%0 Journal Article
%9 ACL : Articles dans des revues avec comité de lecture répertoriées par l'AERES
%A Mogollón, R.
%A Pietri, A.
%A Tam, J.
%A Colas, François
%T Comprehensive characterization of Marine Heatwaves in a coastal Northern Humboldt Current System regional model over recent decades
%D 2023
%L fdi:010088735
%G ENG
%J Ocean Modelling
%@ 1463-5003
%K Marine heatwaves (MHWs) ; Drivers of MHWs ; Northern Humboldt Current System ; CROCO model
%K PACIFIQUE ; HUMBOLDT COURANT
%M ISI:001109868100001
%P 102280 [14 ]
%R 10.1016/j.ocemod.2023.102280
%U https://www.documentation.ird.fr/hor/fdi:010088735
%> https://www.documentation.ird.fr/intranet/publi/2024-01/010088735.pdf
%V 186
%W Horizon (IRD)
%X In this study, a high-resolution hydrodynamic model simulation was used to analyze the three-dimensional characteristics of marine heatwaves (MHWs) in the coastal region of the Northern Humboldt Current System (NHCS) over the period 2000-2019. Three distinct vertical layers were identified. The near-surface layer, extending down to 75 m depth, is identified as the region where both the maximum MHW intensity and cumulative intensity are found, predominantly concentrated along the thermocline depth. The intermediate layer, spanning from 75 to 125 m depth, exhibited the longest MHW durations and the lowest MHW frequencies. MHWs in this layer tend to be of moderate intensity and are often associated with ENSO variability. In contrast, the deep layer, from 125 to 250 m depth, was characterized by short-lived MHWs of low intensity. These MHWs exert a lesser thermal impact on the region. To understand the drivers of MHWs, a composite analysis was performed. The results highlighted the significant role exerted by wind-driven anomalies in the life cycle of MHWs. It was found that the combined effect of a sluggish coastal upwelling circulation and suppressed oceanic heat loss, as a result of weakened winds, preceded the MHW formation. Conversely, the strengthening of winds, which enhanced net heat loss, primarily driven by latent heat flux anomalies, and an enhancement of the cooling effect due to the recovery of the coastal upwelling circulation, are key processes in ending a typical MHW event in the coastal region. These findings expand our understanding of the MHWs and their associated potential drivers and help to reveal which regions are most susceptible to extreme climate events in one of the most productive marine ecosystems worldwide.
%$ 032 ; 020