Planetary Wave Type Oscillations in the Ionosphere: Distinguishing Solar Forcing and Coupling From Below

The ionosphere is mainly influenced by the sun through electromagnetic radiation and particle precipitation. Additionally, upward propagating waves like planetary waves (PW), tides and atmospheric gravity waves (AGW) from the lower and middle atmosphere contribute to the ionospheric variability. PW,...

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Bibliographic Details
Main Authors: Borries, Claudia, Jakowski, Norbert, Jacobi, Christoph, Hoffmann, Peter
Format: Conference Object
Language:unknown
Published: 2009
Subjects:
Online Access:https://elib.dlr.de/62373/
id ftdlr:oai:elib.dlr.de:62373
record_format openpolar
spelling ftdlr:oai:elib.dlr.de:62373 2024-05-19T07:45:42+00:00 Planetary Wave Type Oscillations in the Ionosphere: Distinguishing Solar Forcing and Coupling From Below Borries, Claudia Jakowski, Norbert Jacobi, Christoph Hoffmann, Peter 2009-08 https://elib.dlr.de/62373/ unknown Borries, Claudia und Jakowski, Norbert und Jacobi, Christoph und Hoffmann, Peter (2009) Planetary Wave Type Oscillations in the Ionosphere: Distinguishing Solar Forcing and Coupling From Below. IAGA 2009, 2009-08-23 - 2009-08-30, Sopron, Hungary. Navigation Konferenzbeitrag NonPeerReviewed 2009 ftdlr 2024-04-25T00:16:58Z The ionosphere is mainly influenced by the sun through electromagnetic radiation and particle precipitation. Additionally, upward propagating waves like planetary waves (PW), tides and atmospheric gravity waves (AGW) from the lower and middle atmosphere contribute to the ionospheric variability. PW, mainly originating in the lower atmosphere, have a large impact on the dynamics of the middle atmosphere at middle and high latitudes during winter. Theoretically they are not capable to directly penetrate the F2-region of the ionosphere. However, an indirect impact on the F2-region variability through PW is expected. Planetary wave type oscillations (PWTO) which are observed in F2-region parameters are supposed to be the effect of middle atmosphere PW. The DLR Neustrelitz provides regional maps of the total electron content (TEC), which are calculated from GNSS measurements, since 1995. Hemispheric TEC maps of the North Pole region are consistently available since 2002. These maps are analyzed concerning PWTO. The PWTO are compared with parameters estimating the solar influence. 38-40% of the variations of the relative differential TEC can be described through variations of the solar wind, the F10.7cm radio flux and the geomagnetic activity. They are identified and removed using wavelet analyses. The residual PWTO are compared with PW analyses on stratospheric reanalyses and locally with mesospheric wind measurements. There is a general agreement in the seasonal variation of PW and PWTO. The modulation of tides is suggested to be a mechanism transporting PW energy into the ionosphere. Good agreements are found between the modulation of the semidiurnal tidal wind in the mesosphere and PWTO in TEC. Conference Object North Pole German Aerospace Center: elib - DLR electronic library
institution Open Polar
collection German Aerospace Center: elib - DLR electronic library
op_collection_id ftdlr
language unknown
topic Navigation
spellingShingle Navigation
Borries, Claudia
Jakowski, Norbert
Jacobi, Christoph
Hoffmann, Peter
Planetary Wave Type Oscillations in the Ionosphere: Distinguishing Solar Forcing and Coupling From Below
topic_facet Navigation
description The ionosphere is mainly influenced by the sun through electromagnetic radiation and particle precipitation. Additionally, upward propagating waves like planetary waves (PW), tides and atmospheric gravity waves (AGW) from the lower and middle atmosphere contribute to the ionospheric variability. PW, mainly originating in the lower atmosphere, have a large impact on the dynamics of the middle atmosphere at middle and high latitudes during winter. Theoretically they are not capable to directly penetrate the F2-region of the ionosphere. However, an indirect impact on the F2-region variability through PW is expected. Planetary wave type oscillations (PWTO) which are observed in F2-region parameters are supposed to be the effect of middle atmosphere PW. The DLR Neustrelitz provides regional maps of the total electron content (TEC), which are calculated from GNSS measurements, since 1995. Hemispheric TEC maps of the North Pole region are consistently available since 2002. These maps are analyzed concerning PWTO. The PWTO are compared with parameters estimating the solar influence. 38-40% of the variations of the relative differential TEC can be described through variations of the solar wind, the F10.7cm radio flux and the geomagnetic activity. They are identified and removed using wavelet analyses. The residual PWTO are compared with PW analyses on stratospheric reanalyses and locally with mesospheric wind measurements. There is a general agreement in the seasonal variation of PW and PWTO. The modulation of tides is suggested to be a mechanism transporting PW energy into the ionosphere. Good agreements are found between the modulation of the semidiurnal tidal wind in the mesosphere and PWTO in TEC.
format Conference Object
author Borries, Claudia
Jakowski, Norbert
Jacobi, Christoph
Hoffmann, Peter
author_facet Borries, Claudia
Jakowski, Norbert
Jacobi, Christoph
Hoffmann, Peter
author_sort Borries, Claudia
title Planetary Wave Type Oscillations in the Ionosphere: Distinguishing Solar Forcing and Coupling From Below
title_short Planetary Wave Type Oscillations in the Ionosphere: Distinguishing Solar Forcing and Coupling From Below
title_full Planetary Wave Type Oscillations in the Ionosphere: Distinguishing Solar Forcing and Coupling From Below
title_fullStr Planetary Wave Type Oscillations in the Ionosphere: Distinguishing Solar Forcing and Coupling From Below
title_full_unstemmed Planetary Wave Type Oscillations in the Ionosphere: Distinguishing Solar Forcing and Coupling From Below
title_sort planetary wave type oscillations in the ionosphere: distinguishing solar forcing and coupling from below
publishDate 2009
url https://elib.dlr.de/62373/
genre North Pole
genre_facet North Pole
op_relation Borries, Claudia und Jakowski, Norbert und Jacobi, Christoph und Hoffmann, Peter (2009) Planetary Wave Type Oscillations in the Ionosphere: Distinguishing Solar Forcing and Coupling From Below. IAGA 2009, 2009-08-23 - 2009-08-30, Sopron, Hungary.
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