High resolution general purpose D-layer experiment for EISCAT incoherent scatter radars using selected set of random codes

The ionospheric D-layer is a narrow bandwidth radar target often with a very small scattering cross section. The target autocorrelation function can be obtained by transmitting a series of relatively short coded pulses and computing the correlation between data obtained from different pulses. The sp...

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Published in:Annales Geophysicae
Main Authors: Turunen, T., Westman, A., Häggström, I., Wannberg, G.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/angeo-20-1469-2002
https://angeo.copernicus.org/articles/20/1469/2002/
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spelling ftcopernicus:oai:publications.copernicus.org:angeo35016 2023-05-15T16:04:48+02:00 High resolution general purpose D-layer experiment for EISCAT incoherent scatter radars using selected set of random codes Turunen, T. Westman, A. Häggström, I. Wannberg, G. 2018-09-27 application/pdf https://doi.org/10.5194/angeo-20-1469-2002 https://angeo.copernicus.org/articles/20/1469/2002/ eng eng doi:10.5194/angeo-20-1469-2002 https://angeo.copernicus.org/articles/20/1469/2002/ eISSN: 1432-0576 Text 2018 ftcopernicus https://doi.org/10.5194/angeo-20-1469-2002 2020-07-20T16:27:49Z The ionospheric D-layer is a narrow bandwidth radar target often with a very small scattering cross section. The target autocorrelation function can be obtained by transmitting a series of relatively short coded pulses and computing the correlation between data obtained from different pulses. The spatial resolution should be as high as possible and the spatial side lobes of the codes used should be as small as possible. However, due to the short pulse repetition period (in the order of milliseconds) at any instant, the radar receives detectable scattered signals not only from the pulse illuminating the D-region but also from 3–5 ambiguous-range pulses, which makes it difficult to produce a reliable estimate near zero lag of the autocorrelation function. A new experimental solution to this measurement problem, using a selected set of 40-bit random codes with 4 µs elements giving 600 m spatial resolution is presented. The zero lag is approximated by dividing the pulse into two 20-bit codes and computing the correlation between those two pulses. The lowest altitudes of the E-layer are measured by dividing the pulse into 5 pieces of 8 bits, which allows for computation of 4 lags. In addition, coherent integration of data from four pulses is used for obtaining separately the autocorrelation function estimate for the lowest altitudes and in cases when the target contains structures with a long coherence time. Design details and responses of the experiment are given, and analysed test data are shown. Key words. Radio science (signal processing); Ionosphere (plasma temperature and density; instruments and techniques) Text EISCAT Copernicus Publications: E-Journals Annales Geophysicae 20 9 1469 1477
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description The ionospheric D-layer is a narrow bandwidth radar target often with a very small scattering cross section. The target autocorrelation function can be obtained by transmitting a series of relatively short coded pulses and computing the correlation between data obtained from different pulses. The spatial resolution should be as high as possible and the spatial side lobes of the codes used should be as small as possible. However, due to the short pulse repetition period (in the order of milliseconds) at any instant, the radar receives detectable scattered signals not only from the pulse illuminating the D-region but also from 3–5 ambiguous-range pulses, which makes it difficult to produce a reliable estimate near zero lag of the autocorrelation function. A new experimental solution to this measurement problem, using a selected set of 40-bit random codes with 4 µs elements giving 600 m spatial resolution is presented. The zero lag is approximated by dividing the pulse into two 20-bit codes and computing the correlation between those two pulses. The lowest altitudes of the E-layer are measured by dividing the pulse into 5 pieces of 8 bits, which allows for computation of 4 lags. In addition, coherent integration of data from four pulses is used for obtaining separately the autocorrelation function estimate for the lowest altitudes and in cases when the target contains structures with a long coherence time. Design details and responses of the experiment are given, and analysed test data are shown. Key words. Radio science (signal processing); Ionosphere (plasma temperature and density; instruments and techniques)
format Text
author Turunen, T.
Westman, A.
Häggström, I.
Wannberg, G.
spellingShingle Turunen, T.
Westman, A.
Häggström, I.
Wannberg, G.
High resolution general purpose D-layer experiment for EISCAT incoherent scatter radars using selected set of random codes
author_facet Turunen, T.
Westman, A.
Häggström, I.
Wannberg, G.
author_sort Turunen, T.
title High resolution general purpose D-layer experiment for EISCAT incoherent scatter radars using selected set of random codes
title_short High resolution general purpose D-layer experiment for EISCAT incoherent scatter radars using selected set of random codes
title_full High resolution general purpose D-layer experiment for EISCAT incoherent scatter radars using selected set of random codes
title_fullStr High resolution general purpose D-layer experiment for EISCAT incoherent scatter radars using selected set of random codes
title_full_unstemmed High resolution general purpose D-layer experiment for EISCAT incoherent scatter radars using selected set of random codes
title_sort high resolution general purpose d-layer experiment for eiscat incoherent scatter radars using selected set of random codes
publishDate 2018
url https://doi.org/10.5194/angeo-20-1469-2002
https://angeo.copernicus.org/articles/20/1469/2002/
genre EISCAT
genre_facet EISCAT
op_source eISSN: 1432-0576
op_relation doi:10.5194/angeo-20-1469-2002
https://angeo.copernicus.org/articles/20/1469/2002/
op_doi https://doi.org/10.5194/angeo-20-1469-2002
container_title Annales Geophysicae
container_volume 20
container_issue 9
container_start_page 1469
op_container_end_page 1477
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