On the role of tidal winds in the descending of the high type of sporadic layer (Es)

Author:

Conceição-Santos FredsonORCID,Muella Marcio T.A.H.,Resende Laysa C.A.,Fagundes Paulo R.,Andrioli Vania F.,Batista Paulo P.,Carrasco Alexander J.

Publisher

Elsevier BV

Subject

Space and Planetary Science,Aerospace Engineering,General Earth and Planetary Sciences,Atmospheric Science,Geophysics,Astronomy and Astrophysics

Reference31 articles.

1. Semidiurnal tidal signature in sporadic E occurrence rates from GPS radio occultation measurements at higher midlatitudes;Arras;Ann. Geophys.,2009

2. The formation and vertical movement of dense ionized layers in the ionosphere due to neutral wind shears;Axford;J. Geophys. Res.,1963

3. Metallic ion transport associated with midlatitude intermediate layer development;Bishop;J. Geophys. Res. Space Phys.,2003

4. Simulation of the sporadic E layer response to prereversal associated evening vertical electric field enhancement near dip equator;Carrasco;J. Geophys. Res. Space Phys.,2007

5. Atmospheric Tides: Thermal and Gravitational;Chapman,1970

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