Quasi-periodic imprints in the equatorial troposphere and stratosphere in three decades of reanalysis data

Wavelet analysis is applied to zonal mean zonal wind and temperature fields to represent characteristics of temporal periodic features different from the annual and semi-annual recurrence in the troposphere and stratosphere. A daily database of reanalyses is used for the period 1979-2008, which comp...

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Autores principales: Alexander, P., Rossi, M.
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Acceso en línea:http://hdl.handle.net/20.500.12110/paper_01777971_v121_n3-4_p109_Alexander
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spelling todo:paper_01777971_v121_n3-4_p109_Alexander2023-10-03T15:08:07Z Quasi-periodic imprints in the equatorial troposphere and stratosphere in three decades of reanalysis data Alexander, P. Rossi, M. atmospheric dynamics El Nino-Southern Oscillation latitudinal gradient quasi-biennial oscillation stratosphere temperature gradient trend analysis troposphere wavelet analysis zonal wind Wavelet analysis is applied to zonal mean zonal wind and temperature fields to represent characteristics of temporal periodic features different from the annual and semi-annual recurrence in the troposphere and stratosphere. A daily database of reanalyses is used for the period 1979-2008, which comprises the era of satellite-based data, as some discontinuities have been observed around 1978 in previous studies. Levels for this study have been chosen at 400 and 10 hPa, respectively in the middle troposphere and middle stratosphere. As representative for diverse latitudinal regions we have respectively selected 0°, ±20°, ±40°, ±60°, ±80°. Significant features were only found at the equator. The period of the quasi-biennial oscillation (QBO) is found to exhibit a decreasing trend in time over the 30 years studied. Potential harmonics of the QBO are found in the tropical stratosphere but also troposphere. However, they do not exhibit the same tendency. This fact supports in particular the idea that the QBO and the tropospheric biennial oscillation may be unrelated phenomena. Some of the observed features lie within the known range of variability of the El Niño Southern Oscillation. Faint effects of the 11-year solar cycle variability may have been observed in the troposphere and stratosphere, but no firm assertion may be made due to the low number of observed cycles for this kind of phenomenon in the used data-set time span. Short-term solar variabilities leave no relevant imprint. © 2013 Springer-Verlag Wien. Fil:Alexander, P. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. JOUR info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar http://hdl.handle.net/20.500.12110/paper_01777971_v121_n3-4_p109_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 atmospheric dynamics
El Nino-Southern Oscillation
latitudinal gradient
quasi-biennial oscillation
stratosphere
temperature gradient
trend analysis
troposphere
wavelet analysis
zonal wind
spellingShingle atmospheric dynamics
El Nino-Southern Oscillation
latitudinal gradient
quasi-biennial oscillation
stratosphere
temperature gradient
trend analysis
troposphere
wavelet analysis
zonal wind
Alexander, P.
Rossi, M.
Quasi-periodic imprints in the equatorial troposphere and stratosphere in three decades of reanalysis data
topic_facet atmospheric dynamics
El Nino-Southern Oscillation
latitudinal gradient
quasi-biennial oscillation
stratosphere
temperature gradient
trend analysis
troposphere
wavelet analysis
zonal wind
description Wavelet analysis is applied to zonal mean zonal wind and temperature fields to represent characteristics of temporal periodic features different from the annual and semi-annual recurrence in the troposphere and stratosphere. A daily database of reanalyses is used for the period 1979-2008, which comprises the era of satellite-based data, as some discontinuities have been observed around 1978 in previous studies. Levels for this study have been chosen at 400 and 10 hPa, respectively in the middle troposphere and middle stratosphere. As representative for diverse latitudinal regions we have respectively selected 0°, ±20°, ±40°, ±60°, ±80°. Significant features were only found at the equator. The period of the quasi-biennial oscillation (QBO) is found to exhibit a decreasing trend in time over the 30 years studied. Potential harmonics of the QBO are found in the tropical stratosphere but also troposphere. However, they do not exhibit the same tendency. This fact supports in particular the idea that the QBO and the tropospheric biennial oscillation may be unrelated phenomena. Some of the observed features lie within the known range of variability of the El Niño Southern Oscillation. Faint effects of the 11-year solar cycle variability may have been observed in the troposphere and stratosphere, but no firm assertion may be made due to the low number of observed cycles for this kind of phenomenon in the used data-set time span. Short-term solar variabilities leave no relevant imprint. © 2013 Springer-Verlag Wien.
format JOUR
author Alexander, P.
Rossi, M.
author_facet Alexander, P.
Rossi, M.
author_sort Alexander, P.
title Quasi-periodic imprints in the equatorial troposphere and stratosphere in three decades of reanalysis data
title_short Quasi-periodic imprints in the equatorial troposphere and stratosphere in three decades of reanalysis data
title_full Quasi-periodic imprints in the equatorial troposphere and stratosphere in three decades of reanalysis data
title_fullStr Quasi-periodic imprints in the equatorial troposphere and stratosphere in three decades of reanalysis data
title_full_unstemmed Quasi-periodic imprints in the equatorial troposphere and stratosphere in three decades of reanalysis data
title_sort quasi-periodic imprints in the equatorial troposphere and stratosphere in three decades of reanalysis data
url http://hdl.handle.net/20.500.12110/paper_01777971_v121_n3-4_p109_Alexander
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