Tomographic imaging of the equatorial and low-latitude ionosphere over central-eastern Brazil

A four-dimensional time-dependent tomographic algorithm, named Multi Instrument Data Analysis System (MIDAS), is used to image the equatorial and low-latitude ionosphere over the central-eastern sides of the Brazilian territory. From differential phase data obtained by a chain of ground-based GPS receiver the total electron content (TEC) is estimated and then, together with a modeled ionosphere from International Reference Ionosphere (IRI) model, the electron density distribution is reconstructed and the parameters of the F2-peak layer are accessed from the images. This paper presents the first study of ionospheric tomography using real dual-frequency data from the Brazilian Network for Continuous GPS Monitoring (RBMC). Ionospheric F2-peak electron density (NmF2) accessed from the images are compared to concurrent measurements from three ionosondes installed across Brazil. One year of data during the solar maximum period from March/2001 to February/2002 is used to analyze the seasonal and hourly variation of the F2-layer peak density. The accuracy with which MIDAS images the electron density during geomagnetic quiet periods is investigated through its correlation and deviation with the ionosonde and IRI model data, respectively. The main aspects of the reconstruction results at the equatorial ionization anomaly (EIA) region over Brazil are highlighted and discussed.

[1]  Michael Mendillo,et al.  Storms in the ionosphere: Patterns and processes for total electron content , 2006 .

[2]  P. Kintner,et al.  On the evaluation of Ne gradients at equatorial and low-latitudes during geomagnetically quiet and disturbed periods , 2009 .

[3]  Cathryn N. Mitchell,et al.  A simulation study into constructing of the sample space for ionospheric imaging , 2005 .

[4]  Cathryn N. Mitchell,et al.  Ionospheric imaging of the northern crest of the Equatorial Anomaly , 2003 .

[5]  Bodo W. Reinisch,et al.  International Reference Ionosphere 2000 , 2001 .

[6]  Elena S. Andreeva,et al.  Tomographic investigations of temporal variations of the ionospheric electron density and the implied fluxes , 2003 .

[7]  Cathryn N. Mitchell,et al.  Imaging of the equatorial ionosphere , 2005 .

[8]  L. Kersley Ionospheric tomography and its applications in radio science and geophysical investigations , 2003 .

[9]  C. Mitchell,et al.  Electron density profiles determined from tomographic reconstruction of total electron content obtained from GPS dual frequency data: first results from the South African network of dual frequency GPS receiver stations , 2004 .

[10]  Smitha V. Thampi,et al.  Simulation studies on the tomographic reconstruction of the equatorial and low-latitude ionosphere in the context of the Indian tomography experiment: CRABEX , 2004 .

[11]  Alessandro P. Cerruti,et al.  Scintillation‐producing Fresnel‐scale irregularities associated with the regions of steepest TEC gradients adjacent to the equatorial ionization anomaly , 2010 .

[12]  Michael C. Kelley,et al.  The Earth's Ionosphere : Plasma Physics and Electrodynamics , 1989 .

[13]  C. Mitchell,et al.  Ionospheric storm time dynamics as seen by GPS tomography and in situ spacecraft observations , 2008 .

[14]  Gary S. Bust,et al.  History, current state, and future directions of ionospheric imaging , 2008 .

[15]  J. Klobuchar,et al.  Initial Total Electron Content Results from the Pan American Ionospheric Tomography Campaign. , 1994 .

[16]  Dieter Bilitza,et al.  International reference ionosphere , 1978 .

[17]  Cathryn N. Mitchell,et al.  Ionospheric imaging at mid-latitudes using both GPS and ionosondes , 2007 .

[18]  B. M. Reddy,et al.  Equatorial electric field versus neutral wind control of the equatorialanomaly under quiet and disturbed conditions , 1990 .

[19]  H.-C. Yeh,et al.  The low-latitude ionospheric tomography network (LITN)—initial results , 1997 .

[20]  Elena S. Andreeva,et al.  Some features of the equatorial anomaly revealed by ionospheric tomography , 2000 .

[21]  I. Batista,et al.  Ionospheric variability at Brazilian low and equatorial latitudes: comparison between observations and IRI model , 2004 .

[22]  S. E. Pryse Radio Tomography: A New Experimental Technique , 2003 .

[23]  Ljiljana R. Cander,et al.  Total electron content - A key parameterin propagation: measurement and usein ionospheric imaging , 2004 .

[24]  K. Davies,et al.  Studying the ionosphere with the Global Positioning System , 1997 .

[25]  C. Mitchell,et al.  Imaging of the equatorial ionospheric anomaly over South America—A simulation study of total electron content , 2006 .

[26]  H. Na,et al.  Ground station spacing effects in ionospheric tomography , 1995 .

[27]  D. Bilitza,et al.  International Reference Ionosphere 2007: Improvements and new parameters , 2008 .

[28]  T. Kikuchi,et al.  North-south asymmetry of the equatorial ionospheric anomaly observed in East Asia during the SUNDIAL-87 campaign , 1991 .

[29]  S. E. Pryse,et al.  Total electron content – A key parameter in propagation : measurement and use in ionospheric imaging , 2006 .

[30]  C. Mitchell,et al.  A three-dimensional time-dependent algorithm for ionospheric imaging using GPS , 2003 .