The effect of the high-speed stream following the corotating interaction region on the geomagnetic activities

International audience The high-speed stream following the corotating interaction regions (CIRs) was analyzed. As a result of the analysis, it is found that the geomagnetic field is continuously disturbed in the high-speed stream in question. The geomagnetic disturbances with long duration recurred...

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Main Author: Watari, S.
Other Authors: Communications Research Laboratory, 4-2-1 Nukuikita
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 1997
Subjects:
Online Access:https://hal.science/hal-00316261
https://hal.science/hal-00316261/document
https://hal.science/hal-00316261/file/angeo-15-662-1997.pdf
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spelling ftccsdartic:oai:HAL:hal-00316261v1 2023-11-12T04:26:21+01:00 The effect of the high-speed stream following the corotating interaction region on the geomagnetic activities Watari, S. Communications Research Laboratory 4-2-1 Nukuikita 1997 https://hal.science/hal-00316261 https://hal.science/hal-00316261/document https://hal.science/hal-00316261/file/angeo-15-662-1997.pdf en eng HAL CCSD European Geosciences Union hal-00316261 https://hal.science/hal-00316261 https://hal.science/hal-00316261/document https://hal.science/hal-00316261/file/angeo-15-662-1997.pdf info:eu-repo/semantics/OpenAccess ISSN: 0992-7689 EISSN: 1432-0576 Annales Geophysicae https://hal.science/hal-00316261 Annales Geophysicae, 1997, 15 (6), pp.662-670 [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.STU]Sciences of the Universe [physics]/Earth Sciences info:eu-repo/semantics/article Journal articles 1997 ftccsdartic 2023-10-21T23:08:39Z International audience The high-speed stream following the corotating interaction regions (CIRs) was analyzed. As a result of the analysis, it is found that the geomagnetic field is continuously disturbed in the high-speed stream in question. The geomagnetic disturbances with long duration recurred several rotations between December 1993 and June 1994. These disturbances were associated with a large recurrent coronal hole expanding from the south pole of the Sun. High-speed solar wind from this coronal hole was observed by the IMP-8 satellite during this period. However, the observed intensities of the geomagnetic disturbances were different for each recurrent period. This is explained by the seasonal effect. The disturbed geomagnetic condition continued in the high-speed stream after the passage of the CIRs. The long duration of these disturbances can be explained by the continuous energy input into the Earth's magnetosphere from the high-speed regions following the CIRs. This kind of long-duration geomagnetic disturbance in association with coronal holes has been observed in the declining phase of other solar cycles. The relation between the coronal-hole area and the maximum solar-wind velocity is not good for the well-developed large coronal hole analyzed here. Article in Journal/Newspaper South pole Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) South Pole
institution Open Polar
collection Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe)
op_collection_id ftccsdartic
language English
topic [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences
spellingShingle [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences
Watari, S.
The effect of the high-speed stream following the corotating interaction region on the geomagnetic activities
topic_facet [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences
description International audience The high-speed stream following the corotating interaction regions (CIRs) was analyzed. As a result of the analysis, it is found that the geomagnetic field is continuously disturbed in the high-speed stream in question. The geomagnetic disturbances with long duration recurred several rotations between December 1993 and June 1994. These disturbances were associated with a large recurrent coronal hole expanding from the south pole of the Sun. High-speed solar wind from this coronal hole was observed by the IMP-8 satellite during this period. However, the observed intensities of the geomagnetic disturbances were different for each recurrent period. This is explained by the seasonal effect. The disturbed geomagnetic condition continued in the high-speed stream after the passage of the CIRs. The long duration of these disturbances can be explained by the continuous energy input into the Earth's magnetosphere from the high-speed regions following the CIRs. This kind of long-duration geomagnetic disturbance in association with coronal holes has been observed in the declining phase of other solar cycles. The relation between the coronal-hole area and the maximum solar-wind velocity is not good for the well-developed large coronal hole analyzed here.
author2 Communications Research Laboratory
4-2-1 Nukuikita
format Article in Journal/Newspaper
author Watari, S.
author_facet Watari, S.
author_sort Watari, S.
title The effect of the high-speed stream following the corotating interaction region on the geomagnetic activities
title_short The effect of the high-speed stream following the corotating interaction region on the geomagnetic activities
title_full The effect of the high-speed stream following the corotating interaction region on the geomagnetic activities
title_fullStr The effect of the high-speed stream following the corotating interaction region on the geomagnetic activities
title_full_unstemmed The effect of the high-speed stream following the corotating interaction region on the geomagnetic activities
title_sort effect of the high-speed stream following the corotating interaction region on the geomagnetic activities
publisher HAL CCSD
publishDate 1997
url https://hal.science/hal-00316261
https://hal.science/hal-00316261/document
https://hal.science/hal-00316261/file/angeo-15-662-1997.pdf
geographic South Pole
geographic_facet South Pole
genre South pole
genre_facet South pole
op_source ISSN: 0992-7689
EISSN: 1432-0576
Annales Geophysicae
https://hal.science/hal-00316261
Annales Geophysicae, 1997, 15 (6), pp.662-670
op_relation hal-00316261
https://hal.science/hal-00316261
https://hal.science/hal-00316261/document
https://hal.science/hal-00316261/file/angeo-15-662-1997.pdf
op_rights info:eu-repo/semantics/OpenAccess
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