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 153
... temperature , salinity , and pressure , in the following ways . • As temperature increases , density decreases 16 ( due to thermal expansion ) . • As salinity increases , density increases ( due to the addition of more dissolved ...
... temperature , salinity , and pressure , in the following ways . • As temperature increases , density decreases 16 ( due to thermal expansion ) . • As salinity increases , density increases ( due to the addition of more dissolved ...
Page 154
... temperature and salinity . Blue curves show density , which increases with increasing salinity and decreases with increasing temperature . In high- latitude areas of cold water , temperature has less effect on density than in high - ...
... temperature and salinity . Blue curves show density , which increases with increasing salinity and decreases with increasing temperature . In high- latitude areas of cold water , temperature has less effect on density than in high - ...
Page 370
... Temperature has an even greater effect , with lower temperatures creating higher - viscosity seawater . As a result of this temperature relationship , phyto- plankton and animals that float in colder waters have less need for extensions ...
... Temperature has an even greater effect , with lower temperatures creating higher - viscosity seawater . As a result of this temperature relationship , phyto- plankton and animals that float in colder waters have less need for extensions ...
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