The superposition of ENSO and PDO leads to stronger responses of phytoplankton in the western equatorial Pacific
ID:1179 View Protection:ATTENDEE Updated Time:2024-10-14 10:56:29 Hits:718 Oral Presentation

Start Time:2025-01-14 13:45(Asia/Shanghai)

Duration:15min

Session:S65 Session 65-Oceanic-Atmospheric Processes Over the Indian and Western Pacific Oceans » S65-2Oceanic-Atmospheric Processes over the Indian and Western Pacific Oceans

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Abstract
The El Niño-Southern Oscillation (ENSO) profoundly influences marine ecosystems by reshaping phytoplankton community structures through environmental changes. However, because of limited field observations, the impact of ENSO on phytoplankton communities in the northwestern Pacific has been unclear. Through a comprehensive analysis combining field observations, satellite data, and reanalysis data, we obtained robust evidence of distinct patterns of the impact of El Niño and La Niña events on phytoplankton communities in the northwestern tropical Pacific, particularly within the region of the Mindanao eddy. These patterns contradicted expectations based on studies in the tropical eastern Pacific. During El Niño events, the relative concentrations of diatoms and haptophytes showed a notable increase, whereas during La Niña events, Prochlorococcus was the most abundant phytoplankton. Our analysis also revealed that the Pacific Decadal Oscillation amplified ENSO's impact on phytoplankton communities. This study highlighted the contrasting mechanisms between climate oscillations and marine ecosystem dynamics.
 
Keywords
phytoplankton,climate change,western Pacific,ENSO,PDO
Speaker
Xin Liu
教授 Xiamen University

Submission Author
Xin LIU Xiamen University
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Important Date
  • Conference Date

    Jan 13

    2025

    to

    Jan 17

    2025

  • Sep 27 2024

    Draft paper submission deadline

  • Feb 17 2025

    Registration deadline

Sponsored By
State Key Laboratory of Marine Environmental Science, Xiamen University
Organized By
State Key Laboratory of Marine Environmental Science, Xiamen University
Department of Earth Sciences, National Natural Science Foundation of China
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