Skies remained cloudy for much of Thursday afternoon holding
temperatures in the mid and upper 20s area wide, falling short of the
forecast high of 32 degrees. The clouds were a result of an inversion
in the atmosphere, where warmer air is located above a cooler air mass
near the surface.
Despite a cold front passing early Thursday morning, temperatures aloft
were actually warming. The warm and dry air helped trap
moisture near
the surface, under what is known as an 'inversion'. During the warmer
months, when the sun angle is stronger, an inversion is quick to
dissipate because the higher sun angle allows the atmosphere to warm
faster, helping mix the atmosphere. As we get further and further into
the cooler months the sun angle isn't as strong, so temperatures are not
able to warm as quickly - or efficiently. Sometimes moisture becomes
trapped under that warm layer, leading to either fog or cloud cover
sticking around longer during the day. This can have a major impact on
temperatures during the afternoon.
Skies are beginning to clear from west to east Thursday evening as high
pressure moves in from the west. Temperatures where the skies have
cleared have cooled off already into the teens. Clearing skies and a
light wind may lead to fog early Friday morning. With temperatures
below freezing, freezing fog could become an issue, so watch for slick
spots during the morning.
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