Abstract Marine heatwaves drive ecosystem change across the globe and are, with ongoing global warming, key indicators for the evaluation offuture climates. Marine heatwave drivers are typically compound events of teleconnections and local weather. Strictly locally, marineheatwaves are induced by heat fluxes through the surface of the investigated area, accumulating until the temperatures exceed acertain threshold. For large parts of the world ocean, drivers of the strongest of the marine heatwaves, were shown to have a dominantcontribution from horizontal advection, however, whether the advected water was warmed up through surrounding surface forcing ororiginates from the interior ocean is unknown. Here, on an example from the extreme 2005 eastern Caribbean Sea marine heatwave, Idemonstrate a method that allows spatial and temporal attribution of horizontal advection of heat anomalies to their sources. TheLagrangian back-tracking method, applied within the mixed layer, successfully attributes advective heat-anomaly sources to eitherthe atmosphere (surface) or the ocean (grid-scale lateral mixing and mixed layer base exchange). Furthermore, the spatial origin ofmarine heatwave drivers is seen for the first time, showing the non-locality of marine heatwave drivers. The presented method greatlyexpands the possibilities to attribute drivers of marine heatwaves beyond the local effects and rather to their respective large-scalecauses. Many ecosystems worldwide have already been repeatedly hit by marine heatwaves severe enough to lead to local extinctionevents. Even when ecosystems recover, the next global scale compound event is sure to come with rising temperatures due to climatechange. Tools such as the presented method can greatly improve our understanding of past climate catastrophes, and thus, helpunderstand future risks for our remaining ecosystems.
Ezra Eisbrenner (Fri,) studied this question.