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Radio occultation measurements performed by the satellites CHAMP, GRACE andFORMOSAT-3/COSMIC provide a huge data set for atmospheric and ionosphericinvestigations on a global scale. The data sets are used to extractinformation on sporadic E layers appearing in the lower ionospheric Eregion. This is done by analyzing signal amplitude variations of the GPSL1 signal. Sporadic E altitudes in northern midlatitudes found fromradio occultation measurements are compared with ground-based ionosondesoundings. A large correlation of sporadic E altitudes from these twotechniques is found

Sporadic &lt;i&gt;E&lt;/i&gt; signatures revealed from multi-satellite radio occultation measurements

Sporadic <i>E</i> signatures revealed from multi-satellite radio occultation measurements