Influence of geomagnetic disturbances on mean winds and tides in the mesosphere/lower thermosphere at midlatitudes
<p>Observations of upper mesosphere/lower thermosphere (MLT) wind have been performed at Collm (51.3<span class="inline-formula"><sup>∘</sup></span> N, 13.0<span class="inline-formula"><sup>∘</sup></span> E) and Kazan (56<s...
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Copernicus Publications
2021-12-01
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Series: | Advances in Radio Science |
Online Access: | https://ars.copernicus.org/articles/19/185/2021/ars-19-185-2021.pdf |
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author | C. Jacobi F. Lilienthal D. Korotyshkin E. Merzlyakov E. Merzlyakov G. Stober |
author_facet | C. Jacobi F. Lilienthal D. Korotyshkin E. Merzlyakov E. Merzlyakov G. Stober |
author_sort | C. Jacobi |
collection | DOAJ |
description | <p>Observations of upper mesosphere/lower thermosphere (MLT) wind have been performed at Collm (51.3<span class="inline-formula"><sup>∘</sup></span> N, 13.0<span class="inline-formula"><sup>∘</sup></span> E) and Kazan (56<span class="inline-formula"><sup>∘</sup></span> N, 49<span class="inline-formula"><sup>∘</sup></span> E), using two SKiYMET all-sky meteor radars with similar configuration. Daily vertical profiles of mean winds and tidal amplitudes have been constructed from hourly horizontal winds.
We analyse the response of mean winds and tidal amplitudes to geomagnetic disturbances. To this end, we compare winds and amplitudes for very quiet (Ap <span class="inline-formula">≤</span> 5) and unsettled/disturbed (Ap <span class="inline-formula">≥</span> 20) geomagnetic conditions. Zonal winds in both the mesosphere and lower thermosphere are weaker during disturbed conditions for both summer and winter. The summer equatorward meridional wind jet is weaker for disturbed geomagnetic conditions. Tendencies for geomagnetic effects on mean winds over Collm and Kazan qualitatively agree during most of the year. For the diurnal tide, amplitudes in summer are smaller in the mesosphere and greater in the lower thermosphere, but no clear tendency is seen for winter. Semidiurnal tidal amplitudes increase during geomagnetic active days in summer and winter. Terdiurnal amplitudes are slightly reduced in the mesosphere during disturbed days, but no clear effect
is visible for the lower thermosphere. Overall, while there is a noticeable effect of geomagnetic variability on the mean wind, the effect on tidal amplitudes, except for the semidiurnal tide, is relatively small and partly different over Collm and Kazan.</p> |
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spelling | doaj.art-c0ce7b7bacb64e88bb53b23fbf27f20b2022-12-21T17:49:54ZdeuCopernicus PublicationsAdvances in Radio Science1684-99651684-99732021-12-011918519310.5194/ars-19-185-2021Influence of geomagnetic disturbances on mean winds and tides in the mesosphere/lower thermosphere at midlatitudesC. Jacobi0F. Lilienthal1D. Korotyshkin2E. Merzlyakov3E. Merzlyakov4G. Stober5Institute for Meteorology, Universität Leipzig, Stephanstr. 3, 04103 Leipzig, GermanyInstitute for Meteorology, Universität Leipzig, Stephanstr. 3, 04103 Leipzig, GermanyRadiophysics Department, Kazan (Volga Region) Federal University, Kazan, RussiaRadiophysics Department, Kazan (Volga Region) Federal University, Kazan, RussiaInstitute for Experimental Meteorology, Research and Production Association “Typhoon”, Obninsk, RussiaInstitute of Applied Physics, Microwave Physics, University of Bern, Bern, Switzerland<p>Observations of upper mesosphere/lower thermosphere (MLT) wind have been performed at Collm (51.3<span class="inline-formula"><sup>∘</sup></span> N, 13.0<span class="inline-formula"><sup>∘</sup></span> E) and Kazan (56<span class="inline-formula"><sup>∘</sup></span> N, 49<span class="inline-formula"><sup>∘</sup></span> E), using two SKiYMET all-sky meteor radars with similar configuration. Daily vertical profiles of mean winds and tidal amplitudes have been constructed from hourly horizontal winds. We analyse the response of mean winds and tidal amplitudes to geomagnetic disturbances. To this end, we compare winds and amplitudes for very quiet (Ap <span class="inline-formula">≤</span> 5) and unsettled/disturbed (Ap <span class="inline-formula">≥</span> 20) geomagnetic conditions. Zonal winds in both the mesosphere and lower thermosphere are weaker during disturbed conditions for both summer and winter. The summer equatorward meridional wind jet is weaker for disturbed geomagnetic conditions. Tendencies for geomagnetic effects on mean winds over Collm and Kazan qualitatively agree during most of the year. For the diurnal tide, amplitudes in summer are smaller in the mesosphere and greater in the lower thermosphere, but no clear tendency is seen for winter. Semidiurnal tidal amplitudes increase during geomagnetic active days in summer and winter. Terdiurnal amplitudes are slightly reduced in the mesosphere during disturbed days, but no clear effect is visible for the lower thermosphere. Overall, while there is a noticeable effect of geomagnetic variability on the mean wind, the effect on tidal amplitudes, except for the semidiurnal tide, is relatively small and partly different over Collm and Kazan.</p>https://ars.copernicus.org/articles/19/185/2021/ars-19-185-2021.pdf |
spellingShingle | C. Jacobi F. Lilienthal D. Korotyshkin E. Merzlyakov E. Merzlyakov G. Stober Influence of geomagnetic disturbances on mean winds and tides in the mesosphere/lower thermosphere at midlatitudes Advances in Radio Science |
title | Influence of geomagnetic disturbances on mean winds and tides in the mesosphere/lower thermosphere at midlatitudes |
title_full | Influence of geomagnetic disturbances on mean winds and tides in the mesosphere/lower thermosphere at midlatitudes |
title_fullStr | Influence of geomagnetic disturbances on mean winds and tides in the mesosphere/lower thermosphere at midlatitudes |
title_full_unstemmed | Influence of geomagnetic disturbances on mean winds and tides in the mesosphere/lower thermosphere at midlatitudes |
title_short | Influence of geomagnetic disturbances on mean winds and tides in the mesosphere/lower thermosphere at midlatitudes |
title_sort | influence of geomagnetic disturbances on mean winds and tides in the mesosphere lower thermosphere at midlatitudes |
url | https://ars.copernicus.org/articles/19/185/2021/ars-19-185-2021.pdf |
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