Breaking Ocean Waves: Geometry, Structure and Remote Sensing

ISBN-13: 9783540298274 / Angielski / Twarda / 2007 / 278 str.

Eugene A. Sharkov

Opis

Eugene Sharkov, of the Space Research Institute in Moscow, has here put together the most comprehensive description of the physical findings of an investigation into the spatio-temporal characteristics of the gravity of breaking waves. He s also described the foam activity in the open sea using methods and instruments of optical and microwave remote sensing. Numerous practical applications and illustrations are provided from air-borne, ship-borne and laboratory up-to-date experiments."

Spis treści

1. Introduction.- 2. Random wave breaking fields in atmosphere-ocean system.- 3. Linear and two-dimensional geometry of whitecappings and foam structures.- 4. Life-time of breakings.- 5. Sea drop-spray clouds.- 6. Electrodynamics of close packed media.- 7. Electrodynamics of concentrated drop flows.- 8. Field optical, infrared and microwave remote sensing of air-sea transition zone in the atmosphere-ocean system.

Blurb

This book represents the most comprehensive description of the physical findings of an investigation into the spatio-temporal characteristics of the gravity of breaking waves and the foam activity in open sea by methods and instruments of optical and microwave remote sensing.

The study of physical and electrodynamics' properties of the gravity wave breaking processes and the foam spatio-temporal activity is an important facet of satellite oceanography, ocean engineering, air-sea interaction and ocean remote sensing. In particular, the contribution of foam formations of various types to the mean and the spatio-temporal variations of radio emission, back-scattering, IR and optical parameters of the disturbed sea surface is highly significant. The statistical characteristics of wave breaking and attendant foam forming are very important to ocean wave dynamics. The study and measurement of spatio-temporal characteristics of wave breaking and sea foam formations are of fundamental importance in ocean remote sensing.

Much emphasis is placed on the physical aspects of breaking processes necessary to measure the possibilities and limitations of remote sensing methods in specific observation cases of an oceanic surface. Numerous practical applications and illustrations are provided from air-borne, ship-borne and laboratory up-to-date experiments.