Recent Changes in the Annual Mean Regional Hadley Circulation and Their Impacts on South America

This work employs the regional climate model RegCM4 and observational datasets to investigate the impacts of changes in the intensity and poleward edge of regional HC over South America (HCSA) on the patterns of wind, geopotential height, precipitation, and temperature during the period 1996–2011. S...

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Main Authors: Ana Carolina Vasques Freitas, Tércio Ambrizzi
Format: Article
Language:English
Published: Hindawi Limited 2015-01-01
Series:Advances in Meteorology
Online Access:http://dx.doi.org/10.1155/2015/780205
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spelling doaj-5ab6fa7559964d54b75d77bf108244782020-11-24T22:17:59ZengHindawi LimitedAdvances in Meteorology1687-93091687-93172015-01-01201510.1155/2015/780205780205Recent Changes in the Annual Mean Regional Hadley Circulation and Their Impacts on South AmericaAna Carolina Vasques Freitas0Tércio Ambrizzi1Institute of Astronomy, Geophysics and Atmospheric Sciences, 05508-090 São Paulo, SP, BrazilInstitute of Astronomy, Geophysics and Atmospheric Sciences, 05508-090 São Paulo, SP, BrazilThis work employs the regional climate model RegCM4 and observational datasets to investigate the impacts of changes in the intensity and poleward edge of regional HC over South America (HCSA) on the patterns of wind, geopotential height, precipitation, and temperature during the period 1996–2011. Significant trends of HCSA intensification and poleward expansion are found during the period analyzed. To evaluate the effects of these changes over SA, two composites, representing the intensification and poleward expansion cases, are examined separately. Significant correlations are seen between the temperature, zonal wind, and the HCSA intensity over the northern, central, and southern regions of SA and South Atlantic. Results show that, in both composites, regions with anomalous easterly (westerly) winds coming from (towards) the Atlantic Ocean have negative (positive) correlations with the HCSA intensity and poleward edge. The model performance varies regionally and the southern SA region exhibits better agreement with the observations. The role of the sea surface temperatures in driving the changes in the HCSA is examined. Notable similarity is found in the results for the two cases analyzed, which could indicate that, in most cases, the changes in the intensity and poleward edge of the HCSA are occurring simultaneously.http://dx.doi.org/10.1155/2015/780205
collection DOAJ
language English
format Article
sources DOAJ
author Ana Carolina Vasques Freitas
Tércio Ambrizzi
spellingShingle Ana Carolina Vasques Freitas
Tércio Ambrizzi
Recent Changes in the Annual Mean Regional Hadley Circulation and Their Impacts on South America
Advances in Meteorology
author_facet Ana Carolina Vasques Freitas
Tércio Ambrizzi
author_sort Ana Carolina Vasques Freitas
title Recent Changes in the Annual Mean Regional Hadley Circulation and Their Impacts on South America
title_short Recent Changes in the Annual Mean Regional Hadley Circulation and Their Impacts on South America
title_full Recent Changes in the Annual Mean Regional Hadley Circulation and Their Impacts on South America
title_fullStr Recent Changes in the Annual Mean Regional Hadley Circulation and Their Impacts on South America
title_full_unstemmed Recent Changes in the Annual Mean Regional Hadley Circulation and Their Impacts on South America
title_sort recent changes in the annual mean regional hadley circulation and their impacts on south america
publisher Hindawi Limited
series Advances in Meteorology
issn 1687-9309
1687-9317
publishDate 2015-01-01
description This work employs the regional climate model RegCM4 and observational datasets to investigate the impacts of changes in the intensity and poleward edge of regional HC over South America (HCSA) on the patterns of wind, geopotential height, precipitation, and temperature during the period 1996–2011. Significant trends of HCSA intensification and poleward expansion are found during the period analyzed. To evaluate the effects of these changes over SA, two composites, representing the intensification and poleward expansion cases, are examined separately. Significant correlations are seen between the temperature, zonal wind, and the HCSA intensity over the northern, central, and southern regions of SA and South Atlantic. Results show that, in both composites, regions with anomalous easterly (westerly) winds coming from (towards) the Atlantic Ocean have negative (positive) correlations with the HCSA intensity and poleward edge. The model performance varies regionally and the southern SA region exhibits better agreement with the observations. The role of the sea surface temperatures in driving the changes in the HCSA is examined. Notable similarity is found in the results for the two cases analyzed, which could indicate that, in most cases, the changes in the intensity and poleward edge of the HCSA are occurring simultaneously.
url http://dx.doi.org/10.1155/2015/780205
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