Polar Cap Plasma Convection Measurements and their Relevance to the Real-Time Modeling of the High Latitude Ionosphere
Plasma convection measurements, using Digisonde ionospheric sounders, have been conducted. The plasma convection or ionospheric drift measurements conducted at Thule and Qaanaaq during campaigns from Winter 1983/84 to present provide evidence, that antisunward convection dominates in the polar cap w...
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ftdtic:ADA205703 2023-05-15T16:29:56+02:00 Polar Cap Plasma Convection Measurements and their Relevance to the Real-Time Modeling of the High Latitude Ionosphere Buchau, Jurgen Anderson, David N. Weber, Edward J. Reinisch, Bodo W. Dozois, Claude AIR FORCE GEOPHYSICS LAB HANSCOM AFB MA 1987-05-07 text/html http://www.dtic.mil/docs/citations/ADA205703 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA205703 en eng http://www.dtic.mil/docs/citations/ADA205703 Approved for public release; distribution is unlimited. Document partially illegible. DTIC AND NTIS Atmospheric Physics *IONOSPHERE *CONVECTION *PLASMAS(PHYSICS) MEASUREMENT MAGNETIC FIELDS COMPUTATIONS REAL TIME GREENLAND THEORY DRIFT PROFILES REVERSIBLE PATTERNS IONOSPHERIC MODELS HIGH LATITUDES QUIET REPRINTS POLAR REGIONS VELOCITY ELECTRON DENSITY PE61102F WUAFGL464330805 Text 1987 ftdtic 2016-02-23T07:11:05Z Plasma convection measurements, using Digisonde ionospheric sounders, have been conducted. The plasma convection or ionospheric drift measurements conducted at Thule and Qaanaaq during campaigns from Winter 1983/84 to present provide evidence, that antisunward convection dominates in the polar cap with velocities typical between 300 and 900 m.sec. Drift shears were observed during periods of arc-transition (quiet magnetic conditions). Observations of the plasma drift at Goose Bay show, a drift reversal from westward to eastward around midnight CGLT. Observations at Argentia, typically a suboval/trough station, provide evidence under magnetically disturbed conditions for the midnight reversal of the antisunward flow pattern. However, the data are less consistent under magnetically quiet conditions. The proximity of the station to the boundary between corotating and convecting plasma may at times affect the consistency of the measurements. Recent theoretical calculations of electron density profiles within the high latitude/polar cap ionosphere demonstrate that the diurnal foF2 variation observed at Thule, is controlled by the plasma convections pattern and the associated drift velocities. The model calculations for Bz < 0 and Bz. approx. 0 show factor 2 to 3 differences in Nmax over Thule, supporting the stated importance of convection pattern and velocity measurements for the modelling of the high latitude ionosphere. Reprints. Pub. in The Effect of the Ionosphere on Communication, Navigation, and Surveillance Systems Based on Ionospheric Effects Symposium p659-673, 5-7 May 1987. Text Greenland Qaanaaq Thule Defense Technical Information Center: DTIC Technical Reports database Greenland Qaanaaq ENVELOPE(-69.232,-69.232,77.467,77.467) |
institution |
Open Polar |
collection |
Defense Technical Information Center: DTIC Technical Reports database |
op_collection_id |
ftdtic |
language |
English |
topic |
Atmospheric Physics *IONOSPHERE *CONVECTION *PLASMAS(PHYSICS) MEASUREMENT MAGNETIC FIELDS COMPUTATIONS REAL TIME GREENLAND THEORY DRIFT PROFILES REVERSIBLE PATTERNS IONOSPHERIC MODELS HIGH LATITUDES QUIET REPRINTS POLAR REGIONS VELOCITY ELECTRON DENSITY PE61102F WUAFGL464330805 |
spellingShingle |
Atmospheric Physics *IONOSPHERE *CONVECTION *PLASMAS(PHYSICS) MEASUREMENT MAGNETIC FIELDS COMPUTATIONS REAL TIME GREENLAND THEORY DRIFT PROFILES REVERSIBLE PATTERNS IONOSPHERIC MODELS HIGH LATITUDES QUIET REPRINTS POLAR REGIONS VELOCITY ELECTRON DENSITY PE61102F WUAFGL464330805 Buchau, Jurgen Anderson, David N. Weber, Edward J. Reinisch, Bodo W. Dozois, Claude Polar Cap Plasma Convection Measurements and their Relevance to the Real-Time Modeling of the High Latitude Ionosphere |
topic_facet |
Atmospheric Physics *IONOSPHERE *CONVECTION *PLASMAS(PHYSICS) MEASUREMENT MAGNETIC FIELDS COMPUTATIONS REAL TIME GREENLAND THEORY DRIFT PROFILES REVERSIBLE PATTERNS IONOSPHERIC MODELS HIGH LATITUDES QUIET REPRINTS POLAR REGIONS VELOCITY ELECTRON DENSITY PE61102F WUAFGL464330805 |
description |
Plasma convection measurements, using Digisonde ionospheric sounders, have been conducted. The plasma convection or ionospheric drift measurements conducted at Thule and Qaanaaq during campaigns from Winter 1983/84 to present provide evidence, that antisunward convection dominates in the polar cap with velocities typical between 300 and 900 m.sec. Drift shears were observed during periods of arc-transition (quiet magnetic conditions). Observations of the plasma drift at Goose Bay show, a drift reversal from westward to eastward around midnight CGLT. Observations at Argentia, typically a suboval/trough station, provide evidence under magnetically disturbed conditions for the midnight reversal of the antisunward flow pattern. However, the data are less consistent under magnetically quiet conditions. The proximity of the station to the boundary between corotating and convecting plasma may at times affect the consistency of the measurements. Recent theoretical calculations of electron density profiles within the high latitude/polar cap ionosphere demonstrate that the diurnal foF2 variation observed at Thule, is controlled by the plasma convections pattern and the associated drift velocities. The model calculations for Bz < 0 and Bz. approx. 0 show factor 2 to 3 differences in Nmax over Thule, supporting the stated importance of convection pattern and velocity measurements for the modelling of the high latitude ionosphere. Reprints. Pub. in The Effect of the Ionosphere on Communication, Navigation, and Surveillance Systems Based on Ionospheric Effects Symposium p659-673, 5-7 May 1987. |
author2 |
AIR FORCE GEOPHYSICS LAB HANSCOM AFB MA |
format |
Text |
author |
Buchau, Jurgen Anderson, David N. Weber, Edward J. Reinisch, Bodo W. Dozois, Claude |
author_facet |
Buchau, Jurgen Anderson, David N. Weber, Edward J. Reinisch, Bodo W. Dozois, Claude |
author_sort |
Buchau, Jurgen |
title |
Polar Cap Plasma Convection Measurements and their Relevance to the Real-Time Modeling of the High Latitude Ionosphere |
title_short |
Polar Cap Plasma Convection Measurements and their Relevance to the Real-Time Modeling of the High Latitude Ionosphere |
title_full |
Polar Cap Plasma Convection Measurements and their Relevance to the Real-Time Modeling of the High Latitude Ionosphere |
title_fullStr |
Polar Cap Plasma Convection Measurements and their Relevance to the Real-Time Modeling of the High Latitude Ionosphere |
title_full_unstemmed |
Polar Cap Plasma Convection Measurements and their Relevance to the Real-Time Modeling of the High Latitude Ionosphere |
title_sort |
polar cap plasma convection measurements and their relevance to the real-time modeling of the high latitude ionosphere |
publishDate |
1987 |
url |
http://www.dtic.mil/docs/citations/ADA205703 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA205703 |
long_lat |
ENVELOPE(-69.232,-69.232,77.467,77.467) |
geographic |
Greenland Qaanaaq |
geographic_facet |
Greenland Qaanaaq |
genre |
Greenland Qaanaaq Thule |
genre_facet |
Greenland Qaanaaq Thule |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/ADA205703 |
op_rights |
Approved for public release; distribution is unlimited. Document partially illegible. |
_version_ |
1766019650636742656 |