Blizzards are a defining hazard of the Arctic—not just heavy snow, but a specific meteorological triad: sustained winds ≥35 mph (56 km/h), visibility <¼ mile (400 m) in blowing/falling snow, duration ≥3 hours. The Arctic's open terrain, abundant loose snow, and frequent intense cyclones make it a blizzard factory.
Ground Blizzards: No falling snow—just wind mobilizing existing snowpack. Most dangerous: sudden onset, clear sky above, invisible until you're in it. Common on sea ice and coastal plains.
Synoptic Blizzards: Classic storm systems with heavy snowfall + wind. Can drop 30-50 cm in 24 hrs. Disrupt aviation, marine transport, community supply lines for days.
Polar Lows ("Arctic Hurricanes"): Small (<500 km), intense, short-lived vortices over open water. Hurricane-force winds, convective snow bands. Major hazard for fishing/offshore vessels.
Inuit and Saami languages have precise terms for blizzard types, wind directions, snow conditions, and precursors (e.g., pungniq—Inuktitut for blizzard; čuoika—Saami for drifting snow). Traditional forecasting reads cloud sequences, wind shifts, animal behavior. Modern models (ECMWF, GFS, Arctic-specific WRF) struggle with polar lows and ground blizzards—data sparsity, boundary layer physics, sea ice coupling. Improvement comes from assimilating Indigenous observations, buoy arrays, and targeted dropsondes.