Busca avançada
Ano de início
Entree
(Referência obtida automaticamente do Web of Science, por meio da informação sobre o financiamento pela FAPESP e o número do processo correspondente, incluída na publicação pelos autores.)

Diurnal variation in gravity wave activity at low and middle latitudes

Texto completo
Autor(es):
Andrioli, V. F. [1] ; Fritts, D. C. [2] ; Batista, P. P. [1] ; Clemesha, B. R. [1] ; Janches, D. [3]
Número total de Autores: 5
Afiliação do(s) autor(es):
[1] Inst Nacl Pesquisas Espaciais, BR-12201 Sao Jose Dos Campos, SP - Brazil
[2] GATS Boulder, Boulder, CO - USA
[3] NASA, GSFC, Space Weather Lab, Greenbelt, MD 20771 - USA
Número total de Afiliações: 3
Tipo de documento: Artigo Científico
Fonte: Annales Geophysicae; v. 31, n. 11, p. 2123-2135, 2013.
Citações Web of Science: 4
Resumo

We employ a modified composite day extension of the Hocking (2005) analysis method to study gravity wave (GW) activity in the mesosphere and lower thermosphere using 4 meteor radars spanning latitudes from 7 degrees S to 53.6 degrees S. Diurnal and semidiurnal modulations were observed in GW variances over all sites. Semidiurnal modulation with downward phase propagation was observed at lower latitudes mainly near the equinoxes. Diurnal modulations occur mainly near solstice and, except for the zonal component at Cariri (7 degrees S), do not exhibit downward phase propagation. At a higher latitude (SAAMER, 53.6 degrees S) these modulations are only observed in the meridional component where we can observe diurnal variation from March to May, and semidiurnal, during January, February, October (above 88 km) and November. Some of these modulations with downward phase progression correlate well with wind shear. When the wind shear is well correlated with the maximum of the variances the diurnal tide has its largest amplitudes, i.e., near equinox. Correlations exhibiting variations with tidal phases suggest significant GW-tidal interactions that have different characters depending on the tidal components and possible mean wind shears. Modulations that do not exhibit phase variations could be indicative of diurnal variations in GW sources. (AU)

Processo FAPESP: 12/08769-9 - Estudo das Ondas de Gravidade na Região da Mesosfera e Baixa Termosfera Utilizando Radar Meteórico, Radar de laser e Imageadores CCD All-Sky
Beneficiário:Vânia Fátima Andrioli Novaes Silva
Modalidade de apoio: Bolsas no Brasil - Pós-Doutorado