Gravity wave activity in the lower atmosphere: Seasonal and latitudinal variations

A climatology of gravity wave activity in the lower atmosphere based on high-resolution radiosonde measurements provided by the Australian Bureau of Meteorology is presented. These data are ideal for investigating gravity wave activity and its variation with position and time. Observations from 18 m...

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Published in:Journal of Geophysical Research: Atmospheres
Main Authors: Allen, S., Vincent, R.
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union 1995
Subjects:
Online Access:http://hdl.handle.net/2440/12556
https://doi.org/10.1029/94JD02688
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spelling ftunivadelaidedl:oai:digital.library.adelaide.edu.au:2440/12556 2023-05-15T14:02:51+02:00 Gravity wave activity in the lower atmosphere: Seasonal and latitudinal variations Allen, S. Vincent, R. 1995 application/pdf http://hdl.handle.net/2440/12556 https://doi.org/10.1029/94JD02688 en eng American Geophysical Union Journal of Geophysical Research, 1995; 100(D1):1327-1350 0148-0227 http://hdl.handle.net/2440/12556 doi:10.1029/94JD02688 Vincent, R. [0000-0001-6559-6544] Copyright 1995 American Geophysical Union http://www.agu.org/journals/ABS/1995/94JD02688.shtml Journal article 1995 ftunivadelaidedl https://doi.org/10.1029/94JD02688 2023-02-06T07:12:23Z A climatology of gravity wave activity in the lower atmosphere based on high-resolution radiosonde measurements provided by the Australian Bureau of Meteorology is presented. These data are ideal for investigating gravity wave activity and its variation with position and time. Observations from 18 meteorological stations within Australia and Antarctica, covering a latitude range of 12°S – 68°S and a longitude range of 78°E – 159°E, are discussed. Vertical wavenumber power spectra of normalized temperature fluctuations are calculated within both the troposphere and the lower stratosphere and are compared with the predictions of current gravity wave saturation theories. Estimates of important model parameters such as the total gravity wave energy per unit mass are also presented. The vertical wavenumber power spectra are found to remain approximately invariant with time and geographic location with only one significant exception. Spectral amplitudes observed within the lower stratosphere are found to be consistent with theoretical expectations but the amplitudes observed within the troposphere are consistently larger than expected, often by as much as a factor of about 3. Seasonal variations of stratospheric wave energy per unit mass are identified with maxima occurring during the low-latitude wet season and during the midlatitude winter. These variations do not exceed a factor of about 2. Similar variations are not found in the troposphere where temperature fluctuations are likely to be contaminated by convection and inversions. The largest values of wave energy density are typically found near the tropopause. Simon J. Allen and Robert A. Vincent Article in Journal/Newspaper Antarc* Antarctica The University of Adelaide: Digital Library Journal of Geophysical Research: Atmospheres 100 D1 1327 1350
institution Open Polar
collection The University of Adelaide: Digital Library
op_collection_id ftunivadelaidedl
language English
description A climatology of gravity wave activity in the lower atmosphere based on high-resolution radiosonde measurements provided by the Australian Bureau of Meteorology is presented. These data are ideal for investigating gravity wave activity and its variation with position and time. Observations from 18 meteorological stations within Australia and Antarctica, covering a latitude range of 12°S – 68°S and a longitude range of 78°E – 159°E, are discussed. Vertical wavenumber power spectra of normalized temperature fluctuations are calculated within both the troposphere and the lower stratosphere and are compared with the predictions of current gravity wave saturation theories. Estimates of important model parameters such as the total gravity wave energy per unit mass are also presented. The vertical wavenumber power spectra are found to remain approximately invariant with time and geographic location with only one significant exception. Spectral amplitudes observed within the lower stratosphere are found to be consistent with theoretical expectations but the amplitudes observed within the troposphere are consistently larger than expected, often by as much as a factor of about 3. Seasonal variations of stratospheric wave energy per unit mass are identified with maxima occurring during the low-latitude wet season and during the midlatitude winter. These variations do not exceed a factor of about 2. Similar variations are not found in the troposphere where temperature fluctuations are likely to be contaminated by convection and inversions. The largest values of wave energy density are typically found near the tropopause. Simon J. Allen and Robert A. Vincent
format Article in Journal/Newspaper
author Allen, S.
Vincent, R.
spellingShingle Allen, S.
Vincent, R.
Gravity wave activity in the lower atmosphere: Seasonal and latitudinal variations
author_facet Allen, S.
Vincent, R.
author_sort Allen, S.
title Gravity wave activity in the lower atmosphere: Seasonal and latitudinal variations
title_short Gravity wave activity in the lower atmosphere: Seasonal and latitudinal variations
title_full Gravity wave activity in the lower atmosphere: Seasonal and latitudinal variations
title_fullStr Gravity wave activity in the lower atmosphere: Seasonal and latitudinal variations
title_full_unstemmed Gravity wave activity in the lower atmosphere: Seasonal and latitudinal variations
title_sort gravity wave activity in the lower atmosphere: seasonal and latitudinal variations
publisher American Geophysical Union
publishDate 1995
url http://hdl.handle.net/2440/12556
https://doi.org/10.1029/94JD02688
genre Antarc*
Antarctica
genre_facet Antarc*
Antarctica
op_source http://www.agu.org/journals/ABS/1995/94JD02688.shtml
op_relation Journal of Geophysical Research, 1995; 100(D1):1327-1350
0148-0227
http://hdl.handle.net/2440/12556
doi:10.1029/94JD02688
Vincent, R. [0000-0001-6559-6544]
op_rights Copyright 1995 American Geophysical Union
op_doi https://doi.org/10.1029/94JD02688
container_title Journal of Geophysical Research: Atmospheres
container_volume 100
container_issue D1
container_start_page 1327
op_container_end_page 1350
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