A modeling study of the ionospheric equatorial anomaly based on the FormoSat-3/COSMIC data

碩士 === 國立中央大學 === 太空科學研究所 === 97 === The TaiWan Ionospheric Model (TWIM) is a numerical and phenomenological model of global ionospheric electron density (Ne) and is constructed from monthly-weighted and hourly vertical Ne profiles retrieved from FormoSat3/COSMIC GPS radio occultation measurements....

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Main Authors: Jyun-Ying Huang, 黃俊穎
Other Authors: Lung-Chih Tsai
Format: Others
Language:zh-TW
Published: 2009
Online Access:http://ndltd.ncl.edu.tw/handle/er73ke
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spelling ndltd-TW-097NCU050690112019-05-15T19:19:48Z http://ndltd.ncl.edu.tw/handle/er73ke A modeling study of the ionospheric equatorial anomaly based on the FormoSat-3/COSMIC data 運用臺灣自主電離層數值模式研究電離層赤道異常現象 Jyun-Ying Huang 黃俊穎 碩士 國立中央大學 太空科學研究所 97 The TaiWan Ionospheric Model (TWIM) is a numerical and phenomenological model of global ionospheric electron density (Ne) and is constructed from monthly-weighted and hourly vertical Ne profiles retrieved from FormoSat3/COSMIC GPS radio occultation measurements. TWIM can also provide global F2-layer critical frequency (foF2), peak density height (hmF2), and scale height (HF2) maps to study features of equatorial ionospheric anomaly (EIA). The modeling study investigates the diurnal and seasonal variations of EIA and specifically attempts to account for the latitudinal and longitudinal structures. This paper also shows that the neutral winds could cause the north-south asymmetries and longitudinal variation. Furthermore, the phenomena of EIA were also varied with the solar activity. The foF2 values in 2007 are higher than those in 2008 generally, with the exception in March. This variation and exception match to the different of the observational sunspot number between 2007 and 2008. Lung-Chih Tsai 蔡龍治 2009 學位論文 ; thesis 70 zh-TW
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language zh-TW
format Others
sources NDLTD
description 碩士 === 國立中央大學 === 太空科學研究所 === 97 === The TaiWan Ionospheric Model (TWIM) is a numerical and phenomenological model of global ionospheric electron density (Ne) and is constructed from monthly-weighted and hourly vertical Ne profiles retrieved from FormoSat3/COSMIC GPS radio occultation measurements. TWIM can also provide global F2-layer critical frequency (foF2), peak density height (hmF2), and scale height (HF2) maps to study features of equatorial ionospheric anomaly (EIA). The modeling study investigates the diurnal and seasonal variations of EIA and specifically attempts to account for the latitudinal and longitudinal structures. This paper also shows that the neutral winds could cause the north-south asymmetries and longitudinal variation. Furthermore, the phenomena of EIA were also varied with the solar activity. The foF2 values in 2007 are higher than those in 2008 generally, with the exception in March. This variation and exception match to the different of the observational sunspot number between 2007 and 2008.
author2 Lung-Chih Tsai
author_facet Lung-Chih Tsai
Jyun-Ying Huang
黃俊穎
author Jyun-Ying Huang
黃俊穎
spellingShingle Jyun-Ying Huang
黃俊穎
A modeling study of the ionospheric equatorial anomaly based on the FormoSat-3/COSMIC data
author_sort Jyun-Ying Huang
title A modeling study of the ionospheric equatorial anomaly based on the FormoSat-3/COSMIC data
title_short A modeling study of the ionospheric equatorial anomaly based on the FormoSat-3/COSMIC data
title_full A modeling study of the ionospheric equatorial anomaly based on the FormoSat-3/COSMIC data
title_fullStr A modeling study of the ionospheric equatorial anomaly based on the FormoSat-3/COSMIC data
title_full_unstemmed A modeling study of the ionospheric equatorial anomaly based on the FormoSat-3/COSMIC data
title_sort modeling study of the ionospheric equatorial anomaly based on the formosat-3/cosmic data
publishDate 2009
url http://ndltd.ncl.edu.tw/handle/er73ke
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