I often receive e-mail with questions regarding weather. This week has been no exception. The difference this week is that the questions have been more pertinent to the current weather situation. So, I thought I’d post the questions and answers here.
Jill writes:
My question for you- how do you determine the forecasted accumulation and how accurate is the forecast in the threat of snow for the Mid-south? ( + or – one inch or 1/2 inch tonight & tomorrow )
Here’s the answer:
Snowfall is a little more difficult to forecast in this part of the country because so many conditions have to align for it to occur and the occurrences are few each year. Our forecast is based on computer forecast model data which determines the amount of liquid precipitation that is possible for an area over a given time period. Snowfall amounts are then based on the amount of liquid precip the models forecast. The average liquid to snow ratio is 10 to 1. In other words, on average every tenth of an inch of liquid precipitation translates into one inch of snow. Surface temperatures can cause that average to vary slightly + or -.
Models runs for the past 72 hours have indicated .10″ to .12″ inches of liquid precipitation which would equate to about an inch to an inch and a half. This morning’s model runs were a bit drier indicating .08″ of liquid precip which translates to just over three quarters of an inch of snow. Based on the forecast model trends and the speed of the approaching front I’m thinking most of us will get about a half an inch to an inch. It may vary by a half an inch at most.
Jim writes:
Dear Ron how do you determine the wind chill?
Here’s the answer:
Hi Jim,
The wind chill is how cold people feel when outdoors. The Wind chill is based on the rate of heat loss from exposed skin caused by wind and cold temperatures. As the wind increases it draws heat from the body driving down the skin temperature making it feel colder. For example, yesterday the 6 AM temperature was 14 degrees with a wind speed of 9 mph and a wind chill of 2 degrees. This morning at 6 AM the temperature was 17 with a calm wind so there was no wind chill. Thus, technically it felt 15 degrees warmer today at 6 AM than yesterday at the same time.
Today the wind chill is automatically calculated by our various weather computers so we don’t have to do the math.
The term wind chill and its original mathematic calculation go all the way back to the 40s and an Antarctic explorer named Paul Siple.
The original formula was based on calculations used to determine the time needed to freeze water in a plastic cylinder that was exposed to the elements.
In 2001 the U.S. and Canadian Weather Service developed a new formula to calculate wind chill. The new formula is based on greater scientific knowledge of weather combined with actual human experiments. They used volunteers in a wind tunnel to find out how fast their faces cooled with varying combinations of temperatures and wind speed.
Here is the original formula for calculating wind chill:
T(wc)=0.0817(3.71V**0.5 + 5.81 – 0.25V)(T – 91.4) + 91.4
Here’s the new one:
T(wc)=35.74 + 0.6215T – 35.75 (V**0.16) + 0.4275T (V**0.16)
In the formula T=Temperature in Fahrenheit, V= Wind Speed in miles per hour, and ** refers to an exponent (i.e. V to the .05 power)