Oscillations in atmospheres with tops
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In this article, the authors compared free and forced oscillations of infinite and bounded atmospheres and found that bounded atmosphere can reproduce the free oscillations with accuracy that depends on top height.Abstract:
Free and forced oscillations are compared for infinite and bounded atmospheres. Both continuous and two layer bounded atmospheres are considered. It is found that bounded atmospheres reproduce the free oscillations of the infinite atmosphere with accuracy that depends on top height—they, however, also introduce spurious free oscillations. In studying forced oscillations, the spurious oscillations of bounded atmospheres appear as spurious resonances. In general, bounded atmospheres do not properly respond to oscillations that propagate vertically.read more
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An introduction to dynamic meteorology
TL;DR: The instructor's manual to a work which introduces the fundamental principles of meteorology, explaining storm dynamics and the dynamics of climate and its global implications is described in this paper, where the authors present a detailed discussion of the relationship between meteorology and climate.
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Atmospheric Modeling, Data Assimilation and Predictability
TL;DR: A comprehensive text and reference work on numerical weather prediction, first published in 2002, covers not only methods for numerical modeling, but also the important related areas of data assimilation and predictability.
Book
An introduction to dynamic meteorology
TL;DR: The instructor's manual to a work which introduces the fundamental principles of meteorology, explaining storm dynamics and the dynamics of climate and its global implications is described in this paper, where the authors present a detailed discussion of the relationship between meteorology and climate.
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Survey of planetary-scale traveling waves: the state of theory and observations
TL;DR: In this paper, the gravest-scale transient components of planetary wave activity (periods shorter than a couple of weeks) are linked to the eigenmodes of an unbounded isothermal atmosphere in uniform rotation.
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Introduction to the SPARC Reanalysis Intercomparison Project (S-RIP) and overview of the reanalysis systems
Masatomo Fujiwara,Jonathon S. Wright,Gloria L. Manney,Lesley J. Gray,James Anstey,Thomas Birner,Sean M. Davis,Sean M. Davis,Edwin P. Gerber,V. Lynn Harvey,Michaela I. Hegglin,Cameron R. Homeyer,John A. Knox,Kirstin Krüger,Alyn Lambert,Craig S. Long,Patrick Martineau,Andrea Molod,B. M. Monge-Sanz,Michelle L. Santee,Susann Tegtmeier,Simon Chabrillat,David G. H. Tan,David Jackson,Saroja Polavarapu,Gilbert P. Compo,Gilbert P. Compo,Rossana Dragani,Wesley Ebisuzaki,Yayoi Harada,Chiaki Kobayashi,Will McCarty,Kazutoshi Onogi,Steven Pawson,Adrian Simmons,Krzysztof Wargan,Jeffrey S. Whitaker,Cheng Zhi Zou +37 more
TL;DR: The Stratosphere-troposphere Processes And their Role in Climate (SPARC) Reanalysis Intercomparison Project (S-RIP) is a coordinated activity to compare reanalysis data sets using a variety of key diagnostics.
References
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Journal ArticleDOI
Planetary waves on beta-planes
TL;DR: In this paper, the problem of linearized oscillations of the gaseous envelope of a rotating sphere (with periods in excess of a day) is considered using the β-plane approximation.
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