water specialist.
Although most water
experts appreciate the destructive impact of dams, few oppose them
entirely. IWMI, the World Bank-supported water agency, concluded a
gloomy survey of global water needs in 2025 by noting that "medium
and small dams will almost certainly ... be needed." Postel, whose
book enumerates dams' many liabilities, nevertheless told me, "I
think there's no way we could be supporting a population of 6
billion today without dams. Water comes at uneven times of the year,
and we've got to have a way to store it. The question is how."
RAIN, RAIN, GO
AWAY
Global warming, we
know, is here. Some people think the change chiefly involves
temperature, but the phrase is misleading--it leaves out water.
Nearly every significant indicator of hydrologic activity--rainfall,
snowmelt, glacial melt, evaporation, transpiration, soil moisture,
sedimentation, salinity, and sea level--is changing at an
accelerating pace. Alaskan and Siberian permafrost is beginning to
thaw; in Antarctica scientists are
finding beaches and islands exposed after being covered by ice for
thousands of years. The sea level has risen between four and ten
inches in the last century. Precipitation is increasing, but so are
evaporation, floods, and droughts.
Pick any point of the
hydrologic cycle and note the disruption. One analysis of 1900-1998
data pegged the increase in precipitation at 2 percent over the
century. In water terms this sounds like good news, promising
increased supply, but the changing timing and composition of the
precipitation more than neutralizes the advantage. For one thing, it
is likely that more of the precipitation will fall in intense
episodes, with flooding a reasonable prospect. In addition, while
rainfall will increase, snowfall will decrease. This means that in
watersheds that depend on snowmelt, like the Indus, Ganges,
Colorado, and San Joaquin river basins, less water will be stored as
snow, and more of it will flow in the winter, when it plays no
agricultural role; conversely, less of it will flow in the summer,
when it is most needed. One computer model showed that on the
Animas River at Durango, Colorado, an increase in
temperature of 3.6 degrees Fahrenheit--the global change predicted
from now to 2100--would cause runoff to rise by 85 percent from
January to March but drop by 40 percent from July to September. The
rise in temperature increases the probability and intensity of
spring floods and threatens dam safety, which is predicated on lower
runoff projections. Dams in arid areas also may face increased
sedimentation, since a 10 percent annual increase in precipitation
can double the volume of sediment washed into rivers.
The consequences
multiply. Soil moisture will intensify at the highest northern
latitudes, where precipitation will grow far more than evaporation
and plant transpiration but where agriculture is nonexistent. At the
same time, precipitation will drop over northern mid-latitude
continents in summer months, when ample soil moisture is an
agricultural necessity.
Meanwhile the sea
level will continue to rise as temperatures warm, accelerating
saline contamination of freshwater aquifers and river deltas. This
already has occurred in Florida,
Gaza, and the Nile
River delta.
The temperature rise will cause increased evaporation, which in turn
will lead to a greater incidence of drought. In fact, extreme
water-related events such as storms, floods, and droughts will
become more frequent and intense.
Perhaps most
disturbing of all, the hydrologic cycle is becoming increasingly
unpredictable. This means that the last century's hydrologic
record--the set of assumptions about water on which modern
irrigation is based--is becoming unreliable. Build a dam too large,
and it may not generate its designed power; build it too small, and
it may collapse or flood. Release too little dam runoff in the
spring and risk flood, as the snowmelt cascades downstream with
unexpected volume; release too much and the water won't be available
for farmers when they need it. At a time when water scarcity calls
out for intensified planning, planning itself may be stymied.
WATER WARS OF THE
FUTURE
In the modern era we
fight wars over oil and take water for granted, yet of the two
liquids water is far more capricious and confounding. Oil induces
fear because we sense it can make or break empires; water has
already made and broken quite a few. Think of oil, and you conjure
up gushers, cartels, and economic dominance; think of water and you
contemplate the elixir of life. Oil belongs to whoever owns the land
above it; water, with its sprawling underground aquifers and long
sinuous rivers, complicates ownership and intertwines nations'
fates. Oil promotes grandiosity; water teaches humility.
The handy cliche is
that sooner or later water will cause war. In a quote that caroms
ceaselessly from one water publication to another, World Bank vice
president Ismail Serageldin declared in 1995, "The wars of the next
century will be over water." Many foreign leaders have expressed
similar sentiments. In the late 1980s, Egyptian foreign minister and
soon-to-be U.N. secretary general Boutros Boutros-Ghali said that
the next Middle East war "will be over the waters of the Nile, not politics." Jordan's King Hussein said in 1990
that water was the only issue that could prompt a war between
Jordan and
Israel.
Yet such wars haven't
quite happened. Aaron Wolf, an Oregon State University specialist in water conflicts,
maintains that the last war over water was fought between the
Mesopotamian city states of Lagash and Umma 4,500 years ago.
Wolf has found that during the twentieth century only 7 minor
skirmishes were fought over water while 145 water-related treaties
were signed. He argues that one reason is strategic: in a conflict
involving river water, the aggressor would have to be both
downstream (since the upstream nation enjoys unhampered access to
the river) and militarily superior. As Wolf puts it, "An upstream
riparian would have no cause to launch an attack, and a weaker state
would be foolhardy to do so." And if a powerful downstream nation
retaliates against a water diversion by, say, destroying its weak
upstream neighbor's dam, it still risks the consequences, in the
form of flood or pollution or poison from upstream.
So, until now, water
conflicts have simmered but rarely boiled, perhaps because of the
universality of the need for water. Almost two fifths of the world's
people live in the 214 river basins shared by two or more countries;
the Nile links ten countries, whose
leaders are profoundly aware of one another's hydrologic behavior.
Countries usually manage to cooperate about Water, even in unlikely
circumstances. In 1957, Cambodia, Laos, Thailand, and South
Vietnam formed the Mekong
Committee, which exchanged information throughout the Vietnam War.
Through the 1980s and into the 1990s, Israeli and Jordanian
officials secretly met once or twice a year at a picnic table on the
banks of the Yarmuk River to allocate the river's
water supply; these so-called picnic-table summits occurred while
the two nations disavowed formal diplomatic contact. Jerome Delli
Priscoli, editor of a thoughtful trade journal called Water Policy
and a social scientist at the U.S. Army Corps of Engineers, believes
the whole notion of water conflict is overemphasized: "Water
irrigation helped build early communities and bring those
communities together in larger functional arrangements. Such
community networking was a primary impetus to the growth of
civilization. Indeed, water may actually be one of humanity's great
learning grounds for building community.... The thirst for water may
be more persuasive than the impulse toward conflict."
On the other hand,
water has often been the goal, tool, or target of conflicts that
fall just short of war or that contain non-water-related dimensions.
Recent history is full of examples. In 1965, Syria tried to divert the Jordan
River from Israel, provoking Israeli airstrikes
that forced Syria to abandon the
effort. Colin Powell, chairman of the U.S. Joint Chiefs of Staff
during the 1991 Gulf War, said in 1996 that the United States considered bombing dams
on the Euphrates and Tigris rivers north of Baghdad but
desisted, apparently because of the likelihood of high civilian
casualties. The allies also discussed asking Turkey to reduce the Euphrates flow
at the Ataturk Dam upstream from Iraq. As it was, the
allies targeted Baghdad's
water-supply system while the Iraqis destroyed Kuwait's desalination
plants.
Postel believes water
hostilities are most likely to occur when a river's water is
insufficient to meet projected demand, water allocation is
considered inequitable, and involved nations have made no
water-sharing agreement. In five of the world's most contentious
water basins--the Aral Sea region, the Ganges, the Jordan, the Nile,
and the Tigris-Euphrates--rapid projected population growth--up to
75 percent by 2025--threatens to turn the basins into cauldrons of
hostility. For instance, in the Tigris-Euphrates basin,
Turkey's position
upstream gives it enormous leverage over its downstream neighbors,
Syria and
Iraq. It's likely that
Syria's longtime support of the separatist Kurdistan Workers' Party
in Turkey was at least partly a way of countering Turkey's control
over 80 percent or more of Syria's water supply. But once
Turkey captured
Abdullah Ocalan, a Kurdish guerrilla leader who had lived in
Syria for nearly
two decades, Syria's leverage against
Turkey declined.
Turkey is now in
the midst of a huge dam-building program that will further diminish
the Euphrates's flow into Syria, increasing Syria's grievances.
In the Nile basin the
situation is more volatile, because the downstream nation,
Egypt, dominates the
region. Egypt
already diverts so much Nile water that the river barely flows to
its mouth in the Mediterranean Sea and the Nile delta is subsiding because sediment no
longer reaches it. Nevertheless, Egypt is launching vast new
irrigation projects that will divert even more Nile water. One project will irrigate about
500,000 acres of Egypt's southwestern desert; another
will divert water beneath the Suez Canal to irrigate 625,000 acres
of the Sinai Desert. At the same time,
Ethiopia, the
source of 86 percent of the Nile's
flow, intends to launch its own irrigation and hydroelectric
projects, which could dramatically reduce downstream water. Steve
Lonergan, a specialist in water and security issues at the
University of Victoria, British Columbia, told me, "I don't doubt
that if Ethiopia
starts building water projects that restrict the flow of the Nile,
Egypt will bomb
them."
Even if water wars
remain rare, other sorts of water-related violence already occur
frequently and are certain to increase. Thomas F. Homer-Dixon, a
pioneer in the emerging field of environmental security, cites the
Israeli-Palestinian conflict as an example of how environmental
scarcity affects politics. In his 1999 book, Environment, Scarcity,
and Violence, he argues that the capture by a dominant group of such
resources as water, cropland, and forest occurs most often just at
the point when the resource is becoming scarce and its price is
rising, enabling speculation and increased profits. In the case of
water, that time is now. In Israel water is growing
increasingly scarce; although the nation has been a trailblazer in
the development of water-conservation technologies, it continues to
extract groundwater at an unsustainable rate.
Soon after the
occupation of the West Bank in
1967, Israeli authorities instituted a rationing program that by the
early 1990s gave four times as much water per capita to Israeli
settlers as to Arabs. Israelis also required Arabs to seek
permission to drill wells. When Arabs sought approval to drill over
the West Bank's "Mountain" aquifer,
the biggest aquifer in Israeli-controlled territory, they were
invariably turned down; in other areas permission was given to Arabs
infrequently. In addition, because Israelis had access to more
sophisticated technology, their wells went deeper, often sucking
Arab wells dry or exposing them to saltwater intrusion. Partly as a
result, irrigated Arab farmland dropped from 27 percent to as low as
3.5 percent of the area of all West
Bank cropland. Many Arab farmers abandoned their fields
for towns, where they worked as day laborers, if at all. When the
Palestinians revolted in 1987, the disenfranchised farmers were
presumably primed to participate. "It is reasonable to conclude,"
Homer-Dixon writes, "that water scarcity and its economic effects
contributed to the grievances behind the intifadah."
In this manner, water
scarcity encourages insurgencies. It reduces economic productivity
and forces migration from depleted countryside to ill-prepared city.
Social institutions may break down. Division into ethnic, religious,
or linguistic groups increases. "Water scarcity rarely causes
interstate wars," Homer-Dixon writes. "Rather its impacts are more
insidious and indirect: it constrains economic development and
contributes to a host of corrosive social processes that can, in
turn, produce violence within societies."
OVER THE HORIZON,
CHINA
China is not only the
world's most populous nation, with 1.3 billion people now and 1.5
billion projected by 2050; it also embodies the planet's extremes of
water management and water disaster. China suffers from both
severe droughts and severe floods. It is building what will be the
world's largest dam, and the number of people that the dam will
displace--at least 1.2 million--also will be a record. The
Yellow River is the world's
siltiest river by a factor of nine. At least 50 million rural
Chinese live with an extreme scarcity of drinking water, never mind
water for less immediate uses, such as bathing and sanitation.
The essence of
China's water problem is
that while the nation possesses 21 percent of the world's
population, it has access to only 7 percent of the globe's
freshwater. More specifically, densely populated northern China
includes one third of China's territory, two fifths of its
population, and produces 45 percent of its industrial output but
receives only a quarter of the country's precipitation. One result
is a profound reliance on irrigation: 70 percent of
China's grain
crop grows on irrigated land (compared with 15 percent in the
United
States). This hydrologic riddle is
nothing new: failure to resolve it has ended dynasties and may yet
again. With its ideological claims to legitimacy nullified by its
abandonment of Communism, the current government draws what strength
it can from the nation's huge economic expansion. But the expansion,
volatile and vastly uneven, already has created enormous waves of
social change, such as tens of millions of destitute rural migrants
to the cities and the rising expectation among city dwellers of
running water, indoor toilets, and diets rich in water-intensive
beef and pork. China's recent displays
of wealth are deceptive, since the nation's leaders are forever
trying merely to hold a course amid the country's turbulent
demographic currents. The government consequently takes food-related
issues seriously. Most officials lived through the country's 1959-61
famine, which killed 30 million people, and have no desire to repeat
the experience. That famine only increased Chinese leaders' desire
for grain self-sufficiency. Through the 1990s, that policy required
that at least 95 percent of China's grain be produced
domestically.
The irrigation
system, unfortunately, is a mess. Of China's 30,000 miles of
major rivers, 80 percent are too polluted to support fish. Every
year since 1985, the Yellow River, which flows through the heart of
northern China's farmlands, has
failed to reach its mouth for weeks, and the number of dry days each
year has grown progressively, all the way to 226 days in the drought
year of 1997. For long stretches, the Yellow hasn't even flowed to
Shandong Province, the last province it
waters before reaching the sea. Shandong farmers grow a fifth of
China's wheat and an
eighth of its corn; these days many of them are contemplating a
return to rain-fed agriculture, which means they must drop back to
one crop a year instead of two or three. More serious still, farmers
all over northern China have been depleting
aquifers to grow food. One Chinese survey reported that the water
table beneath the North China Plain had dropped roughly five feet a
year over a recent five-year period.
Rapid
industrialization has intensified water scarcity. Water used in
Chinese industry produces seventy times as much economic value as
water used in agriculture, so industry's needs routinely take
precedence over farmers'. Indeed, one reason Shandong farmers get so little Yellow River water is that it is being
diverted to factories upstream. Moreover, as cities grow, farmland
is taken out of production and turned into industrial and
residential areas. Chinese officials are so desperate to develop new
sources of water for northern China that they are
planning a mammoth diversion that would dwarf Three Gorges Dam in
cost and scope. One route would siphon water from a Yangtze River
tributary, pump it under the Yellow River, and deliver it to the
Beijing region, more than 600 miles away. A U.S.
intelligence study places its cost in the hundreds of billions of
dollars, enough to dampen government expenditures for other projects
for many years into the future. Even that project would probably
serve industrial and residential needs before agricultural ones, and
its environmental damage would be enormous.
In 1994 the extremity
of China's water
situation produced an argument across the globe, in Washington.
Lester Brown, the environmental researcher and founder of the
Worldwatch Institute, claimed that within four decades
China's water
scarcity would compel a huge drop in the country's grain production,
forcing China onto the world
market in such volume that it would price out poorer countries and
induce widespread famine. Most American China experts thought Brown
egregiously overstated China's predicament, but
the U.S. National Intelligence Council took him seriously enough to
sponsor an expensive study. At Sandia National Laboratories
intelligence officers gathered satellite photos to determine
precisely the extent of Chinese agricultural acreage. They found
that Brown greatly underestimated the acreage, which seemed to
discredit his theory, but then, having deflated Brown, the NIC
concluded that China still would need to
import 193 million tons of grain by 2025--an estimate falling only
slightly short of Brown's low-range forecast of 238 million tons by
2030. Meanwhile, Brown's critics were tossing around numbers far
below 100 million tons.
Chinese officials
considered Brown's claims an affront: instead of commending them for
their remarkable economic gains, a Westerner was accusing them of
being poised to starve the world. Brown's motive was to persuade the
Chinese to begin conserving water, but they drew nearly the opposite
conclusion: instead of switching to more lucrative and water-thrifty
export crops, as even Brown's critics (and the NIC) advocated,
Chinese officials tried to prove Brown wrong by increasing grain
production. This meant that Chinese rivers and aquifers would be
depleted at an even faster rate. Although Chinese officials lately
have shown signs of revising this policy, the argument over Brown's
claims still festers. I found this out when I mentioned his name to
Vaclav Smil, author of the estimable 1993 book China's Environmental
Crisis. Smil went off like a firecracker: "Stay off Brown! He's a
nut! He's a guy who predicts the end of the world and massive food
shortages and high prices, yet year after year we have the biggest
surpluses of food and the lowest food prices in history.... Come on,
get serious." And Smil was just getting started.
Of course, all these
estimates are certain to be wrong, or, at best, right for the wrong
reasons. The volume of Chinese grain imports thirty years from now
is unknowable, because so many variables will influence the outcome.
Every estimate takes into account only a fraction of all the
variables and makes different assumptions about the variables used.
Brown downplays the impact of prices, which the optimists believe
will limit meat, grain, and water consumption; on the other hand,
Brown thinks the optimists underestimate the impact of water
scarcity. Will China's agricultural
yields increase, as the optimists assume, or will they stagnate, as
Brown believes? How much money will China invest in
agricultural research? At what rate will China's land erode, its
dams fill with sediment, its water become fouled by industrial waste
and raw sewage? The questions go on and on, and suggest the folly of
predicting production levels decades into the future.
In fact, the
China debate is a
microcosm of the larger argument over the impact of water scarcity
on global food production half a century from now. In this dispute
the optimists and pessimists are more evenly divided. Among the
optimists are the U.N. Food and Agriculture Organization and the
International Food Policy Research Institute, a World
Bank--supported nonprofit; the pessimists include Brown, Postel, and
IWMI, another World Bank--supported nonprofit. In preparation for a
chapter of The World's Water 2000-2001, Peter Gleick found himself
getting into arguments with people on both sides. "I realized that
you can't answer the question without understanding what they're
assuming, whether they tell you that they're assuming it or not,"
Gleick said over the phone. "My conclusion is that people in both
camps don't know the answer--they're making a whole bunch of
assumptions that they aren't telling us. And their crystal ball is
no better than anybody else's."
Gleick focused on
elucidating the disputed range of each of the key variables that
will determine whether the world will be able to feed itself. Among
his variables: Will the world's population in 2050 be closer to 10.7
billion, the U.N's high projection, or 7.3 billion, the U.N's low
projection? Will most people eat 2,300 calories a day, the minimum
level for health set by the FAO, or will they eat 3,300 calories a
day, as people in the wealthier industrialized nations do? What
portion of those calories will come from meat? This is a significant
statistic, since meat consumption requires that grain be fed to
livestock instead of humans. By one estimate, all the grain fed to
U.S. livestock is
equivalent to the amount needed to feed 400 million people. What
will crop yields be? What fraction of crops will be lost to plant
disease, pests, storm damage, harvesting inefficiency, spoilage, and
waste? These sums now are enormous. Diseases, insects, and weeds
destroy about a third of all crops, and a 1997 study estimated that
in the United
States, 27 percent of all edible
food for humans was lost at the retail, consumer, and food-service
levels.
Water scarcity
dictates another set of questions: What will be the water
requirements of the crops grown? A ton of potatoes, for instance,
needs 500 to 1,500 tons of water, while a ton of chicken needs 3,500
to 5,700 tons of water, and a ton of beef needs 15,000 to 70,000
tons of water. What percentage of cropland will be irrigated? How
efficiently will irrigation water be used? At one extreme, flood
irrigation requires a low capital expenditure but wastes a vast
amount of water. At the other extreme, drip irrigation requires
expensive technology but uses water with high efficiency. And will
the water come from rainfall, rivers and streams, lakes and
reservoirs, groundwater, or reclaimed wastewater? As groundwater is
depleted, will other sources be available?
What, finally, will
be the impact of climate change? Gleick calls this "the down card in
the poker game--you can't see it, but you know it's going to be a
factor in all the other answers." If we ignore these questions, he
says, the likelihood increases chat food and water shortages will be
a pivotal feature of twenty-first-century life. "The bottom line,"
he notes, "is that a lot of things have to go right to avoid a
severe crisis."
THE MIRAGE OF BIG
TECHNOLOGY
It is indicative of
the bind we're in that even though technology helped get us into it,
technology also will have to help get us out. Of course,
"technology" includes a wide range of tools, from five-dollar
drip-irrigation bucket kits to the Three Gorges Dam. The optimists'
preference is for big technology, which, as always, seems to promise
a painless way out. The gleam in their eye now is desalination, the
process of turning saltwater into freshwater. "As soon as
desalination technology gets water below, say, thirty cents per
cubic meter, you really run out of a problem," says Aaron Wolf, in
what the pessimists would call an overstatement. Desalination is
useful chiefly as a source for industrial and municipal water in
coastal areas, but the plants are usually too far from farmland to
justify the ample pumping expense--and agriculture consumes 70
percent of all water used by humans. Of the 11,000 desalination
plants that now exist, 60 percent are in the Middle East, where fuel is cheap and state
budgets are relatively flush. The price of desalinated water has
dropped in recent years, but it still typically costs $1 to $2 per
cubic meter. Tantalizingly, a new desalination plant planned for
Tampa,
Florida, will sell
water at 55 cents per cubic meter, but the Gulf water it treats is
less saline than ocean water, and the plant enjoys financing and
energy advantages that may make it unique. As it stands,
desalination accounts for less than 1 percent of human water
needs.
If desalination can't
help us dramatically expand the supply of water, we have no choice
but to reduce our demand for it. Here again, some optimists look to
a high-tech, big-money solution--genetic engineering, which could
produce crops with lower water requirements and higher resistance to
insects, disease, and toxic substances. But the future of genetic
engineering is uncertain because of safety concerns and political
opposition in both Europe and the United
States. "I absolutely believe we
need to work on crop genetics," Gleick says. "But do we bet the
house on it? That's dangerous. I think you have to address all the
food and water questions."
Inevitably, this
means increasing water productivity, getting more "crop per drop."
The potential here is vast, since by some estimates the worldwide
efficiency of agricultural water is 40 percent, which means that
most water diverted for agriculture never even contributes to food
production. Instead, it's lost to evaporation, leaky pipes, unlined
canals, and wasteful irrigation practices. But whereas the Green
Revolution offered a single strategy for increasing crop yield, no
single equivalent exists for increasing water yield. In place of one
approach, many have emerged. They usually use fewer resources, cause
less environmental disruption, and cost less than their
twentieth-century predecessors. In contrast to big projects such as
dams, many of these approaches give local farmers a stake in the
outcome and catalyze them to improve management techniques. "There
is considerable evidence that farmer-controlled small-scale
irrigation has a better record of performance than
government-controlled large- or small-scale systems," writes Mark
Rosegrant, an IFPRI analyst. The list of potentially useful
small-scale methods is long and encompasses technical, managerial,
institutional, and agronomic realms. In some places the best
technique is a traditional one, such as rooftop or mountain-slope
water-harvesting that was ill-advisedly superseded by a big but
ultimately wasteful project.
At the top of most
lists of appropriate water technology is drip irrigation, which was
developed in Israel in the 1960s after
cheap plastic tubing became available. Drip systems deliver water
directly to individual plant roots, eliminating evaporation and
saving water and energy. Drip irrigation not only produces water
efficiency as high as 95 percent but also increases yields, since
plants receive water on a regular basis instead of the boom-and-bust
cycle of flood irrigation. Studies in many countries show that drip
irrigation reduces water use by 30 to 70 percent and increases
yields by 20 to 90 percent. Since only 1 percent of the world's
irrigated lands now use drip and other high-efficiency methods, the
potential for water conservation is huge. In India, for instance; 20
percent of irrigated land may be suitable for the technology.
Drip irrigation's
major liability is its expense, typically $500 to $1,000 per acre,
which has meant that only large farmers growing high-value crops use
it. This is one facet of a huge income gap that irrigation
technology has helped foster: a large majority of the farmers in
developing countries can't afford the tools of irrigation and so are
left out of the global economy. Among them are most of the world's
790 million under-nourished people. To Paul Polak, president of a
Lakewood,
Colorado, nonprofit
called International Development Enterprises, this is "a market
chasm instead of a market niche." IDE has tried to fill it by
working with small businesses in developing countries to design,
field-test, manufacture, and market irrigation technology for poor
farmers. At the low end of its product line is an easy-to-maintain
$5 drip bucket kit, which can irrigate a 10- by 16-foot kitchen
garden with two buckets of water a day. If a farmer grows
income-generating crops, he can make enough money to move up to the
next product in the line, a 55-gallon-drum kit for $26 that can
water a 1,300-square-foot field. In China, where most farms
are smaller than an acre, a poor farmer eventually could irrigate
his entire field with a $300 system. In Nepal and India,
IDE-assisted businesses have sold 10,000 drip kits in two years,
enabling farmers to double yields without increasing water
consumption.(3)
THE DREAM OF THE
OASIS
Las Vegas is America's city of
fantasy, and water, not wealth, is its greatest fantasy of all. The
city that Hoover Dam made possible is the nation's fastest-growing
metropolis in the country's driest state, the perfect manifestation
of the notion that water will never run out. Las Vegas and
the desert don't match: the city looks as if it didn't so much
emerge from its surroundings as get deposited on them. In this
desert of ostentation, water is displayed more lasciviously than
sex. Among the city's hotel casinos, Caesars
Palace laid
down the archetype, festooning its property with fountains and
aqueducts in 1966. Now the Mirage sports a one-acre outcropping of
terraced waterfalls, and a rain forest has been installed beneath a
glass canopy at the entrance. At Treasure
Island the main feature is a naval battle between
British and pirate ships that employs live actors and a large supply
of fireworks; this event attracts a few hundred sidewalk onlookers
five times a night. The Mandalay Bay's grounds include a sandy
beach with three- to four-foot waves. In pursuit of an impressive
water display, I recently chose to stay at the Venetian, which
features--can you guess?--canals, but unfortunately they resemble
nothing so much as brightly lit, elongated bathtubs. The Venetian
even contains a Grand Canal and a
Basilica di San Marco, whose dissimilarities from the originals
include being miniature and plasterboard and on the second floor.
Bewildered tourists wait in line for the chance to pay money to
stripe-shirted "gondoliers," who pole them down the hall, singing
into the air-conditioning ducts.
For all its hydraulic
glory, the Venetian has been upstaged by the Bellagio half a mile
away. There, hotelier Steve Winn spent $40 million on choreographed
spigots that dance to "Singin' in the Rain" and other tunes. Created
by "water feature" specialist WET Design of Universal City,
California, the installation is set within an 11-acre artificial
lake for which the hotel serves as backdrop. Inside the lake are 27
million gallons of water (which a WET Design press release points
out are equivalent to 3,000 swimming pools), 4,500 lights, 798
"MiniShooters," 213 "Oarsmen," 192 "SuperShooters," 350 miles of
electrical wires, 120 miles of electrical cables, and 5 miles of
pipe. The electrical load of this assemblage is 7.5 megawatts,
enough for 7,500 homes. Every half hour, speakers all around the
lake introduce a melody, drawing from an eclectic repertoire that
gives equal billing to Aaron Copland, Luciano Pavarotti, Lionel
Richie, and Marvin Hamlisch. Then, as the music plays, the nozzles
rhythmically spew water in sinuous, synchronous arcs or in pulsed
skyward streams as high as 250 feet. Mist rises lubriciously from
the lake. If the sweating spectators are lucky, some of it wafts
their way. When I asked Carolyn Nott, WET Design's vice president
for business development, why so many Las Vegas hotels feature
water, she had a quick answer: "People in the desert have always
been fascinated by water. It's the idea of the oasis."
I mentioned this
notion to the voluble Pat Mulroy, who as general manager of the
Southern Nevada Water Authority is one of the state's most prominent
officials. Mulroy, whose poufed and bejeweled appearance belies a
canny grasp of western water issues, understands that the "oasis" is
a construct created for Las
Vegas's 30 million tourists a year. The real
Las Vegas is so short of water that
even if it adheres to its current conservation plan, it will
probably run out of Colorado River
water by 2007; then, Mulroy says, "other mechanisms have to come
into play." The "mechanisms," however, are uncertain bets. In the
short term, Mulroy is trying to persuade reluctant Arizonans to sell
part of their allotment of Colorado
River water. In the long run, she is pinning her hopes
on California water, which she
thinks could become available if desalination plants start supplying
California. "That's the only
logical place to go," she says.
Since its institution
in 1995, Las
Vegas's conservation plan has already pared
16 percent off the city's projected water use and is calibrated to
reach 25 percent by 2010. The biggest problem, Mulroy notes, is the
insistence by so many residents on growing lawns: two thirds of the
city's water is used outdoors. The conservation plan has instituted
tiered water rates that force profligate residential users to pay
$900 a month or more for water, and the city limits the size of
front lawns. The hotels, on the other hand, are forgiven their
conspicuous use of water because they are central to Nevada's
economy. "The hotels generate somewhere around 70 percent of the
state's gross product, and they use 8 percent of all the water we
deliver," Mulroy says. "That's not a bad investment." Even so, the
hotels pay top-tier rates for their water, and most use treated gray
water for their displays: the Mirage and Treasure Island share one underground
water-treatment plant, while the Bellagio houses another. Of course,
these facilities are hidden from the hotels' guests, for whom the
illusion of bountiful water is carefully preserved. I found this out
when I asked Mulroy why the hotels don't advise their guests to
reuse towels and stint on water use, as other desert resorts do. She
said, "Las
Vegas sells fantasy. Anything that jars
people back to reality is viewed by those who run the hotels as a
disincentive." It was the next sentence that clicked inside my
brain, as I realized that it summed up the human approach to water
at the end of the twentieth century. "People don't want to live in
reality," she said.
But reality has a way
of forcing its way into human consciousness, and sooner or later we
must acknowledge that our relationship to water is intimate,
complex, and primal: if we abuse it, we inevitably suffer the
consequences. Remove trees from the watershed, and the river below
floods; deplete aquifers, and the land above subsides; pollute or
obstruct the river, and the effects flow all the way to the sea. We
must accommodate ourselves to water, not the other way around.
Neither the pollution of our air and soil nor the destruction of
wilderness nor even the probable extinction of a majority of the
earth's creatures with the threat of catastrophic climate change has
prompted us to change our behavior. Now it is the turn of water, the
very foundation of life, to teach us to be good animals.
(1)
Saudi
Arabia provides perhaps the world's
best example of extravagant groundwater depletion. After helping to
launch the OPEC oil embargo of 1973, Saudis feared other countries
might retaliate with a grain embargo, so they embarked on a program
to make the country self-sufficient in grain. As Postel explains,
the nation subsidized farmers' land, equipment, and water, and paid
them several times the world market price for grain. The result was
that for a short time Saudi Arabia managed to
become a grain exporter. Because of the country's hot, arid climate,
each ton of grain required 3,000 tons of water, triple the usual
ratio. When Saudi
Arabia was forced to make budget
cuts in the mid-1990s, the effort could not be sustained. The
curtailment of subsidies caused grain production to fall by 60
percent. That may be just as well, since Saudi
Arabia otherwise would have run out
of groundwater by 2040. Even now, with a more modest agricultural
program, the Saudis continue to run a significant groundwater
deficit.
(2) In the new lakes,
sport fish stocked for humans' recreation--catfish, bass, and
sunfish, and minnows for all of them to feed on--arrive previously
adapted to stable lake environments and thrive. They prey on the
native fish, which are now disadvantaged by being suited to river
conditions. The humpback chub, native to the Colorado, has an odd-looking hump behind its
head that contains extra muscles connecting to its tail; before the
dam era, it used those muscles to survive in the Colorado's
occasionally torrential waters. Now the chub, like virtually all
other native Lower Colorado fish,
courts extinction. In little more than half a century a foreign fish
population has essentially replaced the Colorado's
native one.
(3) The path of
appropriate water management often isn't smooth. IDE's biggest
success is in Bangladesh, where it has
overseen the sale and installation of 1.3 million treadle pumps
since 1984. Treadle pumps are useful in areas like
Bangladesh s
Ganges delta, where aquifers are
replenished during summer monsoons and the major problem is finding
water during the scorching dry season. Farmers peddle the treadles
for two to six hours a day; the difficulty of pumping water this way
assures its judicious use. Treadle pumps cost $35 and enable farmers
to earn at least $100 a year in increased crop production. In recent
years, however, scientists have discovered that much of the
underground water in the Ganges
delta is contaminated with naturally occurring arsenic. The result
has been what the World Bank calls "perhaps the largest mass
poisoning in history"; 20 million people may be poisoning
themselves, and several hundred thousand already display symptoms.
The difficulty arose after officials promoted wells to counter a
more immediate health problem, the spread of waterborne diseases as
a result of drinking dirty pond water. Although IDE's treadle pumps
are used chiefly for agriculture, not human consumption, Polak says
he assumes that even crops grown with contaminated groundwater are
affected, and IDE has joined a massive effort to replace
contaminated wells. The larger lesson, of course, is that testing
should occur when wells are dug.
Jacques Leslie is the
author of The Mark: A War Correspondent's Memoir of
Vietnam &
Cambodia, published in
1995. He is working on a book about water.
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COPYRIGHT 2000
Harper's Magazine Foundation
in association with
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