Please use this identifier to cite or link to this item: http://hdl.handle.net/2440/12374
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Type: Journal article
Title: Zonal mean and tidal dynamics from space: An empirical examination of aliasing and sampling issues
Author: Forbes, J.
Kilpatrick, M.
Fritts, D.
Manson, A.
Vincent, R.
Citation: Annales Geophysicae, 1997; 15(9):1158-1164
Publisher: European Geosciences Union
Issue Date: 1997
ISSN: 0992-7689
1432-0576
Abstract: Interpretations of space-based measurements of atmospheric parameters in the mesosphere and thermosphere are complicated by large local-time variations at these altitudes. For this reason, satellite orbits are often preferred which precess through all local times one or more times per season. However, the local-time structure of the atmosphere is inherently non-stationary, which can lead to sampling and aliasing difficulties when attempting to deconvolve the measurements into zonal mean and tidal components. In the present study, hourly radar measurements of mesopause-region winds are used to form a mock data base which can be used to gain insight into implications of the aforementioned problems; the use of actual measurements introduces a realistic element of geophysical temporal variability. Assuming zonal symmetry (i.e., migrating tides superimposed on a zonal mean circulation), the radar measurements are sampled from the satellite perspective for orbital inclinations of 57° and 70°, and compared to the ground or true perspective. These comparisons provide realistic estimates of the errors to be expected when attempting to derive mean and tidal components from space-based measurements. For both diurnal and semidiurnal components, and the quoted satellite inclinations, acceptable errors (3–4m/srms) are obtained for data covering 24h local time (i.e., ascending plus descending nodes); the corresponding errors for single-node data (12h local-time coverage) are of order 8–11m/s, and therefore may not represent reliable estimates of the actual tidal components. There exist certain caveats in connection with the latter conclusion which are discussed.
RMID: 0030004019
DOI: 10.1007/s00585-997-1158-z
Published version: http://www.ann-geophys.net/15/1158/1997/
Appears in Collections:Physics publications

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