19998051 Hydrological Cycle

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    Hydrological Cycle

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    The Hydrologic Cycle

    (Water Cycle)

    The path water takes as it circulates from

    the land to the sky and back again. Water

    is recycled this way so we do not run out.So every time you get a drink of water

    remember you are drinking the same

    water the dinosaurs drank.

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    Parts of the hydrologic cycle

    Evaporation

    Condensation

    Precipitation

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    Evaporation

    Evaporation is when

    the sun heats up

    water in rivers or

    lakes or the oceanand turns it into

    vapor or steam. The

    water vapor or

    steam leaves theriver, lake or ocean

    and goes into the

    air.

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    Evapotranspiration

    Evaporation often implicityincludes transpiration fromplants, though togather theyare specifically refered to asEvapotranspiration. Herewater given off through thepores of plants and animals

    joins the atmosphere as avapor.

    Annual Evapotranspirationamounts approximately =505,000 km of water

    From the ocean = 434,000

    km.

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    Condensation

    Water vapor inthe air gets coldand changesback into liquid,formingclouds. This is

    calledcondensation.

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    Precipitation

    Precipitation occurs whenso much water has

    accumulated that the aircannot hold itanymore. The clouds get

    heavy and water falls backto the earth in the form ofrain, hail, sleet or snow.

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    Run-off When the precipitation

    reaches the ground, severalthings can happen to it. First,it might be re-evaporated.For instance, we have all

    seen the mist rising off hotroads after a summershower.

    If it isnt re-evaporated,

    much of the water willbecome RUNOFF that goesinto streams, lakes andrivers as it flows back to the

    ocean.

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    Infiltration

    Some of the precipitation willbe absorbed into the ground.

    This is called INFILTRATION.

    Once in the ground, the water

    can join the earths groundwater supply.

    This is one of the worlds

    largest store house of water.

    The water could also be

    absorbed from the ground by

    the roots of plants.

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    Reservoirs

    The largest reservoir is the collection of

    oceans, accounting for 97% of the Earths

    water. The next largest quantity(2%) is stored

    in solid form in ice caps and glaciers.

    The small amount accounts for

    approximately(75%) of all fresh water reserves

    on the planet. The water contained within allliving organisms represents the smallest

    reservoir

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    Volume of water stored in the water

    cycle reservoirs

    Reservoir Volume of water(106km

    Percent of total%

    Oceans 1370 97.25%

    Icecaps,glaciers 29 2.05%Ground water 9.5 0.68%

    Lakes 0.125 0.01%

    Soil moisture 0.625 0.005%Atmosphere 0.013 0.001%

    Streams&rivers 0.0017 0.0001%

    Biosphere 0.0006 0.00004%

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    Residence times

    The residence time of a reservoir within the

    Hydrological cycle is the average time awater molecule will spend in that reservoir.

    It is a measure of the average age of thewater in that reservoir, though some water

    will spend much less time than average, and

    some much more.

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    Average reservoir residence times

    Reservoir Avg residence time

    Oceans 3,200 years

    Glaciers 20100 years

    Seasonal snow cover 2-6 months

    Soil moisture 1-2 months

    Ground water-shallow 100-200 years

    Ground water-deep 10,000 years

    Lakes 50-100 years

    Rivers 2-6 months

    Atmosphere 9 days

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    Effects on climate

    The water cycle is powered from solarenergy.

    86% of the global evaporation occurs from

    the oceans, reducing their temperature byevaporative cooling.

    Without the cooling effect of evaporation the

    green house effect would lead to a muchhigher surface temperature of 67c, and a

    warmer planet

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    Effects on Biogeochemical cycling

    While the water cycle itself a biogeochemicalcycle, flow of water over and beneath the

    Earth is a key component of the cycling of

    other biogeochemical Runoff is responsible

    for almost all of the transport of eroded

    sediment and phosphorus from land to water

    bodies.

    The salinity of oceans is derived fromerosion and transport of dissolved salts from

    the land.

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    Agriculture

    Industry waste

    Alteration of the chemical composition of the

    atmosphere

    Construction of dams

    Deforestation and Afforestation

    Removal of ground water from wells

    Dont alter the

    water cycle

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    Cont

    Water abstraction from rivers

    Urbanization

    Contributing to climate change

    Withdrawing large amount of fresh water

    Clearing Vegetation and underground water

    Polluting surface and underground water

    Precipitation changes worldwideGlaciers melt-loss of water source

    Over population

    Wild fires accelerate several cycles

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    Discussions

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