Latitudinal variations of the height of the maximum of the daytime equatorial ionospheric F2-layer

Details Latitudinal variations of the height of the maximum of the daytime equatorial ionospheric F2-layer Latitudinal variations of the height of the maximum of the daytime equatorial ionospheric F2-layer

Oct 1987

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1987ge%26ae..27..735l&link_type=abstract

Geomagnetizm i Aeronomiia (ISSN 0016-7940), vol. 27, Sept.-Oct. 1987, p. 735-739. In Russian.

Computer Science

Sound

Daytime, Equatorial Atmosphere, F 2 Region, Magnetic Equator, Vertical Distribution, Drift Rate, Equatorial Regions, Geomagnetic Latitude, Ionospheric Sounding, Midlatitude Atmosphere

Scientific paper

Conditions for the formation of different types of latitudinal variations of hmF2 near the geomagnetic equator are examined on the basis of vertical-sounding data. These variations are found to have a relative minimum at the equator and two maxima at geomagnetic latitudes of 7-10 deg; the formation of these maxima is connected with different dependences of hmF2 on vertical-drift velocity for midlatitude, low-latitude, and equatorial F2-layers. It is shown that the F2-layer discloses either equatorial or midlatitude features depending on the direction and magnitude of the vertical-drift velocity.

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