Characteristics of submesoscale eddy structures within mesoscale eddies in the Gulf of Mexico from 1/48° ECCO estimates

Frontiers in Marine Science

Marine Science

Alexis Chaigneau¹  Corinne B. Trott²  Bulusu Subrahmanyam³  Paul A. Ernst³ 

[1] LEGOS, CNES, CNRS, IRD, UPS, Université de Toulouse, Toulouse, France;Naval Research Laboratory, Stennis Space Center, MS, United States;School of the Earth, Ocean and Environment, University of South Carolina, Columbia, SC, United States;

关键词: submesoscale;    eddies;    mesoscale;    energy cascade;    Gulf of Mexico;    high resolution modelling simulations;    loop current;    satellite oceanography;   

DOI  :  10.3389/fmars.2023.1181676

 received in 2023-03-07, accepted in 2023-05-17,  发布年份 2023

来源: Frontiers

【 摘 要 】

Submesoscale oceanic structures (<10-20 km) such as eddies and fronts are often difficult to describe given the influence of the mesoscale. In order to characterize the surface signatures of submesoscale structures, we utilize a custom spatial filtering function to separate the meso- and large-scale sea surface height (SSH) signal from the small scale SSH signal of 1/48° high resolution estimates provided by NASA’s Estimating the Circulation and Climate of the Oceans (ECCO) project. In this study, we use ECCO estimates from a 14-month global simulation between September 2011 and November 2012 with a 2 km horizontal grid spacing in the Gulf of Mexico. We then use an eddy detection and tracking algorithm to identify persistent circular features on both scales, giving rise to an atlas of submesoscale eddy-like variabilities (SEVs). We briefly investigate the geographic and temporal variability of SEVs as a whole before collocating SEVs inside mesoscale eddies, allowing us to evaluate the characteristics of internal SEVs and the impact of SEVs on mesoscale eddies. We find that SEVs, both anticyclonic and cyclonic, are ubiquitous inside mesoscale eddies with lifetimes longer than a week, accounting for an average of 10-20% of the spatial area and eddy kinetic energy of mesoscale eddies. We also show that internal SEVs are persistently associated with temperature and salinity anomalies in both eddy centers and edges of up to 0.1 °C and 0.05 psu, with anticyclonic internal SEVs being warmer and fresher while cyclonic internal SEVs are colder and saltier. Finally, we examine the life cycle of an anticyclonic Loop Current eddy, demonstrating that the number and intensity of internal SEVs within increases as the eddy approaches separation from the Loop Current until a maximum is obtained just after separation. In light of forthcoming submesoscale SSH observations from NASA’s Surface Water and Ocean Topography (SWOT) mission, our results showcase the variability of submesoscale eddy structures and their possible implications for biogeochemical cycling, the inverse energy cascade, and Loop Current prediction techniques.

【 授权许可】

Unknown   
Copyright © 2023 Ernst, Subrahmanyam, Trott and Chaigneau