Analysing the dissipation of the internal gravity waves in global and regional ocean models.
M2 internal wave amplitude in (a) Altimeter derived data, and (b) NEMO global ocean model
Cyril's Research
FTLE (Finite Time Lyapunov Exponent) field of the Atlantic Ocean, computed from satellite-observed ocean surface currents.
The wiggly lines indicate regions of high FTLE, and whitish ones correspond to the most effective flow barriers in the region.
