Talk Abstract:
In many parts of the global ocean, density compensated temperature (T) and salinity (S) anomalies, known as ocean spice, highlight processes that interleave, stir and eventually mix water from different sources. The unique spatial and temporal structure of upper ocean spice patterns is set by the large-scale dynamics and the balance between different frontal processes, such as subduction, turbulent mixing, and atmospheric forcing that create, distribute and destroy spice. Spice variability also plays a substantial role…