skidoochic
New member
If the surface temperature is below zero, how does the air aloft stay above freezing? Wouldn't the cold air "chill" the warmer air until it was cold enough to produce snow?? Or is that just wishful thinking
This is what I read to generate this question:
A DEEP LAYER OF WARM AIR BETWEEN 5KFT AND 10KFT ABOVE A SHALLOW LAYER OF COLD AIR AT THE SURFACE...the classic set up for freezing rain.
(Its from the NOAA)
This is what I read to generate this question:
A DEEP LAYER OF WARM AIR BETWEEN 5KFT AND 10KFT ABOVE A SHALLOW LAYER OF COLD AIR AT THE SURFACE...the classic set up for freezing rain.
(Its from the NOAA)