Advanced search
Start date
Betweenand
(Reference retrieved automatically from Web of Science through information on FAPESP grant and its corresponding number as mentioned in the publication by the authors.)

Diurnal variation in gravity wave activity at low and middle latitudes

Full text
Author(s):
Andrioli, V. F. [1] ; Fritts, D. C. [2] ; Batista, P. P. [1] ; Clemesha, B. R. [1] ; Janches, D. [3]
Total Authors: 5
Affiliation:
[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
Total Affiliations: 3
Document type: Journal article
Source: Annales Geophysicae; v. 31, n. 11, p. 2123-2135, 2013.
Web of Science Citations: 4
Abstract

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)

FAPESP's process: 12/08769-9 - Study of Gravity Waves In The Mesosphere Lower Thermosphere Region Using Meteor Radar, Lidar and All-Sky CCD Imagers
Grantee:Vânia Fátima Andrioli Novaes Silva
Support Opportunities: Scholarships in Brazil - Post-Doctoral