In 2016, the Southwest Pacific experienced an unprecedented marine heatwave caused by the co-occurrence of two major climate phenomena: El Niño and the negative phase of the Madden-Julian Oscillation. This exceptional situation led to an abnormal increase in ocean surface water temperatures (30-50 m), which remained at record-high levels throughout February 2016.
As part of WP1, which focuses on exposure to thermal stress, an Argo float was deployed on 30 November 2025 from the research vessel Antea during the KASEAOPE3 mission, in order to document the ongoing marine heatwave south of New Caledonia. This event is currently classified as moderate to strong, with temperature anomalies reaching +3°C at the surface according to OSTIA analyses from 25 November 2025 (Copernicus Marine Service). This deployment offers a unique opportunity to observe the vertical structure of the warming associated with this MHW.