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Titlebook: Ocean Waves Breaking and Marine Aerosol Fluxes; Stanis?aw R. Massel Book 2007 Springer-Verlag New York 2007 Aerosol.Dissipation.Ocean.Scal

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發(fā)表于 2025-3-21 17:50:31 | 只看該作者 |倒序瀏覽 |閱讀模式
書目名稱Ocean Waves Breaking and Marine Aerosol Fluxes
編輯Stanis?aw R. Massel
視頻videohttp://file.papertrans.cn/701/700513/700513.mp4
概述Bridges the gap between generalized texts and specialized texts on oceanography.First ocean wave title to specifically focus on wave breaking phenomenon.Can be used as a textbook for graduate students
叢書名稱Atmospheric and Oceanographic Sciences Library
圖書封面Titlebook: Ocean Waves Breaking and Marine Aerosol Fluxes;  Stanis?aw R. Massel Book 2007 Springer-Verlag New York 2007 Aerosol.Dissipation.Ocean.Scal
描述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 generate
出版日期Book 2007
關鍵詞Aerosol; Dissipation; Ocean; Scale; Wind; Wind speed; marine; remote sensing; air pollution and air quality;
版次1
doihttps://doi.org/10.1007/978-0-387-69092-6
isbn_softcover978-1-4419-2269-4
isbn_ebook978-0-387-69092-6Series ISSN 1383-8601 Series E-ISSN 2215-162X
issn_series 1383-8601
copyrightSpringer-Verlag New York 2007
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Mechanics of steep and breaking waves, basic wave parameters, the shape of wave profile can vary, from very gentle to very steep. However, the steepening of the wave profile is not unlimited and for some wave parameters waves lose their stability and break. As in this book we are focusing on the wave breaking, it is quite appropriate to
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Whitecap coverage of the sea surface,med when large numbers of bubbles produced by a wave rise to the surface, and the bright white area of a whitecap arises from multiple light scattering by elements of size comparable to or greater than the wavelength of visible light. These elements are clusters of proximate, closely packed bubbles
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Fundamentals of marine aerosols,er particles and large ions. These constituents can be both natural and anthropogenic, such as liquid seawater drops, dry sea salt particles, dust transport from the deserts by wind, as well as particles resulting from human activities related to industrial processes and agriculture, volcanic erupti
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