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Amplifying effects of multiyear La Niña on phytoplankton biomass in the tropical Pacific

  • Lei Lin*
  • , Kun Xu
  • , Wei Tan*
  • , Jinliang Liu
  • , Bingzhang Chen
  • , Dongyan Liu*
  • *Corresponding author for this work
  • Shandong University of Science and Technology
  • East China Normal University
  • Coastal Carolina University
  • University of Strathclyde
  • Ministry of Natural Resources of the People's Republic of China

Research output: Contribution to journalLetterpeer-review

Abstract

Traditional views suggest that overall phytoplankton biomass in the tropical Pacific should be proportional to La Niña intensity because of enhanced nutrient supplies from equatorial upwelling associated with La Niña intensity. Here, composite analysis of satellite-derived chlorophyll a (Chl a, a proxy for biomass) data across five multiyear La Niña (M-LN) events (1997–2023) showed a double increase in the tropical Pacific average Chl a in the 2nd/3rd years [La Niña(2)] of M-LN compared to the 1st year [La Niña(1)], despite declining La Niña intensities. This unexpected rise is attributed to a ∼ 1-yr lagged response of the off-equatorial phytoplankton to La Niña/El Niño. The lagged response of off-equatorial Chl a to La Niña(1) superimposed with the immediate response of equatorial Chl a to La Niña(2) amplifies overall Chl a levels during La Niña(2). Simulations from Earth System Models support this mechanism. Our findings imply that increased M-LN events may mitigate warming-induced biomass decline in the tropical Pacific.

Original languageEnglish
Article numbere70143
JournalLimnology and Oceanography Letters
Volume11
Issue number3
DOIs
StatePublished - May 2026

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