A January thaw is nothing out of the ordinary here. The very term bespeaks of a well-earned punctuality: a couple months of hard, cold weather, then January shows up, and for a few days the mercury sails to equatorial heights. It’s as if winter has exhaled and is sucking in another huge breath to last until April. No big deal.
And so it was, on January 2, when temperatures in many parts of the North Country completed a nearly sixty-degree upswing in a little over twenty-four hours. With the warmth came rain and fog. And more rain. In Long Lake, town supervisor Thomas Bissell reported that the lake rose four feet in twenty-four hours, something he had never heard of happening before. In Essex County, man-made Minerva Lake was in danger of breaching its dam. Instruments in Newcomb would eventually catch more than four inches of liquid precipitation.
But to the north, the rain was starting to freeze on contact. According to meteorologist Cindy Fitzgibbon, of News Channel 5, in Plattsburgh, what made this winter rain unique was a massive Arctic high-pressure system to our north and east that funneled cold air into the region. At the same time, the jet stream was positioned further north than usual—on a southwest-to-northeast tack-which funneled moisture-laden warm air from the Gulf of Mexico along a stationary front.











