Empirical Modeling of Ionospheric Current Using Empirical Orthogonal Function Analysis and Artificial Neural Network-Reference-Cited by-同舟云学术

Empirical Modeling of Ionospheric Current Using Empirical Orthogonal Function Analysis and Artificial Neural Network

Published:2021-11 Issue:11 Volume:19 Page:
ISSN:1542-7390
Container-title:Space Weather
language:en
Short-container-title:Space Weather

Author:

Owolabi Charles¹²^ORCID,Ruan Haibing³^ORCID,Yamazaki Yosuke⁴^ORCID,Li Jinfeng¹,Zhong Jiahao⁵^ORCID,Eyelade A. V.⁶,Priyadarshi Shishir⁷,Yoshikawa Akimasa⁸^ORCID

Affiliation:

1. Department of Earth and Space Sciences Southern University of Science and Technology Shenzhen China

2. Department of Physics Federal University of Technology Akure Akure Nigeria

3. School of Remote Sensing and Geomatics Engineering Nanjing University of Information Science and Technology Nanjing China

4. GFZ German Research Centre for Geosciences Potsdam Germany

5. Planetary Environmental and Astrobiological Research Laboratory (PEARL) School of Atmospheric Sciences Sun Yat‐Sen University Zhuhai China

6. Department of Physics Universidad de Santiago de Chile Santiago Chile

7. Department of Electronic and Electrical Engineering University of Bath Bath UK

8. International Center for Space Weather Science and Education Kyushu University Fukuoka Japan

Publisher

American Geophysical Union (AGU)

Subject

Atmospheric Science

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021SW002831

Reference55 articles.

1. South Atlantic magnetic anomaly ionization: A review and a new focus on electrodynamic effects in the equatorial ionosphere

2. Spatio-temporal characterization of the equatorial electrojet from CHAMP, Ørsted, and SAC-C satellite magnetic measurements

3. An application of principal component analysis to the interpretation of ionospheric current systems

4. Daytime verticalE×Bdrift velocities inferred from ground-based magnetometer observations at low latitudes

5. Principal components of quiet time temporal variability of equatorial and low-latitude geomagnetic fields

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