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(Reference retrieved automatically from Web of Science through information on FAPESP grant and its corresponding number as mentioned in the publication by the authors.)

Thermospheric Meridional Wind Control on Equatorial Scintillations and the Role of the Evening F-Region Height Rise, E x B Drift Velocities and F2-Peak Density Gradients

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Author(s):
Muella, M. T. A. H. [1] ; de Paula, E. R. [1] ; Fagundes, P. R. [2] ; Bittencourt, J. A. [1] ; Sahai, Y. [2]
Total Authors: 5
Affiliation:
[1] Inst Nacl Pesquisas Espaciais, Div Aeron, Sao Paulo - Brazil
[2] Univ Vale Paraiba, IP&D, Lab Fis & Astron, Sao Paulo - Brazil
Total Affiliations: 2
Document type: Review article
Source: SURVEYS IN GEOPHYSICS; v. 31, n. 5, p. 509-530, SEP 2010.
Web of Science Citations: 11
Abstract

The possible role, on L-band scintillation activity, played by the nighttime magnetic meridional component of the thermospheric horizontal neutral winds, the post-sunset F-layer base height, the electrical field pre-reversal enhancement (PRE) and the latitudinal gradients of the F2-layer peak density is analyzed, considering different cases of scintillation occurrence (and their latitudinal extent) during August and September 2002. The meridional winds were derived over low-latitudes from a modified form of the nonlinear time-dependent servo-model. A chain of two scintillation monitors and three digital ionosondes was operational in Brazil and used to collect, respectively, global positioning system signal amplitude scintillation and ionospheric height (h'F; hpF2) and frequency (foF2) parameters. From the overall behavior in the 2 months analyzed, the results suggest that high near sunset upward vertical plasma drifts are conducive for the generation of spread-F irregularities, whereas large poleward meridional winds tend to suppress the development of plasma bubble irregularities and the occurrence of their associated scintillations. Even when generated, a reduced fountain effect, due to weak electric field PRE, acts for the bubbles to be expanded less effectively to higher latitudes. The results also reveal that high F-layer base and peak heights (at equatorial and off-equatorial latitudes), and intense gradients in the F2-peak density between the dip equator and the equatorial anomaly crests, are favorable conditions for the generation of F-region irregularities and increased scintillation activity. Other distinct features of the controlling factors in the cases of occurrence and non-occurrence of equatorial scintillations are presented and discussed. (AU)

FAPESP's process: 08/05482-5 - Study of generation, evolution and dynamics of ionospheric irregularities at equatorial and low-latitude regions
Grantee:Paulo Roberto Fagundes
Support Opportunities: Regular Research Grants
FAPESP's process: 08/04892-5 - Study of the temporal and spatial dependence between plasma irregularities and total electron content as a basis to the development of a ionospheric scintillation model: simultaneous investigation of ionospheric radiotomography
Grantee:Marcio Tadeu de Assis Honorato Muella
Support Opportunities: Scholarships in Brazil - Post-Doctoral