Oil paintings large and small - everyday inspirations - commissions welcome
Monday, January 30, 2017
THREE AMIGOS
Friday, January 27, 2017
KISSES
Thursday, January 26, 2017
BE MINE
Wednesday, January 25, 2017
MADE MILWAUKEE FAMOUS
Tuesday, January 24, 2017
TWO HEARTS
Monday, January 23, 2017
THE CHUCKS CONNECTION
Sunday, January 22, 2017
Women's March Steamboat Springs
Thursday, January 19, 2017
HOARFROST 101
According to the National Weather Service office in Riverton, Wyoming, the Old English dictionary (c. 1290) defines hoarfrost as "expressing the resemblance of white feathers of frost to an old man's beard."
First, to produce any frost, you need water vapor (gaseous form of water) in the air over cold ground with a surface dew point at least as cold as 32 degrees.
When these water vapor molecules contact a subfreezing surface, such as a blade of grass, they jump directly from the gas state to solid state, a process known as "deposition", leading to a coating of tiny ice crystals.
So what provides the boost for frost to grow into hoarfrost like this?
Generally speaking, you want a much more moist air mass in place. In late fall, winter or early spring, one or more days in a row of freezing fog (fog with air temperatures of 32 degrees or colder) is a perfect scenario.
With more moisture in the air, the interlocking crystal patterns of frost become more intricate and much larger, building up to a greater depth on tree branches, signs, fences, anything. This is hoarfrost.
If there is a light wind, the hoarfrost can accumulate on the downwind side of objects.