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New York Blizzard: Could a Similar Snowstorm Hit France?

New York Blizzard: Could a Similar Snowstorm Hit France?

February 25, 2026 Ahmed Hassan - World News Editor World

A historic blizzard has gripped the Northeastern United States, bringing record snowfall and widespread disruption to millions. While severe winter weather is not uncommon in the region, the intensity of this recent storm – peaking around Monday, February 23, 2026 – has prompted comparisons to some of the most significant snowstorms in decades.

Record Snowfall in New York and Beyond

New York City experienced approximately 50 centimeters (20 inches) of snowfall in Central Park, while LaGuardia Airport recorded 58 centimeters (23 inches). Long Island bore the brunt of the storm, with some areas, including MacArthur Airport, receiving as much as 74 centimeters (29 inches) – the highest accumulation since 1963. The storm prompted a citywide travel ban, which was lifted at noon on Monday, February 24, 2026, and led to the temporary suspension of services on the Long Island Rail Road and NJ Transit.

The impact extended far beyond New York. The storm system, described as a bomb cyclone, affected a vast swathe of the Northeast, from Boston to Washington, D.C. As of noon on Monday, February 24, 2026, approximately 657,000 power outages were reported across the region, including at least 20,000 in New York City and Long Island. Despite the challenging conditions, New York City’s subway and bus systems were largely operational with few delays by early afternoon on Monday.

This event follows a previous record-breaking snowfall in New York City on January 22-23, 2016, when 70 centimeters (28 inches) of snow fell in Central Park – a figure unmatched since meteorological records began in 1869. That storm also caused significant disruption, with vehicles buried under unprecedented snowdrifts.

Can Similar Blizzards Occur in France?

While the Northeastern United States is prone to such intense winter storms, the geographical conditions that contribute to their formation are not readily replicated in France. The key factor is the interaction of frigid polar air with the relatively warmer waters of the Atlantic Ocean. When polar air descends upon the Northeast without first crossing land, it retains its extreme cold. This creates a significant temperature contrast with the Atlantic, fueling the rapid development of a cyclogenesis – a quickly intensifying low-pressure system – and generating heavy snowfall along the coastline.

France, however, is surrounded by seas and the Atlantic Ocean. This means that polar air masses are typically modified before reaching the country, losing some of their intensity. The temperature difference between the air and the ocean is therefore less pronounced, resulting in less powerful cyclonic systems. While France does experience winter storms and snowfall, they are generally less severe and less frequent than those seen in the Northeastern United States.

Nevertheless, France is not immune to significant snow events. Blizzards can occur when cold air interacts with milder air, particularly in mountainous regions. Notable examples include a severe blizzard in Normandy in March 2013, which produced snowdrifts reaching two meters in height. Historical events, such as the blizzard that struck the Beauce region and Paris in early January 1979, and the one in February 1986, demonstrate the potential for substantial snowfall in certain areas.

In the southeast of France, blizzard conditions typically arise from a combination of a deep Mediterranean depression and a polar air mass. Severe episodes were recorded in February 1954 near Perpignan, February 1956 in Provence, and in late December 1970 in the Rhône Valley, resulting in snowdrifts exceeding several meters in height.

while the scale of the recent blizzard in the Northeastern United States is unlikely to be replicated in France due to differing geographical factors, France is still susceptible to significant snowstorms and blizzard conditions, albeit less frequently and generally with less intensity. These events are linked to less intense and extensive low-pressure systems, resulting from a less pronounced thermal conflict between polar and oceanic air.

Further Reading:

  • 80 cm of snow in the Var: the chaos of late February 2001
  • The endless winter… From mid-November to mid-March!
  • The resorts of the Alps buried under several meters of snow!
  • What if March was very dry?
  • Our daily updated weather bulletin
  • Our highly followed and referenced Twitter account in all media!

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