Phytoplankton Community Succession During Spring Blooms in the Changjiang Estuary and Adjacent Waters: Processes and Mechanisms
ID:712 View Protection:ATTENDEE Updated Time:2026-08-31 18:38:58 Hits:48 Poster Presentation

Start Time:2027-01-15 18:30(Asia/Shanghai)

Duration:15min

Session:S10 Session 10 - Advancing marine ecosystem modeling for a predictable and sustainable ocean » S10PS10-Poster

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Abstract
In the Changjiang (Yangtze) Estuary and its adjacent waters, phytoplankton undergo a characteristic succession during spring blooms, with the bloom typically shifting from diatom dominance to dinoflagellate dominance. This transition plays a key role in regulating regional biogeochemical cycling and ecosystem structure. Existing numerical models for this region remain limited in representing this succession. Some represent all phytoplankton as a single state variable, whereas others resolve multiple functional groups only in zero-dimensional box models. Neither approach can mechanistically capture the three-dimensional spatiotemporal dynamics of phytoplankton succession. To address this limitation, we developed a diatom–dinoflagellate dual-group ecological module for the Regional Ocean Modeling System (ROMS). The module explicitly represents 15 state variables and incorporates group-specific physiological traits, including distinct optimal growth temperatures, nutrient half-saturation constants, and optimal light intensities. It is fully coupled online with the three-dimensional hydrodynamic model. This modeling framework enables investigation of how temperature, water-column stratification, and riverine nutrient transport jointly regulate phytoplankton succession during spring blooms in the Changjiang Estuary.
Keywords
Speaker
Yanan WANG
Ocean University of China

Submission Author
Yanan WANG Ocean University of China
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Important Date
  • Conference Date

    Jan 12

    2027

    to

    Jan 15

    2027

  • Jul 21 2026

    Draft paper submission deadline

  • Jan 15 2027

    Registration deadline

Sponsored By
State Key Laboratory of Marine Environmental Science, Xiamen University (MEL)
Department of Earth Sciences, National Natural Science Foundation of China (NSFC)
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