Water distribution on Earth - wikipedia Water distribution on Earth This article 's lead section may be too long for the length of the article. Please help by moving some material from it into the body of the article. Please read the layout guide and lead section guidelines to ensure the section will still be inclusive of all essential details. Please discuss this issue on the article 's talk page. ( May 2018 ) A graphical distribution of the locations of water on Earth Water is distributed across earth. Most water in the Earth 's atmosphere and crust comes from the world ocean 's saline seawater, while freshwater accounts for only 2.5 % of the total. Because the oceans that cover roughly 78 % of the area of the Earth reflect blue light, the Earth appears blue from space, and is often referred to as the blue planet and the Pale Blue Dot. An estimated 1.5 to 11 times the amount of water in the oceans may be found hundreds of miles deep within the Earth 's interior, although not in liquid form. The oceanic crust is young, thin and dense, with none of the rocks within it dating from any older than the breakup of Pangaea. Because water is much denser than any gas, this means that water will flow into the `` depressions '' formed as a result of the high density of oceanic crust. ( On a planet like Venus, with no water, the depressions appear to form a vast plain above which rise plateaux ). Since the low density rocks of the continental crust contain large quantities of easily eroded salts of the alkali and alkaline earth metals, salt has, over billions of years, accumulated in the oceans as a result of evaporation returning the fresh water to land as rain and snow. As a result, the vast bulk of the water on Earth is regarded as saline or salt water, with an average salinity of 35 ‰ ( or 3.5 %, roughly equivalent to 34 grams of salts in 1 kg of seawater ), though this varies slightly according to the amount of runoff received from surrounding land. In all, water from oceans and marginal seas, saline groundwater and water from saline closed lakes amount to over 97 % of the water on Earth, though no closed lake stores a globally significant amount of water. Saline groundwater is seldom considered except when evaluating water quality in arid regions. The remainder of the Earth 's water constitutes the planet 's fresh water resource. Typically, fresh water is defined as water with a salinity of less than 1 percent that of the oceans - i.e. below around 0.35 ‰. Water with a salinity between this level and 1 ‰ is typically referred to as marginal water because it is marginal for many uses by humans and animals. The ratio of salt water to fresh water on Earth is around 40 to 1. The planet 's fresh water is also very unevenly distributed. Although in warm periods such as the Mesozoic and Paleogene when there were no glaciers anywhere on the planet all fresh water was found in rivers and streams, today most fresh water exists in the form of ice, snow, groundwater and soil moisture, with only 0.3 % in liquid form on the surface. Of the liquid surface fresh water, 87 % is contained in lakes, 11 % in swamps, and only 2 % in rivers. Small quantities of water also exist in the atmosphere and in living beings. Of these sources, only river water is generally valuable. Most lakes are in very inhospitable regions such as the glacial lakes of Canada, Lake Baikal in Russia, Lake Khövsgöl in Mongolia, and the African Great Lakes. The North American Great Lakes, which contain 21 % of the world 's fresh water by volume, are the exception. They are located in a hospitable region, which is heavily populated. The Great Lakes Basin is home to 33 million people. The Canadian cities of Toronto, Hamilton, Ontario, St. Catharines, Niagara, Oshawa, Windsor, and Barrie, and the United States cities of Duluth, Milwaukee, Chicago, Gary, Detroit, Cleveland, Buffalo, and Rochester, are all located on shores of the Great Lakes. Although the total volume of groundwater is known to be much greater than that of river runoff, a large proportion of this groundwater is saline and should therefore be classified with the saline water above. There is also a lot of fossil groundwater in arid regions that has never been renewed for thousands of years ; this must not be seen as renewable water. However, fresh groundwater is of great value, especially in arid countries such as India. Its distribution is broadly similar to that of surface river water, but it is easier to store in hot and dry climates because groundwater storages are much more shielded from evaporation than are dams. In countries such as Yemen, groundwater from erratic rainfall during the rainy season is the major source of irrigation water. Because groundwater recharge is much more difficult to accurately measure than surface runoff, groundwater is not generally used in areas where even fairly limited levels of surface water are available. Even today, estimates of total groundwater recharge vary greatly for the same region depending on what source is used, and cases where fossil groundwater is exploited beyond the recharge rate ( including the Ogallala Aquifer ) are very frequent and almost always not seriously considered when they were first developed. Contents 1 Distribution of saline and fresh water 2 Distribution of river water 3 Area, volume, and depth of the world ocean 4 Variability of water availability 5 Water in Earth 's mantle 6 See also 7 References Distribution of saline and fresh water The total volume of water on Earth is estimated at 1.386 billion km3 ( 333 million cubic miles ), with 97.5 % being salt water and 2.5 % being fresh water. Of the fresh water, only 0.3 % is in liquid form on the surface. In addition, the lower mantle of inner earth may hold as much as 5 times more water than all surface water combined ( all oceans, all lakes, all rivers ). Source of water Volume of water in km3 ( cu mi ) % total water % salt water % fresh water % liquid surface fresh water Oceans 7018133800000000000 ♠ 1,338,000,000 ( 321,000,000 ) 96.5 99.0 Pacific Ocean 7017669880000000000 ♠ 669,880,000 ( 160,710,000 ) 48.3 49.6 Atlantic Ocean 7017310410900000000 ♠ 310,410,900 ( 74,471,500 ) 22.4 23.0 Indian Ocean 7017264000000000000 ♠ 264,000,000 ( 63,000,000 ) 19.0 19.5 Southern Ocean 7016718000000000000 ♠ 71,800,000 ( 17,200,000 ) 5.18 5.31 Arctic Ocean 7016187500000000000 ♠ 18,750,000 ( 4,500,000 ) 1.35 1.39 Ice and snow 7016243640000000000 ♠ 24,364,000 ( 5,845,000 ) 1.76 69.6 Glaciers 7016240640000000000 ♠ 24,064,000 ( 5,773,000 ) 1.74 68.7 Antarctic ice sheet 7016216000000000000 ♠ 21,600,000 ( 5,200,000 ) 1.56 61.7 Greenland ice sheet 7015234000000000000 ♠ 2,340,000 ( 560,000 ) 0.17 6.68 Arctic islands 7013835000000000000 ♠ 83,500 ( 20,000 ) 0.006 0.24 Mountain ranges 7013406000000000000 ♠ 40,600 ( 9,700 ) 0.003 0.12 Ground ice and permafrost 7014300000000000000 ♠ 300,000 ( 72,000 ) 0.022 0.86 Groundwater 7016234000000000000 ♠ 23,400,000 ( 5,600,000 ) 1.69 Saline groundwater 7016128700000000000 ♠ 12,870,000 ( 3,090,000 ) 0.93 0.95 Fresh groundwater 7016105300000000000 ♠ 10,530,000 ( 2,530,000 ) 0.76 30.1 Soil moisture 7013165000000000000 ♠ 16,500 ( 4,000 ) 0.0012 0.047 Lakes 7014176400000000000 ♠ 176,400 ( 42,300 ) 0.013 Saline lakes 7013854000000000000 ♠ 85,400 ( 20,500 ) 0.0062 0.0063 Caspian Sea 7013782000000000000 ♠ 78,200 ( 18,800 ) 0.0056 0.0058 Other saline lakes 7012720000000000000 ♠ 7,200 ( 1,700 ) 0.00052 0.00053 Fresh water lakes 7013910000000000000 ♠ 91,000 ( 22,000 ) 0.0066 0.26 87.0 African Great Lakes 7013300700000000000 ♠ 30,070 ( 7,210 ) 0.0022 0.086 28.8 Lake Baikal 7013236150000000000 ♠ 23,615 ( 5,666 ) 0.0017 0.067 22.6 North American Great Lakes 7013221150000000000 ♠ 22,115 ( 5,306 ) 0.0016 0.063 21.1 Other fresh water lakes 7013152000000000000 ♠ 15,200 ( 3,600 ) 0.0011 0.043 14.5 Atmosphere 7013129000000000000 ♠ 12,900 ( 3,100 ) 0.00093 0.037 Swamps 7013114700000000000 ♠ 11,470 ( 2,750 ) 0.00083 0.033 11.0 Rivers 7012212000000000000 ♠ 2,120 ( 510 ) 0.00015 0.0061 2.03 Biological water 7012112000000000000 ♠ 1,120 ( 270 ) 0.000081 0.0032 Distribution of river water The total volume of water in rivers is estimated at 2,120 km3 ( 510 cubic miles ), or 2 % of the surface fresh water on Earth. Rivers and basins are often compared not according to their static volume, but to their flow of water, or surface runoff. The distribution of river runoff across the Earth 's surface is very uneven. Continent or region River runoff ( km3 / year ) Percent of world total North America 7,800 17.9 South America 12,000 27.6 Europe 2,900 6.7 Middle East and North Africa 140 0.3 Sub-Saharan Africa 4,000 9.2 Asia ( excluding Middle East ) 13,300 30.6 Australia 440 1.0 Oceania 6,500 14.9 There can be huge variations within these regions. For example, as much as a quarter of Australia 's limited renewable fresh water supply is found in almost uninhabited Cape York Peninsula. Also, even in well - watered continents, there are areas that are extremely short of water, such as Texas in North America, whose renewable water supply totals only 26 km3 / year in an area of 695,622 km2, or South Africa, with only 44 km3 / year in 1,221,037 km2. The areas of greatest concentration of renewable water are : The Amazon and Orinoco Basins ( a total of 6,500 km3 / year or 15 percent of global runoff ) East Asia Yangtze Basin - 1,000 km3 / year South and Southeast Asia, with a total of 8,000 km3 / year or 18 percent of global runoff Brahmaputra Basin - 900 km3 / year Irrawaddy Basin - 500 km3 / year Mekong Basin - 450 km3 / year Canada, with over 10 percent of world 's river water and large numbers in lakes Mackenzie River - over 250 km3 / year Yukon River - over 150 km3 / year Siberia Yenisey - over 5 % of world 's fresh water in basin - second largest after the Amazon Ob River - over 500 km3 / year Lena River - over 450 km3 / year New Guinea Fly and Sepik Rivers - total over 300 km3 / year in only about 150,000 km2 of basin area. Area, volume, and depth of the world ocean Body of Water Area ( 10 km ) Volume ( 10 km ) Mean Depth ( m ) Atlantic Ocean 82.4 323.6 3,926 Pacific Ocean 165.2 707.6 4,282 Indian Ocean 73.4 291.0 3,963 All oceans and seas 361 1,370 3,796 Variability of water availability Variability of water availability is important both for the functioning of aquatic species and also for the availability of water for human use : water that is only available in a few wet years must not be considered renewable. Because most global runoff comes from areas of very low climatic variability, the total global runoff is generally of low variability. Indeed, even in most arid zones, there tends to be few problems with variability of runoff because most usable sources of water come from high mountain regions which provide highly reliable glacier melt as the chief source of water, which also comes in the summer peak period of high demand for water. This historically aided the development of many of the great civilizations of ancient history, and even today allows for agriculture in such productive areas as the San Joaquin Valley. However, in Australia and Southern Africa, the story is different. Here, runoff variability is much higher than in other continental regions of the world with similar climates. Typically temperate ( Köppen climate classification C ) and arid ( Köppen climate classification B) climate rivers in Australia and Southern Africa have as much as three times the coefficient of variation of runoff of those in other continental regions. The reason for this is that, whereas all other continents have had their soils largely shaped by Quaternary glaciation and mountain building, soils of Australia and Southern Africa have been largely unaltered since at least the early Cretaceous and generally since the previous ice age in the Carboniferous. Consequently, available nutrient levels in Australian and Southern African soils tend to be orders of magnitude lower than those of similar climates in other continents, and native flora compensate for this through much higher rooting densities ( e.g. proteoid roots ) to absorb minimal phosphorus and other nutrients. Because these roots absorb so much water, runoff in typical Australian and Southern African rivers does not occur until about 300 mm ( 12 inches ) or more of rainfall has occurred. In other continents, runoff will occur after quite light rainfall due to the low rooting densities. Climate type ( Köppen ) Mean annual rainfall Typical runoff ratio for Australia and Southern Africa Typical runoff ratio for rest of the world BWh 250 mm ( 10 inches ) 1 percent ( 2.5 mm ) 10 percent ( 25 mm ) BSh ( on Mediterranean fringe ) 350 mm ( 14 inches ) 3 percent ( 12 mm ) 20 percent ( 80 mm ) Csa 500 mm ( 20 inches ) 5 percent ( 25 mm ) 35 percent ( 175 mm ) Caf 900 mm ( 36 inches ) 15 percent ( 150 mm ) 45 percent ( 400 mm ) Cb 1100 mm ( 43 inches ) 25 percent ( 275 mm ) 70 percent ( 770 mm ) The consequence of this is that many rivers in Australia and Southern Africa ( as compared to extremely few in other continents ) are theoretically impossible to regulate because rates of evaporation from dams mean a storage sufficiently large to theoretically regulate the river to a given level would actually allow very little draft to be used. Examples of such rivers include those in the Lake Eyre Basin. Even for other Australian rivers, a storage three times as large is needed to provide a third the supply of a comparable climate in southeastern North America or southern China. It also affects aquatic life, favouring strongly those species able to reproduce rapidly after high floods so that some will survive the next drought. Tropical ( Köppen climate classification A ) climate rivers in Australia and Southern Africa do not, in contrast, have markedly lower runoff ratios than those of similar climates in other regions of the world. Although soils in tropical Australia and southern Africa are even poorer than those of the arid and temperate parts of these continents, vegetation can use organic phosphorus or phosphate dissolved in rainwater as a source of the nutrient. In cooler and drier climates these two related sources tend to be virtually useless, which is why such specialised means are needed to extract the most minimal phosphorus. There are other isolated areas of high runoff variability, though these are basically due to erratic rainfall rather than different hydrology. These include : Southwest Asia The Brazilian Nordeste The Great Plains of the United States Water in Earth 's mantle It is estimated an additional 1.5 to eleven times the amount of water in the oceans is contained in the Earth 's interior, and some scientists have hypothesized that the water in the mantle is part of a `` whole - Earth water cycle ''. The water in the mantle is dissolved in various minerals near the transition zone between Earth 's upper and lower mantle. At temperatures of 1,100 ° C ( 2,010 ° F ) and extreme pressures found deep underground, water breaks down into hydroxyls and oxygen. The existence of water was experimentally predicted in 2002, and direct evidence of the water was found in 2014 based on tests on a sample of ringwoodite. Further evidence for large quantities of water in the mantle was found in observations of melting in the transition zone from the USArray project. Liquid water is not present within the ringwoodite, rather the components of water ( hydrogen and oxygen ) are held within as hydroxide ions. See also Deficit irrigation Water resource management Magmatic water References Jump up ^ USGS - Earth 's water distribution Jump up ^ `` Great Lakes -- U.S. EPA ''. Epa.gov. 2006 - 06 - 28. Retrieved 2011 - 02 - 19. Jump up ^ `` LUHNA Chapter 6 : Historical Landcover Changes in the Great Lakes Region ''. Biology.usgs.gov. 2003 - 11 - 20. Archived from the original on 2012 - 01 - 11. Retrieved 2011 - 02 - 19. Jump up ^ Ghassemi, Fereidoun ( 2007 ). Inter-basin water transfer. Cambridge, Cambridge University Press. ISBN 0 - 521 - 86969 - 2. Jump up ^ `` Archived copy ''. Archived from the original on 2015 - 11 - 01. Retrieved 2015 - 10 - 29. Jump up ^ Reisner, Marc ; Cadillac Desert : The American West and its Disappearing Water ; pp. 438 - 442. ISBN 0 - 14 - 017824 - 4 ^ Jump up to : Where is Earth 's water ?, United States Geological Survey. Jump up ^ Eakins, B.W. and G.F. Sharman, Volumes of the World 's Oceans from ETOPO1, NOAA National Geophysical Data Center, Boulder, CO, 2010. Jump up ^ Water in Crisis : Chapter 2, Peter H. Gleick, Oxford University Press, 1993. Jump up ^ Harder, Ben. `` Inner Earth May Hold More Water Than the Seas ''. National Geographic. Retrieved 14 November 2013. ^ Jump up to : Brown, J.A.H. ; Australia 's surface water resources. ISBN 978 - 0 - 644 - 02617 - 8. Jump up ^ McMahon, T.A. and Finlayson, B.L. ; Global Runoff : Continental Comparisons of Annual Flows and Peak Discharges. ISBN 3 - 923381 - 27 - 1. ^ Jump up to : Peel, Murray C. ; McMahon, Thomas A. & Finlayson, Brian L. ( 2004 ). `` Continental differences in the variability of annual runoff : update and reassessment ''. Journal of Hydrology. 295 ( 1 -- 4 ) : 185 -- 197. Bibcode : 2004JHyd... 295... 185P. doi : 10.1016 / j. jhydrol. 2004.03. 004. Jump up ^ This section uses a slightly modified version of the Köppen system found in The Times Atlas of the World, 7th edition. ISBN 0 - 7230 - 0265 - 7 Jump up ^ Crocket, Christopher ( 5 September 2015 ). `` Quest to trace origin of Earth 's water is ' a complete mess ' ''. Science News. Retrieved 1 October 2015. Jump up ^ Melissa Davey ( 12 Jun 2014 ). `` Earth may have underground ' ocean ' three times that on surface ''. The Guardian. Retrieved 13 Mar 2015. Jump up ^ `` Earth found hiding huge reservoirs of water 400 miles below... but not water as we know it : SCIENCE : Tech Times ''. Tech Times. 16 June 1015. Retrieved 13 October 2015. Jump up ^ Ben Harder ( 7 Mar 2002 ). `` Inner Earth May Hold More Water Than the Seas ''. National Geographic. Retrieved 13 Mar 2015. ^ Jump up to : Becky Oskin ( 12 Mar 2014 ). `` Rare Diamond Confirms That Earth 's Mantle Holds an Ocean 's Worth of Water ''. Scientific American. Retrieved 13 Mar 2015. Jump up ^ HENRY FOUNTAIN ( 6 Jun 2014 ). `` The Earth 's Hidden Ocean ''. New York Times. Retrieved 13 Mar 2015. hide Water Overviews Outline Data Model Properties States Liquid Ice Vapor Steam Forms Deuterium - depleted Semiheavy Heavy Tritiated Hydronium On Earth Cycle Distribution Hydrosphere Hydrology Hydrobiology Origin Pollution Resources management policy Supply Portal Commons Wiktionary Retrieved from `` https://en.wikipedia.org/w/index.php?title=Water_distribution_on_Earth&oldid=840712594 '' Categories : Water and the environment Earth Hidden categories : Wikipedia introduction cleanup from May 2018 All pages needing cleanup Articles covered by WikiProject Wikify from May 2018 All articles covered by WikiProject Wikify Talk Contents About Wikipedia Español فارسی Italiano Edit links This page was last edited on 11 May 2018, at 17 : 24. Text is available under the Creative Commons Attribution - ShareAlike License ; additional terms may apply. By using this site, you agree to the Terms of Use and Privacy Policy. 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Question: 19. the majority of fresh water on our planet comes from
Answer: lakes