Systematic attribution of observed Southern Hemisphere circulation trends to external forcing and internal variability

A critical question in the global warming debate concerns the causes of the observed trends of the Southern Hemisphere (SH) atmospheric circulation over recent decades. Secular trends have been identified in the frequency of occurrence of circulation regimes, namely the positive phase of the Souther...

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Main Authors: C. L. E. Franzke, T. J. O'Kane, D. P. Monselesan, J. S. Risbey, I. Horenko
Format: Article
Language:English
Published: Copernicus Publications 2015-09-01
Series:Nonlinear Processes in Geophysics
Online Access:http://www.nonlin-processes-geophys.net/22/513/2015/npg-22-513-2015.pdf
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author C. L. E. Franzke
T. J. O'Kane
D. P. Monselesan
J. S. Risbey
I. Horenko
author_facet C. L. E. Franzke
T. J. O'Kane
D. P. Monselesan
J. S. Risbey
I. Horenko
author_sort C. L. E. Franzke
collection DOAJ
description A critical question in the global warming debate concerns the causes of the observed trends of the Southern Hemisphere (SH) atmospheric circulation over recent decades. Secular trends have been identified in the frequency of occurrence of circulation regimes, namely the positive phase of the Southern Annular Mode (SAM) and the hemispheric wave-3 pattern which is associated with blocking. Previous studies into the causes of these secular trends have either been purely model based, have not included observational forcing data or have mixed external forcing with indices of internal climate variability impeding a systematic and unbiased attribution of the causes of the secular trends. Most model studies also focused mainly on the austral summer season. However, the changes to the storm tracks have occurred in all seasons and particularly in the austral winter and early spring when midlatitude blocking is most active and stratospheric ozone should not play a role. Here we systematically attribute the secular trends over the recent decades using a non-stationary clustering method applied to both reanalysis and observational forcing data from all seasons. While most previous studies emphasized the importance of stratospheric ozone depletion in causing austral summer SH circulation trends, we show observational evidence that anthropogenic greenhouse gas concentrations have been the major driver of these secular trends in the SAM and blocking when all seasons are considered. Our results suggest that the recovery of the ozone hole might delay the signal of global warming less strongly than previously thought and that effects from all seasons are likely crucial in understanding the causes of the secular trends.
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spelling doaj.art-53470a1d131247348f8d5721855f65f92022-12-22T00:53:03ZengCopernicus PublicationsNonlinear Processes in Geophysics1023-58091607-79462015-09-0122551352510.5194/npg-22-513-2015Systematic attribution of observed Southern Hemisphere circulation trends to external forcing and internal variabilityC. L. E. Franzke0T. J. O'Kane1D. P. Monselesan2J. S. Risbey3I. Horenko4Meteorological Institute and Center for Earth System Research and Sustainability, University of Hamburg, Hamburg, GermanyCSIRO Oceans and Atmosphere, Hobart, AustraliaCSIRO Oceans and Atmosphere, Hobart, AustraliaCSIRO Oceans and Atmosphere, Hobart, AustraliaUniversità della Svizzera Italiana, Lugano, SwitzerlandA critical question in the global warming debate concerns the causes of the observed trends of the Southern Hemisphere (SH) atmospheric circulation over recent decades. Secular trends have been identified in the frequency of occurrence of circulation regimes, namely the positive phase of the Southern Annular Mode (SAM) and the hemispheric wave-3 pattern which is associated with blocking. Previous studies into the causes of these secular trends have either been purely model based, have not included observational forcing data or have mixed external forcing with indices of internal climate variability impeding a systematic and unbiased attribution of the causes of the secular trends. Most model studies also focused mainly on the austral summer season. However, the changes to the storm tracks have occurred in all seasons and particularly in the austral winter and early spring when midlatitude blocking is most active and stratospheric ozone should not play a role. Here we systematically attribute the secular trends over the recent decades using a non-stationary clustering method applied to both reanalysis and observational forcing data from all seasons. While most previous studies emphasized the importance of stratospheric ozone depletion in causing austral summer SH circulation trends, we show observational evidence that anthropogenic greenhouse gas concentrations have been the major driver of these secular trends in the SAM and blocking when all seasons are considered. Our results suggest that the recovery of the ozone hole might delay the signal of global warming less strongly than previously thought and that effects from all seasons are likely crucial in understanding the causes of the secular trends.http://www.nonlin-processes-geophys.net/22/513/2015/npg-22-513-2015.pdf
spellingShingle C. L. E. Franzke
T. J. O'Kane
D. P. Monselesan
J. S. Risbey
I. Horenko
Systematic attribution of observed Southern Hemisphere circulation trends to external forcing and internal variability
Nonlinear Processes in Geophysics
title Systematic attribution of observed Southern Hemisphere circulation trends to external forcing and internal variability
title_full Systematic attribution of observed Southern Hemisphere circulation trends to external forcing and internal variability
title_fullStr Systematic attribution of observed Southern Hemisphere circulation trends to external forcing and internal variability
title_full_unstemmed Systematic attribution of observed Southern Hemisphere circulation trends to external forcing and internal variability
title_short Systematic attribution of observed Southern Hemisphere circulation trends to external forcing and internal variability
title_sort systematic attribution of observed southern hemisphere circulation trends to external forcing and internal variability
url http://www.nonlin-processes-geophys.net/22/513/2015/npg-22-513-2015.pdf
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