The Weather Guys

Over the past weekend, southern Wisconsin experienced its first cold snap of the season with widespread morning lows in the upper 20s on Friday and Saturday mornings.

Often, cold snaps in autumn are short-lived, as this recent example was, affecting usually one or two nights at most.

There are a variety of reasons for this brevity. First, cold snaps at this time of year require a substantial southerly excursion of cold air from high latitude Canada to get us cold. Though the Arctic night creeps ever farther south each day after the autumnal equinox, its southerly progress is slow.

Consequently, cold air production is limited to the very highest latitudes well into November, which means that any cold air that makes it as far south as Madison is not well connected to a broader reservoir of cold air that would allow the cold to remain.

Second, there is little snow on the ground even in central Canada at this time of year and so the cold air that does migrate southward is modified (warmed) to a greater degree on that migration at this time of year than in the late fall and winter when snowcover is widespread.

Third, the lack of snow on the ground in Madison itself limits the longevity of cold snaps. This is even true in the wintertime. Overnight cooling over a snowfield can reinvigorate the chill of a cold snap and render it longer lasting as a result. So, if you were complaining about the cold this weekend, be glad we are still in October and much more likely to experience a quick rebound.

On Wednesday morning, we will officially enter fall as the autumnal equinox occurs at 3:20 a.m.

On Wednesday, in common with every location on Earth, we will enjoy exactly 12 hours of daylight and 12 hours of night.

Of course, 12 hours of daylight in Madison (latitude 43N) is substantially different from 12 hours of daylight at the North Pole (latitude 90N) where the sun will barely be visible above the horizon for the 12 hours of “daylight.” On the very next day, the sun will not appear above the horizon at the Pole and will not come back for six months. As the days march on, the same fate will gradually overtake other latitudes in the Northern Hemisphere until by Dec. 21, the sun will not rise even at 66.5N.

The primary means by which air is warmed is by its contact with the surface of the Earth that, when the sun shines, can absorb radiation and heat up.

A leading consequence of the shortening days, especially at high latitudes, is that air masses can begin to get really cold again. Even as we enjoy one the warmest Septembers in quite some time, the areal extent of the cold wintertime air is growing at high latitudes.

As it encroaches southward from the Pole, the polar jet stream, always on the warm edge of the coldest arctic air, begins to take up residence at lower latitudes bringing with it the powerful storms of late autumn and winter.

So, enjoy these beautiful early fall days we are having in Madison because the cosmic deck is stacked against us.