Observations of intermediate-scale diurnal waves in the equatorial mesosphere and lower thermosphere

Details Observations of intermediate-scale diurnal waves in the equatorial mesosphere and lower thermosphere Observations of intermediate-scale diurnal waves in the equatorial mesosphere and lower thermosphere

Sep 2006

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2006jgra..11110s11l&link_type=abstract

Journal of Geophysical Research, Volume 111, Issue A10, CiteID A10S11

Physics

1

Atmospheric Processes: Middle Atmosphere Dynamics (0341, 0342), Atmospheric Processes: Mesospheric Dynamics, Atmospheric Processes: Tides And Planetary Waves, Atmospheric Processes: Remote Sensing

Scientific paper

The purpose of this study is to seek observational evidence for diurnal, vertically propagating inertia-gravity waves (IGWs) in the mesosphere and lower thermosphere (MLT). Numerical modeling studies indicate that vertically propagating IGWs excited by tropical heating provide a significant source of momentum for the semiannual oscillation (SAO) in the equatorial zonal mean winds. The power spectrum of these waves has a strong diurnal component. We analyze global patterns of ascending and descending node differences in MLT satellite temperatures, which are assumed in this study to be proxies for waves of diurnal period. Juxtaposed upon the planetary-scale features are localized variations with longitudinal wavelengths ranging from 25° to 50°, and with vertical wavelengths between 13 and 25 km. These ``intermediate-scale'' variations are spatially coherent, and persist for several weeks. Their amplitudes generally increase with altitude, while their phase structures suggest both eastward and westward propagation. The variance of wave numbers 9-17 in the MLT is examined in relation to the underlying stratospheric zonal mean zonal gradient winds. Stronger variances generally coincide with periods where the underlying zonal mean winds are relatively light, or unidirectional. The weak inverse association between variance strength and zonal wind magnitude is suggestive of a wave filtering mechanism.

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