4.6 Article

Extratropical Low-Frequency Variability With ENSO Forcing: A Reduced-Order Coupled Model Study

Journal

Publisher

AMER GEOPHYSICAL UNION
DOI: 10.1029/2021MS002530

Keywords

ENSO forcing; midlatitude dynamics; reduced-order models; pullback attractors; ocean-atmosphere interaction; Lyapunov exponents

Funding

  1. Belgian Federal Science Policy Office under European JPI-Climate/JPI-Oceans initiative [B2/20E/P1/ROADMAP]
  2. EU's Horizon 2020 Research and Innovation Programme [820970]
  3. EIT Climate-KIC [190733]
  4. European Institute of Innovation & Technology (EIT), a body of the European Union
  5. H2020 Societal Challenges Programme [820970] Funding Source: H2020 Societal Challenges Programme

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The study examines the impact of ENSO on the extratropics using a simplified model, finding different types of extratropical low-frequency variability associated with varying ENSO forcing. The analysis reveals the coexistence of two chaotic PBAs for certain parameter values under chaotic ENSO forcing, indicating potential challenges for extratropical climate predictions.
The impact of the El Nino-Southern Oscillation (ENSO) on the extratropics is investigated in an idealized, reduced-order model that has a tropical and an extratropical module. Unidirectional ENSO forcing is used to mimick the atmospheric bridge between the tropics and the extratropics. The variability of the coupled ocean-atmosphere extratropical module is then investigated through the analysis of its pullback attractors (PBAs). This analysis focuses on two types of ENSO forcing generated by the tropical module, one periodic and the other aperiodic. For a substantial range of the ENSO forcing, two chaotic PBAs are found to coexist for the same set of parameter values. Different types of extratropical low-frequency variability (LFV) are associated with either PBA over the parameter ranges explored. For periodic ENSO forcing, the coexisting PBAs exhibit only weak nonlinear instability. For chaotic forcing, though, they are quite unstable and certain extratropical perturbations induce transitions between the two PBAs. These distinct stability properties may have profound consequences for extratropical climate predictions: in particular, ensemble averaging may no longer help isolate the LFV signal.

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