A Regime View of the North Atlantic Oscillation and Its Response to Anthropogenic Forcing

The distribution of the daily wintertime North Atlantic Oscillation (NAO) index in the 40-yr ECMWF Re-Analysis (ERA-40) is significantly negatively skewed. Dynamical and statistical analyses both suggest that this skewness reects the presence of two distinct regimes-referred to as "Greenland bl...

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Main Authors: Woollings, T, Hannachi, A, Hoskins, B, Turner, A
Format: Journal article
Language:English
Published: 2010
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author Woollings, T
Hannachi, A
Hoskins, B
Turner, A
author_facet Woollings, T
Hannachi, A
Hoskins, B
Turner, A
author_sort Woollings, T
collection OXFORD
description The distribution of the daily wintertime North Atlantic Oscillation (NAO) index in the 40-yr ECMWF Re-Analysis (ERA-40) is significantly negatively skewed. Dynamical and statistical analyses both suggest that this skewness reects the presence of two distinct regimes-referred to as "Greenland blocking" and "sub-polar jet." Changes in both the relative occurrence and in the structure of the regimes are shown to contribute to the long-term NAO trend over the ERA-40 period. This is contrasted with the simulation of the NAO in 100-yr control and doubled CO2 integrations of the third climate configuration of the Met Office Unied Model (HadCM3). The model has clear deficiencies in its simulation of the NAO in the control run, so its predictions of future behavior must be treated with caution. However, the subpolar jet regime does become more dominant under anthropogenic forcing and, while this change is small it is clearly statistically signicant and does represent a real change in the nature of NAO variability in the model. © 2010 American Meteorological Society.
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spelling oxford-uuid:aaa6bd01-4d48-48a5-b50c-f04ae8958c1a2022-03-27T03:16:40ZA Regime View of the North Atlantic Oscillation and Its Response to Anthropogenic ForcingJournal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:aaa6bd01-4d48-48a5-b50c-f04ae8958c1aEnglishSymplectic Elements at Oxford2010Woollings, THannachi, AHoskins, BTurner, AThe distribution of the daily wintertime North Atlantic Oscillation (NAO) index in the 40-yr ECMWF Re-Analysis (ERA-40) is significantly negatively skewed. Dynamical and statistical analyses both suggest that this skewness reects the presence of two distinct regimes-referred to as "Greenland blocking" and "sub-polar jet." Changes in both the relative occurrence and in the structure of the regimes are shown to contribute to the long-term NAO trend over the ERA-40 period. This is contrasted with the simulation of the NAO in 100-yr control and doubled CO2 integrations of the third climate configuration of the Met Office Unied Model (HadCM3). The model has clear deficiencies in its simulation of the NAO in the control run, so its predictions of future behavior must be treated with caution. However, the subpolar jet regime does become more dominant under anthropogenic forcing and, while this change is small it is clearly statistically signicant and does represent a real change in the nature of NAO variability in the model. © 2010 American Meteorological Society.
spellingShingle Woollings, T
Hannachi, A
Hoskins, B
Turner, A
A Regime View of the North Atlantic Oscillation and Its Response to Anthropogenic Forcing
title A Regime View of the North Atlantic Oscillation and Its Response to Anthropogenic Forcing
title_full A Regime View of the North Atlantic Oscillation and Its Response to Anthropogenic Forcing
title_fullStr A Regime View of the North Atlantic Oscillation and Its Response to Anthropogenic Forcing
title_full_unstemmed A Regime View of the North Atlantic Oscillation and Its Response to Anthropogenic Forcing
title_short A Regime View of the North Atlantic Oscillation and Its Response to Anthropogenic Forcing
title_sort regime view of the north atlantic oscillation and its response to anthropogenic forcing
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