Turbulent diffusivity and turbulent ozone fluxes in the tropo-stratosphere are studied employing simultaneous observations with the Middle and Upper (MU) Atmosphere radar and ozonesondes in Shigaraki, Japan during April 16-24, 1998. A broad region around the tropopause was dynamically active. Maxima of turbulent diffusivity were observed at 8-14 km altitude. Such maxima may produce vertical turbulent ozone fluxes across the tropopause with magnitudes comparable to those required for the global ozone budget. Meso-meteorological ozone intrusions may enhance the fluxes. Copyright 2006 by the American Geophysical Union.
CITATION STYLE
Gavrilov, N. M., Fukao, S., Hashiguchi, H., Kita, K., Sato, K., Tomikawa, Y., & Fujiwara, M. (2006). Combined MU radar and ozonesonde measurements of turbulence and ozone fluxes in the tropo-stratosphere over Shigaraki, Japan. Geophysical Research Letters, 33(9). https://doi.org/10.1029/2005GL024002
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