Publications des scientifiques de l'IRD

Morel Y., Thual S., Delcroix Thierry, Hall N., Alory G. (2018). A theoretical model to analyze the Central to Eastern Pacific El Nino continuum. Ocean Modelling, 130, p. 140-159. ISSN 1463-5003.

Titre du document
A theoretical model to analyze the Central to Eastern Pacific El Nino continuum
Année de publication
2018
Type de document
Article référencé dans le Web of Science WOS:000445228500008
Auteurs
Morel Y., Thual S., Delcroix Thierry, Hall N., Alory G.
Source
Ocean Modelling, 2018, 130, p. 140-159 ISSN 1463-5003
A current scientific issue of great interest is to understand the mechanisms leading to the localization of El Nino events either in the Central (CP) or Eastern Pacific (EP). For this, we derive a reduced gravity mixed layer model for the equatorial ocean with simple nonlinearities, diabatic effects and zonally varying background characteristics. Using the model, we study the propagation of an equatorial Kelvin wave from an initial perturbation. An approximate analytical solution is found for the evolution of the maximum density (or temperature) anomaly created during the passage of the wave. Density anomalies can either peak in the CP or continuously increase until reaching the EP, which is representative of both types of El Nino. Sensitivity tests reveal that both the zonally varying background stratification and diabatic effects are important to determine the density pattern. The EP pattern is obtained for smooth background variations while the CP pattern requires a frontal background structure. Using numerical experiments, we then show how consecutive Kelvin waves can lead to the transition from a CP to an EP pattern. The present theoretical results provide useful insights for understanding El Nino dynamics and diversity in more complete models and observations.
Plan de classement
Limnologie physique / Océanographie physique [032]
Description Géographique
PACIFIQUE
Localisation
Fonds IRD [F B010074062]
Identifiant IRD
fdi:010074062
Contact