@Article{AbduSobrNaka:1985:LoLaSc,
author = "Abdu, Mangalathyil Ali and Sobral, Jos{\'e} Humberto Andrade and
Nakamura, Y",
title = "On the low latitude scanning photometer signatures of equatorial
ionospphere plasma bubbles",
journal = "Revista Brasileira de Geof{\'{\i}}sica",
year = "1985",
volume = "3",
number = ":",
pages = "33--39",
keywords = "AERONOMIA, regi{\~o}es tropicais, fot{\^o}metros, bolhas de
plasma, ionosferas, tropical regions, photometers, ionospheres.",
abstract = "Meridional and east-west scan 6300 night airglow photometers are
being extensively used at the low latitude station Cachoeira
Paulista (23§S 45§W, dip latitude 14§), Brazil, for investigation
of trans-equatorial ionospheric plasma bubble dynamics. The zonal
velocities of the flux tube aligned plasma bubbles can be
determined, in a straightforward way, from the east-west
displacement of the airglow intensity valleys observed by the
east-west scan photometer. On the other hand, the determination of
the other velocity component of the plasma bubble motion (namely,
vertical motion in the equatorial plane)has to be based on the
meridional propagation of the airglow valleys observed by the
meridional scan photometer. Such determinations of the bubbles'
vertical rise velocity should, however, involve considerations on
different bubble parameters such as, for example, the phase of the
bubble event (whether growth, mature or decay phase), the limited
east-west extension, and the often observed westward tilt of the
bubble. In this brief report there were considered in some detail,
possible influences of these different factors on the
interpretation of low latitude scanning photometer data to infer
trans-equatorial plasma bubble dynamics. RESUMO: Medidas de
varredura da luminesc{\^e}ncia do oxig{\^e}nio at{\^o}mico (? =
6300)no per{\'{\i}}odo noturno, nos planos verticais Leste-Oeste
e Norte-Sul (magn{\'e}ticos), em Cachoeira Paulista (23§S 45§W,
inclin{\c{c}}{\~a}o14§), Brasil, tem sido utilizadas em grande
escala no estudo das chamadas bolhas ionosf{\'e}ricas. Tais
bolhas s{\~a}o zonas de deple{\c{c}}{\~a}o de eletron e
{\'{\i}}ons e extendem-se por milhares de quil{\^o}metros ao
longo das linhas de for{\c{c}}a do campo magn{\'e}tico terrestre
e transversalmente, por cerca de algumas dezenas ou centenas de
quil{\^o}metros. As velocidades dessas bolhas, no sentido
leste-oeste, s{\~a}o facilmente determinadas pelas medidas
fotom{\'e}tricas, Por outro lado, velocidade vertical de
propaga{\c{c}}{\~a}o pode ser determinada pela sua
proje{\c{c}}{\~a}o no plano vertical meridional. Contudo a
determinag{\c{c}}{\~a}o da componente vertical envolve
considera{\c{c}}{\~a}o de diversos par{\^a}metros, tais como a
fase da bolha (seja de crescimento, desenvolvida ou de
decaimento), a limitada extens{\~a}o leste-oeste e a
freq{\"u}entemente observada inclina{\c{c}}{\~a}o da bolha para
oeste. Neste trabalho considerou-se poss{\'{\i}}veis
influ{\^e}ncias destes diferentes fatores na
interpreta{\c{c}}{\~a}o de dados fotom{\'e}tricas de baixa
latitude, para inferir sobre a din{\^a}mica da bolha de plasma.",
issn = "0102-261X",
label = "9681",
targetfile = "8739.pdf",
urlaccessdate = "11 maio 2024"
}