Jeff Snyder
EF5
I continue to see mixed freezing rain and sleet. Most of the day, I'd say the predominant precipitation type at my house (on Waterloo E of I35 along the Oklahoma / Logan county border) has been sleet (IP), though we did have heavy enough liquid precip about 30 minutes ago that it started overflowing the gutters (granted, they're clogged with leaves that I haven't had time to remove, but it's interesting nonetheless). I'd say there's ~0.4" of glaze on the grass and branches, but the solid surfaces (i.e. my concrete driveway) has a good deal of sleet on it, so walking isn't too bad (the sleet acts to bite into the glaze ice a bit, giving a little bit of traction).
The Missing or Calm wind obs on the Mesonet can most likely be attributed to frozen anemometers. I just took a stroll down the road, and I'd say sustained winds are 5-10 mph.
I'm quite fascinated by the persistance of the quasi-stationary band of precip that started about 24 hours ago along I44. Asphalt roads are still largely just wet, not surprising given 2" and 4" bare soil temps in the 34-36F range (see http://agweather.mesonet.org/soil/default.html ). The freezing of the roads will be slowed a bit as the freezing process itself, as I'm sure we all know, releases energy (i.e. latent heat of fusion slows the freezing process). I'm still looking to get out tomorrow morning to take some pictures. Some of my favorite winter landscape pics involve glaze ice.
FWIW, news is reporting 100 auto crashed since last night, with 8 fatalities (a count that doesn't include a multi-fatality collision in Okemah along I40 that closed that interstate). Enhanced rainrates expected given possibility of convection yet again tonight. The 00z OUN sounding (http://www.spc.noaa.gov/exper/soundings/07121000_OBS/OUN.gif ) showed ~700 j/kg MUCAPE, with a very impressive warm nose (~10 C at 850mb... in December!). Interestingly, there's also ~45-50 kts of effective shear (~35kts at updraft base / 850mb / increasing to 85kts at the equilibrium level / ~300mb) which may promote a little organization to some of the storms.
EDIT: KTLX base velocity data indicate that the cold air is back down to near 2800-2900 feet in depth. If I recall correctly, the cold air deepened earlier this morning to near 4000 feet, so it's decreased in time lately. This is not surprising given the strength of warm air advection just above the cold dome. Eventually (most likely by tomorrow afternoon), the freezing line should move back northward. Of course, it's important to note that models have a strong tendency to underforecast the speed and intensity of these shallow arctic air intrusions, so I wouldn't be surprised to see subfreezing temps hold on a little longer than models forecast.
The Missing or Calm wind obs on the Mesonet can most likely be attributed to frozen anemometers. I just took a stroll down the road, and I'd say sustained winds are 5-10 mph.
I'm quite fascinated by the persistance of the quasi-stationary band of precip that started about 24 hours ago along I44. Asphalt roads are still largely just wet, not surprising given 2" and 4" bare soil temps in the 34-36F range (see http://agweather.mesonet.org/soil/default.html ). The freezing of the roads will be slowed a bit as the freezing process itself, as I'm sure we all know, releases energy (i.e. latent heat of fusion slows the freezing process). I'm still looking to get out tomorrow morning to take some pictures. Some of my favorite winter landscape pics involve glaze ice.
FWIW, news is reporting 100 auto crashed since last night, with 8 fatalities (a count that doesn't include a multi-fatality collision in Okemah along I40 that closed that interstate). Enhanced rainrates expected given possibility of convection yet again tonight. The 00z OUN sounding (http://www.spc.noaa.gov/exper/soundings/07121000_OBS/OUN.gif ) showed ~700 j/kg MUCAPE, with a very impressive warm nose (~10 C at 850mb... in December!). Interestingly, there's also ~45-50 kts of effective shear (~35kts at updraft base / 850mb / increasing to 85kts at the equilibrium level / ~300mb) which may promote a little organization to some of the storms.
EDIT: KTLX base velocity data indicate that the cold air is back down to near 2800-2900 feet in depth. If I recall correctly, the cold air deepened earlier this morning to near 4000 feet, so it's decreased in time lately. This is not surprising given the strength of warm air advection just above the cold dome. Eventually (most likely by tomorrow afternoon), the freezing line should move back northward. Of course, it's important to note that models have a strong tendency to underforecast the speed and intensity of these shallow arctic air intrusions, so I wouldn't be surprised to see subfreezing temps hold on a little longer than models forecast.
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