Meteorological Source Variability in Atmospheric Gravity Wave Parameters Derived From a Tropical Infrasound Station
Autor: | Läslo Evers, A. Le‐Pichon, Elisabeth Blanc, Graeme Marlton, R. G. Harrison, Pieter Smets, Andrew Charlton-Perez |
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Rok vydání: | 2019 |
Předmět: |
Atmospheric Science
010504 meteorology & atmospheric sciences Atmospheric models Infrasound Microbarometer Geophysics Jet stream 01 natural sciences Atmosphere General Relativity and Quantum Cosmology Space and Planetary Science Earth and Planetary Sciences (miscellaneous) Wavenumber Gravity wave Phase velocity Physics::Atmospheric and Oceanic Physics Geology 0105 earth and related environmental sciences |
Zdroj: | Journal of Geophysical Research: Atmospheres. 124:4352-4364 |
ISSN: | 2169-8996 2169-897X |
Popis: | Gravity waves are an important part of the momentum budget of the atmosphere. Despite this, parameterizations of gravity wave spectra in atmospheric models are poorly constrained. Gravity waves are formed by jet streams, flow over topography and convection, all of which produce pressure perturbations as they propagate over the Earth’s surface, detectable by microbarometer arrays used for sensing infrasound. In this study, observations of gravity waves between 2007 and 2011 at an infrasound station in the Ivory Coast, West Africa are combined with meteorological data to calculate parameters such as intrinsic phase speed and wavenumber. Through spectral analysis, the seasonal and daily variations in all gravity wave parameters are examined. The gravity wave back azimuth varies with the migration of the Inter-Tropical Convergence Zone, a region of intense convection, supporting previous studies. Daily variations in gravity wave arrivals at the station can be linked to two distinct convective cycles over the land and ocean. This was achieved by combining the gravity wave parameters with lightning strikes detected by the Met Office’s Arrival Time Difference lightning detection system. Noise generated by turbulence in the middle of the day was found to attenuate smaller pressure amplitude gravity waves, artificially amplifying the daily variations in some gravity wave parameters. Detection of daily and seasonal variations in gravity wave parameters has the potential be used to improve the representation of gravity wave spectra in atmospheric models. |
Databáze: | OpenAIRE |
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