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Titlebook: IUTAM Symposium on Turbulence in the Atmosphere and Oceans; Proceedings of the I David Dritschel Conference proceedings 2010 Springer Scien

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書(shū)目名稱(chēng)IUTAM Symposium on Turbulence in the Atmosphere and Oceans
副標(biāo)題Proceedings of the I
編輯David Dritschel
視頻videohttp://file.papertrans.cn/461/460647/460647.mp4
概述IUTAM symposia are state of the art in their field;.New fundamental insight into the mechanisms shaping planetary circulations..Includes supplementary material:
叢書(shū)名稱(chēng)IUTAM Bookseries
圖書(shū)封面Titlebook: IUTAM Symposium on Turbulence in the Atmosphere and Oceans; Proceedings of the I David Dritschel Conference proceedings 2010 Springer Scien
描述The text of the Persian poet Rum ˉ ˉ ?, written some eight centuries ago, and reproduced at the beginning of this book is still relevant to many of our pursuits of knowledge, not least of turbulence. The text illustrates the inability people have in seeing the whole thing, the ‘big picture’. Everybody looks into the problem from his/her vi- point, and that leads to disagreement and controversy. If we could see the whole thing, our understanding would become complete and there would be no cont- versy. The turbulent motion of the atmosphere and oceans, at the heart of the observed general circulation, is undoubtedly very complex and dif?cult to understand in its entirety. Even ‘bare’ turbulence, without rotation and strati?cation whose effects are paramount in the atmosphere and oceans, still poses great fundamental ch- lenges for understanding after a century of research. Rotating strati?ed turbulence is a relatively new research topic. It is also far richer, exhibiting a host of distinct wave types interacting in a complicated and often subtle way with long-lived - herent structures such as jets or currents and vortices. All of this is tied together by basic ?uid-dynamical nonlinea
出版日期Conference proceedings 2010
關(guān)鍵詞Dynamics; Ocean; Scale; Tide; algorithms; atmosphere; convection; magnetohydrodynamics; modeling; spheric; flu
版次1
doihttps://doi.org/10.1007/978-94-007-0360-5
isbn_softcover978-94-007-3459-3
isbn_ebook978-94-007-0360-5Series ISSN 1875-3507 Series E-ISSN 1875-3493
issn_series 1875-3507
copyrightSpringer Science+Business Media B.V. 2010
The information of publication is updating

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On spontaneous imbalance and ocean turbulence: generalizations of the Paparella–Young epsilon theorem can now be proved for fairly realistic equations of state that include thermobaric effects, and nonlinearity in both temperature and salinity. The restriction to Boussinesq flow can also be lifted. The increased realism comes at some cost in terms of weakening the constraint on .. The constraint i
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Deep ocean mixing by near-inertial wavesng in the areas where the Richardson number is less than 1/4 and neglecting the relaxation and turbulent diffusion at the boundaries of the mixed region we find the domain of mixed fluid created by the chosen wave packet. The mixing changes the basic stratification in such a way that in the modified
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IUTAM Symposium on Turbulence in the Atmosphere and OceansProceedings of the I
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