For the first time in 40 Years, Panama’s deep and cold ocean waters fail to emerge


Extremely low chlorophyll concentrations in the oceans around Panama (blue = weak, red = high) in February 2025, revealing the failure of the 2025 increase in the Gulf of Panama – for the first time in at least 40 years. Credit: Aaron O’Dea
The natural phenomenon of upwelling, which occurs every year in the Gulf of Panama, failed for the first time in 2025. A study led by scientists from the Tropical Smithsonian Research Institute (Stric) indicates that the weakening of food was the cause of this event. This observation highlights the impact of the climate on fundamental ocean processes and the coastal communities that depend on it.
During the dry season in Central America (generally between December and April), the Northern Alizés generate Upwelling events in the ocean waters of the Gulf of Panama. Upwelling is a process that allows cold waters and rich in nutrients from the depths of the ocean to rise to the surface. This dynamic supports highly productive peaches and helps protect coral reefs against thermal constraint. Thanks to this water movement, the sea along the Panama Pacific beaches remains cooler during the “summer” holiday season.
Stric scientists have studied this phenomenon and their files show that this seasonal rise, which occurs from January to April, was a coherent and predictable characteristic of the Gulf for at least 40 years. However, researchers recently recorded that in 2025, this vital oceanographic process did not occur for the first time. As a result, typical temperature drops and productivity tips during this time of the year were reduced.
In the article recently published in the journal PNAScientists suggest that a significant reduction in wind patterns has been the cause of this unprecedented event, revealing how climate disturbance can quickly change the fundamental ocean processes that have supported coastal fishermen for thousands of years. However, additional research is necessary to determine a more precise cause and its potential consequences for fishing.
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Upwelling events support very productive fisheries and help protect coral reefs from thermal stress. Credit: Natasha Hinojosa
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Chlorophyll concentrations in the oceans around Panama (blue = low, red = high) in February 2024, showing maximum productivity in the Gulf of Panama during a typical period of ascent. Credit: Aaron O’Dea
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THE S / y Eugen seibold The research vessel characterizes the conditions of the ocean and the atmosphere in the Pacific Ocean thanks to a collaboration between the Max Planck Institute for Chemistry and STA. Credit: Steven Paton
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Andrew Sellers took samples during an expedition with the S / Y Eugen Seibold. THE S / y Eugen seibold The research vessel characterizes the conditions of the ocean and the atmosphere in the Pacific Ocean thanks to a collaboration between the Max Planck Institute for Chemistry and STA. Credit: Steven Paton
This observation highlights the growing vulnerability of tropical cross -mounted systems, which, despite their enormous ecological and socioeconomic importance, remain poorly monitored. He also highlights the urgency of strengthening the observation and prediction of ocean climates in the tropical regions of the planet.
This result marks one of the first major results of the collaboration between the S / Y Eugen Seibold research ship of the Max Planck Institute and STA.
More information:
O’dea, Aaron, unprecedented abolition of the Pacific Upwelling of Panama in 2025, Proceedings of the National Academy of Sciences (2025). DOI: 10.1073 / PNAS. 2512056122. DOI.org/10.1073/pnas.2512056122
Supplied by Smithsonian Tropical Research Institute
Quote: For the first time in 40 years, the deep and cold waters of Panama fail to emerge (2025, September 1) recovered on September 2, 2025 from https://phys.org/news/2025-09 years-panama-deep-cold-ocean.html
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