Phase calibration of the EISCAT Svalbard Radar interferometer using optical satellite signatures

Abstract. The link between natural ion-line enhancements in radar spectra and auroral activity has been the subject of recent studies but conclusions have been limited by the spatial and temporal resolution previously available. The next challenge is to use shorter sub-second integration times in co...

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Main Authors: J. M. Sullivan, N. Ivchenko, M. Lockwood, T. Grydel, E. M. Blixt, B. S. Lanchester
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.77.2311
http://www.phys.uit.no/~tom/publications/2006/ag-24-2419.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.77.2311 2023-05-15T16:04:33+02:00 Phase calibration of the EISCAT Svalbard Radar interferometer using optical satellite signatures J. M. Sullivan N. Ivchenko M. Lockwood T. Grydel E. M. Blixt B. S. Lanchester The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.77.2311 http://www.phys.uit.no/~tom/publications/2006/ag-24-2419.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.77.2311 http://www.phys.uit.no/~tom/publications/2006/ag-24-2419.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.phys.uit.no/~tom/publications/2006/ag-24-2419.pdf Instruments and techniques text ftciteseerx 2016-01-08T19:09:12Z Abstract. The link between natural ion-line enhancements in radar spectra and auroral activity has been the subject of recent studies but conclusions have been limited by the spatial and temporal resolution previously available. The next challenge is to use shorter sub-second integration times in combination with interferometric programmes to resolve spatial structure within the main radar beam, and so relate enhanced filaments to individual auroral rays. This paper presents initial studies of a technique, using optical and spectral satellite signatures, to calibrate the received phase of a signal with the position of the scattering source along the interferometric baseline of the EISCAT Svalbard Radar. It is shown that a consistent relationship can be found only if the satellite passage through the phase fringes is adjusted from the passage predicted by optical tracking. This required adjustment is interpreted as being due to the vector between the theoretical focusing points of the two antennae, i.e. the true radar baseline, differing from the baseline obtained by survey between the antenna foot points. A method to obtain a measurement of the true interferometric baseline using multiple satellite passes is outlined. Text EISCAT Svalbard Unknown Svalbard
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
topic Instruments and techniques
spellingShingle Instruments and techniques
J. M. Sullivan
N. Ivchenko
M. Lockwood
T. Grydel
E. M. Blixt
B. S. Lanchester
Phase calibration of the EISCAT Svalbard Radar interferometer using optical satellite signatures
topic_facet Instruments and techniques
description Abstract. The link between natural ion-line enhancements in radar spectra and auroral activity has been the subject of recent studies but conclusions have been limited by the spatial and temporal resolution previously available. The next challenge is to use shorter sub-second integration times in combination with interferometric programmes to resolve spatial structure within the main radar beam, and so relate enhanced filaments to individual auroral rays. This paper presents initial studies of a technique, using optical and spectral satellite signatures, to calibrate the received phase of a signal with the position of the scattering source along the interferometric baseline of the EISCAT Svalbard Radar. It is shown that a consistent relationship can be found only if the satellite passage through the phase fringes is adjusted from the passage predicted by optical tracking. This required adjustment is interpreted as being due to the vector between the theoretical focusing points of the two antennae, i.e. the true radar baseline, differing from the baseline obtained by survey between the antenna foot points. A method to obtain a measurement of the true interferometric baseline using multiple satellite passes is outlined.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author J. M. Sullivan
N. Ivchenko
M. Lockwood
T. Grydel
E. M. Blixt
B. S. Lanchester
author_facet J. M. Sullivan
N. Ivchenko
M. Lockwood
T. Grydel
E. M. Blixt
B. S. Lanchester
author_sort J. M. Sullivan
title Phase calibration of the EISCAT Svalbard Radar interferometer using optical satellite signatures
title_short Phase calibration of the EISCAT Svalbard Radar interferometer using optical satellite signatures
title_full Phase calibration of the EISCAT Svalbard Radar interferometer using optical satellite signatures
title_fullStr Phase calibration of the EISCAT Svalbard Radar interferometer using optical satellite signatures
title_full_unstemmed Phase calibration of the EISCAT Svalbard Radar interferometer using optical satellite signatures
title_sort phase calibration of the eiscat svalbard radar interferometer using optical satellite signatures
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.77.2311
http://www.phys.uit.no/~tom/publications/2006/ag-24-2419.pdf
geographic Svalbard
geographic_facet Svalbard
genre EISCAT
Svalbard
genre_facet EISCAT
Svalbard
op_source http://www.phys.uit.no/~tom/publications/2006/ag-24-2419.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.77.2311
http://www.phys.uit.no/~tom/publications/2006/ag-24-2419.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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