Journal of Geodesy

, Volume 79, Issue 4–5, pp 175–188

Temporal and spatial variability of the bias between TOPEX- and GPS-derived total electron content

Article

DOI: 10.1007/s00190-005-0448-z

Cite this article as:
Brunini, C., Meza, A. & Bosch, W. J Geodesy (2005) 79: 175. doi:10.1007/s00190-005-0448-z

Abstract

Total electron content (TEC) predictions made with the GPS-based la plata ionospheric model (LPIM) and the International Reference Ionosphere (IRI95) model were compared to estimates from the dual-frequency altimeter onboard the TOPEX/Poseidon (T/P) satellite. LPIM and IRI95 were evaluated for the location and time of available T/P data, from January 1997 to December 1998. To investigate temporal and spatial variations of the TEC bias between T/P and each model, the region covered by T/P observations was divided into ten latitude bands. For both models and for all latitudes, the bias was mainly positive (i.e. T/P values were larger); the LPIM bias was lower and less variable than the IRI95 bias. To perform a detailed analysis of temporal and spatial variability of the T/P-LPIM TEC bias, the Earth’s surface was divided into spherical triangles with 9°-sides, and a temporally varying regression model was fitted to every triangle. The highest TEC bias was found over the equatorial anomalies, which is attributed to errors in LPIM. A significant TEC bias was found at 40°N latitude, which is attributed to errors in the T/P Sea State Bias (SSB) correction. To separate systematic errors in the T/P TEC from those caused by LPIM, altimeter range biases estimated by other authors were analysed in connection with the TEC bias. This suggested that LPIM underestimates the TEC, particularly during the Southern Hemisphere summer, while T/P C-band SSB calibration is worse during the Southern Hemisphere winter.

Keywords

Total electron content (TEC) GPS TOPEX/Poseidon 

Copyright information

© Springer-Verlag Berlin Heidelberg 2005

Authors and Affiliations

  1. 1.Facultad de Ciencias Astronómicas y GeofísicasUniversidad Nacional de La Plata and Consejo Nacional de Investigaciones Científicas y TécnicasLa PlataArgentina
  2. 2.Deutsches Geodaetisches ForschungsinstitutMünchenGermany

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