Determination of the altitudinal peak of Cosmic Noise Absorption using a vertical parallax technique

The riometry technique is limited by its inability to directly determine the altitude of the principal ionospheric absorption layer during periods of enhanced Cosmic Noise Absorption (CNA). We describe here a technique based on the simple vertical parallax principle, enabling direct measurements of...

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Bibliographic Details
Main Authors: Terkildsen, M. B., Fraser, B. J., Yamagishi, H.
Other Authors: The University of Newcastle. Faculty of Science & Information Technology, School of Mathematical and Physical Sciences
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union 2004
Subjects:
Online Access:http://hdl.handle.net/1959.13/34004
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spelling ftunivnewcastnsw:uon:3461 2023-05-15T13:45:38+02:00 Determination of the altitudinal peak of Cosmic Noise Absorption using a vertical parallax technique Terkildsen, M. B. Fraser, B. J. Yamagishi, H. The University of Newcastle. Faculty of Science & Information Technology, School of Mathematical and Physical Sciences 2004 http://hdl.handle.net/1959.13/34004 eng eng American Geophysical Union Geophysical Research Letters Vol. 31 10.1029/2003GL019068 auroral ionosphere ionosphere/magnetosphere interactions particle precipitation instruments and techniques magnetospheric physics energetic particles precipitating journal article 2004 ftunivnewcastnsw 2018-07-27T01:12:06Z The riometry technique is limited by its inability to directly determine the altitude of the principal ionospheric absorption layer during periods of enhanced Cosmic Noise Absorption (CNA). We describe here a technique based on the simple vertical parallax principle, enabling direct measurements of this altitude. The technique utilizes the overlapping beams of two closely spaced imaging riometers in Antarctica. Descriptive statistics on peak absorption heights are presented. The altitude determination of a D-region absorption event and an event that occurred in the F-region near 200 km altitude are presented in more detail. The identification of an F-region event using the parallax technique confirms earlier findings that radiowave absorption in the F-region is a potentially significant contributor to CNA. This technique enables a simple and repeatable ground-based measurement of the altitude of the CNA layer peak, and can be extended to estimating precipitation spectra based on peak absorption heights. Article in Journal/Newspaper Antarc* Antarctica NOVA: The University of Newcastle Research Online (Australia)
institution Open Polar
collection NOVA: The University of Newcastle Research Online (Australia)
op_collection_id ftunivnewcastnsw
language English
topic auroral ionosphere
ionosphere/magnetosphere interactions
particle precipitation
instruments and techniques
magnetospheric physics
energetic particles
precipitating
spellingShingle auroral ionosphere
ionosphere/magnetosphere interactions
particle precipitation
instruments and techniques
magnetospheric physics
energetic particles
precipitating
Terkildsen, M. B.
Fraser, B. J.
Yamagishi, H.
Determination of the altitudinal peak of Cosmic Noise Absorption using a vertical parallax technique
topic_facet auroral ionosphere
ionosphere/magnetosphere interactions
particle precipitation
instruments and techniques
magnetospheric physics
energetic particles
precipitating
description The riometry technique is limited by its inability to directly determine the altitude of the principal ionospheric absorption layer during periods of enhanced Cosmic Noise Absorption (CNA). We describe here a technique based on the simple vertical parallax principle, enabling direct measurements of this altitude. The technique utilizes the overlapping beams of two closely spaced imaging riometers in Antarctica. Descriptive statistics on peak absorption heights are presented. The altitude determination of a D-region absorption event and an event that occurred in the F-region near 200 km altitude are presented in more detail. The identification of an F-region event using the parallax technique confirms earlier findings that radiowave absorption in the F-region is a potentially significant contributor to CNA. This technique enables a simple and repeatable ground-based measurement of the altitude of the CNA layer peak, and can be extended to estimating precipitation spectra based on peak absorption heights.
author2 The University of Newcastle. Faculty of Science & Information Technology, School of Mathematical and Physical Sciences
format Article in Journal/Newspaper
author Terkildsen, M. B.
Fraser, B. J.
Yamagishi, H.
author_facet Terkildsen, M. B.
Fraser, B. J.
Yamagishi, H.
author_sort Terkildsen, M. B.
title Determination of the altitudinal peak of Cosmic Noise Absorption using a vertical parallax technique
title_short Determination of the altitudinal peak of Cosmic Noise Absorption using a vertical parallax technique
title_full Determination of the altitudinal peak of Cosmic Noise Absorption using a vertical parallax technique
title_fullStr Determination of the altitudinal peak of Cosmic Noise Absorption using a vertical parallax technique
title_full_unstemmed Determination of the altitudinal peak of Cosmic Noise Absorption using a vertical parallax technique
title_sort determination of the altitudinal peak of cosmic noise absorption using a vertical parallax technique
publisher American Geophysical Union
publishDate 2004
url http://hdl.handle.net/1959.13/34004
genre Antarc*
Antarctica
genre_facet Antarc*
Antarctica
op_relation Geophysical Research Letters Vol. 31
10.1029/2003GL019068
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