The effects of high-frequency ULF wave activity on the spectral characteristics of coherent HF radar returns: a case study
It is now a common practice to employ ground-based radars in an attempt to distinguish between those regions of the Earth's upper atmosphere which are magnetically conjugate to open and closed magnetic field lines. Radar returns from ionospheric irregularities inside the polar cap and cusp regi...
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ftdoajarticles:oai:doaj.org/article:f99a3971c7af4691ab21feefa8745496 2023-05-15T18:34:46+02:00 The effects of high-frequency ULF wave activity on the spectral characteristics of coherent HF radar returns: a case study D. M. Wright T. K. Yeoman E. E. Woodfield 2004-04-01T00:00:00Z https://doi.org/10.5194/angeo-22-1843-2004 https://doaj.org/article/f99a3971c7af4691ab21feefa8745496 EN eng Copernicus Publications https://www.ann-geophys.net/22/1843/2004/angeo-22-1843-2004.pdf https://doaj.org/toc/0992-7689 https://doaj.org/toc/1432-0576 doi:10.5194/angeo-22-1843-2004 0992-7689 1432-0576 https://doaj.org/article/f99a3971c7af4691ab21feefa8745496 Annales Geophysicae, Vol 22, Pp 1843-1849 (2004) Science Q Physics QC1-999 Geophysics. Cosmic physics QC801-809 article 2004 ftdoajarticles https://doi.org/10.5194/angeo-22-1843-2004 2022-12-31T00:07:09Z It is now a common practice to employ ground-based radars in an attempt to distinguish between those regions of the Earth's upper atmosphere which are magnetically conjugate to open and closed magnetic field lines. Radar returns from ionospheric irregularities inside the polar cap and cusp regions generally exhibit large spectral widths in contrast to those which exist on closed field lines at lower latitudes. It has been suggested that the so-called Spectral Width Boundary (SWB) might act as a proxy for the open-closed field line boundary (OCFLB), which would then be an invaluable tool for investigating reconnection rates in the magnetosphere. The exact cause of the increased spectral widths observed at very high latitudes is still subject to considerable debate. Several mechanisms have been proposed. This paper compares a dusk-sector interval of coherent HF radar data with measurements made by an induction coil magnetometer located at Tromsø, Norway (66° N geomagnetic). On this occasion, a number of equatorward excursions of the SWB in the radar backscatter are accompanied by increases in spectral power of ULF waves in the Pc1-2 frequency band as the SWB passes overhead. Thus, these observations support the possibility that high-frequency magnetospheric wave activity at least contribute to the observed spectral characteristics and that such wave activity might play a significant role in the nightside ionosphere. Key words. Ionosphere (auroral ionosphere) – Magnetospheric physics (MHD waves and instabilities) – Radio science (ionospheric physics) Article in Journal/Newspaper Tromsø Directory of Open Access Journals: DOAJ Articles Norway Tromsø Annales Geophysicae 22 5 1843 1849 |
institution |
Open Polar |
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Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Science Q Physics QC1-999 Geophysics. Cosmic physics QC801-809 |
spellingShingle |
Science Q Physics QC1-999 Geophysics. Cosmic physics QC801-809 D. M. Wright T. K. Yeoman E. E. Woodfield The effects of high-frequency ULF wave activity on the spectral characteristics of coherent HF radar returns: a case study |
topic_facet |
Science Q Physics QC1-999 Geophysics. Cosmic physics QC801-809 |
description |
It is now a common practice to employ ground-based radars in an attempt to distinguish between those regions of the Earth's upper atmosphere which are magnetically conjugate to open and closed magnetic field lines. Radar returns from ionospheric irregularities inside the polar cap and cusp regions generally exhibit large spectral widths in contrast to those which exist on closed field lines at lower latitudes. It has been suggested that the so-called Spectral Width Boundary (SWB) might act as a proxy for the open-closed field line boundary (OCFLB), which would then be an invaluable tool for investigating reconnection rates in the magnetosphere. The exact cause of the increased spectral widths observed at very high latitudes is still subject to considerable debate. Several mechanisms have been proposed. This paper compares a dusk-sector interval of coherent HF radar data with measurements made by an induction coil magnetometer located at Tromsø, Norway (66° N geomagnetic). On this occasion, a number of equatorward excursions of the SWB in the radar backscatter are accompanied by increases in spectral power of ULF waves in the Pc1-2 frequency band as the SWB passes overhead. Thus, these observations support the possibility that high-frequency magnetospheric wave activity at least contribute to the observed spectral characteristics and that such wave activity might play a significant role in the nightside ionosphere. Key words. Ionosphere (auroral ionosphere) – Magnetospheric physics (MHD waves and instabilities) – Radio science (ionospheric physics) |
format |
Article in Journal/Newspaper |
author |
D. M. Wright T. K. Yeoman E. E. Woodfield |
author_facet |
D. M. Wright T. K. Yeoman E. E. Woodfield |
author_sort |
D. M. Wright |
title |
The effects of high-frequency ULF wave activity on the spectral characteristics of coherent HF radar returns: a case study |
title_short |
The effects of high-frequency ULF wave activity on the spectral characteristics of coherent HF radar returns: a case study |
title_full |
The effects of high-frequency ULF wave activity on the spectral characteristics of coherent HF radar returns: a case study |
title_fullStr |
The effects of high-frequency ULF wave activity on the spectral characteristics of coherent HF radar returns: a case study |
title_full_unstemmed |
The effects of high-frequency ULF wave activity on the spectral characteristics of coherent HF radar returns: a case study |
title_sort |
effects of high-frequency ulf wave activity on the spectral characteristics of coherent hf radar returns: a case study |
publisher |
Copernicus Publications |
publishDate |
2004 |
url |
https://doi.org/10.5194/angeo-22-1843-2004 https://doaj.org/article/f99a3971c7af4691ab21feefa8745496 |
geographic |
Norway Tromsø |
geographic_facet |
Norway Tromsø |
genre |
Tromsø |
genre_facet |
Tromsø |
op_source |
Annales Geophysicae, Vol 22, Pp 1843-1849 (2004) |
op_relation |
https://www.ann-geophys.net/22/1843/2004/angeo-22-1843-2004.pdf https://doaj.org/toc/0992-7689 https://doaj.org/toc/1432-0576 doi:10.5194/angeo-22-1843-2004 0992-7689 1432-0576 https://doaj.org/article/f99a3971c7af4691ab21feefa8745496 |
op_doi |
https://doi.org/10.5194/angeo-22-1843-2004 |
container_title |
Annales Geophysicae |
container_volume |
22 |
container_issue |
5 |
container_start_page |
1843 |
op_container_end_page |
1849 |
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1766219670278373376 |