Gulf of Panama Upwelling Watch
O'Dea LabMarine ecosystems across time

Gulf of Panama Upwelling Watch

In 2025 the seasonal upwelling that normally dominates the Gulf of Panama failed. It was the first failure in more than forty years of records.

Upwelling brings cool, nutrient-rich water into the sunlit surface layers of the Gulf. The production that follows supports Panama's largest fishery.

Until then the upwelling had arrived every year on record. We reported the failure in PNAS and have monitored the Gulf since, through the return of upwelling in 2026.

NOAA forecasts that the Pacific may now be entering the strongest El Niño since records began in 1950. This page reports what we measure before and through the 2027 upwelling season.

Current conditions

Last cast
Surface, 0 to 10 m
At depth, below 30 m
Lowest oxygen in the column
El Niño (Niño 3.4)
+1.8°C
August 2026. NOAA advisory in effect

Surface water in the Gulf is warm and water at depth is warmer still. Surface heating does not warm water at depth, so the heat has arrived from elsewhere. The cold, low-oxygen water that normally sits at depth through the rainy season is absent. A strong El Niño is moving in from the west.

The coming season

The hypotheses

Trade winds crossing the isthmus of Panama into the Gulf

Every January the trade winds cross the isthmus of Panama and push surface water out of the Gulf. Cold, nutrient-rich water rises to replace it. For three months the Gulf is among the most productive tropical waters anywhere. Panama's fisheries depend on it. In 2025 the upwelling failed for the first time in more than forty years of records.

In 2026 it returned strongly. A strong El Niño is now pushing warm water east across the Pacific in a series of Kelvin waves. These waves depress the boundary between the warm surface water and the cold water beneath. The next season begins in January. We expect one of three outcomes.

A. Upwelling suppressed

The warm layer thickens until the cold water lies deeper than the winds can draw from. Strong winds blow, unlike 2025, but no cold water reaches the surface. This is the classic El Niño suppression described off Peru.

Signature: strong winds, warm surface, thermocline stays deep

B. Upwelling of warm water

Upwelling is strong, but the water that rises is the warm, nutrient-poor water carried east by the Kelvin waves. Production falls. We suspect this has happened before and has never been documented.

Signature: strong winds, shallow thermocline, but warm and nutrient-poor upwelled water

C. An ordinary season

The wind-driven system overrides the El Niño signal and the Gulf behaves normally. Cold, nutrient-rich water reaches the surface and phytoplankton blooms follow. No one has measured a normal season under these conditions.

Signature: shallow thermocline, cold nutrient-rich water close to the surface

Latest update

2018–2024 average, ± 1 SD 2026
Deep water temperature through the year
Water temperature through the year, at the surface and at depth. Each point is one cruise at stations 3, 4 and 5. The grey band is where the Gulf normally sits at that point in the year, taken from 2018 to 2024. Both panels are drawn to the same temperature span, so the two departures can be compared directly. The surface is a little warmer than normal, which the sun and the air could account for. The deep water is far warmer than normal, which they could not.

Earlier updates

Full water column

Anomaly through the whole water column

Show
Temperature anomaly by depth
Reading the figure. Depth runs down the side and time runs across the bottom. Each cell is the difference from normal for that depth in that week of the year, orange for warmer and blue for colder. A healthy upwelling season appears as a block of blue in the first months of the year. The scale stops at five degrees, so the deepest oranges and blues mean five degrees or more. Blank columns are weeks with no cruise. Large swings of either sign between January and April are mostly a matter of timing, since upwelling arriving a week early or late makes a given week of the year look extreme.

Methods

Where these numbers come from

Weekly profiles
A multiparameter sonde lowered through the water column at seven stations across the Bay of Panama. This page uses stations 3, 4 and 5, the deepest and most consistently sampled, which reach 54, 50 and 41 metres.
Record
Continuous since July 2017, roughly weekly, with a gap through 2020. The figures here rest on casts.
Baseline
Anomalies are against 2018–2024, week by week and depth by depth, and are leave-one-out, so no year is ever compared against itself.
Data
The underlying series are published by the STRI Physical Monitoring Program.

Contacts

Steven Paton

Director, Physical Monitoring Program, STRI
The long climate record, winds and rainfall across the isthmus

Andrew Sellers

Postdoctoral fellow, STRI and Max Planck
Biological consequences, food webs and fish energetics

Anabell Cornejo

Physical Monitoring Program, STRI
The weekly cruises and how the measurements are made

Aaron O'Dea

Staff scientist, STRI
The 2025 failure, long-term context and what this season may bring