The response of superpressure balloons to gravity wave motions

Superpressure balloons (SPB), which float on constant density (isopycnic) surfaces, provide a unique way of measuring the properties of atmospheric gravity waves (GW) as a function of wave intrinsic frequency. Here we devise a quasi-analytic method of investigating the SPB response to GW motions. It...

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Published in:Atmospheric Measurement Techniques
Main Authors: Vincent, R., Hertzog, A.
Format: Article in Journal/Newspaper
Language:English
Published: European Geosciences Union 2014
Subjects:
Online Access:http://hdl.handle.net/2440/86712
https://doi.org/10.5194/amt-7-1043-2014
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spelling ftunivadelaidedl:oai:digital.library.adelaide.edu.au:2440/86712 2023-12-24T10:09:56+01:00 The response of superpressure balloons to gravity wave motions Vincent, R. Hertzog, A. 2014 application/pdf http://hdl.handle.net/2440/86712 https://doi.org/10.5194/amt-7-1043-2014 en eng European Geosciences Union Atmospheric Measurement Techniques, 2014; 7(4):1043-1055 1867-1381 1867-8548 http://hdl.handle.net/2440/86712 doi:10.5194/amt-7-1043-2014 Vincent, R. [0000-0001-6559-6544] © Author(s) 2014. CC Attribution 3.0 License. http://dx.doi.org/10.5194/amt-7-1043-2014 Journal article 2014 ftunivadelaidedl https://doi.org/10.5194/amt-7-1043-2014 2023-11-27T23:26:31Z Superpressure balloons (SPB), which float on constant density (isopycnic) surfaces, provide a unique way of measuring the properties of atmospheric gravity waves (GW) as a function of wave intrinsic frequency. Here we devise a quasi-analytic method of investigating the SPB response to GW motions. It is shown that the results agree well with more rigorous numerical simulations of balloon motions and provide a better understanding of the response of SPB to GW, especially at high frequencies. The methodology is applied to ascertain the accuracy of GW studies using 12 m diameter SPB deployed in the 2010 Concordiasi campaign in the Antarctic. In comparison with the situation in earlier campaigns, the vertical displacements of the SPB were measured directly using GPS. It is shown using a large number of Monte Carlo-type simulations with realistic instrumental noise that important wave parameters, such as momentum flux, phase speed and wavelengths, can be retrieved with good accuracy from SPB observations for intrinsic wave periods greater than ca. 10 min. The noise floor for momentum flux is estimated to be ca. 10−4 mPa. R. A. Vincent, and A. Hertzog Article in Journal/Newspaper Antarc* Antarctic The University of Adelaide: Digital Library Antarctic The Antarctic Atmospheric Measurement Techniques 7 4 1043 1055
institution Open Polar
collection The University of Adelaide: Digital Library
op_collection_id ftunivadelaidedl
language English
description Superpressure balloons (SPB), which float on constant density (isopycnic) surfaces, provide a unique way of measuring the properties of atmospheric gravity waves (GW) as a function of wave intrinsic frequency. Here we devise a quasi-analytic method of investigating the SPB response to GW motions. It is shown that the results agree well with more rigorous numerical simulations of balloon motions and provide a better understanding of the response of SPB to GW, especially at high frequencies. The methodology is applied to ascertain the accuracy of GW studies using 12 m diameter SPB deployed in the 2010 Concordiasi campaign in the Antarctic. In comparison with the situation in earlier campaigns, the vertical displacements of the SPB were measured directly using GPS. It is shown using a large number of Monte Carlo-type simulations with realistic instrumental noise that important wave parameters, such as momentum flux, phase speed and wavelengths, can be retrieved with good accuracy from SPB observations for intrinsic wave periods greater than ca. 10 min. The noise floor for momentum flux is estimated to be ca. 10−4 mPa. R. A. Vincent, and A. Hertzog
format Article in Journal/Newspaper
author Vincent, R.
Hertzog, A.
spellingShingle Vincent, R.
Hertzog, A.
The response of superpressure balloons to gravity wave motions
author_facet Vincent, R.
Hertzog, A.
author_sort Vincent, R.
title The response of superpressure balloons to gravity wave motions
title_short The response of superpressure balloons to gravity wave motions
title_full The response of superpressure balloons to gravity wave motions
title_fullStr The response of superpressure balloons to gravity wave motions
title_full_unstemmed The response of superpressure balloons to gravity wave motions
title_sort response of superpressure balloons to gravity wave motions
publisher European Geosciences Union
publishDate 2014
url http://hdl.handle.net/2440/86712
https://doi.org/10.5194/amt-7-1043-2014
geographic Antarctic
The Antarctic
geographic_facet Antarctic
The Antarctic
genre Antarc*
Antarctic
genre_facet Antarc*
Antarctic
op_source http://dx.doi.org/10.5194/amt-7-1043-2014
op_relation Atmospheric Measurement Techniques, 2014; 7(4):1043-1055
1867-1381
1867-8548
http://hdl.handle.net/2440/86712
doi:10.5194/amt-7-1043-2014
Vincent, R. [0000-0001-6559-6544]
op_rights © Author(s) 2014. CC Attribution 3.0 License.
op_doi https://doi.org/10.5194/amt-7-1043-2014
container_title Atmospheric Measurement Techniques
container_volume 7
container_issue 4
container_start_page 1043
op_container_end_page 1055
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