Warming rate jumps to ~0.35°C/decade after 2013-2015, El Nino stripped data shows
After removing El Nino, volcanoes, and solar cycles, researchers find a clear post-2013 acceleration across five datasets.

Researchers analyzing global temperature records removed the effects of El Nino, volcanic eruptions, and solar cycles and found the planet warmed at roughly 0.35°C per decade over the past ten years. For decision-makers, the consequence is simple: the risk is not just rising, it is accelerating, and the signal is statistically hard to ignore.
Global warming appears to have shifted into a faster gear. In a new analysis, after the researchers removed the effects of El Nino, volcanic eruptions, and solar cycles, the planet warmed at roughly 0.35°C per decade over the past ten years.
That is a meaningful break from the recent past. From 1970 to 2015, the warming pace was just under 0.2°C per decade. And the acceleration becomes visible around 2013 to 2015, according to the report.
This matters because the biggest argument climate conversations keep running into is whether we are just seeing natural wiggles. El Nino can push temperatures upward for periods of time, volcanoes can cool the planet by injecting material into the atmosphere, and solar cycles can add another layer of variation. The study tries to peel those factors away, so what remains is closer to the underlying long-term trend. In other words, the headline is not “weather happened.” It is “the underlying pace changed.”
The researchers did not pin their conclusion to a single thermometer archive. The acceleration shows up across five major global temperature datasets, with more than 98% statistical certainty. That “more than 98%” detail is doing a lot of work. Statistically, it means the pattern is unlikely to be a coincidence inside the analysis, and it is visible even when you vary which dataset you look at. For executives, that is the difference between a research curiosity and a risk factor you cannot easily spreadsheet away.
If you are running a business, a pension fund, an infrastructure portfolio, or a regulator-facing strategy, accelerated warming changes the time profile of costs. It affects how quickly heat stress can intensify, how quickly extreme rainfall or drought risks can strain supply chains, and how fast insurance and asset owners adjust pricing for climate-linked hazards. None of those second-order implications are spelled out in the source text, but the core logic is straightforward: faster change compresses the window for adaptation. It can also shift how boards think about capital planning, asset lifecycles, and the cost of delay.
There is also a policy and regulatory layer to this. Climate risk has been creeping into governance for years, often through disclosure rules, stress testing, and requirements that financial institutions quantify exposure. When researchers identify an acceleration that becomes visible around 2013 to 2015 and persists across datasets, regulators and auditors tend to have less tolerance for treating climate as a slow-moving “someday” risk. A faster gear increases the chance that existing guidance will be interpreted more strictly, because the evidence is showing motion now, not just a trend line somewhere in the distant future.
For investors and management teams, this also changes how you evaluate scenarios. Many strategies rely on linear assumptions, implicitly smoothing outcomes over long horizons. The study suggests the warming curve may not be steady, even after accounting for specific natural drivers. That is the kind of detail that can ripple into valuation models, cost curves, and the assumptions behind transition plans. Boards that have been waiting for “clearer confirmation” may not get a cleaner signal than “El Nino stripped, volcanoes stripped, solar cycles stripped, five datasets, more than 98% certainty, and a visible acceleration starting around 2013 to 2015.”
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