Inter ENSO variability and its influence over the South American monsoon system

Previous studies have discussed the interannual variability of a meridional seesaw of dry and wet conditions over South America (SA) associated to the modulation of the South Atlantic Convergence Zone (SACZ). However, they did not explore if the variability inter ENSO (El Niño Southern Osci...

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Main Authors: A. R. M. Drumond, T. Ambrizzi
Format: Article
Language:English
Published: Copernicus Publications 2006-01-01
Series:Advances in Geosciences
Online Access:http://www.adv-geosci.net/6/167/2006/adgeo-6-167-2006.pdf
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spelling doaj-12fcce28f2b04cd78ecfa1a6cfbdce422020-11-25T01:01:57ZengCopernicus PublicationsAdvances in Geosciences1680-73401680-73592006-01-016167171Inter ENSO variability and its influence over the South American monsoon systemA. R. M. DrumondT. AmbrizziPrevious studies have discussed the interannual variability of a meridional seesaw of dry and wet conditions over South America (SA) associated to the modulation of the South Atlantic Convergence Zone (SACZ). However, they did not explore if the variability inter ENSO (El Ni&#241;o Southern Oscillation) can be related to the phase changes of this dipole. To answer this question, an observational work was carried out to explore the atmospheric and Sea Surface Temperature (SST) conditions related to the same ENSO signal and to opposite dipole phases. <P style=&quot;line-height: 20px;&quot;> Rotated Empirical Orthogonal Function (REOF) analysis was applied over normalized Chen precipitation seasonal anomalies in order to find the dipole mode in the Austral Summer (December to February). The fourth rotated mode, explaining 6.6% of the total variance, consists of positive loading over the SACZ region and negative loading over northern Argentina. Extreme events were selected and enhanced activity of SACZ during the Summer season (SACZ+) was identified in nine years: five during La Ni&#241;a events (LN) and two in El Ni&#241;o episodes (EN). On the other hand, inhibited manifestations of this system (SACZ-) were identified in seven years: four in EN and two during LN. <P style=&quot;line-height: 20px;&quot;> Power spectrum analysis indicated that the interannual variability of the precipitation dipole seems to be related to the low frequency and to the quasi-biennial part of ENSO variability. The ENSO events with the same signal can present opposite phases for the dipole. The results suggest that the displacement of the convection over Indonesia and western Pacific can play an important role to modulate the seesaw pattern.http://www.adv-geosci.net/6/167/2006/adgeo-6-167-2006.pdf
collection DOAJ
language English
format Article
sources DOAJ
author A. R. M. Drumond
T. Ambrizzi
spellingShingle A. R. M. Drumond
T. Ambrizzi
Inter ENSO variability and its influence over the South American monsoon system
Advances in Geosciences
author_facet A. R. M. Drumond
T. Ambrizzi
author_sort A. R. M. Drumond
title Inter ENSO variability and its influence over the South American monsoon system
title_short Inter ENSO variability and its influence over the South American monsoon system
title_full Inter ENSO variability and its influence over the South American monsoon system
title_fullStr Inter ENSO variability and its influence over the South American monsoon system
title_full_unstemmed Inter ENSO variability and its influence over the South American monsoon system
title_sort inter enso variability and its influence over the south american monsoon system
publisher Copernicus Publications
series Advances in Geosciences
issn 1680-7340
1680-7359
publishDate 2006-01-01
description Previous studies have discussed the interannual variability of a meridional seesaw of dry and wet conditions over South America (SA) associated to the modulation of the South Atlantic Convergence Zone (SACZ). However, they did not explore if the variability inter ENSO (El Ni&#241;o Southern Oscillation) can be related to the phase changes of this dipole. To answer this question, an observational work was carried out to explore the atmospheric and Sea Surface Temperature (SST) conditions related to the same ENSO signal and to opposite dipole phases. <P style=&quot;line-height: 20px;&quot;> Rotated Empirical Orthogonal Function (REOF) analysis was applied over normalized Chen precipitation seasonal anomalies in order to find the dipole mode in the Austral Summer (December to February). The fourth rotated mode, explaining 6.6% of the total variance, consists of positive loading over the SACZ region and negative loading over northern Argentina. Extreme events were selected and enhanced activity of SACZ during the Summer season (SACZ+) was identified in nine years: five during La Ni&#241;a events (LN) and two in El Ni&#241;o episodes (EN). On the other hand, inhibited manifestations of this system (SACZ-) were identified in seven years: four in EN and two during LN. <P style=&quot;line-height: 20px;&quot;> Power spectrum analysis indicated that the interannual variability of the precipitation dipole seems to be related to the low frequency and to the quasi-biennial part of ENSO variability. The ENSO events with the same signal can present opposite phases for the dipole. The results suggest that the displacement of the convection over Indonesia and western Pacific can play an important role to modulate the seesaw pattern.
url http://www.adv-geosci.net/6/167/2006/adgeo-6-167-2006.pdf
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AT tambrizzi interensovariabilityanditsinfluenceoverthesouthamericanmonsoonsystem
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