Regional radar is mainly clear as clouds gradually increase from a developing low pressure area moving northeastward from the Gulf states. Some widely scattered showers have reached into West Virginia and southwestern Pennsylvania. This low will bring some rain to the area overnight. Current indications are that the next system may end as some wet snow or flurries on Sunday, with little or no accumulation in the immediate area. The models are becoming more consistent on this, but there is still some difference in timing.
Tonight and Tomorrow
Snow Statistics
A couple of weeks ago, we noted that, statistically at least, January snowfall gives virtually no clue to February's amount. Today's chart shows that there is one element which does provide some insight, and that is February temperature. Colder temperatures do correlate to some extent with more snow. As some site visitors have pointed out in earlier comments, however, this is far from a lock. There is a lot of scatter in the data, and some quite cold Februaries have had little or no snow, even a few which averaged below 30° (13° colder than this January). The dashed regression line shows that for each degree the monthly average temperature is below about 44.1°, the expected monthly snow total increases by about ¾". The value of R² indicates that about 25% of the variance in snow amounts is accounted for by the average temperature.
CapitalWeather.com chart from NWS data
DC Comics
Tom Toles' cartoon in today's WaPo commenting on political science:
Here's the statistic Bob Ryan was probably referring to last night: In 54 years of history, Washington National has averaged 0.2 thunderstorms in January out of the 30.6 total per year. This is now the third time thunder has been reported this month. Thunder was last observed in January before this year on New Year's Day, 2003.
Set the TiVo! From the WaPo TV listings comes the news that Doug Hill has escaped the 2½ minute straightjacket to host a 30 minute special about the WeatherBug network tonight. The show is on at
This year's warm start has many people asking how unusual it is for January. The monthly average temperature of 42.7 through yesterday has moved up the charts to 9th place on the 135-year official Washington hit parade.
Whether you believe in the
Southerly winds ahead of a developing low pressure area in the lower Ohio Valley are bringing mild conditions to most of the East Coast this afternoon. Temperatures are above freezing everywhere except northernmost New England, and the 60s are being observed as far north as northern and western West Virginia. Aided by strong upper level support (For the geeks, that means "positive vorticity advection" and a "negative tilt" to the trough axis), squall lines broke out in early afternoon from southern Ohio through Kentucky and in the western Carolinas.
Someone suggested in the previous comments that this weather is so boring it should have a web site called "LowercaseWeather.com". The one thing that is constant about weather is that it will always change. Since things are a little slow now, I had the chance to do some homework.
In the case of snowfall, all bets are off. The chart on the right shows a plot of total snowfall for December vs. January (trace amounts were considered 0). Notice how the points are much more random than in the temperature chart. In fact, the R² value is much less than 0.01; about ¼ of 1% of the variability of January snowfall is explained by the December amount. This is shown by the regression line being almost completely flat. What relationship does exist is actually negative, indicated by the negative coefficient of x in the regression equation. So, there is a non-zero probability that January snowfall will be low when December's is high, but the statistical reliability of that connection is extremely low.




