While frost bit deep across parts of Europe and North America, global temperatures in January held firm near all-time highs, painting a stark picture of our warming planet. New data released by the Copernicus Climate Change Service (C3S) reveals that last month ranked as the fifth-warmest January on record. Crucially, it registered a significant 1.47°C above pre-industrial levels, pushing us ever closer to the 1.5°C warming threshold enshrined in the Paris Agreement.
The tail end of January delivered a brutal reminder of the climate’s erratic nature. Intense cold waves swept through vast swathes of the Northern Hemisphere, driven by frigid Arctic air that plunged further south than is typical. This icy onslaught meant Europe experienced its coldest January since 2010. The freezing conditions didn’t stop there, extending across Siberia and into northern and eastern Europe, even reaching parts of the United States. The result was an average land temperature of -2.34°C, a notable 1.6°C below the 1991-2020 norm.
Simultaneously, the Southern Hemisphere grappled with record-breaking heat, exacerbating extreme conditions. Australia, Chile, and Patagonia bore witness to devastating wildfires that claimed lives and wrought widespread destruction. Meanwhile, torrential rainfall in southern Africa triggered severe flooding in nations like Mozambique, highlighting the dual threats of an unstable climate.
Samantha Burgess, strategic lead for climate at the European Centre for Medium-Range Weather Forecasts, commented on this climatic paradox: “January 2026 delivered a stark reminder that the climate system can sometimes simultaneously deliver very cold weather in one region, and extreme heat in another.” She added, “While human activities continue to drive long-term warming, these recent events highlight that resilience and adaptation to increasing extremes are key to prepare society for heightened climate risk in the future.”
Beyond the atmospheric extremes, the data also underscores a worrying trend in our oceans. Sea temperatures remain unusually high, while sea ice continues its relentless decline at both the Arctic and Antarctic poles.
Sea surface temperatures were among the highest ever recorded for January. Particularly concerning were the exceptionally warm waters found in sections of the North Atlantic and North Pacific. While weaker La Niña conditions in the equatorial Pacific helped keep temperatures closer to average in that region, the overall trend is one of sustained oceanic warmth.
In the Arctic, the extent of ocean covered by sea ice in January was a significant 6 per cent below the norm, marking the third-lowest level ever recorded for the month. The Barents Sea, Baffin Bay, and the Labrador Sea were particularly depleted of ice, areas that have already experienced rapid ice loss in recent years.
Around Antarctica, sea ice levels also dipped below average. While not among the ten lowest January measurements on record, the persistent deficit is a cause for concern in a region critical to global climate regulation.
The pattern of extreme weather extended to precipitation patterns as well. Much of western, southern, and eastern Europe endured wetter-than-average conditions, leading to significant flooding and widespread disruption. The Iberian Peninsula, Italy, Ireland, and the United Kingdom were among the regions that bore the brunt of these deluges.
Conversely, other parts of the globe faced the opposite challenge. Hot and dry conditions prevailed across significant areas of South America and Australia, dramatically increasing the risk of wildfires. In stark contrast, heavy rainfall in regions such as southern Africa, Brazil, and northern Australia resulted in damaging floods, compounding the challenges faced by these communities.
The C3S monthly climate assessments, which inform these findings, are meticulously compiled using the ERA5 dataset. This comprehensive dataset draws upon billions of individual observations gathered from an extensive network of satellites, ships, aircraft, and weather stations spanning the globe. This rigorous data collection allows for a detailed and accurate understanding of the Earth’s climate system and its ongoing changes.
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