Friday February 25, 2011
Heavy Snow Storm
Exceptionally heavy wet snow blanketed much of the region Friday February 25, 2011, coming down at rates of 2" to 3" per hour for a few hours during the early morning. Rapid accumulations lead to what many considered the worst travel scenario of the season to date with deep snow on many roads through the morning commute and beyond into and through most of the afternoon. Slews of accidents were reported on area highways and roads as a result of the treacherous travel conditions. Albany International Airport reported that forty one departures and forty five arrivals were cancelled due to the heavy snow through the late afternoon. Temperatures hovered near 30° through the duration of the storm which created a heavy wet snow, with snow to water ratios running about 7 or 8:1. As a result, the snow stuck to everything leading to beautiful scenes across the region with everything coated in a deep layer of white. Clearing the snow, however, with shovels, snow blowers, and plows, proved to be a difficult task due to its near concrete consistency. Storm accumulations on average ranged from 8"-13" across a wide portion of the region by late Friday afternoon and evening when it ended.
Photographer: WeatherNet 6 Spotter Spencer Conlin: Heavy snow scene in Eagle Bridge, Washington County, 2pm
A sharp line between heavy snow and heavy rain cut through the mid Hudson valley, with an inch to inch and a half of water reported in southern Columbia, southern Berkshire, eastern Ulster, Dutchess and Litchfield counties. Much lighter snowfall accumulations occurred in this region ranging from as little as an inch near Ancramdale, to 3.5" in Alford, MA, (southern Berkshire County), to 4" at Catskill and near 5" at Kinderhook. Existing snow pack in this region absorbed the much of the water precluding any significant issues from flooding. However, flash freezing in elevated areas was observed in portions of this region during the morning and afternoon as wet surfaces froze in spots with temperature fluctuations above and below freezing. Set Up: The storm tracked between Albany and New York City putting the region in the zone where there would be a sharp transition from heavy snow to heavy rain, making for an extremely difficult forecast. The storm itself was fairly flat with only a moderately well developed circulation as compared to a strong coastal Nor'easter which would typically have a well developed and strong circulation. In cases when storms with well developed strong circulations move close to the region they are able to draw warm air north aloft leading to a large zone of mixed sleet and freezing rain in place of snow. In this case, however, some warm air did advance north into the region aloft, but was offset by the substantial cooling processes that were taking place as a result of the strong lift going on and resulting heavy precipitation rates, which produce localized cooling. Therefore, very little sleet was reported during the event with instead a general abrupt change from heavy snow to heavy rain along a sharp rain/snow line. That line moved north through Delaware, Ulster, southern Greene, southern Columbia, to central Berkshire County through the early afternoon before dropping south as the storm moved northeast of the region allowing colder air to return to the southern counties. A strong gusty north to northeast wind north of the rain snow line, induced by the passing surface storm, through the duration of the event maintained a marginally sufficiently deep cold air mass over the Catskills, Mohawk valley, Capital Region to Bennington County, VT on north allowing the precipitation to remain as snow. WeatherNet 6 Observed Snowfall Distribution for the February 25, 2011 Heavy Snow Event
WeatherNet Storm Total Snowfall Reports for February 25, 2011
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