External Dynamic Mechanisms Controlling the Periodic Offshore Blooms in Beibu Gulf

Since offshore waters are less affected by human activities and nutrient‐rich water masses, existing theories on periodic offshore blooms (POB) consider that the POB is proportional to the intensity of ocean fronts (nutrient supply from enhancing vertical mixing), ignoring external nutrient supply and external forcing (climatic oscillations). This study proposes an external dynamic mechanism of the POB on the basis of field observations and long‐term satellite remote sensing data (1981–2022) in Beibu Gulf, which is influenced by remarkable external forcing. A strong thermal front with an inverted‐V structure occurred in the central gulf every winter due to the strong wind stress. The intensity of the front on the east side is weaker due to the intrusion of the west‐Guangdong coastal current (WGCC). However, nutrient supply variation resulted in the POB's different intensity in different areas of the inverted‐V front. Chlorophyll a concentrations in the eastern (nutrients supplied by WGCC) and northern (nutrients supplied by vertical mixing) were obviously higher than that in the western front (limited nutrient supply) in winter. On an interannual scale, the intensity of POB in La Niña years is remarkably stronger than in El Niño years due to the stronger WGCC supplying more nutrients in La Niña. This study suggests that the intensity and range of POB are not proportional to the frontal intensity in the gulf, but are directly driven by the internal forcing (fronts and nutrient supply from WGCC), which is controlled by the external forcing. Plain Language Summary It is accepted that the intensity of periodic offshore blooms (POB) is considered in proportion to the intensity of ocean fronts since the front enhances vertical mixing to upwell eutrophic water to the surface, thus stimulating primary productivity. However, this ignores external nutrient supply and external forcing (climatic oscillations). In this study, a combination of field observations and long‐term satellite remote sensing data (1981–2022) in Beibu Gulf showed that the POB in the gulf are driven by both the frontal activities and the nutrient supply from the water mass dynamics (vertical mixing and west‐Guangdong coastal current). The intrusion of west‐Guangdong coastal current (WGCC) weakens the frontal intensity but increases the Chlorophyll a concentration in the eastern gulf. Additionally, POB in La Niña years are remarkably stronger than that in El Niño years due to the stronger WGCC sup