Storm getting underway with a potpourri of precipitation types across the Houston area

In brief: Houston’s forecast appears mostly on track, with a definite trend toward the heaviest snow and sleet emerging south and east of Houston by Tuesday morning. Accumulations may be as high as several inches under the most persistent bands, with a general coating to few inches elsewhere. Winds will gust near the coast Tuesday morning as well, and a very cold night still looks on tap tomorrow night.

Happening now

Well, our much advertised winter storm is underway across the Houston area. We’ve seen reports of sleet, graupel, rain, and snow across the region. We seem to be settling down into a tiered setup now with snow and sleet north and west, sleet and graupel in the lighter precipitation, and sleet and rain near the coast.

That area of snow and some sleet occurring north and west of Houston is going to gradually fill in and drop south and east through the night. As it does so, we’ll pick up some accumulating snow. As it gets closer to the coast and the potential for banding gets underway, that’s when we may see locally heavy snow anywhere from I-10 southward to the coast.

Forecast for the night

So before 3 AM, look for this potpourri of precipitation types. Again, plain rain should be expected in spots near the coast especially. This is not a surprise and was anticipated ahead of time. After 3 AM, there will be a transition to all sleet and snow and eventually just snow. There is a good chance we will wake up to snow falling tomorrow, although how much on the ground is an open question with a few possibilities. Snow should end from northwest to southeast after 9 AM tomorrow.

Why have we been kind of cagey on snow accumulation numbers?

Those that read us closely can tell we’re throwing out various accumulation numbers based on model data and National Weather Service forecasts but we’re not exactly confident. Now, the event is underway so we should be highly confident, right? Not right. The SREF is a short-range ensemble model, meaning it’s run multiple times with varying snapshots at the beginning to produce a more realistic spread in outcomes. Basically, we want to see how bad or not bad it can get. As of the 3 PM run this afternoon, this model showed snow totals ranging from nada to as much as 7 inches at Hobby Airport.

Now, Hobby Airport almost certainly won’t get 7 inches of snow. It probably won’t get 0.0 inches either. The average on this particular model is around 2 inches, which is reasonable, but there is such a spread in options here that it doesn’t necessarily inspire much confidence. The trouble with this event is that we’re dealing with a wintry mix at the start, we don’t know where banding will establish, we’re in a place that rarely sees weather like this so it’s far outside of the bounds of the climatology (normal) these models use, and we have the Gulf of Mexico in our backyard. All that to say, this stuff is hard. If you want snow, hope for the best. If you do not want snow, hope for the best. May the odds be ever in our favor.

Sleet versus graupel

Here’s a true story. Back in my on-air broadcast days in Utica, NY, I once was describing a day where we had a bunch of graupel fall in Upstate New York and explained what it was. Immediately after the news, I received a call from an older gentleman who told me he had a dictionary in front of him, couldn’t find the word, and proceeded to lambaste me for making up words. I can assure you that it is a real word. So what is it, and how does it differ from sleet?

We’ve gotten reports of sleet and pictures of basically tiny “balls” of ice across the area. When you look at the pictures, however, they look more like Dippin’ Dots than ice pellets (sleet). That’s a tell-tale sign of graupel. The differences? Sleet is straightforward: A snowflake falls, hits a layer of milder air above freezing, melts, and then refreezes in colder air below that, falling as quite literally an ice pellet. Graupel happens when you get water droplets that are still liquid below 32°, (or what is called “supercooled”). The supercooled water droplets collide with and freeze on a snow crystal, a process called riming (which is a homonym of “rhyming”). They basically fall to the ground as snow pellets. They tend to be whiter (hence Dippin’ Dots-like!), whereas sleet is clearer. Sleet melts in your hand, whereas graupel may fall apart or crumble in your hand.

What many of you may have reported as sleet tonight was actually graupel. This is a weird storm because we have a pretty intense layer of dry air from the surface up to about 5,000 feet and from about 12,000 feet up to 30,000 feet. The region of the atmosphere where snowflakes will grow is up above 15,000 feet, so we’re seeing a bit of chaos ongoing above our heads. As the night goes on, this dry air will erode as the atmosphere cools, leading to more regular snow.

Eric will have the latest for you in the morning. Stay safe, stay off the roads tonight, and we’ll see where we are tomorrow!