@Article{ClemeshaBati:2008:GrWaWi,
author = "Clemesha, Barclay Robert and Batista, Paulo Prado",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)}",
title = "Gravity waves and wind-shear in the MLT at 23 S",
journal = "Advances in Space Research",
year = "2008",
volume = "41",
number = "9",
pages = "1471--1476",
keywords = "Gravity waves, AERONOMY, gravity waves, MLT, winds.",
abstract = "We have used the technique suggested by Hocking [Hocking, W. A new
approach to momentum flux determinations using SKiYMET meteor
radars. Ann. Geophys. 23, 2005.] to derive short period wind
variances in the 80-100 km region from meteor radar data. We find
that these fluctuating winds, assumed to correspond to gravity
waves and turbulence, are closely correlated with the vertical
shear of the horizontal tidal winds. This close correlation
suggests that in situ wind shear may be a major source of gravity
waves and turbulence in the MLT. If this is the case, gravity
waves generated in the troposphere and propagating up to the MLT
region, generally assumed to constitute an important influence on
the climatology of the region, may be a less important source of
energy and momentum in the 80-100 kin region than has been
hitherto believed. (C) 2007 COSPAR. Published by Elsevier Ltd. All
rights reserved.",
doi = "10.1016/j.asr.2007.03.085",
url = "http://dx.doi.org/10.1016/j.asr.2007.03.085",
issn = "0273-1177",
language = "en",
targetfile = "gravity waves.pdf",
urlaccessdate = "10 maio 2024"
}