Vertical Eddy Diffusivity in the Lower and Middle Atmosphere:
A Climatology Based on the MU Radar Observations during 1986-1992

Satoshi Kurosaki, Manabu D. Yamanaka, Hiroyuki Hashiguchi,
Radio Atmospheric Science Center, Kyoto University, Uji, Kyoto 611, Japan

Toru Sato
Department of Electrical Engineering II, Kyoto University, Sakyo, Kyoto 606, Japan

and Shoichiro Fukao
Radio Atmospheric Science Center, Kyoto University, Uji, Kyoto 611, Japan


Journal of Atmospheric and Terrestrial Physics , Vol. 58 , No.6, pp.727-734.

Extended from Paper GW-6 (Original title: Meteorological Processes and Troposphere-Stratosphere Interactions Revealed by MST Radar Techniques) presented at the Workshop on Dynamics and Coupling of Ionosphere, Middle and Lower Atmosphere in the 26th URSI General Assembly, Kyoto, Japan, 1 September 1993.
Submitted: January 16, 1994; Received: January 21, 1994; First revision: August 14, 1994; Second revision: September, 1994;
Final manuscript received: November 1, 1994; Accepted: November 23, 1994
Published: April, 1996


ABSTRACT , CONTENTS , CORRECTIONS , FIGURES , REFERENCES , CITATIONS


Abstract
Wind velocity variance due to turbulence in the inertial subrange (spatial scale: 10$^0$-10$^2$ m) has been estimated from a seven-year (1986-1992) database of the echo power spectral width observed by a VHF (46.5 MHz) Doppler radar (the MU radar) in Japan. We study a climatology of the vertical eddy diffusivity $K$ in the tropo-stratosphere (altitude: 5-20 km) and mesosphere (60-90 km) which has been calculated from the observed wind velocity variance. We confirm completely the seasonal variabilities of $K$ suggested by {\sc Fukao}\ \etal\ (1994) based on a three-year database: an annual variation with winter maximum in the tropo-stratosphere, and a semiannual variation with solstice maxima (plus a weak annual variation with summer maximum) in the mesosphere. In this paper we further point out some interannual variabilities of $K$ with a dominant period of about two years, and discuss an overestimation of the median value of $K$ near the tropopausal jet stream.


Contents
1. Introduction
2. MU Radar Observations
3. Vertical Distribution of Annual Median
4. Seasonal Variability
5. Interannual Variability
6. Discussion on Estimation of Median
7. Conclusion


Corrections and Additional Remarks
(Nothing)


List of Tables and Figures


References (Updated after publication)


Citations by Subsequent Papers
(Under construction !!!!!)


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