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contributor authorSasaki, Y. K.
contributor authorChang, L. P.
date accessioned2017-06-09T16:05:18Z
date available2017-06-09T16:05:18Z
date copyright1985/05/01
date issued1985
identifier issn0027-0644
identifier otherams-60635.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4201327
description abstractIn a diagnostic study by expanding global data in normal mode functions, Kasahara and Puri found that for zonal wavenumber one, even the seventh vertical mode (the highest mode they presented) contains about 50% of the energy of the external mode. The vertical normal modes are eigensolutions of the vertical structure equation, and each mode is associated with well?defined physical significance. Consequently, it is of interest to look into the accuracy of representation of, say, the first ten vertical modes in a discretized model because seriously misrepresented normal mode functions may not be able to honestly express the physics embedded in the data to be expanded. Along this line, a systematic method of obtaining matching eigensolutions of the vertical structure equation of a multilayered stratified atmosphere was developed. The resultant eigensolutions were used to investigate the influence of the upper boundary condition, the judicious method of the vertical grid levels and the relative accuracy of a finite?difference and a finite?element method in obtaining the discretized vertical normal mode functions. An important conclusion of this study is that in a discretized model, an inadequate grid resolution in the upper domain may result in considerable misrepresentation of the vertical structure functions even in the lower part of the domain for vertical modes higher than mode 5.
publisherAmerican Meteorological Society
titleNumerical Solution of the Vertical Structure Equation in the Normal Mode Method
typeJournal Paper
journal volume113
journal issue5
journal titleMonthly Weather Review
identifier doi10.1175/1520-0493(1985)113<0782:NSOTVS>2.0.CO;2
journal fristpage782
journal lastpage793
treeMonthly Weather Review:;1985:;volume( 113 ):;issue: 005
contenttypeFulltext


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