Essentials of OceanographyRevised for increased readability, this full-colour text offers an insightful, ecologically-sensitive presentation of the relationship of scientific principles to ocean phenomena. Now better suited for non-major oceanography courses, this edition offers a broader study with a marked reduction in concentrated topic coverage, with a continued emphasis on how we must take more precautions in activities that can modify the environment and learn how to keep these modifications to a minimum. |
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Page 156
... gyres ro- tate in the reverse direction of the adjacent subtropical gyres . ( After Sverdrup et al . , 1942. ) A. Path of ideal geostrophic flow Path of actual geostrophic. 0 ° only by a continuing supply of oxygen . This oxygen is ...
... gyres ro- tate in the reverse direction of the adjacent subtropical gyres . ( After Sverdrup et al . , 1942. ) A. Path of ideal geostrophic flow Path of actual geostrophic. 0 ° only by a continuing supply of oxygen . This oxygen is ...
Page 158
... gyre . Water lit- erally piles up in the center of the subtropical gyre . We find within all such ocean gyres a hill of water that rises as much as 2 meters ( about 6.5 feet ) above the water level at the margins of the gyres . As Ekman ...
... gyre . Water lit- erally piles up in the center of the subtropical gyre . We find within all such ocean gyres a hill of water that rises as much as 2 meters ( about 6.5 feet ) above the water level at the margins of the gyres . As Ekman ...
Page 162
... gyres . The North and South Atlantic Gyres The North Atlantic gyre rotates clockwise and the South Atlantic gyre rotates counterclockwise , in response to the Coriolis effect . As stated , both rotations are driven by the trade winds ...
... gyres . The North and South Atlantic Gyres The North Atlantic gyre rotates clockwise and the South Atlantic gyre rotates counterclockwise , in response to the Coriolis effect . As stated , both rotations are driven by the trade winds ...
Contents
CHAPTER | 5 |
The RossesSounders of the Deep | 11 |
Law of the | 22 |
Copyright | |
31 other sections not shown
Common terms and phrases
air mass algae animals Antarctic areas Atlantic Ocean atmosphere bacteria barrier beach benthic biological bottom carbon cells centimeters chemosynthesis circulation coast coastal concentration continental shelf continental slope continents coral Coriolis effect currents deep deep-ocean density deposits depth developed Earth environment equator equatorial erosion estuary feeding feet Figure fish flow Gulf gyres heat energy Hemisphere high tide hydrogen hydrothermal vents increases islands kilometers latitudes layer lithosphere marine meters miles million moon move North Atlantic nutrients occur ocean basins ocean floor ocean surface ocean water oceanic crust oceanic ridges Oceanography open ocean organisms oxygen Pacific Ocean particles percent Photo photosynthesis phytoplankton plankton plants plate plate tectonics polar produce radiation reef regions rise rocks salinity sand sea level seafloor seawater sediment shore shoreline slope solar South species subtropical surface water tectonics temperature thermocline tide zone tion trenches tropical vapor volcanic warm water molecules wavelength waves whales wind