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Assimilation of sea surface temperature and sea surface height in a two-way nested primitive equation model of the Ligurian Sea

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Academic year: 2021

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Figure 1.1: The difference between the pre-dawn temperature at 1-5 m depths and the temperature at various depths during night (a) and during day (b)
Figure 2.2: Sign convention for the atmospheric fluxes. The heat fluxes (shortwave radia- radia-tion, net longwave radiaradia-tion, latent and sensible heat flux) are positive if heat is transferred from the ocean to the atmosphere
Figure 3.7: Cross-section of the WCC (section B of figure 3.1) of the mean salinity and the mean zonal velocity (in m/s) of the model.
Figure 3.8: Mean velocity (in m/s and normal to the cross-section) of NC  (sec-tion C of figure 3.1) in  func-tion of depth and distance from the coast.
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