Estimation of Planar Trend Model Parameters for Midlatitude Ionosphere


Yildiz S. K., Arikan F.

JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS, vol.125, no.2, 2020 (SCI-Expanded) identifier

  • Publication Type: Article / Article
  • Volume: 125 Issue: 2
  • Publication Date: 2020
  • Doi Number: 10.1029/2019ja027223
  • Journal Name: JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS
  • Journal Indexes: Science Citation Index Expanded (SCI-EXPANDED), Scopus, Aerospace Database, Applied Science & Technology Source, Communication Abstracts, Greenfile, INSPEC, Metadex, Civil Engineering Abstracts
  • Hacettepe University Affiliated: Yes

Abstract

Being under influence of the polar and equatorial regions, the midlatitude ionosphere poses an important challenge in structural modeling. In this study, the general understanding of regional planar trend model is investigated for 2011 by estimation of trend coefficients in the least squares sense. The northern midlatitude is divided into 24 nonoverlapping regions of 10 degrees by 20 degrees in latitude and longitude, respectively. The magnetic conjugates of 24 regions in the Southern Hemisphere are also extracted. The total electron content values are obtained from global ionospheric maps (GIM) with spatial resolution of 2.5 degrees by 5 degrees in latitude and longitude, respectively. The temporal resolution of GIM can be 1 or 2 hr. Estimated planar trend coefficients are used to reconstruct model maps. The difference between GIM and the estimated planar model is obtained in normalized L-2 norm squares sense. It is observed that the planar trend model in latitude and longitude is an agreeable model for total electron content over midlatitude regions for both Northern and Southern Hemispheres. The estimated model parameters generally follow the diurnal, seasonal, and semiannual trend structures of midlatitude ionosphere. The deviations from the model occur mostly during severe disturbances such as geomagnetic storms. The difference between the reconstructed model maps with estimated parameters and GIM is generally under 1% for land and 2% to 5% for ocean regions. The only region that has a very high spread and mostly up to 10% difference with the GIM throughout the year is on the California Current.