Essentials of OceanographyRevised for increased readability and streamlined for clarity, this text is designed to accompany an introductory college-level course in oceanography. This insightful, ecologically sensitive presentation of the relationship of scientific principles to ocean phenomena is made even more relevant to a new generation of teachers and students by pairing new co-author Alan Trujillo with renowned author Harold V. Thurman. *NEW - A new coauthor: - With Thurman's retirement from teaching, Alan Trujillo of Palomar College has been added as co-author for this edition. Alan's ideas and approach will help make this edition as relevant to a new generation of teachers and students as previous editions were to Thurman's contemporaries. *NEW - Changes in chapter organization: - A new Chapter 1, Introduction to Planet Earth, replaces the old Chapter 1 (History of Oceanography). The historical perspective is now included as chapter-opening feature boxes which highlight important events in oceanographic history relevant to chapter-specific material. - New placement of the chapter on plate tectonics (switched with the chapter on sea floor features) ensures that the processes of plate tectonics can be |
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Page 183
... winds Horse latitudes 30 % High High High High High Prevailing westerlies Low Polar front 60 ° Low Low Polar easterlies High Low 111 Figure 6-11 Atmospheric circulation and wind belts of the world . The wind belts of the world are ...
... winds Horse latitudes 30 % High High High High High Prevailing westerlies Low Polar front 60 ° Low Low Polar easterlies High Low 111 Figure 6-11 Atmospheric circulation and wind belts of the world . The wind belts of the world are ...
Page 184
... belts toward the equatorial low - pressure belt constitute the trade winds . These steady winds are named from the ... wind belts . These air masses rise over the dense , cold air moving away from the polar high - pressure caps at the ...
... belts toward the equatorial low - pressure belt constitute the trade winds . These steady winds are named from the ... wind belts . These air masses rise over the dense , cold air moving away from the polar high - pressure caps at the ...
Page 202
... wind belt ( p . 184 ) Polar front ( p . 184 ) Polar high ( p . 183 ) Prevailing westerly wind belt ( p . 184 ) Sea ... Belts of low pressure , where air rises , are generally found at the Equator and at about 60 degrees latitude . The ...
... wind belt ( p . 184 ) Polar front ( p . 184 ) Polar high ( p . 183 ) Prevailing westerly wind belt ( p . 184 ) Sea ... Belts of low pressure , where air rises , are generally found at the Equator and at about 60 degrees latitude . The ...
Contents
Rational Use of Technology? | 3 |
Some Historical Notes | 9 |
Origins | 17 |
Copyright | |
47 other sections not shown
Common terms and phrases
abyssal abyssal plains algae animals Antarctic areas Atlantic Ocean atmosphere beach benthic boundary called carbon caused cells centimeters coast coastal continental continents coral reefs Coriolis effect crust currents deep degrees centigrade density deposits depth diatoms dissolved Earth energy ENSO environment Equator equatorial estuary feet Figure fish flow Gulf gyres heat high tide hydrogen hydrothermal vents increase islands kilometers land latitude layer lithogenous lithosphere longshore magnetic marine mass meters mid-ocean ridge miles million moon move Northern Hemisphere nutrients occur ocean basins ocean floor ocean surface ocean water Oceanography ooze open ocean organisms oxygen Pacific Ocean particles percent Photo photosynthesis phytoplankton plankton plate tectonics polar produce pycnocline regions rock salinity sand sea floor sea level seawater sediment ship shore shoreline slope solar South species surface water temperature thermocline tidal tion transform faults tropical tsunami upwelling vapor volcanic warm water molecules wavelength waves whales wind zone