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Updated: Apr 11, 2026

Investigating the Relationship between Sea Surface Chlorophyll and Major Features of the South China Sea with Satellite Information
Published on: June 13, 2020
Spatiotemporal variations in sea surface chlorophyll-a in the Seto Inland Sea
Gandhi Napitupulu1, Han Soo Lee2, Nobuhito Mori3
1Coastal Hazards and Energy System Science Laboratory, Graduate School of Innovation and Practice for Smart Society, Hiroshima University, 1-5-1 Kagamiyama, Higashi-Hiroshima, 739-8529, Hiroshima, Japan.
Sea surface chlorophyll-a in the Seto Inland Sea shows distinct regional patterns and responses to climate events. Marine heatwaves decrease chlorophyll, while cold spells and typhoons increase it, impacting coastal ecosystem management.
Area of Science:
- Marine Ecology
- Oceanography
- Remote Sensing
Background:
- Sea surface chlorophyll-a (SSC) variability in the Seto Inland Sea (SIS) is influenced by stratification, riverine inputs, oceanic exchange, and extreme climate events.
- The SIS, Japan's largest semi-enclosed coastal system, exhibits complex physical-ecological interactions.
- Understanding SSC dynamics is crucial for coastal ecosystem health and management.
Purpose of the Study:
- To investigate seasonal cycles, long-term shifts, and responses to extreme thermal events of SSC in the SIS using satellite observations from 1998 to 2024.
- To identify distinct physical-ecological regimes within the SIS.
- To quantify the impacts of marine heatwaves (MHWs), marine cold spells (MCSs), and typhoons on SSC.
Main Methods:
- Analysis of satellite-derived sea surface chlorophyll-a (SSC) and sea surface temperature (SST) data from 1998 to 2024.
- Identification and characterization of two distinct physical-ecological regimes: stratification-retention (inner basins) and mixing/intrusion-paced (outer gateways).
- Spectral analysis to confirm annual cycles and monsoonal forcing; detection and analysis of MHWs, MCSs, and typhoon impacts on SSC.
Main Results:
- Two distinct regimes identified: inner basins with high SSC blooms and outer gateways with lower baseline SSC.
- A coherent annual cycle (∼1.01 cycles yr⁻¹) driven by monsoonal forcing was confirmed across all regions.
- Marine heatwaves suppressed SSC (-6% to -15%), while marine cold spells enhanced SSC (+15% to +86%). Typhoon impacts were distance-dependent, with post-storm cooling stimulating phytoplankton growth.
Conclusions:
- Basin confinement and hydrodynamic exchange dictate SSC sensitivity to thermal extremes, with warming-induced stratification limiting nutrients and cooling-induced mixing enhancing productivity.
- This study provides the first basin-wide quantification of distance-dependent storm effects and contrasting MHW-MCS responses in the SIS.
- Findings offer new insights for ecosystem prediction and adaptive coastal management under increasing climate variability.
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