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Benshila R., Durand Fabien, Masson S., Bourdalle-Badie R., Montegut C. D., Papa Fabrice, Madec G. (2014). The upper Bay of Bengal salinity structure in a high-resolution model. Ocean Modelling, 74, 36-52. ISSN 1463-5003

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Lien direct chez l'éditeur doi:10.1016/j.ocemod.2013.12.001

Titre
The upper Bay of Bengal salinity structure in a high-resolution model
Année de publication2014
Type de documentArticle référencé dans le Web of Science WOS:000330576400003
AuteursBenshila R., Durand Fabien, Masson S., Bourdalle-Badie R., Montegut C. D., Papa Fabrice, Madec G.
SourceOcean Modelling, 2014, 74, p. 36-52. ISSN 1463-5003
RésuméSalinity in the Bay of Bengal is highly heterogeneous, with extremely fresh waters found at the surface in the Northern part of the basin, and saltier waters at subsurface as well as to the south. This paper investigates the seasonal structure of sea surface salinity of the Bay in a regional high-resolution model forced by ERA-Interim reanalysis and various precipitation products. Surface circulation is believed to drive the spreading of northern Bay of Bengal fresh waters to the rest of the Indian Ocean. We first present a series of experiments to infer the sensitivity of modeled circulation to various numerical choices. Surface circulation is found to be sensitive to the horizontal resolution of the model, with the 1/12 degrees version appearing much more realistic than the 1/4 degrees version. The sidewall boundary condition is also drastically influencing the characteristics of the western boundary current simulated. We then investigate the sensitivity of the salinity response to the various precipitation products. We observe that ERA-Interim excess precipitation induces a fresh bias in the surface salinity response. Spaceborne precipitation products are more satisfactory. We then identify the pathways of the northern Bay freshwater mass, based on passive tracers experiments. Our model suggests that over timescales of a few months, vertical exchanges between the upper fresh layer and the underlying saltier layer appear to be the main export pathway for the freshwater. The horizontal circulation within the mixed layer also acts to convey fresh waters out of the Bay at these timescales, but in a lesser quantity compared to the vertical export. Beyond its intrinsic interest for the understanding of Bay of Bengal physics, this study highlights the need for a careful design of any realistic numerical model, in three key aspects: the choice of the resolution of the model, the choice of the sub-grid scale parameterizations, and the choice of the forcing fluxes.
Plan de classementLimnologie physique / Océanographie physique [032] ; Sciences fondamentales / Techniques d'analyse et de recherche [020]
Descr. géo.OCEAN INDIEN ; GOLFE DU BENGALE
LocalisationFonds IRD [F B010061752]
Identifiant IRDfdi:010061752
Lien permanenthttp://www.documentation.ird.fr/hor/fdi:010061752

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