The prereversal enhancement in the vertical drift for Fortaleza and the sporadic E layer

• Published in: Journal of atmospheric and solar-terrestrial physics Vol. 67; no. 16; pp. 1610 - 1617
• Main Authors: Carrasco, A.J., Batista, I.S., Abdu, M.A.
• Format: Journal Article
• Language: English
• Published: Oxford Elsevier Ltd 01.11.2005; Elsevier
• Subjects: Earth, ocean, space; Equatorial ionosphere; Exact sciences and technology; External geophysics; Physics of the high neutral atmosphere; Physics of the ionosphere; Physics of the magnetosphere; Prereversal enhancement; Sporadic E-layer; Brazil, Ceara, Fortaleza; Sporadic E-layer; Equatorial ionosphere; Prereversal enhancement; models; Sporadic E; Ionospheric E region; Ionospheric F region; electrical field; Sunset; diurnal variations; Plasma drift; Vertical drift; Ionogram; Time inversion; Quiet day; electrical conductivity
• ISSN: 1364-6826; 1879-1824
• DOI: 10.1016/j.jastp.2005.07.015

Using ionogram-recorded data for the location of Fortaleza ( 3 . 8 ∘ S, 38 . 0 ∘ W; magnetic latitude = - 6 ∘ ), the relation between the evening prereversal enhancement in the vertical F region plasma drift ( E × B ) and the diurnal variation of the sporadic E layer ( Es ) is examined. The database examined corresponds to the period of June 2001. The F region vertical drifts obtained as dh ′ F / dt for quiet days reveal that when the amplitudes of the evening prereversal enhancement (PRE) are higher, an interruption of an ongoing sporadic E layer is observed. A recent investigation by Abdu et al. [2003. Journal of Geophysical Research 108(A6), 1254. doi: 10.1029/2002JA009285.], showed that an upward electric field, intensified during the PRE, can be responsible for the inhibition of the sporadic E layer. In this work, we investigate the possible influence of a modified conductivity on the PRE development. The model developed by Batista et al. [1986. Journal of Geophysical Research 91(A11), 12055–12064.], based on the work of Heelis et al. [1974. Planetary and Space Science 22, 743–756.], was used to test the response of the PRE (its amplitude, time of occurrence and time of inversion) when the electrical conductivity of the E region is modified, specifically around sunset. The real cause of this modified conductivity is not investigated here, but the presence of a sporadic E layer could partially contribute to that. The causes of the agreement or disagreement between the computed and the observed value of vertical drift are discussed.