journal article
LitStream Collection
Equatorial sporadic E and cross-field instability
doi: 10.1007/BF03048126pmid: N/A
The occurrence of sporadic E at an equatorial station during magnetically quiet daytime conditions corresponds almost exactly to the time during which the horizontal component of the earth’s magnetic field is above the mean night time level. Any large decrease of H below the night time level is accompanied by the disappearance of equatorial Es−q reflections precisely for the period when the value of H remains below its night time level.