Diagnosing the Thickness‐Weighted Averaged Eddy‐Mean Flow Interaction From an Eddying North Atlantic Ensemble: The Eliassen‐Palm Flux

• Published in: Journal of Advances in Modeling Earth Systems
• Main Authors: Takaya Uchida, Quentin Jamet, William K. Dewar, Julien Le Sommer, Thierry Penduff, Dhruv Balwada
• Format: Article in Journal/Newspaper
• Language: English
• Published: American Geophysical Union (AGU) 2022
• Subjects: ocean ensemble simulation; eddy‐mean flow interaction; Eliassen‐Palm flux; Gulf Stream; thickness‐weighted averaging; Physical geography; GB3-5030; Oceanography; GC1-1581; north atlantic current; North Atlantic
• Online Access: https://doi.org/10.1029/2021MS002866; https://doaj.org/article/ea4d967406d7423d9b15703a182333bc

Abstract The thickness‐weighted average (TWA) framework, which treats the residual‐mean flow as the prognostic variable, provides a clear theoretical formulation of the eddy feedback onto the residual‐mean flow. The averaging operator involved in the TWA framework, although in theory being an ensemble mean, in practice has often been approximated by a temporal mean. Here, we analyze an ensemble of North Atlantic simulations at mesoscale‐permitting resolution (1/12°). We therefore recognize means and eddies in terms of ensemble means and fluctuations about those means. The ensemble dimension being orthogonal to the temporal and spatial dimensions negates the necessity for an arbitrary temporal or spatial scale in defining the eddies. Eddy‐mean flow feedbacks are encapsulated in the Eliassen‐Palm (E‐P) flux tensor and its convergence indicates that eddy momentum fluxes dominate in the separated Gulf Stream. The eddies can be interpreted to contribute to the zonal meandering of the Gulf Stream and a northward migration of it in the meridional direction. Downstream of the separated Gulf Stream in the North Atlantic Current region, the interfacial form stress convergence becomes leading order in the E‐P flux convergence.