Overview

The atmosphere and the ocean form a coupled system which exchanges heat, momentum and water at the air–sea interface. The interface is dynamic and masses and energy are continually transferred across the air–sea interface. The energy ?ow from the atmosphere to the ocean generates an aerodynamically rough sea surface. If the energy ?ow is su?ciently intense, at some points the surface waves will lose their stability and eventually break. Breaking is a very localized and non-stationary phenomenon that is a source of vorticity and turbulence. Dissipated energy becomes available for mixing the water layers and for whitecapping of various scales. Whitecapping is a strongly nonlinear process, which involves instability of the surface waves with space and time scales several orders of magnitude smaller than those associated with gravity wave motion. Whitecaps are usually formed at or near the crests of the larger waves and occur in groups with successive crests breaking downwind of one another. Wave breaking is the dominant generator of the ‘primary’ marine aerosol (sea salt) and it is a major factor in the air–sea exchange of gases (including carbon dioxide). Most of the aerosol generated from natural waters is in the form of jet and ?lm drops from the bursting of air bubbles (Monahan and Van Patten, 1989). The enriched aerosols associated with the ejected droplets are very - portant in maintaining a source of salt-laden cloud condensation nuclei as well asinterfacial?uxesoftraceconstituents,includingbacteria,viruses,heavym- als, radioactivity and organic material (Kerman, 1986).

Full Product Details

Author:   Stanislaw R. Massel
Publisher:   Springer-Verlag New York Inc.
Imprint:   Springer-Verlag New York Inc.
Edition:   Softcover reprint of hardcover 1st ed. 2007
Volume:   38
Dimensions:   Width: 15.50cm , Height: 1.80cm , Length: 23.50cm
Weight:   0.528kg
ISBN:  

9781441922694

ISBN 10:   1441922695
Pages:   316
Publication Date:   23 November 2010
Audience:   Professional and scholarly ,  Professional & Vocational ,  Postgraduate, Research & Scholarly
Format:   Paperback
Publisher's Status:   Active
Availability:   Out of print, replaced by POD  
We will order this item for you from a manufatured on demand supplier.

Table of Contents

Basic processes near the air—sea interface.- Mechanics of steep and breaking waves.- Spectral and statistical properties of ocean waves.- Experimental insights into mechanisms of wave breaking.- Wave breaking criteria and probability of breaking.- Energy dissipation due to wave breaking.- Whitecap coverage of the sea surface.- Fundamentals of marine aerosols.- Marine aerosol fluxes.- Aerosol flux as a function of sea state parameters.- Seasonal dependence of aerosol fluxes in the Baltic Sea.

Reviews

"From the reviews: ""Massel’s new book describes how to model wave breaking and continues on to show how to use breaking wave models to estimate the production rate of the sea-salt aerosol at the ocean’s surface. … I like the production quality of this book. It has a comfortable size, pleasing font style and size, and sufficient white space to make for easy reading or scanning. The many figures are uniformly styled and formatted … . valuable reference text for researchers studying air–sea interaction and marine aerosols."" (Edgar L Andreas, Bulletin of the American Meteorological Society, March, 2009)"

From the reviews: Massel's new book describes how to model wave breaking and continues on to show how to use breaking wave models to estimate the production rate of the sea-salt aerosol at the ocean's surface. ! I like the production quality of this book. It has a comfortable size, pleasing font style and size, and sufficient white space to make for easy reading or scanning. The many figures are uniformly styled and formatted ! . valuable reference text for researchers studying air--sea interaction and marine aerosols. (Edgar L Andreas, Bulletin of the American Meteorological Society, March, 2009)

Author Information

Stanislaw Massel is currently a professor and the Director of the Institute of Oceanology in Sopot Poland.

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