Essentials of Oceanography"How do the oceans work?" To help readers find the answers, Trujillo and Thurman present & in-depth and rigorous discussions of oceanographic concepts and demystify the science for the layperson. Highlights the interdisciplinary relationship between oceanographic phenomena and how those phenomena affect other Earth systems. Incorporates scientific information from geology, chemistry, physics, and biology to illustrate how each of these disciplines relates to the ocean. Updates content throughout to include some of the most recent developments in oceanography, such as the recent Indian Ocean tsunamis and Hurricanes Katrina, Rita, and Wilma. A readable, informative reference for anyone interested in learning more about our oceans. |
From inside the book
Results 1-3 of 83
Page 216
... move in slightly different directions at slightly different speeds . It is too weak to create ed- dies or whirlpools ( vortexes ) at the surface and so presents no danger to ships . In fact , the Ekman spiral is unnoticeable at the ...
... move in slightly different directions at slightly different speeds . It is too weak to create ed- dies or whirlpools ( vortexes ) at the surface and so presents no danger to ships . In fact , the Ekman spiral is unnoticeable at the ...
Page 249
... Move ? Waves are energy in motion . Waves transmit energy by means of cyclic move- ment through matter . The medium itself ( solid , liquid , or gas ) does not actually travel in the direction of the energy that is passing through it ...
... Move ? Waves are energy in motion . Waves transmit energy by means of cyclic move- ment through matter . The medium itself ( solid , liquid , or gas ) does not actually travel in the direction of the energy that is passing through it ...
Page 250
... move in circular orbits . Thus , waves at the ocean surface are orbital waves ( also called interface waves ) . 8.3 ... move back and forth in direction of energy transmission . These waves transmit energy through all states of matter ...
... move in circular orbits . Thus , waves at the ocean surface are orbital waves ( also called interface waves ) . 8.3 ... move back and forth in direction of energy transmission . These waves transmit energy through all states of matter ...
Contents
I | 3 |
Introduction to Planet Earth | 6 |
Visiting the Deep Ocean Floor | 11 |
Copyright | |
59 other sections not shown
Other editions - View all
Essentials of Oceanography, Eighth Edition: Student Lecture Notebook Alan P. Trujillo,Harold V. Thurman No preview available - 2005 |
Common terms and phrases
algae Antarctic Arctic areas asthenosphere Atlantic Ocean atmosphere atoms beach biogenous called caused chemical coast coastal continents coral Coriolis effect crust deep density deposits depth dissolved drift Earth El Niño energy environment equator equatorial feet Figure fish flow Gulf heat hydrogen hydrothermal vents increases Indian Ocean islands kilometers land latitudes layer lithogenous lithosphere magnetic manganese nodules marine meters mid-ocean ridge miles million Moon move Niño North Atlantic Northern Hemisphere nutrients occur ocean basins ocean floor ocean surface Oceanography ooze organisms oxygen Pacific Ocean particles pattern photosynthesis plankton plate boundaries plate tectonics polar pressure produce pycnocline reef regions rocks salinity sand Scientific American sea floor spreading sea ice sea level seawater sediment shore shoreline slope solar South species Students Sometimes Ask subduction subtropical gyres surface currents surface water temperature thermocline tidal tide tion transform faults Trench tropical tsunami upwelling volcanic warm water molecules waves whales zone