Abstract:
The South Vietnam Upwelling (SVU) develops in
the South China Sea (SCS) under the influence of southwest monsoon winds. To study the role of small spatiotemporal scales on the SVU functioning and variability, a simulation
was performed over 2009–2018 with a high-resolution con-figuration (1 km at the coast) of the SYMPHONIE model im-plemented over the western region of the SCS. Its capability
to represent ocean dynamics and water masses from daily to interannual scales and from coastal to regional areas is quan-titatively demonstrated by comparison with available satel-lite data and four in situ datasets. The SVU interannual vari-ability is examined for the three development areas already
known: the southern (SCU) and northern (NCU) coastal up-welling areas and the offshore upwelling area (OFU). Our high-resolution model, together with in situ observations and
high-resolution satellite data, moreover shows for the first time that upwelling develops over the Sunda Shelf off the
Mekong Delta (MKU). Our results confirm for the SCU and OFU and show for the MKU the role of the mean summer intensity of wind and cy-
clonic circulation over the offshore area in driving the inter-annual variability of the upwelling intensity. They further re-veal that other factors contribute to SCU and OFU variability.First, the intraseasonal wind chronology strengthens (in the case of regular wind peaks occurring throughout the summer for SCU or of stronger winds in July–August for OFU) or weakens (in the case of intermittent wind peaks for SCU) the summer average upwelling intensity. Second, the mesoscale circulation influences this intensity (multiple dipole eddies and associated eastward jets developing along the coast en-hance the SCU intensity). The NCU interannual variability is less driven by the regional-scale wind (with weaker monsoon
favoring stronger NCU) and more by the mesoscale circulation in the NCU area: the NCU is prevented (favored) when alongshore (offshore) currents prevail.
