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The Water Cycle Must Have This Type of Energy to Continue

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Continuous movement of water on, above and below the surface of the Earth

Diagram of the water cycle

The water cycle, also known as the hydrologic cycle or the hydrological cycle, is a biogeochemical cycle that describes the continuous movement of water on, above and below the surface of the Earth. The mass of water on Earth remains fairly constant over time but the partitioning of the water into the major reservoirs of ice, fresh water, saline water (salt water) and atmospheric water is variable depending on a wide range of climatic variables. The water moves from one reservoir to another, such as from river to ocean, or from the ocean to the atmosphere, by the physical processes of evaporation, transpiration, condensation, precipitation, infiltration, surface runoff, and subsurface flow. In doing so, the water goes through different forms: liquid, solid (ice) and vapor. The ocean plays a key role in the water cycle as it is the source of 86% of global evaporation.[1]

The water cycle involves the exchange of energy, which leads to temperature changes. When water evaporates, it takes up energy from its surroundings and cools the environment. When it condenses, it releases energy and warms the environment. These heat exchanges influence climate.

The evaporative phase of the cycle purifies water which then replenishes the land with freshwater. The flow of liquid water and ice transports minerals across the globe. It is also involved in reshaping the geological features of the Earth, through processes including erosion and sedimentation. The water cycle is also essential for the maintenance of most life and ecosystems on the planet.

Description

Diagram of the water cycle

Video of the Earth's water cycle (NASA)[2]

Overall process

The water cycle is powered from the energy emitted by the sun. This energy heats water in the ocean and seas. Water evaporates as water vapor into the air. Some ice and snow sublimates directly into water vapor. Evapotranspiration is water transpired from plants and evaporated from the soil. The water molecule H
2 O has smaller molecular mass than the major components of the atmosphere, nitrogen (N
2 ) and oxygen (O
2 ) and hence is less dense. Due to the significant difference in density, buoyancy drives humid air higher. As altitude increases, air pressure decreases and the temperature drops (see Gas laws). The lower temperature causes water vapor to condense into tiny liquid water droplets which are heavier than the air, and which fall unless supported by an updraft. A huge concentration of these droplets over a large area in the atmosphere become visible as cloud, while condensation near ground level is referred to as fog.

Atmospheric circulation moves water vapor around the globe; cloud particles collide, grow, and fall out of the upper atmospheric layers as precipitation. Some precipitation falls as snow, hail, or sleet, and can accumulate in ice caps and glaciers, which can store frozen water for thousands of years. Most water falls as rain back into the ocean or onto land, where the water flows over the ground as surface runoff. A portion of this runoff enters rivers, with streamflow moving water towards the oceans. Runoff and water emerging from the ground (groundwater) may be stored as freshwater in lakes. Not all runoff flows into rivers; much of it soaks into the ground as infiltration. Some water infiltrates deep into the ground and replenishes aquifers, which can store freshwater for long periods of time. Some infiltration stays close to the land surface and can seep back into surface-water bodies (and the ocean) as groundwater discharge. Some groundwater finds openings in the land surface and emerges as freshwater springs. In river valleys and floodplains, there is often continuous water exchange between surface water and ground water in the hyporheic zone. Over time, the water returns to the ocean, to continue the water cycle.

The ocean plays a key role in the water cycle. The ocean holds "97% of the total water on the planet; 78% of global precipitation occurs over the ocean, and it is the source of 86% of global evaporation".[1]

Physical processes

Processes leading to movements and phase changes in water

The water cycle involves the following processes:

Advection
The movement of water through the atmosphere.[3] Without advection, water that evaporated over the oceans could not precipitate over land. Atmospheric rivers that move large volumes of water vapor over long distances are an example of advection.[4]
Canopy interception
The precipitation that is intercepted by plant foliage eventually evaporates back to the atmosphere rather than falling to the ground.
Condensation
The transformation of water vapor to liquid water droplets in the air, creating clouds and fog.[5]
Deposition
This refers to changing of water vapor directly to ice.
Evaporation
The transformation of water from liquid to gas phases as it moves from the ground or bodies of water into the overlying atmosphere.[6] The source of energy for evaporation is primarily solar radiation. Evaporation often implicitly includes transpiration from plants, though together they are specifically referred to as evapotranspiration. Total annual evapotranspiration amounts to approximately 505,000 km3 (121,000 cu mi) of water, 434,000 km3 (104,000 cu mi) of which evaporates from the oceans.[7] 86% of global evaporation occurs over the ocean.[8]
Infiltration
The flow of water from the ground surface into the ground. Once infiltrated, the water becomes soil moisture or groundwater.[9] A recent global study using water stable isotopes, however, shows that not all soil moisture is equally available for groundwater recharge or for plant transpiration.[10]
Percolation
Water flows vertically through the soil and rocks under the influence of gravity.
Precipitation
Condensed water vapor that falls to the Earth's surface. Most precipitation occurs as rain, but also includes snow, hail, fog drip, graupel, and sleet.[11] Approximately 505,000 km3 (121,000 cu mi) of water falls as precipitation each year, 398,000 km3 (95,000 cu mi) of it over the oceans.[7] [12] The rain on land contains 107,000 km3 (26,000 cu mi) of water per year and a snowing only 1,000 km3 (240 cu mi).[12] 78% of global precipitation occurs over the ocean.[8]
Runoff
The variety of ways by which water moves across the land. This includes both surface runoff and channel runoff. As it flows, the water may seep into the ground, evaporate into the air, become stored in lakes or reservoirs, or be extracted for agricultural or other human uses.
Snow melt
The runoff produced by melting snow.
Sublimation
The state change directly from solid water (snow or ice) to water vapor by passing the liquid state.[13]
Subsurface flow
The flow of water underground, in the vadose zone and aquifers. Subsurface water may return to the surface (e.g. as a spring or by being pumped) or eventually seep into the oceans. Water returns to the land surface at lower elevation than where it infiltrated, under the force of gravity or gravity induced pressures. Groundwater tends to move slowly and is replenished slowly, so it can remain in aquifers for thousands of years.
Transpiration
The release of water vapor from plants and soil into the air.

Residence times

Average reservoir residence times [14]
Reservoir Average residence time
Antarctica 20,000 years
Oceans 3,200 years
Glaciers 20 to 100 years
Seasonal snow cover 2 to 6 months
Soil moisture 1 to 2 months
Groundwater: shallow 100 to 200 years
Groundwater: deep 10,000 years
Lakes (see lake retention time) 50 to 100 years
Rivers 2 to 6 months
Atmosphere 9 days

The residence time of a reservoir within the hydrologic cycle is the average time a water molecule will spend in that reservoir (see adjacent table). It is a measure of the average age of the water in that reservoir.

Groundwater can spend over 10,000 years beneath Earth's surface before leaving. Particularly old groundwater is called fossil water. Water stored in the soil remains there very briefly, because it is spread thinly across the Earth, and is readily lost by evaporation, transpiration, stream flow, or groundwater recharge. After evaporating, the residence time in the atmosphere is about 9 days before condensing and falling to the Earth as precipitation.

The major ice sheets – Antarctica and Greenland – store ice for very long periods. Ice from Antarctica has been reliably dated to 800,000 years before present, though the average residence time is shorter.[15]

In hydrology, residence times can be estimated in two ways.[ citation needed ] The more common method relies on the principle of conservation of mass (water balance) and assumes the amount of water in a given reservoir is roughly constant. With this method, residence times are estimated by dividing the volume of the reservoir by the rate by which water either enters or exits the reservoir. Conceptually, this is equivalent to timing how long it would take the reservoir to become filled from empty if no water were to leave (or how long it would take the reservoir to empty from full if no water were to enter).

An alternative method to estimate residence times, which is gaining in popularity for dating groundwater, is the use of isotopic techniques. This is done in the subfield of isotope hydrology.

Water in storage

The water cycle describes the processes that drive the movement of water throughout the hydrosphere. However, much more water is "in storage" for long periods of time than is actually moving through the cycle. The storehouses for the vast majority of all water on Earth are the oceans. It is estimated that of the 1,386,000,000 km3 of the world's water supply, about 1,338,000,000 km3 is stored in oceans, or about 97%. It is also estimated that the oceans supply about 90% of the evaporated water that goes into the water cycle.[16] The Earth's ice caps, glaciers, and permanent snowpack stores another 24,064,000 km3 accounting for only 1.7% of the planet's total water volume. However, this quantity of water is 68.7% of all freshwater on the planet.[17]

Changes caused by humans

Water cycle intensification due to climate change

Extreme weather will be progressively more common as the Earth warms.[18] : Figure SPM.6

The sixth IPCC Assessment Report projects changes in average soil moisture that can disrupt agriculture and ecosystems. A reduction in soil moisture by one standard deviation means that average soil moisture will approximately match the ninth driest year between 1850 and 1900 at that location.

Since the middle of the 20th century, human-caused climate change has resulted in observable changes in the global water cycle.[19] : 85 The IPCC Sixth Assessment Report in 2021 predicted that these changes will continue to grow significantly at the global and regional level.[19] : 85 These findings are a continuation of scientific consensus expressed in the IPCC Fifth Assessment Report from 2007 and other special reports by the Intergovernmental Panel on Climate Change which had already stated that the water cycle will continue to "intensify" throughout the 21st century.[20]

Glacial retreat is also an example of a changing water cycle, where the supply of water to glaciers from precipitation cannot keep up with the loss of water from melting and sublimation. Glacial retreat since 1850 due to global warming has been extensive.[21] : 1273

Changes due to other human activities

Water cycle showing human influences and major pools and fluxes.[22]

Human activities, other than those that lead to global warming from greenhouse gas emissions, can also alter the water cycle. The IPCC Sixth Assessment Report stated that there is "abundant evidence that changes in land use and land cover alter the water cycle globally, regionally and locally, by changing precipitation, evaporation, flooding, groundwater, and the availability of freshwater for a variety of uses".[23] : 1153

Examples for such land use changes are converting fields to urban areas or clearing forests. Such changes can affect the ability of soils to soak up surface water. Deforestation can also "directly reduce soil moisture, evaporation and rainfall locally but can also cause regional temperature changes that affect rainfall patterns".[23] : 1153 Aquifer drawdown or overdrafting and the pumping of fossil water increases the total amount of water in the hydrosphere because water that was "previously in the ground is now in direct contact with the atmosphere, being available for evaporation".[23] : 1153

Biogeochemical cycling

While the water cycle is itself a biogeochemical cycle, flow of water over and beneath the Earth is a key component of the cycling of other biogeochemicals.[24] Runoff is responsible for almost all of the transport of eroded sediment and phosphorus from land to waterbodies.[25] The salinity of the oceans is derived from erosion and transport of dissolved salts from the land. Cultural eutrophication of lakes is primarily due to phosphorus, applied in excess to agricultural fields in fertilizers, and then transported overland and down rivers. Both runoff and groundwater flow play significant roles in transporting nitrogen from the land to waterbodies.[26] The dead zone at the outlet of the Mississippi River is a consequence of nitrates from fertilizer being carried off agricultural fields and funnelled down the river system to the Gulf of Mexico. Runoff also plays a part in the carbon cycle, again through the transport of eroded rock and soil.[27]

Slow loss over geologic time

The hydrodynamic wind within the upper portion of a planet's atmosphere allows light chemical elements such as Hydrogen to move up to the exobase, the lower limit of the exosphere, where the gases can then reach escape velocity, entering outer space without impacting other particles of gas. This type of gas loss from a planet into space is known as planetary wind.[28] Planets with hot lower atmospheres could result in humid upper atmospheres that accelerate the loss of hydrogen.[29]

Historical interpretations

Floating land mass

In ancient times, it was widely thought that the land mass floated on a body of water, and that most of the water in rivers has its origin under the earth. Examples of this belief can be found in the works of Homer (circa 800 BCE).

Hebrew Bible

In the ancient Near East, Hebrew scholars observed that even though the rivers ran into the sea, the sea never became full. Some scholars conclude that the water cycle was described completely during this time in this passage: "The wind goeth toward the south, and turneth about unto the north; it whirleth about continually, and the wind returneth again according to its circuits. All the rivers run into the sea, yet the sea is not full; unto the place from whence the rivers come, thither they return again" (Ecclesiastes 1:6-7).[30] Scholars are not in agreement as to the date of Ecclesiastes, though most scholars point to a date during the time of King Solomon, son of David and Bathsheba, "three thousand years ago,[30] there is some agreement that the time period is 962–922 BCE.[31] Furthermore, it was also observed that when the clouds were full, they emptied rain on the earth (Ecclesiastes 11:3). In addition, during 793–740 BCE a Hebrew prophet, Amos, stated that water comes from the sea and is poured out on the earth (Amos 5:8).[32]

In the Biblical Book of Job, dated between 7th and 2nd centuries BCE,[31] there is a description of precipitation in the hydrologic cycle,[30] "For he maketh small the drops of water: they pour down rain according to the vapour thereof; which the clouds do drop and distil upon man abundantly" (Job 36:27-28).

Understanding of precipitation and percolation

In the Adityahridayam (a devotional hymn to the Sun God) of Ramayana, a Hindu epic dated to the 4th century BCE, it is mentioned in the 22nd verse that the Sun heats up water and sends it down as rain. By roughly 500 BCE, Greek scholars were speculating that much of the water in rivers can be attributed to rain. The origin of rain was also known by then. These scholars maintained the belief, however, that water rising up through the earth contributed a great deal to rivers. Examples of this thinking included Anaximander (570 BCE) (who also speculated about the evolution of land animals from fish[33]) and Xenophanes of Colophon (530 BCE).[34] Chinese scholars such as Chi Ni Tzu (320 BCE) and Lu Shih Ch'un Ch'iu (239 BCE) had similar thoughts.[35]

The idea that the water cycle is a closed cycle can be found in the works of Anaxagoras of Clazomenae (460 BCE) and Diogenes of Apollonia (460 BCE). Both Plato (390 BCE) and Aristotle (350 BCE) speculated about percolation as part of the water cycle. Aristotle correctly hypothesized that the sun played a role in the Earth's hydraulic cycle in his book Meteorology, writing "By it [the sun's] agency the finest and sweetest water is everyday carried up and is dissolved into vapor and rises to the upper regions, where it is condensed again by the cold and so returns to the earth.", and believed that clouds were composed of cooled and condensed water vapor.[36] [37]

Up to the time of the Renaissance, it was wrongly assumed that precipitation alone was insufficient to feed rivers, for a complete water cycle, and that underground water pushing upwards from the oceans were the main contributors to river water. Bartholomew of England held this view (1240 CE), as did Leonardo da Vinci (1500 CE) and Athanasius Kircher (1644 CE).

Discovery of the correct theory

The first published thinker to assert that rainfall alone was sufficient for the maintenance of rivers was Bernard Palissy (1580 CE), who is often credited as the "discoverer" of the modern theory of the water cycle. Palissy's theories were not tested scientifically until 1674, in a study commonly attributed to Pierre Perrault. Even then, these beliefs were not accepted in mainstream science until the early nineteenth century.[38]

See also

  • Bioprecipitation
  • Deep water cycle – Movement of water in the deep Earth
  • Ecohydrology
  • Global meteoric water line
  • Moisture advection
  • Moisture recycling
  • Planetary boundaries – Limits not to be exceeded if humanity wants to survive in a safe ecosystem
  • Water resources – Sources of water that are potentially useful

References

  1. ^ a b "Water Cycle | Science Mission Directorate". science.nasa.gov. Archived from the original on 2018-01-15. Retrieved 2018-01-15 .
  2. ^ NASA (2012-01-12). "NASA Viz: The Water Cycle: Following The Water". svs.gsfc.nasa.gov . Retrieved 2022-09-28 .
  3. ^ "advection". National Snow and Ice Data Center. Archived from the original on 2018-01-16. Retrieved 2018-01-15 .
  4. ^ "Atmospheric River Information Page". NOAA Earth System Research Laboratory.
  5. ^ "condensation". National Snow and Ice Data Center. Archived from the original on 2018-01-16. Retrieved 2018-01-15 .
  6. ^ "evaporation". National Snow and Ice Data Center. Archived from the original on 2018-01-16. Retrieved 2018-01-15 .
  7. ^ a b "The Water Cycle". Dr. Art's Guide to Planet Earth. Archived from the original on 2011-12-26. Retrieved 2006-10-24 . {{cite web}}: CS1 maint: unfit URL (link)
  8. ^ a b "Salinity | Science Mission Directorate". science.nasa.gov. Archived from the original on 2018-01-15. Retrieved 2018-01-15 .
  9. ^ "Hydrologic Cycle". Northwest River Forecast Center. NOAA. Archived from the original on 2006-04-27. Retrieved 2006-10-24 .
  10. ^ Evaristo, Jaivime; Jasechko, Scott; McDonnell, Jeffrey J. (September 2015). "Global separation of plant transpiration from groundwater and streamflow". Nature. 525 (7567): 91–94. Bibcode:2015Natur.525...91E. doi:10.1038/nature14983. PMID 26333467. S2CID 4467297.
  11. ^ "precipitation". National Snow and Ice Data Center. Archived from the original on 2018-01-16. Retrieved 2018-01-15 .
  12. ^ a b "Estimated Flows of Water in the Global Water Cycle". www3.geosc.psu.edu. Archived from the original on 2017-11-07. Retrieved 2018-01-15 .
  13. ^ "sublimation". National Snow and Ice Data Center. Archived from the original on 2018-01-16. Retrieved 2018-01-15 .
  14. ^ "Chapter 8: Introduction to the Hydrosphere". 8(b) the Hydrologic Cycle. PhysicalGeography.net. Archived from the original on 2016-01-26. Retrieved 2006-10-24 .
  15. ^ Jouzel, J.; Masson-Delmotte, V.; Cattani, O.; Dreyfus, G.; Falourd, S.; Hoffmann, G.; Minster, B.; Nouet, J.; Barnola, J. M.; Chappellaz, J.; Fischer, H.; Gallet, J. C.; Johnsen, S.; Leuenberger, M.; Loulergue, L.; Luethi, D.; Oerter, H.; Parrenin, F.; Raisbeck, G.; Raynaud, D.; Schilt, A.; Schwander, J.; Selmo, E.; Souchez, R.; Spahni, R.; Stauffer, B.; Steffensen, J. P.; Stenni, B.; Stocker, T. F.; Tison, J. L.; Werner, M.; Wolff, E. W. (10 August 2007). "Orbital and Millennial Antarctic Climate Variability over the Past 800,000 Years" (PDF). Science. 317 (5839): 793–796. Bibcode:2007Sci...317..793J. doi:10.1126/science.1141038. PMID 17615306. S2CID 30125808.
  16. ^ "The Water Cycle summary". USGS Water Science School. Archived from the original on 2018-01-16. Retrieved 2018-01-15 .
  17. ^ Water Science School. "Ice, Snow, and Glaciers and the Water Cycle". USGS. US Department of the Interior. Retrieved October 17, 2022.
  18. ^ IPCC, 2021: Summary for Policymakers. In: Climate Change 2021: The Physical Science Basis. Contribution of Working Group I to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change [Masson-Delmotte, V., P. Zhai, A. Pirani, S.L. Connors, C. Péan, S. Berger, N. Caud, Y. Chen, L. Goldfarb, M.I. Gomis, M. Huang, K. Leitzell, E. Lonnoy, J.B.R. Matthews, T.K. Maycock, T. Waterfield, O. Yelekçi, R. Yu, and B. Zhou (eds.)]. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA, pp. 3−32, doi:10.1017/9781009157896.001.
  19. ^ a b Arias, P.A., N. Bellouin, E. Coppola, R.G. Jones, G. Krinner, J. Marotzke, V. Naik, M.D. Palmer, G.-K. Plattner, J. Rogelj, M. Rojas, J. Sillmann, T. Storelvmo, P.W. Thorne, B. Trewin, K. Achuta Rao, B. Adhikary, R.P. Allan, K. Armour, G. Bala, R. Barimalala, S. Berger, J.G. Canadell, C. Cassou, A. Cherchi, W. Collins, W.D. Collins, S.L. Connors, S. Corti, F. Cruz, F.J. Dentener, C. Dereczynski, A. Di Luca, A. Diongue Niang, F.J. Doblas-Reyes, A. Dosio, H. Douville, F. Engelbrecht, V.  Eyring, E. Fischer, P. Forster, B. Fox-Kemper, J.S. Fuglestvedt, J.C. Fyfe, et al., 2021: Technical Summary. In Climate Change 2021: The Physical Science Basis. Contribution of Working Group I to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change [Masson-Delmotte, V., P. Zhai, A. Pirani, S.L. Connors, C. Péan, S. Berger, N. Caud, Y. Chen, L. Goldfarb, M.I. Gomis, M. Huang, K. Leitzell, E. Lonnoy, J.B.R. Matthews, T.K. Maycock, T. Waterfield, O. Yelekçi, R. Yu, and B. Zhou (eds.)]. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA, pp. 33−144. doi:10.1017/9781009157896.002.
  20. ^ Alley, Richard; et al. (February 2007). "Climate Change 2007: The Physical Science Basis" (PDF). International Panel on Climate Change. Archived from the original (PDF) on February 3, 2007.
  21. ^ Fox-Kemper, B., H.T. Hewitt, C. Xiao, G. Aðalgeirsdóttir, S.S. Drijfhout, T.L. Edwards, N.R. Golledge, M. Hemer, R.E. Kopp, G.  Krinner, A. Mix, D. Notz, S. Nowicki, I.S. Nurhati, L. Ruiz, J.-B. Sallée, A.B.A. Slangen, and Y. Yu, 2021: Ocean, Cryosphere and Sea Level Change. In Climate Change 2021: The Physical Science Basis. Contribution of Working Group I to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change [Masson-Delmotte, V., P. Zhai, A. Pirani, S.L.  Connors, C. Péan, S. Berger, N. Caud, Y. Chen, L. Goldfarb, M.I. Gomis, M. Huang, K. Leitzell, E. Lonnoy, J.B.R. Matthews, T.K. Maycock, T. Waterfield, O. Yelekçi, R. Yu, and B. Zhou (eds.)]. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA, pp. 1211–1362
  22. ^ Abbott, Benjamin W.; Bishop, Kevin; Zarnetske, Jay P.; Minaudo, Camille; Chapin, F. S.; Krause, Stefan; Hannah, David M.; Conner, Lafe; Ellison, David; Godsey, Sarah E.; Plont, Stephen; Marçais, Jean; Kolbe, Tamara; Huebner, Amanda; Frei, Rebecca J. (2019). "Human domination of the global water cycle absent from depictions and perceptions" (PDF). Nature Geoscience. 12 (7): 533–540. doi:10.1038/s41561-019-0374-y. ISSN 1752-0894.
  23. ^ a b c Douville, H., K. Raghavan, J. Renwick, R.P. Allan, P.A. Arias, M. Barlow, R. Cerezo-Mota, A. Cherchi, T.Y. Gan, J. Gergis, D.  Jiang, A.  Khan, W.  Pokam Mba, D.  Rosenfeld, J. Tierney, and O.  Zolina, 2021: Water Cycle Changes. In Climate Change 2021: The Physical Science Basis. Contribution of Working Group I  to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change [Masson-Delmotte, V., P. Zhai, A. Pirani, S.L. Connors, C. Péan, S. Berger, N. Caud, Y. Chen, L. Goldfarb, M.I. Gomis, M. Huang, K. Leitzell, E. Lonnoy, J.B.R. Matthews, T.K. Maycock, T. Waterfield, O. Yelekçi, R. Yu, and B. Zhou (eds.)]. Cambridge University Press, Cambridge, United Kingdom and New York, NY, USA, pp. 1055–1210, doi:10.1017/9781009157896.010.
  24. ^ "Biogeochemical Cycles". The Environmental Literacy Council. Archived from the original on 2015-04-30. Retrieved 2006-10-24 .
  25. ^ "Phosphorus Cycle". The Environmental Literacy Council. Archived from the original on 2016-08-20. Retrieved 2018-01-15 .
  26. ^ "Nitrogen and the Hydrologic Cycle". Extension Fact Sheet. Ohio State University. Archived from the original on 2006-09-01. Retrieved 2006-10-24 .
  27. ^ "The Carbon Cycle". Earth Observatory. NASA. 2011-06-16. Archived from the original on 2006-09-28. Retrieved 2006-10-24 .
  28. ^ Nick Strobel (June 12, 2010). "Planetary Science". Archived from the original on September 17, 2010. Retrieved September 28, 2010.
  29. ^ Rudolf Dvořák (2007). Extrasolar Planets. Wiley-VCH. pp. 139–40. ISBN978-3-527-40671-5 . Retrieved 2009-05-05 .
  30. ^ a b c Morris, Henry M. (1988). Science and the Bible (Trinity Broadcasting Network ed.). Chicago, IL: Moody Press. p. 15.
  31. ^ a b Metzger, Bruce M.; Coogan, Michael D. (1993). The Oxford Companion to the Bible . New York, NY: Oxford University Press. pp. 369. ISBN978-0195046458.
  32. ^ Merrill, Eugene H.; Rooker, Mark F.; Grisanti, Michael A. (2011). The World and the Word. Nashville, TN: B&H Academic. p. 430. ISBN 9780805440317.
  33. ^ Kazlev, M.Alan. "Palaeos: History of Evolution and Paleontology in science, philosophy, religion, and popular culture : Pre 19th Century". Archived from the original on 2014-03-02.
  34. ^ James H. Lesher. "Xenophanes' Scepticism" (PDF). pp. 9–10. Archived from the original (PDF) on 2013-07-28. Retrieved 2014-02-26 .
  35. ^ The Basis of Civilization – water Science?. International Association of Hydrological Science. 2004. ISBN9781901502572 – via Google Books.
  36. ^ Roscoe, Kelly (2015). Aristotle: The Father of Logic. Rosen Publishing Group. p. 70. ISBN9781499461275.
  37. ^ Precipitation: Theory, Measurement and Distributio. Cambridge University Press. 2006. p. 7. ISBN9781139460019.
  38. ^ James C.I. Dodge. Concepts of the hydrological Cycle. Ancient and modern (PDF). International Symposium OH
    2     'Origins and History of Hydrology', Dijon, May 9–11, 2001. Archived (PDF) from the original on 2014-10-11. Retrieved 2014-02-26 .

External links

  • The Water Cycle, United States Geological Survey
  • The Water Cycle for Kids, United States Geological Survey
  • The Water Cycle: Following The Water (NASA Visualization Explorer with videos)

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Source: https://en.wikipedia.org/wiki/Water_cycle

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