First Results from a Comparison of Ground-Based Ionospheric Measurements in the Southern Hemisphere and the USU Global Ionospheric Model

The F-layer parameters N_mF_2 and h_mF_2 have been derived from measurements made at two Antarctic stations for quiet days during the austral summer and winter of 1982. Siple (76°S, 84°W) and Halley (76°S, 27°W) are both sited near L≈4.2 and use essentially identical digital HF sounding radars. Even...

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Main Authors: Berkey, F. T., Sojka, Jan Josef, Jarvis, M. J.
Format: Text
Language:unknown
Published: Hosted by Utah State University Libraries 1987
Subjects:
Online Access:https://digitalcommons.usu.edu/physics_facpub/121
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author Berkey, F. T.
Sojka, Jan Josef
Jarvis, M. J.
author_facet Berkey, F. T.
Sojka, Jan Josef
Jarvis, M. J.
author_sort Berkey, F. T.
collection Utah State University: DigitalCommons@USU
description The F-layer parameters N_mF_2 and h_mF_2 have been derived from measurements made at two Antarctic stations for quiet days during the austral summer and winter of 1982. Siple (76°S, 84°W) and Halley (76°S, 27°W) are both sited near L≈4.2 and use essentially identical digital HF sounding radars. Even under quiet conditions, systematic differences in N_mF_2 and h_mF_2 can be observed at the two sites. Insight into the source of these differences can be obtained from a comparison of the ionospheric data with theoretical data derived from the USU global ionospheric model. Under austral winter conditions, a relatively good model-observational comparison is obtained. However, for austral summer conditions this agreement is poorer, apparently due to the simplicity of the neutral wind incorporated into the ionospheric model.
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geographic Antarctic
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op_collection_id ftutahsudc
op_relation https://digitalcommons.usu.edu/physics_facpub/121
op_rights Copyright for this work is held by the author. Transmission or reproduction of materials protected by copyright beyond that allowed by fair use requires the written permission of the copyright owners. Works not in the public domain cannot be commercially exploited without permission of the copyright owner. Responsibility for any use rests exclusively with the user. For more information contact the Institutional Repository Librarian at digitalcommons@usu.edu.
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spelling ftutahsudc:oai:digitalcommons.usu.edu:physics_facpub-1120 2025-04-13T14:09:24+00:00 First Results from a Comparison of Ground-Based Ionospheric Measurements in the Southern Hemisphere and the USU Global Ionospheric Model Berkey, F. T. Sojka, Jan Josef Jarvis, M. J. 1987-01-01T08:00:00Z https://digitalcommons.usu.edu/physics_facpub/121 unknown Hosted by Utah State University Libraries https://digitalcommons.usu.edu/physics_facpub/121 Copyright for this work is held by the author. Transmission or reproduction of materials protected by copyright beyond that allowed by fair use requires the written permission of the copyright owners. Works not in the public domain cannot be commercially exploited without permission of the copyright owner. Responsibility for any use rests exclusively with the user. For more information contact the Institutional Repository Librarian at digitalcommons@usu.edu. All Physics Faculty Publications results comparison ground-based ionospheric measurements southern hemisphere USU global ionospheric model Physics text 1987 ftutahsudc 2025-03-19T07:13:28Z The F-layer parameters N_mF_2 and h_mF_2 have been derived from measurements made at two Antarctic stations for quiet days during the austral summer and winter of 1982. Siple (76°S, 84°W) and Halley (76°S, 27°W) are both sited near L≈4.2 and use essentially identical digital HF sounding radars. Even under quiet conditions, systematic differences in N_mF_2 and h_mF_2 can be observed at the two sites. Insight into the source of these differences can be obtained from a comparison of the ionospheric data with theoretical data derived from the USU global ionospheric model. Under austral winter conditions, a relatively good model-observational comparison is obtained. However, for austral summer conditions this agreement is poorer, apparently due to the simplicity of the neutral wind incorporated into the ionospheric model. Text Antarc* Antarctic Utah State University: DigitalCommons@USU Antarctic Austral Siple ENVELOPE(-83.917,-83.917,-75.917,-75.917)
spellingShingle results
comparison
ground-based
ionospheric measurements
southern hemisphere
USU
global ionospheric model
Physics
Berkey, F. T.
Sojka, Jan Josef
Jarvis, M. J.
First Results from a Comparison of Ground-Based Ionospheric Measurements in the Southern Hemisphere and the USU Global Ionospheric Model
title First Results from a Comparison of Ground-Based Ionospheric Measurements in the Southern Hemisphere and the USU Global Ionospheric Model
title_full First Results from a Comparison of Ground-Based Ionospheric Measurements in the Southern Hemisphere and the USU Global Ionospheric Model
title_fullStr First Results from a Comparison of Ground-Based Ionospheric Measurements in the Southern Hemisphere and the USU Global Ionospheric Model
title_full_unstemmed First Results from a Comparison of Ground-Based Ionospheric Measurements in the Southern Hemisphere and the USU Global Ionospheric Model
title_short First Results from a Comparison of Ground-Based Ionospheric Measurements in the Southern Hemisphere and the USU Global Ionospheric Model
title_sort first results from a comparison of ground-based ionospheric measurements in the southern hemisphere and the usu global ionospheric model
topic results
comparison
ground-based
ionospheric measurements
southern hemisphere
USU
global ionospheric model
Physics
topic_facet results
comparison
ground-based
ionospheric measurements
southern hemisphere
USU
global ionospheric model
Physics
url https://digitalcommons.usu.edu/physics_facpub/121