Proposed scheme for modeling of ocean equatorial currents in the phase of El Niño and La Niña: Implementation of the mesoscale turbulence theory

• Published in: Dynamics of atmospheres and oceans 2021-06, Vol.94, p.101220, Article 101220
• Main Authors: Arsen'yev, Sergey А., Eppelbaum, Lev V., Ermakov, Natalya Yu
• Format: Article
• Language: English
• Subjects: El Niño; La Niña; Mathematical modelling of natural disasters; Mesoscale turbulence; Ocean equatorial currents
• ISSN: 0377-0265; 1872-6879
• DOI: 10.1016/j.dynatmoce.2021.101220

•The theory of mesoscale turbulence firstly applied for modeling of the equatorial Pacific Ocean currents.•Currents at the Earth’s equator in the La Niño phase have a four-tier vertical structure.•El Niño is consequence of nutational oscillations and the gravity influence of the Moon, Sun and Jupiter. El Niño is a phenomenon of the catastrophic increase of surface temperature in the eastern part of the Pacific Ocean. It has a significant impact to weather of the American continent and western regions of the tropical Pacific, as well as on the weather and climate of entirely the Earth. Most important factors influencing El Niño are the wind, ocean currents and slope of the water surface (and temperature resulting from these factors) at the equator in the Pacific Ocean. The paper considers results of mathematical modeling of the equatorial Pacific Ocean currents in the El Niño and La Niña phases using the theory of mesoscale turbulence. This theory has been successfully tested in modeling of global circulation of atmosphere and ocean (Arsen’yev et al., 2010) and it has been able to calculate the ocean current changes at equator under changing external conditions. It is shown that the water currents at the equator have a four-tier vertical structure. The surface trade-wind current is located above the subsurface undercurrent, below which we observe the intermediate current, turning into the equatorial deep counter flow. When El Niño begins, the currents are rearranged, change signs and sometimes merge with each other. In the phase of maximum development of the phenomenon there is a two-tier structure: (1) surface current heading the American coast is underlain (below the depth of 440 m) by (2) deep equatorial current directed to the Indonesian coast. The theoretical calculations are compared with the physical observations of ocean currents in the El Niño and La Niña phases. The obtained results indicate that the proposed mathematical apparatus makes it possible to explain the set of physical observations in the Pacific Ocean.