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Gravity wave occurrence statistics derived from paired COSMI
Details of Research
Title
Gravity wave occurrence statistics derived from paired COSMIC/FORMOSAT3 observations
Abstract
The analysis presented provides statistical information on the occurrence of gravity waves using the dense sampling geometry provided by the COSMIC/FORMOSAT3 constellation. This is achieved by deriving profiles of the gravity wave temperature perturbations from satellite observation and then identifying profile pairs; the magnitude of the cross S-transform derived from normalized profile pairs is then compared with Monte Carlo simulations to determine whether the same wave can be observed in both profiles. This procedure allows the percentage of paired observations which contain the same wave packet to be derived at a given significance level. This study shows that the occurrence of coherent waves varies strongly as a function of latitude and season. The latitudinal variation observed is demonstrated to be at least partially related to the preferential occurrence of long horizontal wavelength gravity waves at the equator. However, other factors obviously also have an impact, for example seasonal variations in the occurrence in the subtropics seem to be linked to critical level filtering above the subtropical winter jet. The use of the discussed methodology in identifying profile pairs which should be used in the calculation of gravity wave characteristics, such as horizontal wavelength, is also considered. Application of this technique as a quality control step seems to reduce biases introduced into the horizontal wavelength distribution when uncorrelated profile pairs are used to derive phase information. Thus, it is highly recommended to apply some statistical technique to identify profile pairs which include the same wave before applying schemes to derive horizontal wavelength and/or momentum fluxes. © 2012. American Geophysical Union. All Rights Reserved.
Details
1st Author
McDonald, A.
Author
McDonald, A.
Year
2012
Journal
Journal of Geophysical Research Atmospheres
Volume
117
Number
15
DOI
10.1029/2011JD016715
URL
https://www.scopus.com/inward/recor.....88f4929184a728ae8a3aabb50
Publisher
Blackwell Publishing Ltd
Keywords
Monte Carlo methods
Wavelength, Coherent waves
Critical level
Latitudinal variation
Momentum flux
Monte Carlo Simulation
Phase information
S transforms
Satellite observations
Seasonal variation
Statistical information
Statistical techniques
Temperature perturbations
Wave characteristics
Wavelength distribution, Gravity waves, atmospheric modeling
COSMIC
FORMOSAT-3
gravity wave
latitudinal gradient
momentum transfer
Monte Carlo analysis
sampling
satellite imagery
seasonal variation
temperature profile
transform
wavelength
Other
Citation
McDonald, A. (2012). Gravity wave occurrence statistics derived from paired COSMIC/FORMOSAT3 observations. Journal of Geophysical Research Atmospheres, 117(15)
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McDonald, A.,
Gravity wave occurrence statistics derived from paired COSMI
. Antarctica NZ, accessed 01/08/2026, https://adam.antarcticanz.govt.nz/nodes/view/64223, 10.1029/2011JD016715