Cross-Shelf Exchange in the Southwestern Atlantic Shelf Climatology and Extreme Events

Publicado en	Frontiers in Marine Science ( IF 5.247 )
Autores	Berden, Giuliana & Piola, Alberto & Palma, Elbio
Año de publicación	2022
DOI	https://doi.org/10.3389/fmars.2022.855183
Afiliaciones	Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires, Buenos Aires, Argentina Consejo Nacional de Investigaciones Científicas y Técnicas (CONICET), Buenos Aires, Argentina Departamento Oceanografía, Servicio Hidrografía Naval, Buenos Aires, Argentina Unidad Mixta Internacional - Instituto Franco-Argentino Sobre Estudios del Clima y sus Impactos, Buenos Aires, Argentina Departamento de Física, Universidad Nacional del Sur and Instituto Argentino de Oceanografía/CONICET, Bahía Blanca, Argentina
Programa	Inter-American Institute for Global Change Research (IAI) grants CRN3070 (US National Science Foundation grant GEO-1128040) and SGP-HW 017. IAI/CONICET grant RD3347, FONCYT grant PICT2016-0557, and SECYT-UNS grant 24-F079.
Proyecto	SGP-HW 017
Keywords	cross-shelf exchange western boundary current Brazil-Malvinas Confluence continental shelf high frequency variability extreme events
	Cross-Shelf Exchange in the Southwestern Atlantic Shelf Climatology and Extreme Events.pdf

Abstract

The variability and drivers of the cross-shelf exchanges between the Southwestern Atlantic shelf and the open ocean from 30 to 40°S are analyzed using a high-resolution ocean model reanalysis at daily resolution. The model's performance was first evaluated using altimetry data, and independent mooring and hydrographic data collected in the study area. Model transports are in overall good agreement with all other estimates. The record-mean (1993&ndash2018) cross-shore transport is offshore, 2.09 ± 1.60 Sv. 73% of the shelf-open ocean exchange occurs in the vicinity of Brazil-Malvinas Confluence (~38°S) and 20% near 32°S. This outflow is mostly contributed by northward alongshore transport through 40°S (63%) and the remaining by southward transport through 30°S (37%). The cross-shore flow presents weak seasonal variations, with a maximum in austral summer, and high variability at subannual and weekly time scales. The latter is mainly associated with abrupt wind changes generated by synoptic atmospheric systems. Alongshore wind variations set up sea-level changes in the inner shelf which in turn drive large anomalies in the associated geostrophic alongshore flow. The difference in inner shelf sea-level anomalies at 30 and 40°S is a good indicator of cross-shelf exchange at seasonal and shorter time scales. Episodes of extreme offshore transport that reach up to 9.45 Sv and last about 2 days are driven by convergence of these alongshore flows over the shelf. Large exports of shelf waters lead to freshening of the upper open ocean as revealed by in-situ and satellite observations. In contrast, onshore extreme events drive open ocean water intrusions of up to 6.53 Sv and last <4 days. These inflows, particularly the subtropical waters from the Brazil Current, induce a substantial salinification of the outer shelf.