Framework to Extract Extreme Phytoplankton Bloom Events with Remote Sensing Datasets: A Case Study

• Published in: Remote sensing (Basel, Switzerland) Vol. 14; no. 15; p. 3557
• Main Authors: Lu, Wenfang, Gao, Xinyu, Wu, Zelun, Wang, Tianhao, Lin, Shaowen, Xiao, Canbo, Lai, Zhigang
• Format: Journal Article
• Language: English
• Published: Basel MDPI AG 01.08.2022
• Subjects: Baroclinic instability; Chlorophyll; chlorophyll-a concentration; Climate change; Datasets; Ecosystems; Heat waves; marine bloom events; Marine ecosystems; Nutrients; Phytoplankton; Plankton; Remote sensing; remote sensing reconstruction; South China Sea; Stratification; submesoscale activity; Surface temperature; Temperature gradients; Trends; Upwelling; Wind; Winter; Luzon
• ISSN: 2072-4292; 2072-4292
• DOI: 10.3390/rs14153557

The chlorophyll-a concentration (CHL) is an essential climate variable. Extremes of CHL events directly reflect the condition of marine ecosystems. Here, we applied the statistical framework for defining marine heatwaves to study the extremes of winter CHL blooms off the Luzon Strait (termed as LZB), northeastern South China Sea (SCS), from a set of remote sensing data. The application was enabled by a recent gap-free CHL dataset, the SCSDCT data. We present the basic properties and the long-term trends of these LZB events, which had become fewer but stronger in recent years. We further statistically analyze the LZB events’ controlling factors, including the submesoscale activity quantified by a heterogeneous index or surface temperature gradients. It was revealed that the submesoscale activity was also a vital modulating factor of the bloom events in addition to the well-understood wind and upwelling controls. This modulation can be explained by the stratification introduced by submesoscale mixed-layer instabilities. In the winter, the intensified winter monsoon provides a background front and well-mixed upper layer with replenished nutrients. During the wind relaxation, submesoscale baroclinic instabilities developed, leading to rapid stratification and scattered submesoscale fronts. Such a scenario is favorable for the winter blooms. For the first time, this study identifies the bloom events in a typical marginal sea and highlights the linkage between these events and submesoscale activity. Furthermore, the method used to identify extreme blooms opens up the possibility for understanding trends of multiple marine extreme events under climate change.