QBO of the Equatorial-Stratospheric Winds Revisited: New Methods to Verify the Dominance of 28-Month Cycle
The equatorial-stratospheric wind that shows a Quasi Biennial Oscillation (22–32 months) has been revisited using a dual statistical detail regarding the search of the dominance harmonics. Data were used from the Freie Universitat of Berlin since 1953 for different heights combining the observations...
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2011-03-01
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Series: | International Journal of Ocean and Climate Systems |
Online Access: | https://doi.org/10.1260/1759-3131.2.1.19 |
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doaj-c3849db4e26346ecb9da2f7a1419a6592020-11-25T01:40:35ZengSAGE PublishingInternational Journal of Ocean and Climate Systems1759-31311759-314X2011-03-01210.1260/1759-3131.2.1.1910.1260_1759-3131.2.1.19QBO of the Equatorial-Stratospheric Winds Revisited: New Methods to Verify the Dominance of 28-Month CycleA. MazzarellaA. GiuliacciI. LiritzisThe equatorial-stratospheric wind that shows a Quasi Biennial Oscillation (22–32 months) has been revisited using a dual statistical detail regarding the search of the dominance harmonics. Data were used from the Freie Universitat of Berlin since 1953 for different heights combining the observations of the three radiosonde stations. The dominant period of 28 months has been reaffirmed but with a discernible amplitude and a phase, respectively, inversely varying with height. Such a cycle suggests an estimate for the coming easterly equatorial wind occurrence at 15 hPa level at the end of 2009. The 28-month harmonic is found to take about a year to descend from 15 to 70 hPa with a progressive lag of about 1 month/km. At the top of the stratosphere, easterlies dominate, while at the bottom, westerlies are more likely to be found. Correlation with sunspot numbers and seasonal rainfall is discussed.https://doi.org/10.1260/1759-3131.2.1.19 |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
A. Mazzarella A. Giuliacci I. Liritzis |
spellingShingle |
A. Mazzarella A. Giuliacci I. Liritzis QBO of the Equatorial-Stratospheric Winds Revisited: New Methods to Verify the Dominance of 28-Month Cycle International Journal of Ocean and Climate Systems |
author_facet |
A. Mazzarella A. Giuliacci I. Liritzis |
author_sort |
A. Mazzarella |
title |
QBO of the Equatorial-Stratospheric Winds Revisited: New Methods to Verify the Dominance of 28-Month Cycle |
title_short |
QBO of the Equatorial-Stratospheric Winds Revisited: New Methods to Verify the Dominance of 28-Month Cycle |
title_full |
QBO of the Equatorial-Stratospheric Winds Revisited: New Methods to Verify the Dominance of 28-Month Cycle |
title_fullStr |
QBO of the Equatorial-Stratospheric Winds Revisited: New Methods to Verify the Dominance of 28-Month Cycle |
title_full_unstemmed |
QBO of the Equatorial-Stratospheric Winds Revisited: New Methods to Verify the Dominance of 28-Month Cycle |
title_sort |
qbo of the equatorial-stratospheric winds revisited: new methods to verify the dominance of 28-month cycle |
publisher |
SAGE Publishing |
series |
International Journal of Ocean and Climate Systems |
issn |
1759-3131 1759-314X |
publishDate |
2011-03-01 |
description |
The equatorial-stratospheric wind that shows a Quasi Biennial Oscillation (22–32 months) has been revisited using a dual statistical detail regarding the search of the dominance harmonics. Data were used from the Freie Universitat of Berlin since 1953 for different heights combining the observations of the three radiosonde stations. The dominant period of 28 months has been reaffirmed but with a discernible amplitude and a phase, respectively, inversely varying with height. Such a cycle suggests an estimate for the coming easterly equatorial wind occurrence at 15 hPa level at the end of 2009. The 28-month harmonic is found to take about a year to descend from 15 to 70 hPa with a progressive lag of about 1 month/km. At the top of the stratosphere, easterlies dominate, while at the bottom, westerlies are more likely to be found. Correlation with sunspot numbers and seasonal rainfall is discussed. |
url |
https://doi.org/10.1260/1759-3131.2.1.19 |
work_keys_str_mv |
AT amazzarella qbooftheequatorialstratosphericwindsrevisitednewmethodstoverifythedominanceof28monthcycle AT agiuliacci qbooftheequatorialstratosphericwindsrevisitednewmethodstoverifythedominanceof28monthcycle AT iliritzis qbooftheequatorialstratosphericwindsrevisitednewmethodstoverifythedominanceof28monthcycle |
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1725044827222966272 |