GRAYSONCO.WX wrote:What exactly does does TrekkerCC's post mean in regards to tomorrow's precip type?
Well, I'm just noting trends at the moment; through, it can have an effect for the future. Models have errors in them; some of them are inherent to the model themselves - the way a model solves the complex equations to generate a guess on how the atmosphere will evolve, chaos in a non-linear atmosphere will intrude, and the models don't have observations for every point in the atmosphere and has to "guess" the atmospheric state, especially upper-air, where the observations are spaced out by in some cases hundreds or thousands of miles. It is good to note if the models are handling track of the upper low (given it might change how much precipitation we will get and how much dynamic cooling occurs) and other data, since the models might be error prone due to all these reasons. If the forecasted temperature is too warm, then it might mean something in marginal events.
Short answer: If the models are forecasting too warm temperatures during the event, the rain will transition to snow quicker than projected and it might totally change over in places (such as DFW metroplex) that are currently forecast to have a rain/snow mix. Usually, very slight changes in atmospheric conditions can be the difference between a snow or rain event. Right now, the models from 12 hours ago slightly over-estimated the low level temperatures observed, if this continues, it might mean that the atmosphere might change over to snow quicker than what the models are forecasting. Now, like iorange55 said, it might not make a difference, but in these marginal events, even slight differences in the atmosphere can cause a event to go from rain to snow.
But to illustrate how critical the factors in marginal events can be: In 2007 or 2008, we had an ice event, where Ft. Worth got ice accumulations of 1/4"+ (ice storm criteria) from heavy freezing rain, but in Dallas, the heavy precipitation brought down the warmth from above to prevent surface temperatures from getting below freezing until the end of the event - in Dallas, we ended up with light ice accumulations. The models didn't see the full extent of the warmer air being brought down by downdrafts during heavy precipitation.
edit: slight clarification