North Atlantic Oscillation response to the Madden–Julian Oscillation in a coupled climate model

Daniel T. Skinner; Adrian J. Matthews; David P. Stevens

doi:10.1002/wea.4215

North Atlantic Oscillation response to the Madden–Julian Oscillation in a coupled climate model

Daniel T. Skinner^*
, Adrian J. Matthews
, David P. Stevens

^*Corresponding author for this work

School of Geographical Sciences

Research output: Contribution to journal › Article (Academic Journal) › peer-review

11 Citations (Scopus)

Abstract

Understanding and predicting the state of the North Atlantic Oscillation (NAO) is key to forecasting the weather in the United Kingdom (UK). It has been shown that particular phases of the Madden–Julian Oscillation (MJO) act as precursors to either NAO+ or NAO− events. We assess the ability of the UK Met Office coupled climate model (HadGEM3-GC3.1-MM) to simulate these NAO responses at lead times of 1–2 weeks and show that improvements are needed in the modelling of MJO teleconnection patterns.

Original language	English
Pages (from-to)	201-205
Number of pages	5
Journal	Weather
Volume	77
Issue number	6
Early online date	30 May 2022
DOIs	https://doi.org/10.1002/wea.4215
Publication status	Published - 1 Jun 2022

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abstract = "Understanding and predicting the state of the North Atlantic Oscillation (NAO) is key to forecasting the weather in the United Kingdom (UK). It has been shown that particular phases of the Madden–Julian Oscillation (MJO) act as precursors to either NAO+ or NAO− events. We assess the ability of the UK Met Office coupled climate model (HadGEM3-GC3.1-MM) to simulate these NAO responses at lead times of 1–2 weeks and show that improvements are needed in the modelling of MJO teleconnection patterns.",

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AB - Understanding and predicting the state of the North Atlantic Oscillation (NAO) is key to forecasting the weather in the United Kingdom (UK). It has been shown that particular phases of the Madden–Julian Oscillation (MJO) act as precursors to either NAO+ or NAO− events. We assess the ability of the UK Met Office coupled climate model (HadGEM3-GC3.1-MM) to simulate these NAO responses at lead times of 1–2 weeks and show that improvements are needed in the modelling of MJO teleconnection patterns.

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North Atlantic Oscillation response to the Madden–Julian Oscillation in a coupled climate model

Abstract

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