Windrows in the ocean

Submesoscale processes

Windrows in the ocean

Submesoscale processes

The animation shows the evolution of submesoscale fronts (a warm front between two cold fronts) simulated by LES model.

Northern Hemisphere
(a) Instantaneous buoyancy field, (b) surface buoyancy field, © horizontal velocity u, (d) vertical velocity w

The animation below shows the mixed layer baroclinic instability simulated by LES model.

Northern Hemisphere
(a) Instantaneous temperature field, (b) surface temperature, © vertical velocity at z=-1.8m, (d) vertical velocity w at z=-9.1m
Northern Hemisphere
Instantaneous vertical velocity
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Jinliang Liu
Postdoc Scholar in the Department of Earth System Science