By Weilin W. Hou
ISBN-10: 0819496316
ISBN-13: 9780819496317
This is often an introductory textual content that provides the main optical ocean sensing ideas. it really is compatible for pros and bosses in comparable disciplines, in addition to scholars who're attracted to exploring profession paths in distant sensing of the sea or ocean engineering.
The ebook begins with a quick review of the most branches of ocean learn, together with actual, chemical, organic, and geological oceanography, in addition to biogeochemistry. the elemental optical houses of the sea are awarded subsequent, through underwater and distant sensing subject matters, similar to diver visibility; lively underwater imaging innovations and comparability to sonars; ocean colour distant sensing concept and algorithms; lidar concepts in bathymetry, chlorophyll, temperature, and subsurface layer explorations; microwave sensing of floor gains together with sea floor peak, roughness, temperature, sea ice, salinity and wind; in addition to infrared sensing of the ocean floor temperature.
structures and instrumentation also are one of the issues of debate, from learn vessels to unmanned underwater and aerial cars, moorings and floats, and observatories. built-in strategies and destiny sensing wishes are touched directly to wrap up the textual content. a good portion of the ebook depends upon sketches and illustrations to show principles, even supposing rigorous derivations are sometimes used while worthy.
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Additional info for Ocean Sensing and Monitoring: Optics and Other Methods (SPIE Press Tutorial Text TT98)
Example text
It is caused by the rotation of the earth. , an astronaut in space observing Earth), it is an odd concept to grasp for an observer within the rotational system (someone on Earth), the concept being that things tend to turn right if you live on the Northern Hemisphere, and left on the Southern Hemisphere, as if there is a force pushing them. This is called the Coriolis force. A simple example can be seen in Fig. 3. For the observer inside the rotating coordinates (on the surface of the earth), it is not obvious.
G. (1976). Marine Optics, Amsterdam: Elsevier. “Oceanic ridges,” Cambridge Encyclopedia (2005). Thurman, H. V. (1996). Introductory Oceanography, 5th ed. Upper Saddle River: Prentice-Hall. Oceanography Overview 19 Additional Reading Martin, S. (2004). An Introduction to Ocean Remote Sensing. Cambridge: Cambridge University Press. Miller, C. B. (2004). Biological Oceanography. New York: John Wiley and Sons. Pond, S. and Pickard, G. (1983). Introductory Dynamical Oceanography, 2nd ed. Oxford: Pergamon Press.
Due to the vast volume of the ocean, it has an almost unlimited capacity to absorb carbon dioxide as part of the chemical process (Cambridge Encyclopedia, 2005). Unfortunately, the rate of carbon dioxide absorbed by Oceanography Overview 17 the oceans is limited by the rate of exchange of surface water with the deeper ocean; once the surface water has been saturated with carbon dioxide, it can no longer absorb it. The deeper water has less carbon dioxide and thus can absorb more. In short, the rate of carbon dioxide absorption depends on the time it takes surface water to mix with the deeper layers of ocean water.
Ocean Sensing and Monitoring: Optics and Other Methods (SPIE Press Tutorial Text TT98) by Weilin W. Hou
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