MAGNETIC VARIATION INSIDE THE PRINCIPAL AURORAL ZONE

Research on the distance-variability of the magnetic field components within the auroral zone was conducted with a Briunelli magnetic variation recorder at Nagurskaya Bay (Franz Josef Land). The magnetic field variation was recorded on film, continuously from the 13th of April to the 6th of May and...

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Main Authors: Fel'dshtein ,Ya I., Kurdina,E. I.
Other Authors: DIRECTORATE OF SCIENTIFIC INFORMATION SERVICES OTTAWA (ONTARIO)
Format: Text
Language:English
Published: 1960
Subjects:
Online Access:http://www.dtic.mil/docs/citations/AD0610928
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0610928
id ftdtic:AD0610928
record_format openpolar
spelling ftdtic:AD0610928 2023-05-15T15:07:03+02:00 MAGNETIC VARIATION INSIDE THE PRINCIPAL AURORAL ZONE Fel'dshtein ,Ya I. Kurdina,E. I. DIRECTORATE OF SCIENTIFIC INFORMATION SERVICES OTTAWA (ONTARIO) 1960-09 text/html http://www.dtic.mil/docs/citations/AD0610928 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0610928 en eng http://www.dtic.mil/docs/citations/AD0610928 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS (*GEOMAGNETISM FRANZ JOSEF LAND) AURORAE ARCTIC REGIONS MAGNETIC PROPERTIES MEASUREMENT INSTRUMENTATION GEOPHYSICS USSR Text 1960 ftdtic 2016-02-18T18:06:29Z Research on the distance-variability of the magnetic field components within the auroral zone was conducted with a Briunelli magnetic variation recorder at Nagurskaya Bay (Franz Josef Land). The magnetic field variation was recorded on film, continuously from the 13th of April to the 6th of May and was compared with the magnetograms of the Tikhaya Bay magnetic observatory, a distance of 108 km from Nagurskaya. For a quantitative comparison of the mobile recorder traces and the magnetograms of the constantly operating observatory, momentary values of the departures of H and Z from the quiet field were used at moments when the field assumed characteristic extreme (maximum or minimum) values. These extremes were taken in sequence, just as they occurred in the mobile recorder data, and practically all of them coincided in time with the extremes at Tikhaya Bay. From the corresponding pairs of departures from the quiet field values the calculated correlation coefficients are given in tabular form. The able also shows the ratios of the correlation coefficients to the dispersion; these ratios are an indication of the reliability of the computed correlation coefficients. Trans. of Problemy Arktiki i Artarktiki (USSR) 1960, no. 3, p. 118-119. Also available from NRC mi$0.50, ph$1.50 as C-3467, 2p. Text Arctic Franz Josef Land Defense Technical Information Center: DTIC Technical Reports database Arctic Franz Josef Land ENVELOPE(55.000,55.000,81.000,81.000) Tikhaya ENVELOPE(156.797,156.797,51.193,51.193)
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic (*GEOMAGNETISM
FRANZ JOSEF LAND)
AURORAE
ARCTIC REGIONS
MAGNETIC PROPERTIES
MEASUREMENT
INSTRUMENTATION
GEOPHYSICS
USSR
spellingShingle (*GEOMAGNETISM
FRANZ JOSEF LAND)
AURORAE
ARCTIC REGIONS
MAGNETIC PROPERTIES
MEASUREMENT
INSTRUMENTATION
GEOPHYSICS
USSR
Fel'dshtein ,Ya I.
Kurdina,E. I.
MAGNETIC VARIATION INSIDE THE PRINCIPAL AURORAL ZONE
topic_facet (*GEOMAGNETISM
FRANZ JOSEF LAND)
AURORAE
ARCTIC REGIONS
MAGNETIC PROPERTIES
MEASUREMENT
INSTRUMENTATION
GEOPHYSICS
USSR
description Research on the distance-variability of the magnetic field components within the auroral zone was conducted with a Briunelli magnetic variation recorder at Nagurskaya Bay (Franz Josef Land). The magnetic field variation was recorded on film, continuously from the 13th of April to the 6th of May and was compared with the magnetograms of the Tikhaya Bay magnetic observatory, a distance of 108 km from Nagurskaya. For a quantitative comparison of the mobile recorder traces and the magnetograms of the constantly operating observatory, momentary values of the departures of H and Z from the quiet field were used at moments when the field assumed characteristic extreme (maximum or minimum) values. These extremes were taken in sequence, just as they occurred in the mobile recorder data, and practically all of them coincided in time with the extremes at Tikhaya Bay. From the corresponding pairs of departures from the quiet field values the calculated correlation coefficients are given in tabular form. The able also shows the ratios of the correlation coefficients to the dispersion; these ratios are an indication of the reliability of the computed correlation coefficients. Trans. of Problemy Arktiki i Artarktiki (USSR) 1960, no. 3, p. 118-119. Also available from NRC mi$0.50, ph$1.50 as C-3467, 2p.
author2 DIRECTORATE OF SCIENTIFIC INFORMATION SERVICES OTTAWA (ONTARIO)
format Text
author Fel'dshtein ,Ya I.
Kurdina,E. I.
author_facet Fel'dshtein ,Ya I.
Kurdina,E. I.
author_sort Fel'dshtein ,Ya I.
title MAGNETIC VARIATION INSIDE THE PRINCIPAL AURORAL ZONE
title_short MAGNETIC VARIATION INSIDE THE PRINCIPAL AURORAL ZONE
title_full MAGNETIC VARIATION INSIDE THE PRINCIPAL AURORAL ZONE
title_fullStr MAGNETIC VARIATION INSIDE THE PRINCIPAL AURORAL ZONE
title_full_unstemmed MAGNETIC VARIATION INSIDE THE PRINCIPAL AURORAL ZONE
title_sort magnetic variation inside the principal auroral zone
publishDate 1960
url http://www.dtic.mil/docs/citations/AD0610928
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0610928
long_lat ENVELOPE(55.000,55.000,81.000,81.000)
ENVELOPE(156.797,156.797,51.193,51.193)
geographic Arctic
Franz Josef Land
Tikhaya
geographic_facet Arctic
Franz Josef Land
Tikhaya
genre Arctic
Franz Josef Land
genre_facet Arctic
Franz Josef Land
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/AD0610928
op_rights APPROVED FOR PUBLIC RELEASE
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