BigB0882 wrote:I thought ULLs usually result in a colder air column from top to bottom, typically resulting in more snow than frozen rain. You can still have big pockets of warm air above the service with an ULL passing over?
Well, you will have cooling due to the upper level system coming in at the mid-levels. However, the depth of cold air near the surface is very shallow. There will be a warm tongue at about 5,000ft in the air. When you have very dry atmospheric column and then precipitation falling into it, you can get cooling due to the effects of evaporation of precipitation in very dry air. However, the column will already be saturated from the top down and little or no evaporative cooling will take place, so no cooling from evaporative processes will occur to cool the "warm nose". The cold at the surface will come from cold air advection, or transport of cold air from the north and west(due to the winds). Due to the warm air nose around 5,000ft that will be above freezing, it will melt all the precipitation to liquid form. We will get re-freezing of the precipitation before it reaches the surface or "sleet". Before the transition to sleet, the rain will freeze on contact or more commonly know as freezing rain. It is very unlikely, but possible, that we might transition to some light snow on Sunday. Models are keeping us all sleet during the weekend, but if the cold air gets deeper and erodes the warm nose over the weekend and if the models are underestimating the depth of the cold air, we might go over to snow at the very end. However, expect mostly ice from either freezing rain or sleet throughout this event.