Capturing dense shelf water cascading with a high-resolution ocean reanalysis

Abstract. Dense shelf water cascading (DSWC) is an oceanographic process that occurs when dense shelf water overflows over the shelf edge downslope toward the deep sea. Monitored in the northwestern Mediterranean by moorings since 1993 in the Lacaze-Duthiers Canyon and since 2005 in the Cap de Creus Canyon, numerical modeling with reanalysis extends this timeline further into the past. This study investigates a regional reanalysis (1987–2021) validated against mooring observations at 750–1000 m depth. The reanalysis successfully reproduces observed intense DSWC (IDSWC) events from 1999, 2000, 2005, 2006, 2012, 2013, and 2018 while identifying one previously unreported event in 1987 and detecting no IDSWC between 1988 and 1998. The reanalysis effectively matches 84 % of observed IDSWC days within the same week and 56 % on the exact date. Instead of assimilating IDSWC events from mooring observations to resolve the cascading process, the model relies solely on the seawater density on the shelf and revealed the seawater properties along the canyon that caused IDSWC. This work highlights the importance of high-resolution reanalyses in investigating the impacts of mesoscale processes on larger scales in the deep ocean.

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Publication Details

Journal
Ocean science
Published
2025-10-02
DOI
https://doi.org/10.5194/os-21-2169-2025
Primary Topic
Oceanographic and Atmospheric Processes
Type
article
Field-Weighted Citation Impact
0.00

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article

Capturing dense shelf water cascading with a high-resolution ocean reanalysis

Marc Cerdà-Domènech, David Amblàs, Pere Puig, Cristián Florindo-López et al.
Ocean science
Oceanographic and Atmospheric Processes
article

Capturing dense shelf water cascading with a high-resolution ocean reanalysis

Marc Cerdà-Domènech, David Amblàs, Pere Puig, Cristián Florindo-López, Jesús Peña‐Izquierdo, Laia Romero, Xavier Durrieu de Madron, Víctor Estella-Pérez, Anna Sànchez‐Vidal, Antoni Calafat, Marta Arjona-Camas, Helena Fos
article en

Abstract

Abstract. Dense shelf water cascading (DSWC) is an oceanographic process that occurs when dense shelf water overflows over the shelf edge downslope toward the deep sea. Monitored in the northwestern Mediterranean by moorings since 1993 in the Lacaze-Duthiers Canyon and since 2005 in the Cap de Creus Canyon, numerical modeling with reanalysis extends this timeline further into the past. This study investigates a regional reanalysis (1987–2021) validated against mooring observations at 750–1000 m depth. The reanalysis successfully reproduces observed intense DSWC (IDSWC) events from 1999, 2000, 2005, 2006, 2012, 2013, and 2018 while identifying one previously unreported event in 1987 and detecting no IDSWC between 1988 and 1998. The reanalysis effectively matches 84 % of observed IDSWC days within the same week and 56 % on the exact date. Instead of assimilating IDSWC events from mooring observations to resolve the cascading process, the model relies solely on the seawater density on the shelf and revealed the seawater properties along the canyon that caused IDSWC. This work highlights the importance of high-resolution reanalyses in investigating the impacts of mesoscale processes on larger scales in the deep ocean.

Ocean scienceVol. 21(5)
Centre National de la Recherche Scientifique (FR), Université de Perpignan (FR), Institut Català de Ciències del Clima (ES), Institut de Ciències del Mar (ES), Universitat de Barcelona (ES)
Institut Français de Recherche pour l'Exploitation de la Mer, Generalitat de Catalunya, Institució Catalana de Recerca i Estudis Avançats, Centre National de la Recherche Scientifique, Ministerio de Ciencia e Innovación, Universitat de Barcelona, Agencia Estatal de Investigación
Openalex Percentile: Top 72%
Oceanographic and Atmospheric Processes
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