Unprecedented suppression of Panama’s Pacific upwelling in 2025

A Aaron O’Dea A Andrew J. Sellers (Smithsonian Tropical Research Institute) C Carmen Pérez-Medina (Smithsonian Tropical Research Institute) J Javier Pardo Díaz (Smithsonian Tropical Research Institute) A Alexandra Guzmán Bloise (Smithsonian Tropical Research Institute) C Christopher Pöhlker M Michał T. Chiliński (Multiphase Chemistry Department, Max Planck Institute for Chemistry) H Hedy M. Aardema (Climate Geochemistry Department, Max Planck Institute for Chemistry) J Jonathan D. Cybulski (Smithsonian Tropical Research Institute) L Lena Heins (Climate Geochemistry Department, Max Planck Institute for Chemistry) S Steven R. Paton (Smithsonian Tropical Research Institute) H Hans A. Slagter (Climate Geochemistry Department, Max Planck Institute for Chemistry) R Ralf Schiebel (Climate Geochemistry Department, Max Planck Institute for Chemistry) G Gerald H. Haug

Abstract

The Gulf of Panama’s (GOP) seasonal upwelling system has consistently delivered cool, nutrient-rich waters via northerly trade winds every January–April for at least 40 y. Here, we document the failure of this normally highly predictable phenomenon in 2025. Data suggest that the cause was a reduction in Panama wind-jet frequency, duration, and strength, possibly related to the Intertropical Convergence Zone (ITCZ) position during the 2024–2025 La Niña, though the mechanisms remain unclear. Nevertheless, the consequences are likely significant, including decreases in fisheries productivity and exacerbated thermal stress on corals that typically benefit from upwelling’s cooling. This event underscores how climate disruption can threaten wind-driven tropical upwelling systems, which remain poorly monitored and studied despite their importance to ecology and coastal economies.

Article Details

Volume / Issue Vol. 122, Issue 36
Published September 09, 2025
ISSN 0027-8424
Publisher National Academy of Sciences

Authors (14)

A

Aaron O’Dea

A

Andrew J. Sellers

Smithsonian Tropical Research Institute

C

Carmen Pérez-Medina

Smithsonian Tropical Research Institute

J

Javier Pardo Díaz

Smithsonian Tropical Research Institute

A

Alexandra Guzmán Bloise

Smithsonian Tropical Research Institute

C

Christopher Pöhlker

M

Michał T. Chiliński

Multiphase Chemistry Department, Max Planck Institute for Chemistry

H

Hedy M. Aardema

Climate Geochemistry Department, Max Planck Institute for Chemistry

J

Jonathan D. Cybulski

Smithsonian Tropical Research Institute

L

Lena Heins

Climate Geochemistry Department, Max Planck Institute for Chemistry

S

Steven R. Paton

Smithsonian Tropical Research Institute

H

Hans A. Slagter

Climate Geochemistry Department, Max Planck Institute for Chemistry

R

Ralf Schiebel

Climate Geochemistry Department, Max Planck Institute for Chemistry

G

Gerald H. Haug