Isopycnal Variability in Spicy Regions
Understanding along-isopycnal temperature–salinity variability and its role in isopycnal mixing across the global ocean
About this project
In regions of the ocean where temperature and salinity vary along density surfaces in compensating ways — what oceanographers call “spicy” regions — the thermohaline structure can be highly variable without any net change in density. This variability, sometimes referred to as spice, is not dynamically inert. It modulates isopycnal mixing, influences tracer transport, and leaves a measurable imprint on acoustic propagation.
This project focuses on characterizing along-isopycnal temperature–salinity variability across spicy regions of the global ocean and understanding its role in setting isopycnal mixing rates. A central question is how this variability is generated, how it evolves as it is stirred by mesoscale and submesoscale flows, and at what scales it is ultimately dissipated. These questions are relevant not only for understanding tracer budgets but also for improving how mixing is represented in ocean models.
We use a combination of observational datasets — including Argo floats, glider surveys, and shipboard measurements — to characterize spice variability across different ocean basins and dynamical regimes. Analysis focuses on identifying the dominant processes controlling along-isopycnal variance and how mixing length scales vary with large-scale forcing conditions.
Interested in joining this project?
We are looking for graduate students with interest in observational oceanography, data analysis, and ocean mixing. If you would like to learn more, please reach out.