APPEARANCE OF ENHANCED VLF-EMISSIONS ON 8 KC/S OBSERVED ALONG A N-S CHAIN OF STATIONS
VLF-emissions on 8 kc/s have been recorded simultaneously along a chain of stations in N-S direction: Tromso, Lycksele, Oslo and Chambon la Foret, covering a latitude difference from 70 degrees to 48 degrees N. It is shown that the polar VLF-emissions recorded close to the auroral zone at Tromso dur...
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ftdtic:AD0640470 2023-05-15T18:33:48+02:00 APPEARANCE OF ENHANCED VLF-EMISSIONS ON 8 KC/S OBSERVED ALONG A N-S CHAIN OF STATIONS Harang,L. NORWEGIAN INST OF COSMIC PHYSICS UNIV OF OSLO 1966-06-15 text/html http://www.dtic.mil/docs/citations/AD0640470 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0640470 en eng http://www.dtic.mil/docs/citations/AD0640470 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Atmospheric Physics (*ATMOSPHERICS VERY LOW FREQUENCY) NORWAY MAGNETIC STORMS ELECTROMAGNETIC RADIATION PROPAGATION METEOROLOGICAL PHENOMENA Text 1966 ftdtic 2016-02-18T19:32:18Z VLF-emissions on 8 kc/s have been recorded simultaneously along a chain of stations in N-S direction: Tromso, Lycksele, Oslo and Chambon la Foret, covering a latitude difference from 70 degrees to 48 degrees N. It is shown that the polar VLF-emissions recorded close to the auroral zone at Tromso during the night also can be traced on the records from Oslo with amplitudes of about 1/k00 - 1/500 of the Tromso amplitudes. A new type of VLF-emissions has been shown to appear at the stations Lycksele - Oslo, but not appearing at Tromso and Cambon la Foret. These low-latitude VLF-emissions appear during day time. There is thus a time difference of about 12 hours in the mean appearance of these two types of VLF-emissions. It is further pointed out that whereas the polar VLF-bursts appear during weak or moderate geomagnetic storms and in many cases a coincidence in details appears between the amplitudes of the VLF-bursts and the geomagnetic variations, the low-latitude emission appear in the day and start after the commencement of a great geomagnetic storm, usually 10-16 hours after the start. There are thus reasons to believe that the two types of VLF-emissions, the polar type recorded close to the auroral zone, and the low-latitude type recorded 5 degrees - 10 degrees to the south of the auroral zone are produced by different primary processes of excitation. (Author) See also AD-628 281. Text Tromso Tromso Defense Technical Information Center: DTIC Technical Reports database Norway Tromso ENVELOPE(16.546,16.546,68.801,68.801) |
institution |
Open Polar |
collection |
Defense Technical Information Center: DTIC Technical Reports database |
op_collection_id |
ftdtic |
language |
English |
topic |
Atmospheric Physics (*ATMOSPHERICS VERY LOW FREQUENCY) NORWAY MAGNETIC STORMS ELECTROMAGNETIC RADIATION PROPAGATION METEOROLOGICAL PHENOMENA |
spellingShingle |
Atmospheric Physics (*ATMOSPHERICS VERY LOW FREQUENCY) NORWAY MAGNETIC STORMS ELECTROMAGNETIC RADIATION PROPAGATION METEOROLOGICAL PHENOMENA Harang,L. APPEARANCE OF ENHANCED VLF-EMISSIONS ON 8 KC/S OBSERVED ALONG A N-S CHAIN OF STATIONS |
topic_facet |
Atmospheric Physics (*ATMOSPHERICS VERY LOW FREQUENCY) NORWAY MAGNETIC STORMS ELECTROMAGNETIC RADIATION PROPAGATION METEOROLOGICAL PHENOMENA |
description |
VLF-emissions on 8 kc/s have been recorded simultaneously along a chain of stations in N-S direction: Tromso, Lycksele, Oslo and Chambon la Foret, covering a latitude difference from 70 degrees to 48 degrees N. It is shown that the polar VLF-emissions recorded close to the auroral zone at Tromso during the night also can be traced on the records from Oslo with amplitudes of about 1/k00 - 1/500 of the Tromso amplitudes. A new type of VLF-emissions has been shown to appear at the stations Lycksele - Oslo, but not appearing at Tromso and Cambon la Foret. These low-latitude VLF-emissions appear during day time. There is thus a time difference of about 12 hours in the mean appearance of these two types of VLF-emissions. It is further pointed out that whereas the polar VLF-bursts appear during weak or moderate geomagnetic storms and in many cases a coincidence in details appears between the amplitudes of the VLF-bursts and the geomagnetic variations, the low-latitude emission appear in the day and start after the commencement of a great geomagnetic storm, usually 10-16 hours after the start. There are thus reasons to believe that the two types of VLF-emissions, the polar type recorded close to the auroral zone, and the low-latitude type recorded 5 degrees - 10 degrees to the south of the auroral zone are produced by different primary processes of excitation. (Author) See also AD-628 281. |
author2 |
NORWEGIAN INST OF COSMIC PHYSICS UNIV OF OSLO |
format |
Text |
author |
Harang,L. |
author_facet |
Harang,L. |
author_sort |
Harang,L. |
title |
APPEARANCE OF ENHANCED VLF-EMISSIONS ON 8 KC/S OBSERVED ALONG A N-S CHAIN OF STATIONS |
title_short |
APPEARANCE OF ENHANCED VLF-EMISSIONS ON 8 KC/S OBSERVED ALONG A N-S CHAIN OF STATIONS |
title_full |
APPEARANCE OF ENHANCED VLF-EMISSIONS ON 8 KC/S OBSERVED ALONG A N-S CHAIN OF STATIONS |
title_fullStr |
APPEARANCE OF ENHANCED VLF-EMISSIONS ON 8 KC/S OBSERVED ALONG A N-S CHAIN OF STATIONS |
title_full_unstemmed |
APPEARANCE OF ENHANCED VLF-EMISSIONS ON 8 KC/S OBSERVED ALONG A N-S CHAIN OF STATIONS |
title_sort |
appearance of enhanced vlf-emissions on 8 kc/s observed along a n-s chain of stations |
publishDate |
1966 |
url |
http://www.dtic.mil/docs/citations/AD0640470 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=AD0640470 |
long_lat |
ENVELOPE(16.546,16.546,68.801,68.801) |
geographic |
Norway Tromso |
geographic_facet |
Norway Tromso |
genre |
Tromso Tromso |
genre_facet |
Tromso Tromso |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/AD0640470 |
op_rights |
APPROVED FOR PUBLIC RELEASE |
_version_ |
1766218443088986112 |