Salinity-driven Thermocline Transients in a Wind- and Thermohaline-forced Isopycnic Coordinate Model of the North Atlantic

TLDR

Freshwater flux forcing is a key factor influencing thermocline ventilation. The study presents an isopycnic‑coordinate oceanic circulation model aimed at simulating thermodynamically and mechanically driven flow in realistic basins, with special emphasis on diabatic surface processes and thermocline ventilation. The model, resolved on a 2° mesh over 10–60°N, uses 10 isopycnic layers plus an active mixed layer, and is forced from an isohaline initial state by seasonally varying wind stress, radiative and freshwater fluxes, and surface thermal relaxation. After ~15 years of spinup, the model reaches a quasi‑stationary circulation with pronounced subtropical mode‑water formation and increasing salinity contrast between subtropics and subpolar regions, and low‑viscosity experiments indicate thermohaline processes are insensitive to dynamic noise at the grid resolution limit.

Abstract

An isopycnic-coordinate oceanic circulation model formulated with the aim of simulating thermodynamically and mechanically driven flow in realistic basins is presented. Special emphasis is placed on the handling of diabatic surface processes and on thermocline ventilation. The model performance is illustrated by a 30-year spinup run with coarse horizontal resolution (2° mesh) in a domain with North Atlantic topography extending from 10° to 60°N latitude. The vertical structure encompasses 10 isopycnic layers in steps of 0.2 σ units, capped by a thermodynamically active mixed layer. From an initially isohaline state with isopycnals prescribed by zonally averaged climatology, the model is forced by seasonally varying wind stress, radiative and freshwater fluxes, and by a thermal relaxation process at the surface. After a mechanical spinup time of about 15 years, a quasi-stationary pattern of mean circulation and annual variability ensues, characterized by pronounced subtropical mode-water formation and a gradual growth in the salinity contrast between the subtropics and the subpolar region. The effect of the freshwater flux forcing on the ventilation of the thermocline is a key point of discussion. Finally, a low-viscosity experiment suggests that the thermohaline processes represented in the model are quite insensitive to dynamic noise development at the grid resolution limit.