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contributor authorBrowning, G. L.
contributor authorKreiss, H-O.
contributor authorvan de Kamp, D. W.
date accessioned2017-06-09T14:36:00Z
date available2017-06-09T14:36:00Z
date copyright2000/02/01
date issued2000
identifier issn0022-4928
identifier otherams-22546.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4159008
description abstractRecently, a mathematical theory has been developed that proves that there are two main components of the solution of the forced dynamical system that describes a mesoscale storm driven by cooling and heating processes. The component that contains most of the energy of the solution (and is therefore called the dominant component) satisfies a simple nonlinear system devoid of gravity and sound waves. The residual component of the solution satisfies a forced gravity wave equation and essentially does not interact with the dominant component. The mathematical theory also provides information about the amplitude, wavelength, and period of the gravity waves. In the paper entitled ?Comments on ?Use of ducting theory in an observed case of gravity waves,?? Dr. F. M. Ralph has claimed that the new gravity wave theory is not consistent with profiler observations of vertical velocity in his earlier paper entitled ?Observations of a mesoscale ducted gravity wave.? Here it is shown that the new theory is completely consistent with profilers that have documented error bounds on the vertical velocity measurements. In the case that the new theory is claimed to be inconsistent with observational data, the data were obtained from a profiler with undocumented accuracy of the vertical velocity measurements in the precipitating case, and the two components of the solution were not properly separated.
publisherAmerican Meteorological Society
titleComments on “Observations of a Mesoscale Ducted Gravity Wave”
typeJournal Paper
journal volume57
journal issue4
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(2000)057<0595:COOOAM>2.0.CO;2
journal fristpage595
journal lastpage598
treeJournal of the Atmospheric Sciences:;2000:;Volume( 057 ):;issue: 004
contenttypeFulltext


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