A study of seasonal variations of gravity wave intensity in thelower thermosphere using LF D1 wind observations and a numerical model

The data of the regular low-frequency D1 E-region observations at Collm, Germany (52°N, 15°E) in 1983–1999 are used for estimations of the intensity of short-period perturbations of the horizontal drift velocity at 85–110 km altitude. A simple half-hourly-difference numerical filter is used to ex...

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Main Authors: N. M. Gavrilov, Ch. Jacobi
Format: Article
Language:English
Published: Copernicus Publications 2004-01-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/22/35/2004/angeo-22-35-2004.pdf
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spelling doaj-6898f9085d0a4cec95a3e22cdd03c1ae2020-11-25T00:34:31ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762004-01-0122354510.5194/angeo-22-35-2004A study of seasonal variations of gravity wave intensity in thelower thermosphere using LF D1 wind observations and a numerical modelN. M. Gavrilov0Ch. Jacobi1Saint-Petersburg State University, Department of Atmospheric Physics, Petrodvorets, 198904, RussiaUniversity of Leipzig, Institute for Meteorology, 3 Stephanstrasse, 04103 Leipzig, GermanyThe data of the regular low-frequency D1 E-region observations at Collm, Germany (52°N, 15°E) in 1983–1999 are used for estimations of the intensity of short-period perturbations of the horizontal drift velocity at 85–110 km altitude. A simple half-hourly-difference numerical filter is used to extract perturbations with time scales of 0.7–3 h. </p><p style="line-height: 20px;"> The average monthly standard deviations of short-period perturbations of the zonal velocity near altitude 83 km have a main maximum in summer, a smaller maximum in winter, and minimum values at the equinoxes. At higher altitudes the summer maximum is shifted towards the spring months, and a second maximum of perturbation amplitudes appears in autumn at altitudes near and above 100 km. The seasonal changes in the standard deviations of meridional velocity show the maxima in spring and summer. A numerical model describing the propagation of a set of harmonics modeling a spectrum of internal gravity waves in the atmosphere is used for the interpretation of observed seasonal variations of wind perturbation intensity. Numerical modeling reveals that the observed altitude changes in the seasonal variations of the drift velocity standard deviations may be explained by a superposition of IGWs generated at different levels in the troposphere and middle atmosphere. IGWs generated in the stratospheric and mesospheric jet stream may have substantial amplitudes at altitudes near and above 100 km, where they may modify the seasonal variations, which are typical for IGWs propagating from the troposphere.<br><br> <b>Key words.</b> Meteorology and atmospheric dynamics (middle atmosphere dynamics; waves and tides) – Ionosphere (ionospheric irregularities)https://www.ann-geophys.net/22/35/2004/angeo-22-35-2004.pdf
collection DOAJ
language English
format Article
sources DOAJ
author N. M. Gavrilov
Ch. Jacobi
spellingShingle N. M. Gavrilov
Ch. Jacobi
A study of seasonal variations of gravity wave intensity in thelower thermosphere using LF D1 wind observations and a numerical model
Annales Geophysicae
author_facet N. M. Gavrilov
Ch. Jacobi
author_sort N. M. Gavrilov
title A study of seasonal variations of gravity wave intensity in thelower thermosphere using LF D1 wind observations and a numerical model
title_short A study of seasonal variations of gravity wave intensity in thelower thermosphere using LF D1 wind observations and a numerical model
title_full A study of seasonal variations of gravity wave intensity in thelower thermosphere using LF D1 wind observations and a numerical model
title_fullStr A study of seasonal variations of gravity wave intensity in thelower thermosphere using LF D1 wind observations and a numerical model
title_full_unstemmed A study of seasonal variations of gravity wave intensity in thelower thermosphere using LF D1 wind observations and a numerical model
title_sort study of seasonal variations of gravity wave intensity in thelower thermosphere using lf d1 wind observations and a numerical model
publisher Copernicus Publications
series Annales Geophysicae
issn 0992-7689
1432-0576
publishDate 2004-01-01
description The data of the regular low-frequency D1 E-region observations at Collm, Germany (52°N, 15°E) in 1983–1999 are used for estimations of the intensity of short-period perturbations of the horizontal drift velocity at 85–110 km altitude. A simple half-hourly-difference numerical filter is used to extract perturbations with time scales of 0.7–3 h. </p><p style="line-height: 20px;"> The average monthly standard deviations of short-period perturbations of the zonal velocity near altitude 83 km have a main maximum in summer, a smaller maximum in winter, and minimum values at the equinoxes. At higher altitudes the summer maximum is shifted towards the spring months, and a second maximum of perturbation amplitudes appears in autumn at altitudes near and above 100 km. The seasonal changes in the standard deviations of meridional velocity show the maxima in spring and summer. A numerical model describing the propagation of a set of harmonics modeling a spectrum of internal gravity waves in the atmosphere is used for the interpretation of observed seasonal variations of wind perturbation intensity. Numerical modeling reveals that the observed altitude changes in the seasonal variations of the drift velocity standard deviations may be explained by a superposition of IGWs generated at different levels in the troposphere and middle atmosphere. IGWs generated in the stratospheric and mesospheric jet stream may have substantial amplitudes at altitudes near and above 100 km, where they may modify the seasonal variations, which are typical for IGWs propagating from the troposphere.<br><br> <b>Key words.</b> Meteorology and atmospheric dynamics (middle atmosphere dynamics; waves and tides) – Ionosphere (ionospheric irregularities)
url https://www.ann-geophys.net/22/35/2004/angeo-22-35-2004.pdf
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