High resolution geomagnetic field observations at Terra Nova bay, Antarctica
he preliminary results obtained from the analysis in the micropulsation frequency range of high time resolution magnetic field data recorded at the Antarctic Italian geomagnetic observatory at Terra Nova Bay for 11 consecutive days in February 1994 are reported. The spectral index over the whole Pcl...
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ftingv:oai:www.earth-prints.org:2122/1678 2024-06-09T07:38:54+00:00 High resolution geomagnetic field observations at Terra Nova bay, Antarctica Lepidi, S. Villante, U. Vellante, M. Palangio, P. Meloni, A. Lepidi, S.; Dipartimento di Fisica, Università dell'Aquila, Italy Villante, U.; Dipartimento di Fisica, Università dell'Aquila, Italy Vellante, M.; Dipartimento di Fisica, Università dell'Aquila, Italy Palangio, P.; Istituto Nazionale di Geofisica, Roma, Italy Meloni, A.; Istituto Nazionale di Geofisica, Roma, Italy Dipartimento di Fisica, Università dell'Aquila, Italy Istituto Nazionale di Geofisica, Roma, Italy 1996-05 2836533 bytes application/pdf http://hdl.handle.net/2122/1678 en eng 3/39 (1996) http://hdl.handle.net/2122/1678 open Geomagnetic pulsations spectral index wave polarization Antartica 04. Solid Earth::04.05. Geomagnetism::04.05.05. Main geomagnetic field article 1996 ftingv 2024-05-15T08:06:18Z he preliminary results obtained from the analysis in the micropulsation frequency range of high time resolution magnetic field data recorded at the Antarctic Italian geomagnetic observatory at Terra Nova Bay for 11 consecutive days in February 1994 are reported. The spectral index over the whole Pcl-Pc5 frequency range is of the order of 3.5 and its value significantly increases beyond about 50 mHz. Spectral peaks in the Pc3 frequency range are common, especially during the daytime hours, and are probably due to the direct penetration of upstream waves in the cusp region. From the local time distribution of the micro pulsation power, a signifi - cant activity enhancement around the local magnetic noon emerges, in agreement with previous observations. The analysis of the signal polarisation characteristics in the horizontal plane shows a predominant CW polarisation in the Pcl-Pc3 frequency ranges with the major axis of the polarisation ellipse in the first quadrant. JCR Journal open Article in Journal/Newspaper Antarc* Antarctic Antarctica antartic* Earth-Prints (Istituto Nazionale di Geofisica e Vulcanologia) Antarctic Terra Nova Bay The Antarctic |
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Open Polar |
collection |
Earth-Prints (Istituto Nazionale di Geofisica e Vulcanologia) |
op_collection_id |
ftingv |
language |
English |
topic |
Geomagnetic pulsations spectral index wave polarization Antartica 04. Solid Earth::04.05. Geomagnetism::04.05.05. Main geomagnetic field |
spellingShingle |
Geomagnetic pulsations spectral index wave polarization Antartica 04. Solid Earth::04.05. Geomagnetism::04.05.05. Main geomagnetic field Lepidi, S. Villante, U. Vellante, M. Palangio, P. Meloni, A. High resolution geomagnetic field observations at Terra Nova bay, Antarctica |
topic_facet |
Geomagnetic pulsations spectral index wave polarization Antartica 04. Solid Earth::04.05. Geomagnetism::04.05.05. Main geomagnetic field |
description |
he preliminary results obtained from the analysis in the micropulsation frequency range of high time resolution magnetic field data recorded at the Antarctic Italian geomagnetic observatory at Terra Nova Bay for 11 consecutive days in February 1994 are reported. The spectral index over the whole Pcl-Pc5 frequency range is of the order of 3.5 and its value significantly increases beyond about 50 mHz. Spectral peaks in the Pc3 frequency range are common, especially during the daytime hours, and are probably due to the direct penetration of upstream waves in the cusp region. From the local time distribution of the micro pulsation power, a signifi - cant activity enhancement around the local magnetic noon emerges, in agreement with previous observations. The analysis of the signal polarisation characteristics in the horizontal plane shows a predominant CW polarisation in the Pcl-Pc3 frequency ranges with the major axis of the polarisation ellipse in the first quadrant. JCR Journal open |
author2 |
Lepidi, S.; Dipartimento di Fisica, Università dell'Aquila, Italy Villante, U.; Dipartimento di Fisica, Università dell'Aquila, Italy Vellante, M.; Dipartimento di Fisica, Università dell'Aquila, Italy Palangio, P.; Istituto Nazionale di Geofisica, Roma, Italy Meloni, A.; Istituto Nazionale di Geofisica, Roma, Italy Dipartimento di Fisica, Università dell'Aquila, Italy Istituto Nazionale di Geofisica, Roma, Italy |
format |
Article in Journal/Newspaper |
author |
Lepidi, S. Villante, U. Vellante, M. Palangio, P. Meloni, A. |
author_facet |
Lepidi, S. Villante, U. Vellante, M. Palangio, P. Meloni, A. |
author_sort |
Lepidi, S. |
title |
High resolution geomagnetic field observations at Terra Nova bay, Antarctica |
title_short |
High resolution geomagnetic field observations at Terra Nova bay, Antarctica |
title_full |
High resolution geomagnetic field observations at Terra Nova bay, Antarctica |
title_fullStr |
High resolution geomagnetic field observations at Terra Nova bay, Antarctica |
title_full_unstemmed |
High resolution geomagnetic field observations at Terra Nova bay, Antarctica |
title_sort |
high resolution geomagnetic field observations at terra nova bay, antarctica |
publishDate |
1996 |
url |
http://hdl.handle.net/2122/1678 |
geographic |
Antarctic Terra Nova Bay The Antarctic |
geographic_facet |
Antarctic Terra Nova Bay The Antarctic |
genre |
Antarc* Antarctic Antarctica antartic* |
genre_facet |
Antarc* Antarctic Antarctica antartic* |
op_relation |
3/39 (1996) http://hdl.handle.net/2122/1678 |
op_rights |
open |
_version_ |
1801376064652443648 |