Titlebook: Mesoscale Meteorology - Theories, Observations and Models; Douglas K. Lilly,Tzvi Gal-Chen Book 1983 Springer Science+Business Media B.V. 1

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Initialization of Mesoscale Models: The Possible Impact of Remotely Sensed Data and radiation, be replaced by their discrete analogues. Regardless of the specific method of discretization, there is an explicit or implicit requirement that the initial conditions be specified at grid points which are often different than “observation points”.

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A Review of Meso-Scale Disturbances in Cold Air Masses years different modes of formation, including haro-clinic instability and CISK have been suggested in order to explain these phenomena. The paper gives a general overview of what is known about these systems, including some as yet un-published work.

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漂亮

Frontogenesis During the November 15, 1980 Storm of STREXork has been done in quantifying frontogenesis in such situations. Also, multiple frontal penetrations by instrumented aircraft allow accurate quantification of the frontogenetic processes above the surface.

Choreography

Symmetric Instabilitybility is one of only a very few instabilities which are known to have distinctly mesoscale characteristics. The physical nature of the instability and the conditions under which it may occur are described in this chapter.

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Conditional Symmetric Instability: A Theory for Rainbands within Extratropical Cyclonesatures are clearly associated with frontal circulations, others occur away from fronts and thus appear to require different theoretical explanations. A number of such theories are here reviewed with particular emphasis on the theory of symmetric instability, and a case study of a band possibly associated with symmetric instability is presented.

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