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February 13–17, 2021 North American winter storm

Category 3 winter storm and ice storm in the United States

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Satellite image of the large winter storm , also known as "Winter Storm Uri", over the Eastern United States on February 16, 2021.
NASA · Public domain

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The storm resulted in the National Weather Service issuing various winter weather alerts impacting over 170 million Americans. Over 9.9 million people in the U.S. and Mexico experienced blackouts, many due to a major power crisis in Texas, which became the largest in the U.S. since the Northeast blackout of 2003. The storm contributed to a severe cold wave that affected most of North America. The storm also brought severe destructive weather to Southeastern United States, including several tornadoes. On February 16, there were at least 20 direct fatalities and 13 indirect fatalities attributed to the storm; by January 2, 2022, the death toll had risen to at least 290, including 276 people in the United States and 14 people in Mexico. A subsequent data analysis using a technique that examined the total number of reported deaths during and immediately after the storm estimated that about 700 people were killed by the storm during the week in which the power outages were most widespread.

The National Oceanic and Atmospheric Administration officially documented US$26.5 billion in damage in the United States from the winter storm. It was also the deadliest winter storm in North America since the 1993 Storm of the Century, which killed 318 people.

Meteorological history

On February 13, a frontal storm developed off the coast of the Pacific Northwest and moved ashore, before moving southeastward, with the storm becoming disorganized in the process. During this time, the storm reached a minimum pressure of 992 millibars (29.3 inHg) over the Rocky Mountains. On the same day, The Weather Channel gave the storm the unofficial name Winter Storm Uri; the Federal Communications Commission adopted the name in their reports from February 17. From February 12 to 13, a trough dipped southward from Northern California into northern Mexico, which channeled moisture from Texas towards the storm, as the system moved southeastward. Over the next couple of days, the storm began to develop as it entered the Southern United States and moved into Texas. From February 13 to 14, a second, much larger trough developed over Central United States, aided by a southward shift from the polar vortex, while the winter storm moved into Texas. The trough became fully developed by February 15, channeling significant amounts of moisture into the winter storm and also contributing to a historic cold wave that affected most of the Central and Eastern United States. Winds in the jet stream reached 170 mph (275 km/h) around the trough. On February 15, the system developed a new surface low off the coast of the Florida Panhandle, as the storm turned northeastward and expanded in size.

On February 16, the storm developed another low-pressure center to the north as the system grew more organized, while moving towards the northeast. Later that day, the storm broke in half, with the newer storm moving northward into Quebec, while the original system moved off the East Coast of the U.S. By the time the winter storm exited the U.S. late on February 16, the combined snowfall from the multiple winter storms within the past month had left nearly 75% of the contiguous United States covered by snow, which was the largest amount of snow cover seen in the United States since early 2003. On February 17, the storm's secondary low dissipated as the system approached landfall on Newfoundland, intensifying in the process. At 12:00 UTC that day, the storm's central pressure reached 985 millibars (29.1 inHg), as the center of the storm moved over Newfoundland. On the same day, the storm was given the name Belrem by the Free University of Berlin. The storm continued to strengthen as it moved across the North Atlantic, with the storm's central pressure dropping to 960 millibars (28 inHg) by February 19. On February 20, the storm developed a second low-pressure area and gradually began to weaken, as it moved northwestward towards Iceland. Afterward, the storm turned westward and moved across southern Greenland on February 22, weakening even further as it did so. The storm then stalled south of Greenland, while continuing to weaken, before dissipating on February 24.

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