@Article{ClemeshaSimo:1990:CoPaEn,
author = "Clemesha, Barclay Robert and Simonich, Dale Martin",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)}",
title = "Comments on a paper entitled {"}Gravity wave generation of
simultaneous auroral sporadic-E layers and sudden neutral sodium
layers{"} by S. Kirkwood and P.N. Collis",
journal = "Journal of Atmospheric and Solar-Terrestrial Physics",
year = "1990",
volume = "52",
number = "1",
pages = "85--86",
keywords = "gravity waves, auroral sporadic-E layers, neutral sodium layers.",
abstract = "KIRKWOOD and COLLIS (1989) have suggested that the sudden sodium
layers (SSLs) which have been observed at high latitudes (von ZAHN
et al., 1987; von ZAHN and HANSEN, 1988; GARDNER et al., 1986)
might be produced by strong downward neutral winds, probably
produced by gravity waves resulting from Joule heating caused by
auroral precipitation. They show that the presence of such a wind
could produce enhanced concentrations of minor atmospheric
constituents provided two conditions were met: (1) the vertical
wind would have to decrease rapidly with decreasing height (in
Kirkwood and Collis's model it was reduced to zero just below the
height at which the layer was to be formed), and (2) the mixing
ratio of the minor constituent would have to increase with height
above this point. The suggestion of Kirkwood and Collis is an
interesting one, especially in view of the fact that the
alternative mechanisms which have been suggested in the literature
(CLEMESHA et al., 1978, 1980; von ZAHN et al., 1987; CLEMESHA et
al., 1988) have not been shown to explain all the observed
characteristics of enhanced sodium layers. Unfortunately, however,
there appear to be two fatal flaws in the proposed mechanism.",
issn = "1364-6826",
label = "7082",
language = "en",
targetfile = "1-s2.0-0021916990901187-main.pdf",
urlaccessdate = "01 maio 2024"
}