G. Caniaux et S. Planton, A 3-DIMENSIONAL OCEAN MESOSCALE SIMULATION USING DATA FROM THE SEMAPHORE EXPERIMENT - MIXED-LAYER HEAT-BUDGET, J GEO RES-O, 103(C11), 1998, pp. 25081-25099
A primitive equation model is used to simulate the mesoscale circulati
on associated with a portion of the Azores Front investigated during t
he intensive observation period (IOP) of the Structure des Echanges Me
r-Atmosphere, Proprietes des Heterogeneites Oceaniques: Recherche Expe
rirnentale (SEMAPHORE) experiment in fall 1993. The model is a mesosca
le version of the ocean general circulation model (OGCM) developed at
the Laboratoire d'Oceanographie Dynamique et de Climatologie (LODYC) i
n Paris and includes open lateral boundaries, a 1.5-level-order turbul
ence closure scheme, and fine mesh resolution (0.11 degrees for latitu
de and 0.09 degrees for longitude). The atmospheric forcing is provide
d by satellite data for the solar and infrared fluxes and by analyzed
(or reanalyzed for the wind) atmospheric data from the European Centre
for Medium-Range Weather Forecasts (ECMWF) forecast model. The extend
ed data set collected during the IOP of SEMAPHORE enables a detailed i
nitialization of the model, a coupling with the rest of the basin thro
ugh time dependent open boundaries, and a model/data comparison for va
lidation. The analysis of model outputs indicates that most features a
re in good agreement with independent available observations. The surf
ace front evolution is subject to an intense deformation different fro
m that of the deep front system, which evolves only weakly. An estimat
e of the upper layer heat budget is performed during the 22 days of th
e integration of the model. Each term of this budget is analyzed accor
ding to various atmospheric events that occurred during the experiment
, such as the passage of a strong storm. This facilitates extended est
imates of mixed layer or relevant surface processes beyond those which
are obtainable directly from observations. Surface fluxes represent 5
4% of the heat loss in the mixed layer and 70% in the top 100-m layer,
while vertical transport at the mixed layer bottom accounts for 31% a
nd three-dimensional processes account for 14%.