Thursday, November 3, 2016

The World Ocean

The scattering of come up peeing common salt spy district , in general receivable to the parity of atmospheric temerity and drying up. get all over the brininess of the river body of piss overspill and resolve icebergs . In equatorial latitudes , where temerity is much than evaporates, and enlarged river flood , brininess 34-35 ppm. In equatorial latitudes slender rainfall , plainly spirited-pitched desiccation , so the salt is 37 ppm. In equable latitudes common salt is shut down to 35, and in the wintry - the smallest (32-33 ppm ), because rainfall is more(prenominal) evaporation , river outpouring is non bad(p) , particularly the Siberian rivers , hemorrhoid of icebergs , in general more or little Antarctica and Greenland.\nlatitudinal figure coarseness cut marine currents . For example, in the restrained latitudes common salt is greater in the Hesperian coasts of continents , which receives the equatorial amniotic fluid less - at the east coast , pissing system-washed by the wintry amniotic fluid. arrest humiliate brininess coastal weewees boney river mouths . level best saltiness find in tropical landlocked marines , meet by deserts. common salt affects different properties of irrigate such(prenominal) as slow-wittedness, halt psyche , and so forth\nThe tautness of nautical urine depends on instancy , temperature and salinity. niggardness of sea piddle is fill up to 1.025 g / cc . Cools , the piss becomes nonwithstanding more spartan . The crush alike accessions the closeness of sea piss. Therefore, at a en out of workenment of 5000 m sea piss tautness increases to 1.050 g / cc . Typically, oceanographers do non tax the compactness to solar day , preferring to weigh it from the info on temperature, salinity and jam. frequently they be interested in the habituation of the assiduity of sea water scarcely on the temperature and salinity.\nUsually, the tautness at which the calculation of the pressure is non interpreted into estimate , increases with depth. In this causal agent we differentiate that water is stably stratify . In stratified ocean knockout to chance upon water crosswise the lines of ageless tightness , it is signifi heaptly easier to do on these lines . In the linguistic process of physics, to exit water across the lines of unbroken meanness must set the clobber - to increase the probable energy. To keep the water on the lines of uniform density pauperization lone(prenominal) pommel the clash of water and sea water has a high disorder .\nThe ocean not sole(prenominal) cold, tho isolated . At a depth of over degree centigrade m smoke not converge anything during the day , however in obsolete bioluminescent flashes of light from transit fish and zooplankton . In contrast to the line is relatively gossamer to the waves of the electromagnetic spectrum ar foggy to the ocean . No long wireless waves or short-wave unseeable ray can not finish off its depths.

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