The São Luís 30 MHz coherent scatter ionospheric radar: System description and initial results

[1] A new 30 MHz coherent scatter ionospheric radar has been operating at the equatorial station at Sao Luis (2.33°S, 44°W, dip latitude 1.3°S), Brazil, since December 2000. This VHF radar has a peak power of only 8 kW but uses long coded pulses and a high PRF with coherent integration to achieve good sensitivity. Two side-by-side square antenna arrays composed of 16 5-element Yagi antennas directed vertically are used for transmission and reception. This radar measures the backscattered signals from E and F region ionospheric irregularities. In the standard operational mode, the irregularity intensity, as well as the vertical and zonal velocities using Doppler analysis and interferometry, respectively, are determined. We initially present a brief description of the radar system, signal characteristics and data processing, followed by some of the initial observations. Electrojet echoes ranged from about 94 to 108 km in altitude with the strongest echoes coming from about 104 km and with an uplift to about 110 km occurring in the late afternoon. Echoes from the valley region (150 km echoes) were strong, quasi-periodic with periods of about 10 to 15 minutes, and had the necklace shape observed at others sites. F region bottom-type, bottomside, and topside (plumes) spread F layers were observed at night. The large-scale topside F region plumes, moving eastward and upward, reached altitudes of about 1,400 km and were preceded by bottom-type layers around 400 km altitude that were moving westward. The characteristics of the echoes were similar to those observed by the JULIA radar at Jicamaca, Peru. However, some differences in the behavior of the echoes between the two sites were noted.

[1]  O. Røyrvik Drift and aspect sensitivity of scattering irregularities in the upper equatorial E region , 1982 .

[2]  Ronald F. Woodman,et al.  Oblique VHF radar spectral studies of the equatorial electrojet , 1975 .

[3]  C. J. Zamlutti,et al.  Association between plasma bubble irregularities and airglow disturbances over Brazilian low latitudes , 1980 .

[4]  Donald T. Farley,et al.  Long wavelength irregularities in the equatorial electrojet , 1982 .

[5]  V. K. Anandan,et al.  First observations of equatorial spread F from Indian MST radar , 1995 .

[6]  Donald T. Farley,et al.  Theory of equatorial electrojet plasma waves: new developments and current status , 1985 .

[7]  W. Ecklund,et al.  On the nature of 150‐km radar echoes over the magnetic dip equator , 2000 .

[8]  D. T. Farley,et al.  High-resolution radar measurements of turbulent structure in the equatorial electrojet , 1994 .

[9]  B. Balsley Measurement of electron drift velocities in the night-time equatorial electrojet , 1969 .

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

[11]  D. T. Farley,et al.  Vertical structure of the VHF backscattering region in the equatorial electrojet and the gradient drift instability , 1975 .

[12]  W. Swartz CUPRI observations of persistence asymmetry reversals in up‐down vertical type‐I echoes from the equatorial electro jet above Alcântara, Brazil , 1997 .

[13]  J. Delloue,et al.  Midlatitude E region coherent backscatter observed simultaneously at two HF radar frequencies , 1996 .

[14]  D. Hysell,et al.  JULIA radar studies of equatorial spread F , 1998 .

[15]  E. R. Paula,et al.  Equatorial electrojet irregularities investigations using a back-scatter radar and a digisonde at São Luı́s: some initial results , 2002 .

[16]  S. Musman,et al.  Imaging spread‐F structures using GPS observations at Alcântara, Brazil , 1997 .

[17]  Ronald F. Woodman,et al.  Equatorial spread F: Implications of VHF radar observations , 1970 .

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

[19]  Erhan Kudeki,et al.  High resolution observations of 150 km echoes at Jicamarca , 1993 .

[20]  David L. Hysell,et al.  JULIA radar studies of electric fields in the equatorial electrojet , 1997 .

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

[22]  J. L. Scali,et al.  Equatorial F region irregularity morphology during an equinoctial month at solar minimum , 1999 .

[23]  Elisabeth Blanc,et al.  Kilometric irregularities in the E and F regions of the daytime equatorial ionosphere observed by a high resolution HF radar , 1996 .

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

[25]  B. Balsley Electric fields in the equatorial ionosphere: A review of techniques and measurements , 1973 .

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

[27]  M. A. Abdu,et al.  Equatorial F region vertical plasma drifts: Seasonal and longitudinal asymmetries in the American sector , 1986 .

[28]  B. Fejer,et al.  Electric field and plasma density measurements in the strongly driven daytime equatorial electrojet: 1. The unstable layer and gradient drift waves , 1987 .

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

[30]  R. Tsunoda Enhanced velocities and a shear in daytime Esq over Kwajalein and their relationship to 150 km echoes over the dip equator , 1994 .

[31]  Ronald F. Woodman,et al.  Radar observations of F region equatorial irregularities , 1976 .

[32]  A. Patra,et al.  Equatorial E region irregularities: a review of recent observations , 2002 .

[33]  I. Batista,et al.  Equatorial spread F statistics in the American longitudes: Some problems relevant to ESF description in the IRI scheme , 2000 .

[34]  David L. Hysell,et al.  Long term studies of equatorial spread F using the JULIA radar at Jicamarca , 2002 .

[35]  E. Blanc,et al.  Interpretation of equatorial electrojet irregularities observed with a broad beam HF zenithal radar , 1999 .

[36]  B. Balsley Evidence of a stratified echoing region at 150 kilometers in the vicinity of the magnetic equator during daylight hours , 1964 .