Page 298 - (DK) The Ultimate Visual Dictionary 2nd Ed.
P. 298

GEOLOGY, GEOGRAPHY, AND METEOROLOGY
       Oceans and seas                                                                 SURFACE CURRENTS


                                                                                                     GREENWICH
                                                                       180°
                                                                          160°
                                                                                                      MERIDIAN
                                                                                 120°
                                                                                      80°
       OCEANS AND SEAS COVER ABOUT 70 PERCENT of the Earth’s                                   40°      0°
       surface and account for about 97 percent of its total
       water. These oceans and seas play a crucial role in                                  East  Greenlan d   Curr ent
       regulating temperature variations and
       determining climate. Their waters absorb          Al a s k a  Cu r r e n t      L a bra d or  Current
       heat from the Sun, especially in tropical   North Pa ci fi c  Current              North   Atlantic Current
       regions, and the surface currents distribute
       it around the Earth, warming overlying                                Flor ida  Cu rr ent
       air masses and neighboring land in             PA C IFIC                    Gulf  Stream  Ca n a ri es  Cu rre nt
                                                      NO RTH
                                                       GYRE                             NO RTH
       winter and cooling them in summer.                                               ATL ANTIC
                                                                                         GYRE
       The oceans are never still. Differences   North  Equatoria l  Cu rren t      Nor th  E quatoria l  Curre nt
       in temperature and salinity drive
                                                       E qu a t o ri al  C ou n t er c ur re nt
       deep current systems, while surface                                      S o u th  E q u a t o r i a l  Cu r r e n t  Equ a to ri al
                                                                                                 Countercurr en t
       currents are generated by winds                 S o ut h  E qu a t o ri a l  C urr e n t
       blowing over the oceans. All currents
       are deflected—to the right in the                                 Per u  C u r r e nt
       Northern Hemisphere, to the left in                                                 Br a z il  Cu rr en t  Ben g u el a  Cu r r ent
       the Southern Hemisphere—as a result                                                     ATLANTI C
                                                                                                SOUTH
       of the Earth’s rotation. This deflective                                                  GYRE
       factor is known as the Coriolis force.               SOUTH          Hum b old t  Cur r ent
                                                            PA CIFIC
       A current that begins on the surface is              GYRE                     Falkla nd  Current
       immediately deflected. This current in
       turn generates a current in the layer of water
       beneath, which is also deflected. As the movement   An t a r ct i c  C ir c um p o l ar  C u rr en t
       is transmitted downward, the deflections form an
       Ekman spiral. The waters of the oceans and seas are
       also moved by the constant ebb and flow of tides. These
       are caused by the gravitational pull of the Moon and Sun.                       80°      40°     0°
                                                                                 120°
       The highest tides (Spring tides) occur at full and new Moon;     180°  160°                   GREENWICH
                                                                                                      MERIDIAN
       the lowest tides (neap tides) occur at first and last quarter.
                                                                                     OFFSHORE CURRENTS
            SALT CONTENT OF SEAWATER     Surface   Wind drives   Cold-water   Surface       Pack-ice formation
                                         ocean   water along   upwelling     ocean          increases water
                             Others      current  coast      replaces warm   current        salinity and density
          Potassium          1.9%                            surface water
             1.1%
                             Calcium
         Magnesium           1.2%
             3.7%
                              Sulfate
                              7.6%
            Sodium
             30.2%



                             Chloride
                             54.3%

                                                      Continental slope      Cold, dense      Continental
                                                                             water sinks      slope
                                             COLD-WATER UPWELLING
                                             (SOUTHERN HEMISPHERE)                POLAR BOTTOM WATER

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