Results of Polar Ionospheric Plasma Observation by the Rocket S-210JA-29 (f. Polar Ionosphere) (Proceedings of the Second Symposium on Coordinated Observations of the Ionosphere and the Magnetosphere in the Polar Regions : Part II)

In order to measure the electron density and density irregularities in the polar ionosphere sounding rocket S-210JA-29 was fired at 19h15m (LT) on July 12, 1977 from Syowa Station, Antarctica. The observational results show that there exists an E_s layer in the altitude region between 85 km and 115...

Full description

Bibliographic Details
Main Authors: Shigeru MIYAZAKI, Hirotaka MORI, Tadahiko OGAWA
Format: Article in Journal/Newspaper
Language:English
Published: National Institute of Polar Research 1980
Subjects:
geo
Online Access:https://doi.org/10.15094/00008161
https://doaj.org/article/463ab1dd6b0f46ca9b8093878096cfcb
id fttriple:oai:gotriple.eu:oai:doaj.org/article:463ab1dd6b0f46ca9b8093878096cfcb
record_format openpolar
spelling fttriple:oai:gotriple.eu:oai:doaj.org/article:463ab1dd6b0f46ca9b8093878096cfcb 2023-05-15T14:04:55+02:00 Results of Polar Ionospheric Plasma Observation by the Rocket S-210JA-29 (f. Polar Ionosphere) (Proceedings of the Second Symposium on Coordinated Observations of the Ionosphere and the Magnetosphere in the Polar Regions : Part II) Shigeru MIYAZAKI Hirotaka MORI Tadahiko OGAWA 1980-03-01 https://doi.org/10.15094/00008161 https://doaj.org/article/463ab1dd6b0f46ca9b8093878096cfcb en other eng National Institute of Polar Research doi:10.15094/00008161 0085-7289 2432-079X https://doaj.org/article/463ab1dd6b0f46ca9b8093878096cfcb undefined Antarctic Record, Iss 69, Pp 126-136 (1980) geo Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 1980 fttriple https://doi.org/10.15094/00008161 2023-01-22T19:12:23Z In order to measure the electron density and density irregularities in the polar ionosphere sounding rocket S-210JA-29 was fired at 19h15m (LT) on July 12, 1977 from Syowa Station, Antarctica. The observational results show that there exists an E_s layer in the altitude region between 85 km and 115 km, and its electron density is 2-4×10^4/cm^3, and the electron density above 115 km is decreasing. The values of the measured electron density profile are rather low compared with the nighttime electron density profiles which were observed until now. The profiles of the electrostatic noise spectrum show remarkable changes against the altitude. The amolitudes of spectrum of the electrostatic noise become great in the region between 95 km and 106 km in the ascending time and between 103 km and 112 km in the descending time. The amplitudes of spectrum have a peak value at 1-2 kHz and the spectrum spreads out to the higher frequency region. Assuming that the observed spectrum of the electrostatic noise to be a natural one, these irregularities seem to be caused partly by a two-stream plasma instability mechanism. Article in Journal/Newspaper Antarc* Antarctica Unknown Syowa Station
institution Open Polar
collection Unknown
op_collection_id fttriple
language English
topic geo
spellingShingle geo
Shigeru MIYAZAKI
Hirotaka MORI
Tadahiko OGAWA
Results of Polar Ionospheric Plasma Observation by the Rocket S-210JA-29 (f. Polar Ionosphere) (Proceedings of the Second Symposium on Coordinated Observations of the Ionosphere and the Magnetosphere in the Polar Regions : Part II)
topic_facet geo
description In order to measure the electron density and density irregularities in the polar ionosphere sounding rocket S-210JA-29 was fired at 19h15m (LT) on July 12, 1977 from Syowa Station, Antarctica. The observational results show that there exists an E_s layer in the altitude region between 85 km and 115 km, and its electron density is 2-4×10^4/cm^3, and the electron density above 115 km is decreasing. The values of the measured electron density profile are rather low compared with the nighttime electron density profiles which were observed until now. The profiles of the electrostatic noise spectrum show remarkable changes against the altitude. The amolitudes of spectrum of the electrostatic noise become great in the region between 95 km and 106 km in the ascending time and between 103 km and 112 km in the descending time. The amplitudes of spectrum have a peak value at 1-2 kHz and the spectrum spreads out to the higher frequency region. Assuming that the observed spectrum of the electrostatic noise to be a natural one, these irregularities seem to be caused partly by a two-stream plasma instability mechanism.
format Article in Journal/Newspaper
author Shigeru MIYAZAKI
Hirotaka MORI
Tadahiko OGAWA
author_facet Shigeru MIYAZAKI
Hirotaka MORI
Tadahiko OGAWA
author_sort Shigeru MIYAZAKI
title Results of Polar Ionospheric Plasma Observation by the Rocket S-210JA-29 (f. Polar Ionosphere) (Proceedings of the Second Symposium on Coordinated Observations of the Ionosphere and the Magnetosphere in the Polar Regions : Part II)
title_short Results of Polar Ionospheric Plasma Observation by the Rocket S-210JA-29 (f. Polar Ionosphere) (Proceedings of the Second Symposium on Coordinated Observations of the Ionosphere and the Magnetosphere in the Polar Regions : Part II)
title_full Results of Polar Ionospheric Plasma Observation by the Rocket S-210JA-29 (f. Polar Ionosphere) (Proceedings of the Second Symposium on Coordinated Observations of the Ionosphere and the Magnetosphere in the Polar Regions : Part II)
title_fullStr Results of Polar Ionospheric Plasma Observation by the Rocket S-210JA-29 (f. Polar Ionosphere) (Proceedings of the Second Symposium on Coordinated Observations of the Ionosphere and the Magnetosphere in the Polar Regions : Part II)
title_full_unstemmed Results of Polar Ionospheric Plasma Observation by the Rocket S-210JA-29 (f. Polar Ionosphere) (Proceedings of the Second Symposium on Coordinated Observations of the Ionosphere and the Magnetosphere in the Polar Regions : Part II)
title_sort results of polar ionospheric plasma observation by the rocket s-210ja-29 (f. polar ionosphere) (proceedings of the second symposium on coordinated observations of the ionosphere and the magnetosphere in the polar regions : part ii)
publisher National Institute of Polar Research
publishDate 1980
url https://doi.org/10.15094/00008161
https://doaj.org/article/463ab1dd6b0f46ca9b8093878096cfcb
geographic Syowa Station
geographic_facet Syowa Station
genre Antarc*
Antarctica
genre_facet Antarc*
Antarctica
op_source Antarctic Record, Iss 69, Pp 126-136 (1980)
op_relation doi:10.15094/00008161
0085-7289
2432-079X
https://doaj.org/article/463ab1dd6b0f46ca9b8093878096cfcb
op_rights undefined
op_doi https://doi.org/10.15094/00008161
_version_ 1766276362143793152