A numerical study on the interpretation of data from open atmospheric balloon soundings

Wrong information may be extracted from balloon soundings if neither appropriate interpretation and processing nor evaluations of certain inevitable distortions or artifacts on atmospheric measurements are performed. A numerical code that finds solutions to the dynamical and thermal equations descri...

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Autor principal: Alexander, Pedro M.
Publicado: 2005
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Acceso en línea:https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_08948763_v44_n3_p357_Alexander
http://hdl.handle.net/20.500.12110/paper_08948763_v44_n3_p357_Alexander
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spelling paper:paper_08948763_v44_n3_p357_Alexander2023-06-08T15:47:58Z A numerical study on the interpretation of data from open atmospheric balloon soundings Alexander, Pedro M. Acoustic waves Data processing Gravity waves Numerical analysis Optimization Oscillations Velocity measurement Artifacts Atmospheric measurements Balloon sounding Numerical codes Meteorological balloons airflow balloon observation data interpretation wind measurement Wrong information may be extracted from balloon soundings if neither appropriate interpretation and processing nor evaluations of certain inevitable distortions or artifacts on atmospheric measurements are performed. A numerical code that finds solutions to the dynamical and thermal equations describing an open balloon in the atmosphere is used to develop flight simulations under diverse conditions. The results are then employed to point out that a valid determination of values for diverse variables is intrinsically difficult. It is shown that the distance between the balloon and gondola may be chosen to optimize the information to be obtained from observations obtained during ascent and descent, so that even without an accurate balloon-tracking system, it may be possible to reconstruct horizontal wind fluctuations from the measurements. Vertical air oscillations may be only grossly inferred in some cases. The propagation direction of gravity waves detected during a sounding may be inferred and vertical wavelengths may typically be determined with a 10% accuracy. Air velocity measurements performed during flotation may be used to find shears. © 2005 American Meteorological Society. Fil:Alexander, P. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. 2005 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_08948763_v44_n3_p357_Alexander http://hdl.handle.net/20.500.12110/paper_08948763_v44_n3_p357_Alexander
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic Acoustic waves
Data processing
Gravity waves
Numerical analysis
Optimization
Oscillations
Velocity measurement
Artifacts
Atmospheric measurements
Balloon sounding
Numerical codes
Meteorological balloons
airflow
balloon observation
data interpretation
wind measurement
spellingShingle Acoustic waves
Data processing
Gravity waves
Numerical analysis
Optimization
Oscillations
Velocity measurement
Artifacts
Atmospheric measurements
Balloon sounding
Numerical codes
Meteorological balloons
airflow
balloon observation
data interpretation
wind measurement
Alexander, Pedro M.
A numerical study on the interpretation of data from open atmospheric balloon soundings
topic_facet Acoustic waves
Data processing
Gravity waves
Numerical analysis
Optimization
Oscillations
Velocity measurement
Artifacts
Atmospheric measurements
Balloon sounding
Numerical codes
Meteorological balloons
airflow
balloon observation
data interpretation
wind measurement
description Wrong information may be extracted from balloon soundings if neither appropriate interpretation and processing nor evaluations of certain inevitable distortions or artifacts on atmospheric measurements are performed. A numerical code that finds solutions to the dynamical and thermal equations describing an open balloon in the atmosphere is used to develop flight simulations under diverse conditions. The results are then employed to point out that a valid determination of values for diverse variables is intrinsically difficult. It is shown that the distance between the balloon and gondola may be chosen to optimize the information to be obtained from observations obtained during ascent and descent, so that even without an accurate balloon-tracking system, it may be possible to reconstruct horizontal wind fluctuations from the measurements. Vertical air oscillations may be only grossly inferred in some cases. The propagation direction of gravity waves detected during a sounding may be inferred and vertical wavelengths may typically be determined with a 10% accuracy. Air velocity measurements performed during flotation may be used to find shears. © 2005 American Meteorological Society.
author Alexander, Pedro M.
author_facet Alexander, Pedro M.
author_sort Alexander, Pedro M.
title A numerical study on the interpretation of data from open atmospheric balloon soundings
title_short A numerical study on the interpretation of data from open atmospheric balloon soundings
title_full A numerical study on the interpretation of data from open atmospheric balloon soundings
title_fullStr A numerical study on the interpretation of data from open atmospheric balloon soundings
title_full_unstemmed A numerical study on the interpretation of data from open atmospheric balloon soundings
title_sort numerical study on the interpretation of data from open atmospheric balloon soundings
publishDate 2005
url https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_08948763_v44_n3_p357_Alexander
http://hdl.handle.net/20.500.12110/paper_08948763_v44_n3_p357_Alexander
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