Articles | Volume 36, issue 4
https://doi.org/10.5194/angeo-36-1099-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/angeo-36-1099-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Regular paper
| 
15 Aug 2018
Regular paper |
| 15 Aug 2018
| 15 Aug 2018
On the short-term variability of turbulence and temperature in the winter mesosphere
Gerald A. Lehmacher
CORRESPONDING AUTHOR
Department of Physics & Astronomy, Clemson University, Clemson, South Carolina, USA
Miguel F. Larsen
Department of Physics & Astronomy, Clemson University, Clemson, South Carolina, USA
Richard L. Collins
Geophysical Institute, University of Alaska, Fairbanks, Alaska, USA
Aroh Barjatya
Department of Physical Sciences, Embry-Riddle Aeronautical University, Daytona Beach, Florida, USA
Boris Strelnikov
Leibniz-Institute for Atmospheric Physics, Kühlungsborn, Germany
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Boris Strelnikov, Artur Szewczyk, Irina Strelnikova, Ralph Latteck, Gerd Baumgarten, Franz-Josef Lübken, Markus Rapp, Stefanos Fasoulas, Stefan Löhle, Martin Eberhart, Ulf-Peter Hoppe, Tim Dunker, Martin Friedrich, Jonas Hedin, Mikhail Khaplanov, Jörg Gumbel, and Aroh Barjatya
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The WADIS sounding rocket mission utilized multi-point turbulence measurements in the mesosphere by different techniques, i.e., with ionization gauges carried by rockets and ground-based MAARSY and EISCAT radars. Results show that turbulence energy dissipation rates oscillate in space and time with amplitude of up to 2 orders of magnitude. Spatial oscillations show the same wavelengths as atmospheric gravity waves. Temporal variability reveals periods of atmospheric tides and gravity waves.
David L. Hysell, Miguel Larsen, and Michael Sulzer
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Radar observations of the E- and F-region ionosphere from the Arecibo Observatory made during moderately disturbed conditions are presented. Plasma irregularities in both ionospheric regions were observed. We investigate the role of neutral atmospheric dynamics and instabilities in causing the ionospheric disturbances. A number of viable instability mechanisms rooted in neutral dynamics are identified.
G. A. Lehmacher, M. F. Larsen, and C. L. Croskey
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Subject: Terrestrial atmosphere and its relation to the sun | Keywords: Turbulence
A quasi-experimental coastal region eddy diffusivity applied in the APUGRID model
Silvana Maldaner, Michel Stefanello, Luis Gustavo N. Martins, Gervásio Annes Degrazia, Umberto Rizza, Débora Regina Roberti, Franciano S. Puhales, and Otávio C. Acevedo
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In this paper, quasi-empirical convective eddy diffusivity parameterizations for a coastal site are obtained. In the derivation we used Taylor's theory of statistical diffusion and sonic anemometer observations collected at 11 levels on a 140 m high tower in a convective planetary boundary layer. The test of the derived coefficients was solved by solving the equation of diffusion–advection by the fractional step/locally one-dimensional (LOD) methods.
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Short summary
We used sounding rockets to obtain four high-resolution temperature profiles in the mesosphere over a limited area. We found consistent deep isothermal and adiabatic layers, but variable and finely structured turbulence preferentially in the lower stable mesosphere. Accompanying tracer releases showed horizontal winds in the lower thermosphere with extreme shears and 200 m s−1 winds under moderately disturbed geomagnetic conditions, and convection-like structures just below the mesopause.
We used sounding rockets to obtain four high-resolution temperature profiles in the mesosphere...
