For most, highs Monday reached the upper 30's. This was warmer than what I had thought we would be. But hey, at least it didn't end up cooler.
A new coating of snow can have an effect on high temperatures during the day, but also low temperatures at night. Even with sun, afternoon highs will be cooler than surrounding locations with little to no snow. The reason? It's a term called: Albedo. Snow has a high albedo. This means that most of the shortwave radiation that is produced by the sun and used to warm the surface of the earth is reflected back to space. Whereas a ground that doesn't have much snow, dirty snow or is bare is able to absorb that radiation.
Temperatures Monday afternoon were cooler than surrounding locations. Just look at the highs for today.
Strong temperature inversions can also hinder how warm afternoon highs reach. This happens when warmer air moves in a few thousand feet above the surface of the earth. Meanwhile, temperatures at the surface don't warm quite as fast. A perfect example of that happening: snow on the ground and winds within the jet stream shifting around to the southwest. Similar to what is going to happen the next couple of days.
Noon Tuesday |
3pm Tuesday |
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