Physically Based Flux Modeling
Center for Ocean-Atmospheric Prediction Studies
Florida State University
Several Considerations in Modeling Fluxes
Gravity waves U10 > 7 m s-1
Capillary waves ~2 < U10 < 7 m s-1
2. Rising and Falling Seas (Departures from Equilibrium)
· HEXOS results and other observational studies found
· Increasing stresses for rising seas
· In the absence of swell
· How often is swell absent in the open ocean?
· A lot of people have said it's important, but how do we model it?
· Observations show differences in directions of wind and wave propagation can have a large systematic impact!
· Two horizontal dimensions.
· Non-isotropic roughness length.
5. Dodging the Issue of Sea State
· Winds are not the only remotely sensed 'surface forcing.'