Characteristics of the ionospheric irregularities over Brazilian longitudinal sector

Based on the data obtained from a network of GPS L1 band receivers deployed in Brazil, we present here the characteristics of the 400 m ionospheric irregularities during magnetically quiet and disturbed conditions.The network is composed of 12 GPS scintillation monitors and covers the latitudinal region from the magnetic equator up to the southern crest of the Equatorial Ionization Anomaly (EIA), which is characterized by large horizontal gradients in the electron density distribution. Some results on equatorial spread F statistics obtained from digisonde data over Cachoeira Paulista (22.41 o S, 45 o W, dip latitude 14.89 o S) and from ionosonde data over Tucumán (64.5 o W, 27 o S, dip latitude 13.71 o S) are also used in this work to complement the results from GPS network. The effects of local time, season, latitude, longitude, background ionization, solar cycle and magnetic activity on the ionospheric irregularities are presented. The ionospheric irregularity zonal velocities determined by magnetically east-west spaced GPS receivers are also presented. The influence of the ionospheric irregularities on GPS based navigational systems is discussed. These observations, complemented by computational simulations, may improve our understanding of the factors responsible for the generation, growth and dynamics of the equatorial F region plasma irregularities .

[1]  P. J. Sultan,et al.  Linear theory and modeling of the Rayleigh‐Taylor instability leading to the occurrence of equatorial spread F , 1996 .

[2]  M. A. Abdu,et al.  Outstanding problems in the equatorial ionosphere–thermosphere electrodynamics relevant to spread F , 2001 .

[3]  Paul M. Kintner,et al.  Global Positioning System measurements of the ionospheric zonal apparent velocity at Cachoeira Paulista in Brazil , 2000 .

[4]  E. R. Paula,et al.  Multi-technique investigations of storm-time ionospheric irregularities over the São Luís equatorial station in Brazil , 2004 .

[5]  B. Fejer Natural ionospheric plasma waves , 1996 .

[6]  P. Banerjee,et al.  Estimation of Minimum Separation of Geostationary Satellites for Satellite-Based Augmentation System (SBAS) from Equatorial Ionospheric Scintillation Observations , 2003, Journal of Navigation.

[7]  L. Scherliess,et al.  Storm time dependence of equatorial disturbance dynamo zonal electric fields , 1997 .

[8]  M. Kelley Equatorial spread-F: recent results and outstanding problems , 1985 .

[9]  P. Kintner,et al.  Ionospheric irregularity zonal velocities over Cachoeira Paulista , 2002 .

[10]  M. A. Abdu,et al.  Magnetic declination control of the equatorial F region dynamo electric field development and spread F , 1981 .

[11]  P. Banerjee,et al.  Errors in position‐fixing by GPS in an environment of strong equatorial scintillations in the Indian zone , 2004 .

[12]  L. Scherliess,et al.  Time dependent response of equatorial ionospheric electric fields to magnetospheric disturbances , 1995 .

[13]  Paul M. Kintner,et al.  Development and use of a GPS ionospheric scintillation monitor , 2001, IEEE Trans. Geosci. Remote. Sens..

[14]  Paul M. Kintner,et al.  Fading timescales associated with GPS signals and potential consequences , 2001 .

[15]  S. Basu,et al.  Ionospheric effects of major magnetic storms during the International Space Weather Period of September and October 1999: GPS observations, VHF/UHF scintillations, and in situ density structures at middle and equatorial latitudes , 2001 .

[16]  E. R. Paula,et al.  Effects of the vertical plasma drift velocity on the generation and evolution of equatorial spread F , 1999 .

[17]  R. Tsunoda,et al.  Control of the seasonal and longitudinal occurrence of equatorial scintillations by the longitudinal gradient in integrated E region Pedersen conductivity , 1985 .

[18]  H. Takahashi,et al.  Magnetospheric disturbance induced equatorial plasma bubble development and dynamics: A case study in Brazilian sector , 2003 .

[19]  Paul M. Kintner,et al.  Equatorial anomaly effects on GPS scintillations in brazil , 2003 .

[20]  S. Skone,et al.  Limitations in GPS receiver tracking performance under ionospheric scintillation conditions , 2001 .

[21]  T. Maruyama A diagnostic model for equatorial spread F, 1, Model description and application to electric field and neutral wind effects , 1988 .

[22]  J. Bittencourt,et al.  Spread F plasma bubble vertical rise velocities determined from spaced ionosonde observations , 1983 .

[23]  Paul M. Kintner,et al.  Mapping and Survey of Plasma Bubbles over Brazilian Territory , 2007 .

[24]  I. Batista,et al.  Equatorial spread-F occurrence statistics in the American longitudes: Diurnal, seasonal and solar cycle variations , 1998 .