I. Introduction
Prolonged discrete warm water anomalies have had a significant impact on marine ecosystems. Marine heat waves (MHW) are events characterized by anomalously warm water occurring within a specific time frame, described in terms of duration, intensity, evolution rate, and spatial extent. Warm water events at the sea surface can be classified as MHW if they persist for at least five consecutive days, with temperatures exceeding the 90th percentile of historical baseline temperatures over a minimum period of 30 years. These heat waves can be attributed to oceanographic and atmospheric processes [1].