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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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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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 |
work_keys_str_mv |
AT alexanderpedrom anumericalstudyontheinterpretationofdatafromopenatmosphericballoonsoundings AT alexanderpedrom numericalstudyontheinterpretationofdatafromopenatmosphericballoonsoundings |
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1768541943155916800 |