(Credit: Melinda Nagy/Shutterstock)
In a Nutshell
- Coral skeletons from the Galápagos Islands show that ocean temperature swings tied to El Niño are now stronger than at any point in the last 1,000 years.
- The sharpest increase in strength happened in just the last several decades, matching the pace of rising global temperatures.
- This modern surge exceeds the range produced by the study’s simulations of natural climate variability and natural climate forcing.
El Niño has a way of turning entire regions upside down. It floods parts of South America, dries out Australia, bleaches coral reefs, and rattles farming and fishing economies worldwide. For decades, scientists have wondered whether the recent run of intense El Niño events is just bad luck, or a sign that the climate system itself is shifting into a rougher gear. A new study digging into 1,000 years of coral skeletons from the Galápagos Islands offers rare long-range evidence: eastern Pacific El Niño has strengthened beyond anything in the coral record over the past millennium, and the sharpest jump lands squarely in the modern warming era.
Researchers pulled this deep history out of coral skeletons collected around the Galápagos Islands, a place that sits right in the bullseye of the strongest El Niño swings on the planet. Corals build their skeletons layer by layer, year after year, locking in tiny chemical clues about the ocean temperatures they lived through. By reading those clues in both living coral and long-dead coral fragments, the team behind the study, published in the journal Science, pieced together a temperature record stretching back roughly 1,000 years, long before thermometers or satellites existed.
What they found was not a slow, steady climb. Ocean temperature swings in the eastern Pacific stayed fairly calm and steady from around the year 1000 through the mid-1800s. Then swings started creeping upward in the late 1800s, and took off sharply over the last 40 years or so. When researchers compared this modern spike to computer models that simulate natural climate swings without any human-caused warming, the real-world coral data ran well beyond what those models produced on their own.
How Scientists Read 1,000 Years of El Niño History in Coral
As corals grow, the chemistry of their skeletons shifts with ocean conditions, leaving clues scientists use to reconstruct past temperatures. By measuring those chemical signals layer by layer, researchers can track ocean temperatures year by year, going back centuries, much like tree rings reveal past rainfall.
For this study, researchers analyzed 28 coral records from 13 colonies across five islands in the Galápagos chain, chosen because it sits at the heart of what scientists call the eastern Pacific El Niño zone, where temperature swings during big El Niño events are typically the most extreme anywhere in the ocean. They split the data into three time periods: a “preindustrial” stretch from the year 1000 to 1850, a “20th century” stretch from roughly 1850 to 1983, and a “modern” period starting in 1984. Comparing swings across those three windows let the team measure how much stronger, or weaker, El Niño-driven temperature spikes have become over time.
Each of the three periods turned out to be clearly different from the others, with swings growing stronger the closer researchers got to the present. Modern ocean temperature swings in the region were about 36.5 percent stronger than during the preindustrial period, and about 16.2 percent stronger than during the 20th century. The team also noticed that warm spikes in the modern era leaned harder toward extreme heat, meaning strong El Niño warming events, rather than mild ones, are driving much of the increase.
Testing the El Niño Surge Against Climate Models
To rule out the possibility that this was just a random blip, the researchers compared their coral findings against twelve climate models simulating natural climate influences such as volcanic eruptions, solar shifts, and the ocean’s own internal ups and downs, without modern human-caused warming. Across the models, the increase recorded in the Galápagos corals exceeded the 95 percent range produced in those natural-forcing simulations, making it unusual compared with what natural variability alone tended to produce.
Coral records from a different part of the Pacific, the Line Islands further west, told a similar but less dramatic story. Temperature swings there were also higher in modern times than in the past, up about 33.8 percent compared to preindustrial levels, but the increase was fuzzier and overlapped more with older natural swings. This fits with what many climate models have predicted: warming-driven increases in El Niño strength should show up more clearly, and sooner, in the eastern Pacific, near places like the Galápagos, than in the central Pacific.
Broader historical climate records backed up the coral evidence. The team checked their findings against reconstructions built from a mix of coral, tree rings, and other sources spanning wider stretches of the Pacific. Several of those records also pointed to rising El Niño swings in recent decades, though the timing did not always line up as neatly, something the researchers link to known limitations in how those blended records are built. None of the records, including the Galápagos coral, showed any clear shift in El Niño behavior tied to historic climate events like the Little Ice Age or the Medieval Warm Period, reinforcing that the recent change stands apart from anything the system has done naturally in centuries.
Why a Stronger El Niño Matters
A stronger El Niño is not an abstract statistic. Bigger swings in ocean temperature translate directly into more extreme droughts, floods, and heat stress on coral reefs and marine life, on top of an ocean that is already warming overall. The study’s authors point out that El Niño events already carry enormous economic and ecological costs worldwide, and that continued strengthening would deepen those impacts both inside and outside the tropical Pacific.
Coral skeletons rarely make headlines, but this record offers something rare: a long, physical memory of the ocean that stretches back centuries before humans started burning fossil fuels at scale. It shows that eastern Pacific El Niño swings stayed in a fairly narrow, stable range for most of the last thousand years, then broke out of that range within living memory during the modern warming era. That pattern adds weight to warnings that a warming world may be doing more than lifting the ocean’s average temperature, since the same record shows one of the planet’s most disruptive climate patterns now swinging harder than at any point in centuries.
Paper Notes
Limitations
Coral coverage becomes sparse before 1500 CE, which limits how confidently earlier centuries can be compared to more recent ones. Modern and 20th-century Galápagos samples came mostly from the northernmost islands in the archipelago, while preindustrial samples came mostly from the central archipelago, so the team applied a geographic correction to account for known differences in variability across the region, though they note the modern period still showed significantly higher variability even without that correction. In the Line Islands, seawater changes unrelated to temperature complicate the coral chemical signal, which the authors say may explain why the central Pacific results were less distinct than the Galápagos findings. Gaps in data coverage across both regions, and differences in how much of the last thousand years each set of records actually samples, could also contribute to differences between sites. The authors describe their comparison with climate models as informative context rather than a formal study pinning down the exact cause of the change.
Funding and Disclosures
Grants from the US National Science Foundation and the UK Natural Environment Research Council, awarded to several of the paper’s authors, supported the work. The authors state they have no competing interests.
Publication Details
Paper Title: “Recent strengthening of eastern Pacific ENSO in the last millennium paleorecord”
Authors: J. E. Cole, D. M. Thompson, K. A. Dyez, C. J. Tripp, A. W. Tudhope, M. Lofverstrom, S. Stevenson, J. M. Okun, A. E. Lawman, J. L. Conroy, J. T. Overpeck, G. Jimenez, and R. L. Edwards
Journal: Science
Released online on August 27, 2026
Data associated with the study are available through the NOAA-NCEI World Data Service for Paleoclimatology.







