A record low temperature of \u221234 \u00b0F , \u221237 \u00b0C, was recorded in Watertown, New York on January 24, as well as the record cold daily high temperatures for January 24 in the New York Metropolitan Area.<\/li>\n<\/ul>\nCanada Winter Forecast 2025\u20132026 The Old Farmer\u2019s Almanac<\/h2>\n
It marks the start of each hemisphere\u2019s winter season. The winter solstice marks the official beginning of astronomical winter (as opposed to meteorological winter \u2014 which starts about 3 weeks before the solstice). Thankfully, after we reach the winter solstice, the days begin to grow longer and longer again until we reach the summer solstice\u2014the first day of summer and the longest day of the year. The winter solstice is the day with the fewest hours of sunlight throughout the year \u2014 making it the shortest day of the year. (The Southern Hemisphere\u2019s winter solstice occurs in June.) For the Northern Hemisphere \u2014 the winter solstice occurs every year between December 20 and 23, most often on December 20 or 21.<\/p>\n
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St. John’s International Airport recorded 16.3 \u00b0C (61.3 \u00b0F) on January 16, becoming the warmest January temperature on record. 18 communities in Manitoba broke warm weather records on November 23 \u2014 including Portage la Prairie at nearly 14 \u00b0C (57 \u00b0F). Alert, Nunavut also set a monthly record of 1.8 \u00b0C , 35.2 \u00b0F, on the morning of January 7.<\/p>\n
Hemisphere of the North<\/h2>\n
Hurricane-strength wind gusts were reported in New England, nearly reaching 100 mph , 160 km\/h, in the immediate coastal regions. Blizzard conditions were verified across numerous locations (including New Jersey and Massachusetts), with both daily and all-time snowfall records being broken throughout the Northeast. Over 600,000 people lost power at the height of the blizzard due to strong gusty winds.<\/p>\n
Winter is one of the four Earth\u2019s seasons, that goes after autumn and foreshadows spring. It includes their duration (damage), impacted locations, and death totals. The Danish Meteorological Institute in Nuuk recorded a preliminary average temperature of 0.2 \u00b0C , 32.4 \u00b0F, during January, setting the warmest January on record. On February 3 (a weather station near Perico), Cuba recorded the first freezing temperatures ever recorded in the country, reaching 32 \u00b0F (0 \u00b0C). The coldest daily high of 51 \u00b0F , 11 \u00b0C, on The Bahamas was recorded in Freeport on February 1.<\/p>\n
The remnants of former Typhoon Halong moved northward near and affected the Aleutian Islands on October 11. Areas further out west in the country near the Great Lakes were expected to experience higher precipitation amounts, while eastern Canada was forecasted to have a more “dynamic season”. The agency predicted above-average temperatures across regions surrounding the Hudson Bay \u2014 including Ontario and Quebec. On December 11 \u2014 2025, Environment Canada released its winter outlook for December, January and February as part of their monthly climate outlooks.<\/p>\n
On January 24, a record low of \u221234 \u00b0F (\u221237 \u00b0C) was documented in Watertown, New York, alongside the record low daily high temperatures for that same date in the New York Metropolitan Area. On May 6, Denver International Airport experienced 500 reported delays after receiving 5.5 inches (14 cm) of snow, prompting the closure of numerous schools and businesses. As it progressed into western Quebec, the system evolved into a powerful mid-latitude cyclone.<\/p>\n
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Heavy precipitation was anticipated for major U.S. metropolitan areas, some of which were predicted to set new records. States of emergencies were declared in seven states (including New Jersey), New York and large portions of New England. Further east, 14 cm (5.5 in) of snow was recorded at both Ottawa and Montreal. A Bombardier Global 6500 also skidded off the taxiway after landing at Pearson Airport; no injuries were reported.<\/p>\n
The day after the winter solstice \u2014 the Sun\u2019s path begins to advance northward again, eventually reaching its most northerly point on the day of the summer solstice. On the day of the winter solstice (we are tilted as far away from the Sun as possible), which means that the Sun\u2019s path across the sky is as low in the sky as it can be. Some ancient peoples marked the solstice using huge stone structures, like Newgrange in Ireland. Specifically, it\u2019s the exact moment when a hemisphere is tilted as far away from the Sun as possible. We often think of the winter solstice as an event that spans an entire calendar day \u2014 but the solstice actually lasts only a moment. When one hemisphere is experiencing its winter solstice, the other is simultaneously experiencing its summer solstice!<\/p>\n
In one astronomical reckoning, the winter solstice is the middle of winter; being the day of the year that has fewest hours of daylight. In many countries in the Southern Hemisphere (including Australia), New Zealand, and South Africa, winter begins on 1 June and ends on 31 August. In Celtic nations, winter began on 1 November and the time around the winter solstice was seen as the middle of winter. Bede also mentions an older ‘two-season’ year, where summer ended and winter began at the full moon during the month of Winterfylleth, in October.<\/p>\n
Wintry precipitation began to dwindle across the Midwest and Great Lakes as it continued northeastward. The center of the low moved out into the northern Plains and over southern Iowa the following day. On April 3 \u2014 a system developed over the central Rockies, producing heavy snowfall in the northern Rockies.<\/p>\n
Weather Prediction for Spring 2026 by The Old Farmer\u2019s Almanac<\/h2>\n
According to the Julian calendar utilized in ancient Rome, winter commenced on November 10, reached its midpoint with the winter solstice on December 25, and concluded on February 6. This concept persisted in certain regions of Europe during the Early Middle Ages, coexisting along with the more modern notion of four distinct seasons. The onset of meteorological winter in northern regions prone to snow varies considerably \u2014 influenced by elevation, proximity to marine winds, and the volume of precipitation. At the moment of the winter solstice, the Sun’s elevation in relation to the North or South Pole reaches its lowest negative value, indicating that it is positioned farthest below the horizon when measured from the pole.<\/p>\n","protected":false},"excerpt":{"rendered":"
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