Storm Kristin was a compact, catastrophic and record-breaking extratropical cyclone that severely impacted Portugal, as well as parts of the Mediterranean and Southeastern Europe in late January 2026. Storm Kristin was the twenty-sixth storm of the 2025–26 European windstorm season, and the eleventh to be named by the south-western naming group, which consists of France, Spain, Portugal, Belgium, and Luxembourg. Kristin was named by the IPMA on 27 January, as a significant impact was forecast. The impact of Kristin and its successors was described as a humanitarian crisis by a researcher in extreme weather and climate change. Kristin achieved record-breaking status by rapidly intensifying in the hours before landfall. Kristin made landfall at peak intensity in the Leiria district, which resulted in extremely intense winds in multiple Portuguese districts. The IPMA measured the strongest gust in Portuguese history, surpassing the record of Hurricane Leslie in 2018. The extreme wind gusts of more than 200 km/h were attributed to a sting jet, that developed as the cyclone made landfall. A storm like Kristin had an estimated return period of 80–90 years, based on a reanalysis. Before disappearing, Kristin also affected Spain severely and caused heavy precipitation and thunderstorms in Italy and Greece. Kristin especially affected the Portuguese districts of Leiria, Coimbra, and Santarém severely, but also affected other districts in Portugal such as the Lisbon district. After moving through Portugal, Kristin also struck Spain with wind gusts of more than 170 km/h. As a result of Kristin, Portugal experienced its largest blackout in history. Around 1,000,000 customers in Portugal were without power, according to E-Redes. Approximately 170,000 customers experienced power outages in Andalusia. Kristin caused long-lasting and widespread communication outages in Portugal, lasting for several months. Kristin was responsible for a significant ecological impact in parts of Portugal, as tens of millions of trees fell, which raised concerns for potential wildfires in the summer of 2026. The storm had a widespread and severe impact on emotional well-being in the affected areas. Kristin prompted national and international solidarity actions and humanitarian aid efforts. Over 2,000 injuries were reported in Portugal, 177 direct and 2,000 indirect. Furthermore, 14 deaths were attributed to Kristin in Portugal, six direct and eight indirect. One death and 12 injuries were reported in Spain. Estimated monetary losses in Portugal were more than €6 billion, which was more than 1.6% of the country's GDP in 2026, making Kristin the most damaging storm on record for Portugal. Initial government estimates indicated losses of €1.2 billion in Spain, bringing the total amount of losses by Kristin to more than €7.2 billion. Kristin's successor, storm Leonardo, was responsible for causing major floodings in parts of Portugal, which exacerbated the impact of Kristin.
Storm name On 27 January, the IPMA used the name "Kristin" for the twenty-sixth storm of the 2025–26 European windstorm season and the eleventh storm to be named by the south-western naming group, as red warnings were issued for parts of Portugal. Kristin is a Scandinavian name and its meanings are "Christian" or "follower of Christ".
Meteorological history
At the end of January 2026, there was a persistent anticyclonic blocking between Greenland and Scandinavia, which resulted in the polar jet descending in latitude, resulting in a very favorable configuration for the strong development of low-pressure areas. Under influence of storm Joseph, also named Marilu by the FUB, a secondary low formed. This secondary low was named Kristin by the IPMA, as a significant impact was forecast for parts of Portugal. Enabled by very dynamic and favorable atmospheric conditions, Kristin rapidly intensified in the night before it made landfall. During its explosive cyclogenesis, Kristin deepened to a minimum atmospheric pressure of 975 hPa. In the hours before Kristin made landfall in the Leiria district, the storm developed a sting jet, which is a rare phenomenon that exclusively happens in extratropical cyclones with a warm core.
Around 4:45 AM UTC, Kristin made landfall as an extremely powerful storm in the Leiria district, with gusts exceeding 200 km/h in some parts of the Leiria and Coimbra districts. In Soure, which is a municipality in the Coimbra district, a gust of 208.8 km/h has been measured, exceeding the previous record of 176.4 km/h by Leslie in 2018. Unofficially, a gust of 238 km/h has been measured in Lavos, which is also a parish in the Coimbra district. The Monte Real Air Base, which is located in the Leiria district, reported a gust of 178 km/h before the anemometer got damaged. The Leiria aerodrome measured a gust of 156.2 km/h, according to the IPMA. Lisbon measured a peak gust of 115 km/h. Doppler weather radar imagery were indicative of wind speeds in excess of 216 km/h (>60 m/s) at an altitude of 600 metres during Kristin's peak intensity. After moving through Portugal, Kristin caused strong winds and excessive precipitation in Spain. A maximum gust of 174 km/h was measured in Dehesa del Camarate by the AEMET. A gust of 156 km/h was measured in Villena. Gusts of 150.5 km/h were recorded in Benizalón, which is one of the strongest gusts ever recorded in Almería, alongside with gusts of 131 km/h in Carboneras, 124 km/h in Xodos, 118 km/h in Laujar de Andarax, 116.3 km/h in the Calar Alto mountains, 113.8 km/h in Albox, and 111 km/h in Garuccha. A maximum gust of 108 km/h was measured in Cáceres. In A Gándara, a gust of 120.6 km/h was measured. Madrid experienced snow, which happens a couple times per year.
Effect of climate change According to a research conducted by Manning et al. (2018), the frequency of extreme windstorms increases with 25–35% as a result of climate change. The main cause is the increased contribution of storms that develop a sting jet as a result of the global warming. Kristin had a sting jet, which was responsible for its intensity, according to the IPMA. Global warming also alters large-scale atmospheric circulations, which contributes to environments being more favorable for rapid cyclogenesis and persistent cyclonic influences.
Warnings and preparation
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