Seasonal and Interannual Variabilities of Vertical Eddy Diffusivity
Observed by the MU Radar

Manabu D. Yamanaka, Satoshi Kurosaki, Shoichiro Fukao, H. Hashiguchi, Toshitaka Tsuda and Susumu Kato
Radio Atmospheric Science Center, Kyoto University, Uji, Kyoto 611, Japan


Advances in Space Research , Vol. 14 , No.9, pp.(9)277-(9)280.

Paper No. C.2-S.2.10 presented at a symposium entitled ``The Middle Atmosphere: Its Energetics, Chemistry and Dynamics and Coupling to Regions Above and Below'' in the 29th COSPAR Plenary Meeting, the World Space Congress, Washington D.C., USA, 28 August-5 September 1992.
First draft: February, 1992;
Submitted: August 1993, Accepted: September 1993
Published: September, 1994


ABSTRACT , CONTENTS , CORRECTIONS , FIGURES , REFERENCES , CITATIONS


Abstract
The vertical eddy diffusivity in the troposphere, lower stratosphere and mesosphere has been observed by the MU radar every month since January 1986. Semiannual variations are dominantly detected in the mesosphere. Annual variations with maxima in winter dominates in the lower stratosphere, while annual maxima in the mesosphere exist in summer. Quasi-biennial variabilities are also analyzed. These observational results are interpreted by the gravity-wave breaking theory.


Contents
Introduction
MU Radar Observations
Seasonal Variability
Interannual Variability
Theoretical Interpretation
Conclusions


Corrections and Additional Remarks
Fukao et al. (1992) was published as Fukao et al. (1994) cited below.


List of Figures (no tables)


References (Updated after publication)
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