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 85
Page 21
... tion , the structure of the deep Protoearth is thought to have been homogenous producing ) , = ( homo alike , genous = which means that it had a uniform com- position throughout . The structure of Pro- toearth changed , however , when ...
... tion , the structure of the deep Protoearth is thought to have been homogenous producing ) , = ( homo alike , genous = which means that it had a uniform com- position throughout . The structure of Pro- toearth changed , however , when ...
Page 142
... tion and condensation removes huge amounts of heat energy from the low - latitude oceans and adds huge amounts of heat energy to the heat - deficient higher latitudes . In addition , the heat released when sea ice forms further moder ...
... tion and condensation removes huge amounts of heat energy from the low - latitude oceans and adds huge amounts of heat energy to the heat - deficient higher latitudes . In addition , the heat released when sea ice forms further moder ...
Page 366
... tion in 1866 , and was a multimillionaire by age 40. Agassiz was a friend of Charles Wyville Thomson of the Challenger Expedition ( see Chapter 5 ) , and his successor Sir John Murray , who helped prepare the reports from the voy- age ...
... tion in 1866 , and was a multimillionaire by age 40. Agassiz was a friend of Charles Wyville Thomson of the Challenger Expedition ( see Chapter 5 ) , and his successor Sir John Murray , who helped prepare the reports from the voy- age ...
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