A new ionospheric model for wide area differential GPS: the multiple shell approach
Explore the source record for details and available documents.
GPS WADGPS total electron content ionosphere valid↗
Engineering topics
Reyes, M. J.
Publications and source records attributed to Reyes, M. J..
A new ionospheric model for wide area differential GPS: the multi-shell approach
In this paper we report on recent developments we made concerning a WADGPS ionospheric model. The new model is a simple extension of the currently used single- shell ionospheric model.
GPS WADGPS total electron content ionosphere valid↗
A new ionospheric model for wide area differential GPS: the multiple shell approach
Explore the source record for details and available documents.
Global Positioning System (GPS)↗
Global Ionospheric TEC Variations During January 10, 1997 Storm
The ionospheric storm evolution process was monitored during the January 10, 1997 magnetic cloud event, through measurements of the inonospheric total electron content (TEC) from 150 GPS stations. The first significant response of the inonospheric TEC to the geomagnetic storm was at 0300 UT as an auroral/subauroral enhancement around the Alaskan evening sector.
Global Ionospheric TEC ionospheric storm magnetic ↗
Do ionospheric Storms Have Common TEX Variation Features
Explore the source record for details and available documents.
TEX GPS network ionospheric storm global scales au↗
Global Ionospheric TEC Perturbations Monitored by the GPS Global Network During Two Northern Hemisphere Winter Storms
The global evolution of two major ionospheric storms, occurring on November 4, 1993 and November 26, 1994, respectively, is studied using measurements of total electron content (TEC) obtained from a worldwide network of ground-based GPS receivers.
Northern hemisphere winter storms total electron c↗
Global Ionospheric TEC Changes Monitored by GPS Network During Nov/93 Storm
Explore the source record for details and available documents.
TEC TEC Changes GPS GPS Network Total electron con↗