Towards multi-purpose IS radar experiments
The EISCAT incoherent scatter radars routinely perform simultaneous measurements of E- and F-regions of the ionosphere. In addition several experiments exist for measuring pulse-to-pulse correlations from the D-region. However, the D-region experiments have quite limited range extents and the short...
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ftdoajarticles:oai:doaj.org/article:5bbd1acc0f814b86a3cf168c7935518f 2023-05-15T16:04:48+02:00 Towards multi-purpose IS radar experiments I. I. Virtanen M. S. Lehtinen J. Vierinen 2008-08-01T00:00:00Z https://doi.org/10.5194/angeo-26-2281-2008 https://doaj.org/article/5bbd1acc0f814b86a3cf168c7935518f EN eng Copernicus Publications https://www.ann-geophys.net/26/2281/2008/angeo-26-2281-2008.pdf https://doaj.org/toc/0992-7689 https://doaj.org/toc/1432-0576 doi:10.5194/angeo-26-2281-2008 0992-7689 1432-0576 https://doaj.org/article/5bbd1acc0f814b86a3cf168c7935518f Annales Geophysicae, Vol 26, Pp 2281-2289 (2008) Science Q Physics QC1-999 Geophysics. Cosmic physics QC801-809 article 2008 ftdoajarticles https://doi.org/10.5194/angeo-26-2281-2008 2022-12-31T14:48:13Z The EISCAT incoherent scatter radars routinely perform simultaneous measurements of E- and F-regions of the ionosphere. In addition several experiments exist for measuring pulse-to-pulse correlations from the D-region. However, the D-region experiments have quite limited range extents and the short lags suffer from F-region echoes, which are difficult to properly handle with standard decoding methods. In this paper it is demonstrated with real data how D-region experiments can be designed to produce continuous lag profiles extending above the F-region maximum. The large range coverage is attained for all lags shorter than the longest transmission pulse and it allows one to properly include the F-region echoes in the analysis. The large coverage is not needed for pulse-to-pulse lags because E- and F-regions do not have this long correlation times. The lag profiles with large range extent also provide a useful measurement of the upper parts of the ionosphere. The experiments utilise new kind of phase coding technique, which has estimation accuracy comparable to that of alternating codes though the code sequence is very short. No special decoding method is applied to the codes, because the lag profile inversion method automatically adapts to any kind of transmission codes provided transmission samples are available. The computing resources needed for real-time lag profile inversion with two different kinds of goals are also discussed here: 1) real-time monitoring of the results and 2) use of inverted lag profiles as a way to permanently store the data. While it was possible to accomplish real-time monitoring with a standard high-end desktop workstation, the higher resolution requirement for permanent data storage purposes is a much more critical task, requiring the use of larger-scale parallel processing. Article in Journal/Newspaper EISCAT Directory of Open Access Journals: DOAJ Articles Annales Geophysicae 26 8 2281 2289 |
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Directory of Open Access Journals: DOAJ Articles |
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English |
topic |
Science Q Physics QC1-999 Geophysics. Cosmic physics QC801-809 |
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Science Q Physics QC1-999 Geophysics. Cosmic physics QC801-809 I. I. Virtanen M. S. Lehtinen J. Vierinen Towards multi-purpose IS radar experiments |
topic_facet |
Science Q Physics QC1-999 Geophysics. Cosmic physics QC801-809 |
description |
The EISCAT incoherent scatter radars routinely perform simultaneous measurements of E- and F-regions of the ionosphere. In addition several experiments exist for measuring pulse-to-pulse correlations from the D-region. However, the D-region experiments have quite limited range extents and the short lags suffer from F-region echoes, which are difficult to properly handle with standard decoding methods. In this paper it is demonstrated with real data how D-region experiments can be designed to produce continuous lag profiles extending above the F-region maximum. The large range coverage is attained for all lags shorter than the longest transmission pulse and it allows one to properly include the F-region echoes in the analysis. The large coverage is not needed for pulse-to-pulse lags because E- and F-regions do not have this long correlation times. The lag profiles with large range extent also provide a useful measurement of the upper parts of the ionosphere. The experiments utilise new kind of phase coding technique, which has estimation accuracy comparable to that of alternating codes though the code sequence is very short. No special decoding method is applied to the codes, because the lag profile inversion method automatically adapts to any kind of transmission codes provided transmission samples are available. The computing resources needed for real-time lag profile inversion with two different kinds of goals are also discussed here: 1) real-time monitoring of the results and 2) use of inverted lag profiles as a way to permanently store the data. While it was possible to accomplish real-time monitoring with a standard high-end desktop workstation, the higher resolution requirement for permanent data storage purposes is a much more critical task, requiring the use of larger-scale parallel processing. |
format |
Article in Journal/Newspaper |
author |
I. I. Virtanen M. S. Lehtinen J. Vierinen |
author_facet |
I. I. Virtanen M. S. Lehtinen J. Vierinen |
author_sort |
I. I. Virtanen |
title |
Towards multi-purpose IS radar experiments |
title_short |
Towards multi-purpose IS radar experiments |
title_full |
Towards multi-purpose IS radar experiments |
title_fullStr |
Towards multi-purpose IS radar experiments |
title_full_unstemmed |
Towards multi-purpose IS radar experiments |
title_sort |
towards multi-purpose is radar experiments |
publisher |
Copernicus Publications |
publishDate |
2008 |
url |
https://doi.org/10.5194/angeo-26-2281-2008 https://doaj.org/article/5bbd1acc0f814b86a3cf168c7935518f |
genre |
EISCAT |
genre_facet |
EISCAT |
op_source |
Annales Geophysicae, Vol 26, Pp 2281-2289 (2008) |
op_relation |
https://www.ann-geophys.net/26/2281/2008/angeo-26-2281-2008.pdf https://doaj.org/toc/0992-7689 https://doaj.org/toc/1432-0576 doi:10.5194/angeo-26-2281-2008 0992-7689 1432-0576 https://doaj.org/article/5bbd1acc0f814b86a3cf168c7935518f |
op_doi |
https://doi.org/10.5194/angeo-26-2281-2008 |
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Annales Geophysicae |
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26 |
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8 |
container_start_page |
2281 |
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2289 |
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