Frost is a thin layer of ice on a solid surface which forms from water vapor in an above freezing atmosphere coming in contact with a solid surface whose temperature is below freezing and resulting in a phase change from water vapor a gas to ice a solid as the water vapor reaches the freezing point in temperate climates it most commonly appears on surfaces near the ground as fragile.
Frost on roof above freezing.
Low temperatures overnight were generally in the.
Mon 06 oct 2008 19 38 20 gmt frost at 35 degrees.
Something i implied above but didn t say explicitly is that when frost forms on the roof the roof is below freezing.
We had a chilly start to the day with frost in many countryside locations.
On a long cold spell these objects will cool down to below 0 celsius.
As it cools below 35 degrees water condenses on it.
In other words the sequence might be as follows.
2 the car roof cools radiatively.
Have you ever wondered why frost can form on nights when the temperatures only fall to 36 or 37 degrees.
How can that be.
The phenomenon of water freezing on objects like the ground parked cars motorbikes etc is due to thermal inertia.
Look at the entirety of your roof is the frost melting unevenly and not due to the sun s heat.
That is how we get a frost without a freeze.
The plot below shows a 24 hour trace of the temperature measured at 0 5 meters above the ground in blue at 2 meters above the ground in red and at 3 meters above.
So the air can be above freezing and the surface of your car or the roof of your house can be colder than the air and colder than freezing causing a frost even though the air temperature is above freezing.
Ice at least at atmospheric pressure cannot form above the melting point of water 0 celsius.
Does your garage have a frosted roof and the rest of your home does not or vice versa.
1 initially the air and the car are at temperature 37 f and the dew point is 35.
If the dew point is below freezing the water vapor condenses as ice freezing as frost.
In other words the sequence might be as follows.
The kentucky mesonet recently added some extra temperature sensors at varying heights that show just why this could occur.
So ice can form even if the temperature of the surrounding air is above freezing.
1 initially the air and the car are at temperature 37 f and the dew point is 35.
The radiative cooling effect is strong enough to lower the temperature of surfaces exposed to the sky by several degrees below the ambient air temperature.