Decoding of Barker-coded incoherent scatter measurements by means ofmathematical inversion

The standard analysis of Barker-coded incoherent scatter experiments is based on a matched filter with an impulse response which is a mirror image of the code itself. The method produces small sidelobes which cause contamination from regions outside the nominal range gate. A corresponding effect is...

Full description

Bibliographic Details
Published in:Annales Geophysicae
Main Authors: B. Damtie, M. S. Lehtinen, T. Nygrén
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2004
Subjects:
Q
Online Access:https://doi.org/10.5194/angeo-22-3-2004
https://doaj.org/article/c89067e3100f4e0498f525aa166a45af
id ftdoajarticles:oai:doaj.org/article:c89067e3100f4e0498f525aa166a45af
record_format openpolar
spelling ftdoajarticles:oai:doaj.org/article:c89067e3100f4e0498f525aa166a45af 2023-05-15T16:04:45+02:00 Decoding of Barker-coded incoherent scatter measurements by means ofmathematical inversion B. Damtie M. S. Lehtinen T. Nygrén 2004-01-01T00:00:00Z https://doi.org/10.5194/angeo-22-3-2004 https://doaj.org/article/c89067e3100f4e0498f525aa166a45af EN eng Copernicus Publications https://www.ann-geophys.net/22/3/2004/angeo-22-3-2004.pdf https://doaj.org/toc/0992-7689 https://doaj.org/toc/1432-0576 doi:10.5194/angeo-22-3-2004 0992-7689 1432-0576 https://doaj.org/article/c89067e3100f4e0498f525aa166a45af Annales Geophysicae, Vol 22, Pp 3-13 (2004) Science Q Physics QC1-999 Geophysics. Cosmic physics QC801-809 article 2004 ftdoajarticles https://doi.org/10.5194/angeo-22-3-2004 2022-12-31T01:33:23Z The standard analysis of Barker-coded incoherent scatter experiments is based on a matched filter with an impulse response which is a mirror image of the code itself. The method produces small sidelobes which cause contamination from regions outside the nominal range gate. A corresponding effect is also encountered in the lag direction, where individual lag estimates are biased by the variation of the plasma autocorrelation function around the nominal lag value. The present paper introduces a new method of analysing Barker-coded experiments by means of stochastic inversion. Since it does not apply a decoding filter, it does not suffer from drawbacks caused by the sidelobes of the range ambiguity function. The method combines the profile of each full lag and a number of surrounding fractional lags into a single inversion problem. Error analysis also indicates that the statistical accuracy given by inversion is better than that obtained by means of standard decoding. Furthermore, the inversion method gives a possibility to reduce the bias due to the variation of the autocorrelation around the nominal lag. In this paper the method is described and applied to data obtained by means of the EISCAT Svalbard radar. In addition, it is shown that mathematical inversion can be used instead of the the conventional height integration. Key words. Radio science (ionospheric physics; signal processing; instruments and techniques) Article in Journal/Newspaper EISCAT Svalbard Directory of Open Access Journals: DOAJ Articles Svalbard Annales Geophysicae 22 1 3 13
institution Open Polar
collection 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
B. Damtie
M. S. Lehtinen
T. Nygrén
Decoding of Barker-coded incoherent scatter measurements by means ofmathematical inversion
topic_facet Science
Q
Physics
QC1-999
Geophysics. Cosmic physics
QC801-809
description The standard analysis of Barker-coded incoherent scatter experiments is based on a matched filter with an impulse response which is a mirror image of the code itself. The method produces small sidelobes which cause contamination from regions outside the nominal range gate. A corresponding effect is also encountered in the lag direction, where individual lag estimates are biased by the variation of the plasma autocorrelation function around the nominal lag value. The present paper introduces a new method of analysing Barker-coded experiments by means of stochastic inversion. Since it does not apply a decoding filter, it does not suffer from drawbacks caused by the sidelobes of the range ambiguity function. The method combines the profile of each full lag and a number of surrounding fractional lags into a single inversion problem. Error analysis also indicates that the statistical accuracy given by inversion is better than that obtained by means of standard decoding. Furthermore, the inversion method gives a possibility to reduce the bias due to the variation of the autocorrelation around the nominal lag. In this paper the method is described and applied to data obtained by means of the EISCAT Svalbard radar. In addition, it is shown that mathematical inversion can be used instead of the the conventional height integration. Key words. Radio science (ionospheric physics; signal processing; instruments and techniques)
format Article in Journal/Newspaper
author B. Damtie
M. S. Lehtinen
T. Nygrén
author_facet B. Damtie
M. S. Lehtinen
T. Nygrén
author_sort B. Damtie
title Decoding of Barker-coded incoherent scatter measurements by means ofmathematical inversion
title_short Decoding of Barker-coded incoherent scatter measurements by means ofmathematical inversion
title_full Decoding of Barker-coded incoherent scatter measurements by means ofmathematical inversion
title_fullStr Decoding of Barker-coded incoherent scatter measurements by means ofmathematical inversion
title_full_unstemmed Decoding of Barker-coded incoherent scatter measurements by means ofmathematical inversion
title_sort decoding of barker-coded incoherent scatter measurements by means ofmathematical inversion
publisher Copernicus Publications
publishDate 2004
url https://doi.org/10.5194/angeo-22-3-2004
https://doaj.org/article/c89067e3100f4e0498f525aa166a45af
geographic Svalbard
geographic_facet Svalbard
genre EISCAT
Svalbard
genre_facet EISCAT
Svalbard
op_source Annales Geophysicae, Vol 22, Pp 3-13 (2004)
op_relation https://www.ann-geophys.net/22/3/2004/angeo-22-3-2004.pdf
https://doaj.org/toc/0992-7689
https://doaj.org/toc/1432-0576
doi:10.5194/angeo-22-3-2004
0992-7689
1432-0576
https://doaj.org/article/c89067e3100f4e0498f525aa166a45af
op_doi https://doi.org/10.5194/angeo-22-3-2004
container_title Annales Geophysicae
container_volume 22
container_issue 1
container_start_page 3
op_container_end_page 13
_version_ 1766400381550592000