Articles | Volume 33, issue 3
https://doi.org/10.5194/angeo-33-371-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/angeo-33-371-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Observation of electron biteout regions below sporadic E layers at polar latitudes
G. A. Lehmacher
CORRESPONDING AUTHOR
Department of Physics & Astronomy, Clemson University, Clemson, SC, USA
M. F. Larsen
Department of Physics & Astronomy, Clemson University, Clemson, SC, USA
C. L. Croskey
Department of Electrical Engineering, The Pennsylvania State University, University Park, PA, USA
Related authors
Gerald A. Lehmacher, Miguel F. Larsen, Richard L. Collins, Aroh Barjatya, and Boris Strelnikov
Ann. Geophys., 36, 1099–1116, https://doi.org/10.5194/angeo-36-1099-2018, https://doi.org/10.5194/angeo-36-1099-2018, 2018
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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.
Gerald A. Lehmacher, Miguel F. Larsen, Richard L. Collins, Aroh Barjatya, and Boris Strelnikov
Ann. Geophys., 36, 1099–1116, https://doi.org/10.5194/angeo-36-1099-2018, https://doi.org/10.5194/angeo-36-1099-2018, 2018
Short summary
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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.
David L. Hysell, Miguel Larsen, and Michael Sulzer
Ann. Geophys., 34, 927–941, https://doi.org/10.5194/angeo-34-927-2016, https://doi.org/10.5194/angeo-34-927-2016, 2016
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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.
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The descent of a sporadic E layer near 95km was observed with two rockets during a geomagnetically very quiet period. Four wind profiles showed that the location was surprisingly consistent with the neutral wind shear and a small electric field. Both electron probes found deep depletions just below the layers, which could be due to charged mesospheric smoke particles. Those have recently been detected in the mesosphere, but not yet in immediate connection with sporadic E.
The descent of a sporadic E layer near 95km was observed with two rockets during a...