Frequency dependent power fluctuations: a feature of the ESR system or physical?
International audience The k-dependence of the received power in high signal-to-noise ratio (SNR) conditions, occurring for naturally enhanced ion-acoustic lines (NEIALs) and for real satellites, is investigated by using the EISCAT Svalbard Radar (ESR), where the data are recorded in eight separate...
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ftuniversailles:oai:HAL:hal-00329165v1 2024-04-28T08:17:34+00:00 Frequency dependent power fluctuations: a feature of the ESR system or physical? Ogawa, Y. Forme, F. Buchert, S. C. Solar-Terrestrial Environment Laboratory Nagoya (STEL) Nagoya University Centre d'étude des environnements terrestre et planétaires (CETP) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS) 2000 https://hal.science/hal-00329165 https://hal.science/hal-00329165/document https://hal.science/hal-00329165/file/angeo-18-1224-2000.pdf en eng HAL CCSD European Geosciences Union hal-00329165 https://hal.science/hal-00329165 https://hal.science/hal-00329165/document https://hal.science/hal-00329165/file/angeo-18-1224-2000.pdf info:eu-repo/semantics/OpenAccess ISSN: 0992-7689 EISSN: 1432-0576 Annales Geophysicae https://hal.science/hal-00329165 Annales Geophysicae, 2000, 18 (9), pp.1224-1230 [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 2000 ftuniversailles 2024-04-04T17:32:49Z International audience The k-dependence of the received power in high signal-to-noise ratio (SNR) conditions, occurring for naturally enhanced ion-acoustic lines (NEIALs) and for real satellites, is investigated by using the EISCAT Svalbard Radar (ESR), where the data are recorded in eight separate channels using different frequencies. For the real satellites we find large variations of the relative powers from event to event, which is probably due to a different number of pulses catching the satellite over the integration period. However, the large power difference remains unexpected in one case. Over short time scale ( < 10 s) the relative power difference seems to be highly stable. For most NEIAL events the differences between channels are within noise level. In a few cases variations of the relative power well above both the estimated and expected 1-sigma level occur over a signal preintegrated profile. We thus suggest that the frequency dependence of the power in NEIAL events has its origin in the scattering medium itself as the most plausible explanation. Key words: Ionosphere (auroral ionosphere; plasma waves and instabilities; instruments and techniques) Article in Journal/Newspaper EISCAT Svalbard Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQ |
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Open Polar |
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Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQ |
op_collection_id |
ftuniversailles |
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 Ogawa, Y. Forme, F. Buchert, S. C. Frequency dependent power fluctuations: a feature of the ESR system or physical? |
topic_facet |
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.STU]Sciences of the Universe [physics]/Earth Sciences |
description |
International audience The k-dependence of the received power in high signal-to-noise ratio (SNR) conditions, occurring for naturally enhanced ion-acoustic lines (NEIALs) and for real satellites, is investigated by using the EISCAT Svalbard Radar (ESR), where the data are recorded in eight separate channels using different frequencies. For the real satellites we find large variations of the relative powers from event to event, which is probably due to a different number of pulses catching the satellite over the integration period. However, the large power difference remains unexpected in one case. Over short time scale ( < 10 s) the relative power difference seems to be highly stable. For most NEIAL events the differences between channels are within noise level. In a few cases variations of the relative power well above both the estimated and expected 1-sigma level occur over a signal preintegrated profile. We thus suggest that the frequency dependence of the power in NEIAL events has its origin in the scattering medium itself as the most plausible explanation. Key words: Ionosphere (auroral ionosphere; plasma waves and instabilities; instruments and techniques) |
author2 |
Solar-Terrestrial Environment Laboratory Nagoya (STEL) Nagoya University Centre d'étude des environnements terrestre et planétaires (CETP) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS) |
format |
Article in Journal/Newspaper |
author |
Ogawa, Y. Forme, F. Buchert, S. C. |
author_facet |
Ogawa, Y. Forme, F. Buchert, S. C. |
author_sort |
Ogawa, Y. |
title |
Frequency dependent power fluctuations: a feature of the ESR system or physical? |
title_short |
Frequency dependent power fluctuations: a feature of the ESR system or physical? |
title_full |
Frequency dependent power fluctuations: a feature of the ESR system or physical? |
title_fullStr |
Frequency dependent power fluctuations: a feature of the ESR system or physical? |
title_full_unstemmed |
Frequency dependent power fluctuations: a feature of the ESR system or physical? |
title_sort |
frequency dependent power fluctuations: a feature of the esr system or physical? |
publisher |
HAL CCSD |
publishDate |
2000 |
url |
https://hal.science/hal-00329165 https://hal.science/hal-00329165/document https://hal.science/hal-00329165/file/angeo-18-1224-2000.pdf |
genre |
EISCAT Svalbard |
genre_facet |
EISCAT Svalbard |
op_source |
ISSN: 0992-7689 EISSN: 1432-0576 Annales Geophysicae https://hal.science/hal-00329165 Annales Geophysicae, 2000, 18 (9), pp.1224-1230 |
op_relation |
hal-00329165 https://hal.science/hal-00329165 https://hal.science/hal-00329165/document https://hal.science/hal-00329165/file/angeo-18-1224-2000.pdf |
op_rights |
info:eu-repo/semantics/OpenAccess |
_version_ |
1797582075373551616 |