<< Here in Texas, one-quarter inch of ice shuts down our schools, roads and most businesses. I know, I know. I'll hear all about how them Yankees can drive on ice but us cats down south are terrified of the frozen stuff. Bring it on. I hate cold weather. >>
Monte, don't believe
all the BS you hear about Northerners driving on ice like it's dry concrete. That's arguably the case if, and only if, the temperature is
really low (so that there is less chance for pressure and friction to melt the ice surface and form a micro-thin film of water under the tires.
That's what makes ice slippery).
A couple decades ago, AAA (sorry, that's American Automobile Association for benefit of our international readers) published results of a test of the distance required to stop a car on ice in dry conditions at freezing point (32°F. or 0°C., take your pick), vs. the distance required to stop the same car, same surface condition, at 0°F (-17.8°C.). A car skidded
four times farther at freezing point than it did at the colder temperature. (Sorry, I can't remember the test speed, other than that it was the same for both observations; the relationship between the results probably is nonlinear if the test speed is higher or lower.)
There are some curious implications of the AAA study. Remember science in school, where we learned that no matter how cold the air temperature is inside a freezer, the temperature of its ice cubes (so long as the ice contains nothing but water) is always at the freeze point? (That's the principle behind survival in a snow cave or an igloo.) Why wouldn't the effect of friction and pressure (from the weight of a vehicle) have the same on stopping distance on ice, irrespective of air temperature. I've never read this anywhere, but I'll venture a SWAG: I suspect the key is that the ambient (air) temperature lowers the temperature of the vehicle's tires enough below the freezing point to inhibit the melting effect and lessen (or prevent completely) the formation of the slippery thin layer of water beneath the tires. Can any physicist or engineer out there confirm or blow away my gut-hunch guess?
I grew up in Central Virginia and lived a few years in Ohio and Massachusetts. I found it
much easier to drive in winter there than here in the Washington, DC, area. Why? Two reasons: (1) When there's ice, it tends to form just below the freeze point because of the warming influence of the nearby Chesapeake Bay and the ocean; and (2) the drivers, because there are many transients (foreign diplomats, government employees, and immigrants) from warm climates where ice is a sometime thing, if ever. (What's the most dangerous thing on the road here? A mammoth SUV with diplomatic plates on it. Â

)
I agree with what I think you're saying: A Texas ice storm is scary. In late November 1982 when I was moving from El Paso to Northern Virginia, my spouse and I surfed the leading edge of a storm that turned from snow to freezing rain somewhere east of Abilene. It was a really interesting experience in an overloaded 17-year-old VW. We finally ran out of it around Fort Worth.
FWIW, we have about 1/4 inch of ice on everything here in Virginia as I write this. Freezing rain is still falling. The temp has been just above freezing all day, and probably will drop tonight. It might not be possible to get out of my neighborhood tomorrow morning.