Using colour in auroral imaging

The prototype of an auroral colour camera named Rainbow was run at the Auroral Station in Adventdalen, Svalbard, Norway, during a Finnish optical campaign in February, 2004. Instead of narrow band-pass filters and grey-scale images, this imager records colour images of the aurora using four wide-ban...

Full description

Bibliographic Details
Published in:Canadian Journal of Physics
Main Authors: Partamies, N, Syrjäsuo, M, Donovan, E
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 2007
Subjects:
Online Access:http://dx.doi.org/10.1139/p06-090
http://www.nrcresearchpress.com/doi/pdf/10.1139/p06-090
id crcansciencepubl:10.1139/p06-090
record_format openpolar
spelling crcansciencepubl:10.1139/p06-090 2023-12-17T10:17:44+01:00 Using colour in auroral imaging Partamies, N Syrjäsuo, M Donovan, E 2007 http://dx.doi.org/10.1139/p06-090 http://www.nrcresearchpress.com/doi/pdf/10.1139/p06-090 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Physics volume 85, issue 2, page 101-109 ISSN 0008-4204 1208-6045 General Physics and Astronomy journal-article 2007 crcansciencepubl https://doi.org/10.1139/p06-090 2023-11-19T13:38:44Z The prototype of an auroral colour camera named Rainbow was run at the Auroral Station in Adventdalen, Svalbard, Norway, during a Finnish optical campaign in February, 2004. Instead of narrow band-pass filters and grey-scale images, this imager records colour images of the aurora using four wide-band channels (a colour CCD) with the field-of-view of about 150°. In this study, we show the results of fitting the four Rainbow channels (cyan-magenta, cyan-green, yellow-magenta, yellow-green) to reconstruct the traditionally filtered auroral wavelengths: green (557.7 nm), red (630.0 nm), and blue (427.8 nm), which were simultaneously recorded by the meridian scanning photometer (MSP) at the same station. This fit is qualitatively extremely good and almost linear throughout the data. In studying the auroral evolution during substorms, there is no significant difference whether MSP or Rainbow data are used. However, due to wide-band colour channels, the background illumination has a strong effect on the Rainbow data. During low signal levels (only background or faint aurora) the reconstruction errors are larger. The data for this study were captured on 21 February 2004. The time period of interest includes a substorm sequence, which is examined using colour auroral images and data from the MSP. PACS No.: 94.20.Ac Article in Journal/Newspaper Adventdalen Svalbard Canadian Science Publishing (via Crossref) Svalbard Norway Adventdalen ENVELOPE(16.264,16.264,78.181,78.181) Canadian Journal of Physics 85 2 101 109
institution Open Polar
collection Canadian Science Publishing (via Crossref)
op_collection_id crcansciencepubl
language English
topic General Physics and Astronomy
spellingShingle General Physics and Astronomy
Partamies, N
Syrjäsuo, M
Donovan, E
Using colour in auroral imaging
topic_facet General Physics and Astronomy
description The prototype of an auroral colour camera named Rainbow was run at the Auroral Station in Adventdalen, Svalbard, Norway, during a Finnish optical campaign in February, 2004. Instead of narrow band-pass filters and grey-scale images, this imager records colour images of the aurora using four wide-band channels (a colour CCD) with the field-of-view of about 150°. In this study, we show the results of fitting the four Rainbow channels (cyan-magenta, cyan-green, yellow-magenta, yellow-green) to reconstruct the traditionally filtered auroral wavelengths: green (557.7 nm), red (630.0 nm), and blue (427.8 nm), which were simultaneously recorded by the meridian scanning photometer (MSP) at the same station. This fit is qualitatively extremely good and almost linear throughout the data. In studying the auroral evolution during substorms, there is no significant difference whether MSP or Rainbow data are used. However, due to wide-band colour channels, the background illumination has a strong effect on the Rainbow data. During low signal levels (only background or faint aurora) the reconstruction errors are larger. The data for this study were captured on 21 February 2004. The time period of interest includes a substorm sequence, which is examined using colour auroral images and data from the MSP. PACS No.: 94.20.Ac
format Article in Journal/Newspaper
author Partamies, N
Syrjäsuo, M
Donovan, E
author_facet Partamies, N
Syrjäsuo, M
Donovan, E
author_sort Partamies, N
title Using colour in auroral imaging
title_short Using colour in auroral imaging
title_full Using colour in auroral imaging
title_fullStr Using colour in auroral imaging
title_full_unstemmed Using colour in auroral imaging
title_sort using colour in auroral imaging
publisher Canadian Science Publishing
publishDate 2007
url http://dx.doi.org/10.1139/p06-090
http://www.nrcresearchpress.com/doi/pdf/10.1139/p06-090
long_lat ENVELOPE(16.264,16.264,78.181,78.181)
geographic Svalbard
Norway
Adventdalen
geographic_facet Svalbard
Norway
Adventdalen
genre Adventdalen
Svalbard
genre_facet Adventdalen
Svalbard
op_source Canadian Journal of Physics
volume 85, issue 2, page 101-109
ISSN 0008-4204 1208-6045
op_rights http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining
op_doi https://doi.org/10.1139/p06-090
container_title Canadian Journal of Physics
container_volume 85
container_issue 2
container_start_page 101
op_container_end_page 109
_version_ 1785585436360441856