A stationary boundary was draped across the Adirondacks of New York into portions of central and northern New England from December 20th through 22nd with several disturbances delivering precipitation. An impressive battle between mild to warm moist air, south of the boundary with temperatures in the 50s, overriding a very cold, dense shallow air mass with temperatures in the teens and 20s in New York but single digits just north across the border into Canada.
First round of wintry precipitation fell across northern New York, especially along the Canadian border during Friday afternoon (December 20th). Most of the precipitation fell as freezing rain, approximately 1/4 to 1/3 of ice accumulation, along with some sleet. The second round began during the late morning and early afternoon hours of December 21st and peaked during the evening and overnight hours. An additional 1/2 to 1 inch of ice accumulation as well as 1 to 2 inches of sleet occurred in portions of northern New York.
The greatest impact was along the Canadian border, especially the St. Lawrence River Valley with widespread tree and utility line damage as well as numerous vehicle accidents. Tens of dozens of customers were without power from hours to days across the region. Similar areas as the Ice Storm of January 1998, but not the severity as precipitation and ice accumulation was half of the 1998 storm.
Ice jams also developed during this time period as runoff from melting snow and rainfall swelled area rivers. River rises were enough to break up and move ice cover, resulting in scattered ice jams.