TY - JOUR
T1 - Using Principal Component Analysis of Satellite and Ground Magnetic Data to Model the Equatorial Electrojet and Derive Its Tidal Composition
AU - Soares, Gabriel
AU - Yamazaki, Yosuke
AU - Morschhauser, Achim
AU - Matzka, Jürgen
AU - Pinheiro, Katia J.
AU - Stolle, Claudia
AU - Alken, Patrick
AU - Yoshikawa, Akimasa
AU - Hozumi, Kornyanat
AU - Kulkarni, Atul
AU - Supnithi, Pornchai
N1 - Funding Information:
The results presented in this paper rely on the data collected at HUA, KOU, ABG, TTB, TAM, PHU, and GUA. We thank Instituto Geofísico del Perú, Institut de Physique du Globe de Paris, Indian Institude of Geomagnetism, Observatório Nacional/GFZ German Research Centre for Geosciences, and United States Geological Survey (USGS) for supporting HUA, KOU, ABG, TTB, TAM, PHU, and GUA operation, and INTERMAGNET for promoting high standards of geomagnetic observatory practice. The CHAMP satellite was operated by the German Aerospace Center (DLR) and GFZ German Research Centre for Geosciences. The Swarm satellite mission is operated by the European Space Agency (ESA). The Ørsted and SAC-C projects received extensive support from the Danish government, the Argentine Commission on Space Initiatives, NASA, ESA, CNES, and DARA. GFZ German Research Centre for Geosciences is acknowledged for providing the geomagnetic Kp index. Natural Resources Canada is acknowledged for providing the F10.7 solar flux data. This study was financed in part by the Coordenação de Aperfeiçoamento de Pessoal de Nível Superior—Brasil (CAPES)—Finance Codes 1799579 and 88882.447071/2019-01 (G.B.S. PhD research grant). Y.Y. was partially supported by the Deutsche Forschungsgemeinschaft (DFG) Grant YA-574-3-1. G.B.S, J.M., and C.S. were partly supported by the DFG Priority Program SPP1788 DynamicEarth. K.P. acknowledges the support of Fundação de Amparo à Pesquisa do Estado do Rio de Janeiro (FAPERJ/Brazil, Grant E-26/202.748/2019). K.H. was partially supported by JSPS KAKENHI Grant 20H00197. Open Access funding enabled and organized by Projekt DEAL.
Funding Information:
The results presented in this paper rely on the data collected at HUA, KOU, ABG, TTB, TAM, PHU, and GUA. We thank Instituto Geofísico del Perú, Institut de Physique du Globe de Paris, Indian Institude of Geomagnetism, Observatório Nacional/GFZ German Research Centre for Geosciences, and United States Geological Survey (USGS) for supporting HUA, KOU, ABG, TTB, TAM, PHU, and GUA operation, and INTERMAGNET for promoting high standards of geomagnetic observatory practice. The CHAMP satellite was operated by the German Aerospace Center (DLR) and GFZ German Research Centre for Geosciences. The Swarm satellite mission is operated by the European Space Agency (ESA). The Ørsted and SAC‐C projects received extensive support from the Danish government, the Argentine Commission on Space Initiatives, NASA, ESA, CNES, and DARA. GFZ German Research Centre for Geosciences is acknowledged for providing the geomagnetic Kp index. Natural Resources Canada is acknowledged for providing the F10.7 solar flux data. This study was financed in part by the Coordenação de Aperfeiçoamento de Pessoal de Nível Superior—Brasil (CAPES)—Finance Codes 1799579 and 88882.447071/2019‐01 (G.B.S. PhD research grant). Y.Y. was partially supported by the Deutsche Forschungsgemeinschaft (DFG) Grant YA‐574‐3‐1. G.B.S, J.M., and C.S. were partly supported by the DFG Priority Program SPP1788 DynamicEarth. K.P. acknowledges the support of Fundação de Amparo à Pesquisa do Estado do Rio de Janeiro (FAPERJ/Brazil, Grant E‐26/202.748/2019). K.H. was partially supported by JSPS KAKENHI Grant 20H00197. Open Access funding enabled and organized by Projekt DEAL.
Publisher Copyright:
© 2022. The Authors.
PY - 2022/9
Y1 - 2022/9
N2 - The intensity of the equatorial electrojet (EEJ) shows temporal and spatial variability that is not yet fully understood nor accurately modeled. Atmospheric solar tides are among the main drivers of this variability but determining different tidal components and their respective time series is challenging. It requires good temporal and spatial coverage with observations, which, previously could only be achieved by accumulating data over many years. Here, we propose a new technique for modeling the EEJ based on principal component analysis (PCA) of a hybrid ground-satellite geomagnetic data set. The proposed PCA-based model (PCEEJ) represents the observed EEJ better than the climatological EEJM-2 model, especially when there is good local time separation among the satellites involved. The amplitudes of various solar tidal modes are determined from PCEEJ based tidal equation fitting. This allows to evaluate interannual and intraannual changes of solar tidal signatures in the EEJ. On average, the obtained time series of migrating and nonmigrating tides agree with the average climatology available from earlier work. A comparison of tidal signatures in the EEJ with tides derived from neutral atmosphere temperature observations show a remarkable correlation for nonmigrating tides such as DE3, DE2, DE4, and SW4. The results indicate that it is possible to obtain a meaningful EEJ spectrum related to solar tides for a relatively short time interval of 70 days.
AB - The intensity of the equatorial electrojet (EEJ) shows temporal and spatial variability that is not yet fully understood nor accurately modeled. Atmospheric solar tides are among the main drivers of this variability but determining different tidal components and their respective time series is challenging. It requires good temporal and spatial coverage with observations, which, previously could only be achieved by accumulating data over many years. Here, we propose a new technique for modeling the EEJ based on principal component analysis (PCA) of a hybrid ground-satellite geomagnetic data set. The proposed PCA-based model (PCEEJ) represents the observed EEJ better than the climatological EEJM-2 model, especially when there is good local time separation among the satellites involved. The amplitudes of various solar tidal modes are determined from PCEEJ based tidal equation fitting. This allows to evaluate interannual and intraannual changes of solar tidal signatures in the EEJ. On average, the obtained time series of migrating and nonmigrating tides agree with the average climatology available from earlier work. A comparison of tidal signatures in the EEJ with tides derived from neutral atmosphere temperature observations show a remarkable correlation for nonmigrating tides such as DE3, DE2, DE4, and SW4. The results indicate that it is possible to obtain a meaningful EEJ spectrum related to solar tides for a relatively short time interval of 70 days.
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U2 - 10.1029/2022JA030691
DO - 10.1029/2022JA030691
M3 - Article
AN - SCOPUS:85138707378
SN - 2169-9380
VL - 127
JO - Journal of Geophysical Research: Space Physics
JF - Journal of Geophysical Research: Space Physics
IS - 9
M1 - e2022JA030691
ER -