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Numerical modification of atmospheric models to include the feedback of oceanic currents on air-sea fluxes in ocean-atmosphere coupled models
Abstract : In this note we present the modification to bring to an atmospheric model to account for relative winds (i.e. the difference between the near-surface winds and the oceanic currents) instead of absolute winds in the computation of air-sea fluxes. Because of the implicit treatment of the bottom boundary condition in most atmospheric models the use of relative winds involves a modification of both the surface layer parameterization and the tridiagonal matrix for vertical turbulent diffusion.
https://hal.inria.fr/hal-01184711
Contributor : Florian Lemarié Connect in order to contact the contributor
Submitted on : Monday, August 17, 2015 - 2:25:08 PM
Last modification on : Tuesday, October 19, 2021 - 11:00:28 AM
Long-term archiving on: : Wednesday, November 18, 2015 - 12:10:32 PM
Contributor : Florian Lemarié Connect in order to contact the contributor
Submitted on : Monday, August 17, 2015 - 2:25:08 PM
Last modification on : Tuesday, October 19, 2021 - 11:00:28 AM
Long-term archiving on: : Wednesday, November 18, 2015 - 12:10:32 PM
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RT-464.pdf
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