A method for determination of internal gravity wave parameters from a vertical temperature or density profile measurement in the Earth’s atmosphere |
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Authors: | V N Gubenko A G Pavelyev R R Salimzyanov V E Andreev |
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Institution: | 1.Kotelnikov Institute of Radio Engineering and Electronics,Russian Academy of Sciences,Fryazino, Moscow oblast,Russia |
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Abstract: | A method for determination of internal gravity wave (IGW) parameters from a single vertical temperature or density profile
measurement in the Earth’s atmosphere has been developed. This method may be used for the analysis of profiles measured by
any techniques in which the accuracy is enough to measure small (∼1%) amplitudes of the temperature or density fluctuations
in the atmosphere. The criterion for the IGW identification has been formulated and argued. In the case when this criterion
is satisfied then analyzed fluctuations can be considered as wave-induced. The method is based upon the analysis of relative
amplitude thresholds of the temperature or density wave field and upon linear IGW saturation theory in which amplitude thresholds
are restricted by dynamical instability processes in the atmosphere. In order to approbate the method we have used data of
simultaneous radiosonde measurements of the temperature and wind velocity in the Earth’s stratosphere where the saturated
IGW propagation has been detected. It is shown that the application of the method to radio occultation temperature data gives
the possibility to identify IGWs in the Earth’s lower stratosphere and to determine values of key wave parameters. |
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