TY - JOUR
T1 - Ionospheric Current Variations by Empirical Orthogonal Function Analysis
T2 - Solar Activity Dependence and Longitudinal Differences
AU - Owolabi, Charles
AU - Ruan, Haibing
AU - Yamazaki, Y.
AU - Kaka, R. O.
AU - Akinola, O. O.
AU - Yoshikawa, Akimasa
N1 - Funding Information:
The first author is indebted to Prof. Jiuhou Lei for his guidance over the years in the pursuit of understanding the ionospheric electrodynamics and to Prof. Yufeng Lin for his support and encouragement during this work. This work was supported by the National Natural Science Foundation (NSF) of China (Grant numbers: 41804151 & 42074186), and Natural Science Foundation of Jiangsu Province (Grant Number: BK20211036). The authors are thankful to the LISN, AMBER, INTERMAGNET, AUTUMNX, WDC, CARISMA, SAMBA, EMBRACE, MAGDAS/CPMN and WAMNET members for providing the geomagnetic data used in this study. The LISN is a project led by Boston College in collaboration with the Geophysical Institute of Peru, and other institutions that provide information for the benefit of the scientific community. The AMBER is operated by Boston College and funded by NASA and AFOSR. The CARISMA network is operated by the University of Alberta, funded by the Canadian Space Agency. The SAMBA is also operated by UCLA and funded by NSF. The AUTUMNX is funded through the Canadian Space Agency/Geospace Observatories (GO) Canada Program. The MAGDAS/CPMN network is operated by the International Center for Space Weather Science and Education, Kyushu University, Fukuoka, Japan and funded by the Japan Society for the Promotion of Science (JSPS). The authors appreciate the IAGA for providing a quasi‐dipole geomagnetic coordinate calculator. The authors are very grateful to SPDF/GSFC for providing records of F10.7 flux indices used in the present study. The authors thank the Helmholtz Center Potsdam, German Research Center for Geosciences GFZ for providing records of the IQDs. The authors thank the editor and two anonymous reviewers for their helpful comments and suggestions that greatly improved this paper.
Funding Information:
The first author is indebted to Prof. Jiuhou Lei for his guidance over the years in the pursuit of understanding the ionospheric electrodynamics and to Prof. Yufeng Lin for his support and encouragement during this work. This work was supported by the National Natural Science Foundation (NSF) of China (Grant numbers: 41804151 & 42074186), and Natural Science Foundation of Jiangsu Province (Grant Number: BK20211036). The authors are thankful to the LISN, AMBER, INTERMAGNET, AUTUMNX, WDC, CARISMA, SAMBA, EMBRACE, MAGDAS/CPMN and WAMNET members for providing the geomagnetic data used in this study. The LISN is a project led by Boston College in collaboration with the Geophysical Institute of Peru, and other institutions that provide information for the benefit of the scientific community. The AMBER is operated by Boston College and funded by NASA and AFOSR. The CARISMA network is operated by the University of Alberta, funded by the Canadian Space Agency. The SAMBA is also operated by UCLA and funded by NSF. The AUTUMNX is funded through the Canadian Space Agency/Geospace Observatories (GO) Canada Program. The MAGDAS/CPMN network is operated by the International Center for Space Weather Science and Education, Kyushu University, Fukuoka, Japan and funded by the Japan Society for the Promotion of Science (JSPS). The authors appreciate the IAGA for providing a quasi-dipole geomagnetic coordinate calculator. The authors are very grateful to SPDF/GSFC for providing records of F10.7 flux indices used in the present study. The authors thank the Helmholtz Center Potsdam, German Research Center for Geosciences GFZ for providing records of the IQDs. The authors thank the editor and two anonymous reviewers for their helpful comments and suggestions that greatly improved this paper.
Publisher Copyright:
© 2021. American Geophysical Union. All Rights Reserved.
PY - 2022/1
Y1 - 2022/1
N2 - The solar quiet (Sq) ionospheric current variations exhibit spatial and temporal patterns that can be identified by the prevailing eigenmodes based on the empirical orthogonal function (EOF) analysis. In this study, the Sq current function over the American and European/African sectors are derived using ground magnetometer data from 2006 to 2019 based on the spherical harmonic analysis technique. Subsequently, we decomposed the Sq current function into eigenmodes by applying the EOF analysis, where the first three eigenmodes capture 96% of the overall Sq current variance. Additionally, these eigenmodes are utilized to model the Sq current function and compare its properties between the two longitudinal sectors. We observed that the EOF model could reconstruct the observed Sq current function with the first three eigenmodes in both longitudinal sectors. Moreover, the EOF model unveils a clear association of the Sq current function with several driven features, such as magnetic latitude, local time, season, and solar activity. Both longitudinal sectors had comparable Sq current patterns under varying solar activity, while their amplitudes varied. Besides, the newly developed model could reproduce a refined Sq current variability over the two longitudinal sectors as long as the observed Sq variations have sufficient duration. Our EOF model shows that the variations of the Sq current function with solar activity can be explained by the first three eigenmodes, which could be used as a basis for further numerical modeling of the Sq current variations.
AB - The solar quiet (Sq) ionospheric current variations exhibit spatial and temporal patterns that can be identified by the prevailing eigenmodes based on the empirical orthogonal function (EOF) analysis. In this study, the Sq current function over the American and European/African sectors are derived using ground magnetometer data from 2006 to 2019 based on the spherical harmonic analysis technique. Subsequently, we decomposed the Sq current function into eigenmodes by applying the EOF analysis, where the first three eigenmodes capture 96% of the overall Sq current variance. Additionally, these eigenmodes are utilized to model the Sq current function and compare its properties between the two longitudinal sectors. We observed that the EOF model could reconstruct the observed Sq current function with the first three eigenmodes in both longitudinal sectors. Moreover, the EOF model unveils a clear association of the Sq current function with several driven features, such as magnetic latitude, local time, season, and solar activity. Both longitudinal sectors had comparable Sq current patterns under varying solar activity, while their amplitudes varied. Besides, the newly developed model could reproduce a refined Sq current variability over the two longitudinal sectors as long as the observed Sq variations have sufficient duration. Our EOF model shows that the variations of the Sq current function with solar activity can be explained by the first three eigenmodes, which could be used as a basis for further numerical modeling of the Sq current variations.
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U2 - 10.1029/2021JA029903
DO - 10.1029/2021JA029903
M3 - Article
AN - SCOPUS:85124383953
SN - 2169-9380
VL - 127
JO - Journal of Geophysical Research: Space Physics
JF - Journal of Geophysical Research: Space Physics
IS - 1
M1 - e2021JA029903
ER -