Our Water Resources Resources and Man The Malthusian trap The kinds of resources – renewable resources – Nonrenewable resources – Potentially renewable resources The nature of exhaustibility Food is the most basic of all our needs SELFACTUALIZATION ESTEEM SOCIAL SECURITY PHYSIOLOGICAL MASLOW’S HIERARCHY OF NEEDS Thomas Malthus (1766-1834) In “An Essay on the Principles of Population”, published in 1798, Thomas Malthus argued that while population increases in geometric progression, the resources to sustain this growth do not. Thus, if population grows too much faster than food production, this growth is checked by famine, disease, and war. Thomas Malthus 5000 4000 3000 The sustainable levels for Isle Royale inhabitants 2000 50 40 30 20 10 0 1000 1900 1920 1940 1960 1980 2000 Wolf population Moose population This should ordinarily signal disaster. Take the case of wolves and moose at Isle Royale National Park, Lake Superior, for instance. Relative to the 1820 level World’s population, a little over a billion at the time of Malthus, has multiplied about six-fold since then. Measured in inflation-adjusted dollars, world’s total output, now about $40 trillion, was about $700 billion at the time of Malthus. Clearly, economic growth has been more strongly exponential than that of the demand (population growth) that created it. 45 Economy 30 Population 15 0 1800 1850 1900 1950 2000 Source: A. Maddison, Monitoring the World Economy 1820-1992 (OECD, Paris, 1995). World Grain Output 2 3 6 3 4 2 2 1 0 0 World Population Gross World Product 1 The growth in world’s grain output has been faster than population but world economy has growth even faster. Values relative to 1950 6 Gross World Product World Grain Production 4 2 World Population 0 1950 1960 1970 1980 1990 2000 Adam Smith (1723-1790), the British philosopher and economist, argued, in his celebrated treatise An Inquiry into the Nature and Causes of the Wealth of Nations (1776), that every individual in pursuing his or her own good is led, as if by an invisible hand, to achieve the best good for all. Therefore any interference with free competition by the government is almost certain to be injurious. First Green Revolution in this century took place in developed countries during 1950-70. First Green Revolution Second Green Revolution has occurred in developing countries since mid-1960s. First Green Revolution Second Green Revolution 2.0 400 1.5 300 1.0 200 0.5 1940 1960 1980 Per Capita Grain Availability (kg per year) World Grain Production (billion tons per year) Despite the tremendous strides in world grain production, per capita grain availability has remained unchanged since the mid-1970s*. 100 2000 *Lester R. Brown: “Facing the Prospect of Food Scarcity” in STATE OF THE WORLD 1997 (Worldwatch Institute, 1997) Currently, the annual food production world-wide, including grains, poultry, seafood and meat, is about 4 billion tons per year, or about 4½ lbs per person per day. But per capita food consumption varies, worldwide, from ~1500 lbs per year in America, to ~1000 lbs per year in Mediterranean/ Middle East region, and about 500 lbs per year in India and South Asia. 15 Desert Mean Annual Temperature ( o C) Grassland 30 Tropical Forest Farmland Deciduous Forest (seasonal loss of leaves) Being largely Coniferous Forest stenohumid (green year-round) as well as stenothermal, 0 agricultural Arctic and alpine treeless areas crops impose 0 100 200 300 400 a rather Mean annual precipitation (cm) restricted range of climatic conditions. Farmland therefore tends to be in short supply. Most of the Earth is covered by water Land (29%) Oceans (71%) “...water, water, every where nor any drop to drink!” But the supply of land too is limited... In use Oceans (71%) Land (29%) Potential farming 8% Tropical forests Cultivated Grazed 11% 10% 14% Forests, semi-arid 6% Arid Ice, snow, deserts, mountains (51%) and barely a fifth of it is available for farming related activities. Unusable Potential grazing Economic growth exacerbates the demand for water, e.g., • with economic growth at 7-10% per year, poultry consumption is rising at the rate of 15% per year in India, Indonesia and China the water demands of this nontraditional industry are only likely to grow; • we need about 250,000 gallons of water to produce a ton of corn, 375,000 gallons to produce a ton of wheat, 1,000,000 gallons to produce a ton of rice, and 7,500,000 of water to produce a ton of beef. •to which we should also add industry’s needs. U.S.A. Public (6%) Farming (41%) China Industry (7%) Public (10%) Industry (11%) PowerPlant (38%) Farming (85%) PowerPlant (2%) this comparison of U.S. and China shows how economic growth necessitates increased use of Source: Worldwatch Institute water for nonagricultural purposes. How much water do we have? The hydrological cycle Ignoring such long-term effects as the changes in atmospheric storage conditions, run-off filling the ocean basins etc., hydrological cycle is merely the recycling of water between land and oceans. http://ww2010.atmos.uiuc.edu/(Gh)/guides/mtr/hyd/smry.rxml How much water in the hydrosphere? Conventional estimate assumes a total groundwater storage of about 1,700 quadrillion gallons. This gives the estimate of hydrosphere’s total water content as 3.5x1020 gallons. Underground water (0.5%) Surface water (0.02%) Atmospheric moisture (0.001%) Oceans (97%) Ice (1.2%) An alternate assumption is that pores in sediments contain about 80,000 quadrillion gallons of groundwater (almost 50 times the conventional estimate). This yields an estimate of about 4x1020 gallons of water in the Ice (1%) entire hydroshere. Surface water (0.002%) Atmosphere (0.001%) Groundwater (19%) Groundwater (19%) Oceans (80%) As is evident from the comparison of water use in the U.S. and China, economic growth necessitates increasing use of water for power generation. U.S.A. Public (6%) Farming (41%) China Industry (7%) Public (10%) Industry (11%) PowerPlant (38%) Source: Worldwatch Institute Farming (85%) PowerPlant (2%) Global mean temperature change through the past century Temperature Change (ºC) 0.6 0.3 0.0 - 0.3 5-year running average - 0.6 Source: NOAA and NASA 1900 1950 2000 Sea level relative to 1951-70 (cm) The global mean sea-level rise through last century 8 4 0 -4 5-year running average -8 -12 1900 1950 2000 Source: T.P. Barnett, in CLIMATE CHANGE (IPCC Working Group Report: Cambridge University Press, 1990) DT (oC) 0 0 0.3 0.6 0.9 1.2 Depth (m) 100 200 300 The 1950-91 hydrographic data off California coast show that sea surface waters (0-100m) became ~0.8oC warmer in the 35-year period between 1950-56 and 1985-91; which 400 Distance off California coast (km) 500 400 300 200 raised the sea level surface by 3.1+0.7 cm. Note: Warming by 1oC the top 100 m of ocean with 15oC temperature and 3.4% salinity should raise the sea level by ~2.2 cm. Source: D. Roemmich, SCIENCE: v. 257, p. 373-375 (July 17, 1992). 0 100 95 1985-91 90 1950-56 85 80 Steric height (dynamic cm) 500 100 Steric height (dynamic cm) Sea surface off California has risen by about 2 cm, on average, between 1950 and 1991 100 95 19851991 90 85 80 500 19501956 400 300 200 100 Distance off California coast (km) 0 Dean Roemmich: Ocean warming and sea level rise along the southwest U.S. coast [Science: 257 ( 373-375), 1992] The availability of water too is a limiting factor. An average human needs about 300,000 gallons of water annually, including 250,000 gallons for growing food. Indeed, nations with under 150,000 gallons of annual per capita water supply face severe limits to their growth. Mass of the present hydrosphere Considering all sediments* Conventional estimates Total mass Share of the Total mass Share of the (trillion tons) hydrosphere (trillion tons) hydrosphere Oceans Pore water in the sediments Ice-caps, glaciers Rivers, lakes Atmospheric moisture 1,370,000 80% Total hydrosphere 1,720,313 100% 330,000 18.8% 20,000 1.2% 300 0.02% 13 0.0008% 1,370,000 97% 7,000 0.5% 20,000 1.4% 300 0.02% 13 0.0009% 1,397,313 100% *Karl K. Turekian: GLOBAL ENVIRONMENTAL CHANGE (Prentice Hall, 1996) Seafood is an important source of animal protein worldwide, nonetheless. World fish harvest: Annual fish harvest (million tons) Note that Indian Ocean has the least yield. Area Volume (106 km2) (106 km3) Pacific Ocean 165.2 707.6 Atlantic Ocean 82.4 323.6 Indian Ocean 73.4 291.0 Primary production (gC/m2/yr) World fish production* Oceanic 50 Coastal 100 Upwelling 300 Average number of trophic Ocean area steps 2 (km ) 325x106 (90%) 36x106 (9.9%) 36x104 (0.1%) * J.H. Ryther: Science, 166 (1969): 72-76 5 3 15 Net transfer efficiency Total fish production (tons/yr) 0.0001 0.033 1.1 1.63x106 (<1%) 120 x106 (~50%) 120x106 (~50%) Even the maximum possible yield from world’s oceans can hardly suffice. Annual fish harvests of the leading nations. Seafood is already a major source of animal protein in the Asian diet. That Climate Thing • Global warming and its consequences • The anthropogenic contributions U.S. 20th Century Natural Disaster Fatality-Frequency Plots* Cummulative Number of Events per Year 10 Floods Tornadoes Hurricanes Earthquakes Floods 3 Tornadoes 1 Hurricanes 0.3 0.1 Earthquakes 0.03 0.01 1 3 10 30 100 300 1,000 3,000 10,000 Number of Fatalities per Event * S.P. Nishenko and C.C. Barton: “Scaling Laws for Natural Disaster Fatalities” in REDUCTION AND PREDICTABILITY OF NATURAL DISASTERS (Eds: Rundle, Turcotte and Klein) (Addison-Wesley, 1996) Disasters* by type: 1971-96 High wind: 21% Man-made disasters: 34% Total: 8,219,000 Flood: 19% Other natural disasters: 21% Volcanoes: 1% Earthquake: 8% Landslides: 3% Drought & Famine: 6% * International Federation of Red Cross and Red Crescent Societies (The Economist, Sept 6, 1997) Global mean temperature change through last century Temperature Change ( oC) 0.6 0.3 1950-60 Mean level 0.0 - 0.3 5-year running average - 0.6 1900 1950 Source: Thomas Karl and C. Bruce Baker: GLOBAL WARMING UPDATE (NCDC-NOAA, 1994) 2000 Sea level relative to 1951-70 (cm) The global mean sea-level rise through last century 8 4 Mean 1951-1970 level 0 -4 5-year running average -8 -12 1900 1950 2000 Source: T.P. Barnett, in CLIMATE CHANGE (IPCC Working Group Report: Cambridge University Press, 1990) Winter conditions in Eastern Europe through the past millenium, based on manuscript records* 0.8 Little Ice Age o D T ( C) 0.4 0 -0.4 -0.8 800 1000 1200 1400 * J. Imbrie & K.P. Imbrie: ICE AGES (Enslow Publishers, 1979) 1600 1800 2000 DT (oC) 0 0 0.3 0.6 0.9 1.2 Depth (m) 100 200 300 The 1950-91 hydrographic data off California coast show that the sea surface waters (0-100m) became ~0.8oC warmer in the 35-year period between 1950-56 and 1985-91; which 400 Distance off California coast (km) 500 400 300 200 raised the sea level surface by 3.1+0.7 cm. Note: Warming by 1oC the top 100 m of ocean with 15oC temperature and 3.4% salinity should raise the sea level by ~2.2 cm. Source: D. Roemmich, SCIENCE: v. 257, p. 373-375 (July 17, 1992). 0 100 95 1985-91 90 1950-56 85 80 Steric height (dynamic cm) 500 100 Global warming will hurt the poor nations most! 20% 0% - 20% - 40% - 60% Change in average national crop yield by the year 2,060 compared to yield corresponding to no change in climate (based on the ocean-atmosphere coupling model) - SCIENCE NEWS, Aug 1992 Evaporation 60,000 km3 Evaporation 320,000 km3 Precipitation 285,000 km3 Precipitation 95,000 km3 Run-off 35,000 km3 Ocean Storage 1,370,000,000 km3 The Hydrological Cycle diversions (billion m 3/yr) Flow of Colorado River below all major dams and Colorado River 40 United States 30 Mexico 20 10 1900 1920 1940 1960 1980 2000 Sandra Postel: Forging a Sustainable Water Strategy (STATE OF THE WORLD 1996: Worldwatch Institute , 1996) 80 Stream Flow into Aral Sea (billion m 3 /year) Drying of the Aral Sea Aral Sea 60 40 20 0 1940 1960 1980 2000 Sandra Postel: Forging a Sustainable Water Strategy (STATE OF THE WORLD 1996: Worldwatch Institute , 1996) A century of human induced sea level rise* Removable volume (in 1012 m3) North America High plains Southwest California Africa and Asia Sahara Sahel (soil water) Arabia Aral (Sea: 1960) Aral (groundwater) Caspian (Sea) Caspian (groundwater) Worldwide Deforestation Wetland reduction Dams Total Extraction rate (in 1010 m3/yr) Sea-level rise Estimated sea-level rate (mm/yr) change to date (mm) 4.0 3.0 10.0 1.20 1.00 1.30 0.03 0.03 0.04 1.10 0.92 1.20 600.0 0.1 500.0 1.1 2.2 56.0 220.0 1.00 0.34 1.60 2.70 3.70 0.77 0.47 0.03 0.01 0.04 0.08 0.10 0.02 0.01 0.56 0.28 0.89 2.20 3.10 1.30 0.78 3.3 8.6 -1.9 4.90 0.20 - 0.14 0.01 - 3.40 1.30 -5.20 1406.7 19.20 0.54 11.80 * Walter Newman and Rhodes Fairbridge: The Management of Sea-level Rise (NATURE, v. 320, p. 319-328, 1986). Dork Sahagian, Frank Schwartz and David Jacobs: Direct Anthropogenic Contributions to Sea-level Rise in the Twentieth Century (NATURE: v. 367, p. 54-57, 1994). The 1900-94 trends reveal a general tendency towards greater precipitation (a) at higher latitudes and (b) on land Change in precipitation (1900-94) 20% 0% -20% Thomas Karl, Neville Nicholls & Jonathan Gregory: THE COMING CLIMATE, Scientific American, May 1997 Comparing the 1900-94 precipitation change with (a) latitude and (b) land area Precipitation Change (%, 1900-94) Latitude - 10 0 10 20 0 1 2 40oN 0o 40oS -1 Land, as % of Global Surface Area Evaporation 60,000 km3 Evaporation 320,000 km3 Precipitation 95,000 km3 Precipitation 285,000 km3 Run-off 35,000 km3 Ocean Storage 1,370,000,000 km3 The Hydrological Cycle In summary, Human ingenuity has defied the “Malthusian Trap”, that the power of population exceeds that of the earth. This has resulted in modifying the most basic of nature’s processes - the hydrological cycle. Perhaps technology defies the Gandhian dictum, that “nature has enough for our need, but not for our greed”.