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
- Table 1.
List of the GRATMAC standard observations.
- Fig. 1.
Vertical profiles of the annual medians of vertical eddy diffusivity $K$
observed by the MU radar during 1986-1992 in (a) the mesosphere and (b)
the upper troposphere and lower stratosphere,
compared with standard model profiles indicated by dashed curves
({\sc Ogawa}\ and\ {\sc Shimazaki},\ 1975;
{\sc Massie}\ and\ {\sc Hunten},\ 1981).
- Fig. 2.
Vertical-temporal plots of the monthly medians of vertical eddy diffusivity
$K$ observed by the MU radar during 1986-1992 in (a) the mesosphere and (b)
the upper troposphere and lower stratosphere.
- Fig. 3.
Same as Fig.\ 2 but for 12-month running-averaged data.
- Fig. 4.
Power spectra of vertical eddy diffusivity $K$ observed by the MU radar
during 1986-1992 in the lower stratosphere.
- Fig. 5.
Vertical-temporal plots of the 12-month running-averaged monthly medians of
zonal wind velocity observed by the MU radar during 1986-1992 in
the upper troposphere and lower stratosphere.
- Fig. 6.
Same as Fig.\ 1(b) but including samples of $\sigma^2$ with values
which are negative or smaller than the accuracy.
- Fig. 7.
Same as (a) Fig.\ 2(b) and (b) Fig.\ 3(b) but including samples of
$\sigma^2$ with values which are negative or smaller than the accuracy.
References
(Updated after publication)
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Citations by Subsequent Papers
(Under construction !!!!!)
-
List of Original Papers
by M. D. Yamanaka
-
Bibliography
by any authors
M. D. YAMANAKA homepage (English)
E-mail : yamanaka@kurasc.kyoto-u.ac.jp