@InProceedings{MuellaPaSoDiLa:2009:CoPoOb,
author = "Muella, M{\'a}rcio and Paula, Eurico Rodrigues de and Sobral,
Jos{\'e} Humberto Andrade and Groves and Directorate, KeithSpace
Vehicles and Laboratory, Air Force Research",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)} and {Instituto Nacional de
Pesquisas Espaciais (INPE)}",
title = "Conjugate point obseration of kilometer and meter scales
irregularity zonal drift velocities",
booktitle = "Proceedings...",
year = "2009",
organization = "Iaga, 2009.",
keywords = "ionospheric irregularities, GPS and VHF systems, irregularity
drifts.",
abstract = "Simultaneous observations of VHF and L-band scintillations were
carried out during the Conjugate Point Equatorial Experiment
(COPEX) campaign held from October 1st to December 10th 2002 over
four sites in the Brazilian territory. The main objective of this
campaign was to study the ionospheric bubbles dynamics and spatial
distribution to investigate their generation mechanisms and their
development along the same magnetic field line. The GPS
(scintillation monitors) and VHF receivers were installed at Campo
Grande (20.5o S, 54.7o W, -22.3o dip angle), Alta Floresta (9.7oS,
56.0o W, -3.38o dip angle), Cachimbo (9.5oS, 54.8oW, -4.25o dip
angle) and Boa Vista (2.8o N, 60.7o W, -22.0o dip angle). In this
work we will focus only in the zonal spaced GPS (1.575 GHz) and
VHF (240 MHz) receivers data. These receivers were set up to
estimate ionospheric irregularities zonal velocities. The 100 m
east-west magnetically spaced GPS receivers (SCINTMON)
configuration was adopted to estimate the zonal velocity of the
irregularities at 350 km height with a Fresnel scale size of about
400 m. The VHF receivers measured the zonal velocities of the
irregularities with scale size of about 1 km from signals received
by the geostationary satellites Fleetsat 7 (- 100o W) and Fleetsat
8 (-23o W) and using two sets of two antennas spaced about 100 m
in the magnetic east-west direction. The velocities measured by
these two methods were compared and the limitations and errors in
the zonal velocity calculations for both methods are discussed.",
conference-location = "Sopron, Hungary",
conference-year = "23-30 Aug.",
language = "en",
urlaccessdate = "12 maio 2024"
}