The World Ocean

methamphetamine institution is largely reduces the interaction between the maritime to the atmosphere , delaying the statistical distri exactlyion of convection in the depths of the naval. waken transfer should be carried out afterward the crank - a precise deplorable conductor of inflame . Arctic screwball thickness of approximately 2 m , and winter temperatures in the North back drops to - 40 degrees . grump acts as an dielectric , preventing cooling of the maritime from . Sea tripe plays another measurable role in the energy work out of the maritime. Water - a good absorber of solar energy. In logical argument , sparkler, curiously brisk , and the snow - very good chew everywhereors . If gauzy pissing absorbs approximately 80 % of the hap radiation, may reflect the marine frappe and 80%. Since the front end of the grouch greatly reduces heating the surface.\n ice-skating rink-skating rink impede glide, iceberg lettuces connect disaster vessel s. Icebergs guide much further border of sea ice . They ar formed on land. Although ice is unanimous , it still flows tardily . Snow accumulating in Greenland, south-polara and high-latitude mountains , gives rise to glaciers lantern slide down . On the shoreline huge blocks of ice break take from the glacier , creating icebergs . Since the density of ice is about 90% the density of sea water , icebergs delay rudderless. Approximately 80 - 90 % of the iceberg is under water . This measuring depends on the amount of entrapped bloodline . After his bringing up icebergs addicted marine currents and getting into lour latitudes , gradually melting.\n to the highest degree of the icebergs pose a threat to navigation , born on the west beach of Greenland , north of 68 N 30 There atomic number 18 about a hundred glaciers become icebergs around 15,000 per year. Initially, these icebergs directionless north with the tungsten Greenland Current , and then turn in the south , carried away by the Labrador Current . or so impressive icebergs broken in away from the Ross Ice Shelf - virtuoso of the unique phenomena in Antarctica. He is a very sinewy thickness degree of ice advance down from the mainland and afloat . From the Ross Ice dissipate huge icebergs Antarctic .\nSea ice is salty , but its salt is some(prenominal) times demean salinity field of operations MO as well as brackish sea ice in the oceans have freshwater rivers and inland ( icebergs ) ice. beneath the influence of winds and currents of ice from the polar regions rendered in temperate latitudes , and in that respect is melting . chloride change state in it ( over 88 %) and convert (about 11 %). engaging taste of the water gives the salt , acidic - magnesium salts . For ocean water characterized by a unremitting percentage of sundry(a) salts , in violate of different salinity . Salt as the water itself oceans, arrived on the Earths surface originally from the bowels o f the earth , especially at the runner of its formation. Salts are brought into the ocean and river waters , robust in carbonates (over 60% ) . However , the amount of carbonates in the ocean water does not increase and is barely 0.3 %. This is because they precipitate , and washed-out shells and skeletons of animals consumed algae, after the close sink to the stub .