Webberweather53
Meteorologist
It always has been a cold rain here. Nothing has changed.Let me guess...the models are trending warmer and upstate Sc is looking like a cold rain now?
Yes, it's more like 1" Radial ZR:3-4" QPF according to this study. Stronger winds actually enhance ice accrual efficiency because it increases the rate of evaporative cooling, the rate of sensible heat transfer from cooler surrounding air to slightly warmer adjacent air near a freezing object that's undergoing latent heating & stronger winds increase a horizontal cross section's mass flux (of ice), all serving to increase ice accumulation efficiency at higher wind speeds. The effect is pretty small until wind speeds begin to approach exceed 10-15 knots.
"It is inferred that the increasing wind speed replaces air near the ice surface warmed by latent heat release, alters the droplet collision efficiency, increases the horizontal mass flux, and promotes evaporational cooling. Although, the data show that these processes are not as noticeable in the ILRs until wind speed reaches >15 kt, and may rely on the thermodynamic environment as well. Wind gusts had a similar influence on ILR with an increasing trend in ILR as wind gusts increased."
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As for surface temperatures, your intuition is correct in that there's a strong temperature dependency, with wet bulb temperatures above -1C (~30F) experiencing significantly lower ice liquid ratios (ILRs) than those with temperatures between -4 to -1C. The relationship reverses and lower ILRs are observed for temps lower than about -4C (~25F), as the low-mid levels usually become more supportive of sleet instead of freezing rain, in environments where the surface temperatures are this cold or colder.
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They also found rather unsurprisingly, that ice accumulation efficiency is dependent on precipitation rate with the largest changes in ILRs between rain equivalent rates of a few hundredths to a tenth or so per hour, with it asymptoting towards ILRs of about 1:7.5 or so in heavy precipitation.
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Plenty of models have ice well into the upstate? And models have trended colder. Only model that is warm is the euro with its over amp idea and trying to drive the LP directly into the CAD and that isn’t going to happen. Even if you had the over amp wave like the euro, it would deviate around the CAD and you’d deal with a stronger warm nose which means nothing here as we were going to be ICE regardless.It always has been a cold rain here. Nothing has changed.
Most of the models have me at 33 and rain for a good portion of the event . But even if that was to drop a degree of two, that still wouldn't give me (or others in similar setup) a big event. As you said, we need the lower dew point to web bulb down into the upper 20s. Ice cycles are pretty but it means your losing a lot to run off.For a really big ice storm, you usually want to see dews in the 10s or even single digits, low-mid 20s as shown verbatim on the 3km aren't ideal but potentially just enough to get the job done for a low-moderate end icing event.
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We'll see. And I'll gladly come on here and eat crow if I have to. I'm just not feeling this one at all. We'll see where it goes in the next 24 hrs. For some reason even with a strong high in decent position the cold air push isn't what it should be. Even the NAM is very borderline which is telling to me. Anywhere south of 74 in NC is on the outside looking in if you ask me.Plenty of models have ice well into the upstate? And models have trended colder. Only model that is warm is the euro with its over amp idea and trying to drive the LP directly into the CAD and that isn’t going to happen. Even if you had the over amp wave like the euro, it would deviate around the CAD and you’d deal with a stronger warm nose which means nothing here as we were going to be ICE regardless.
The NAM isn’t even in its wheelhouse yet. We are still dealing with the Hr69 to Hr84 nam. Still have at least 24 hours minimum before we even get into the NAMs range.We'll see. And I'll gladly come on here and eat crow if I have to. I'm just not feeling this one at all. We'll see where it goes in the next 24 hrs. For some reason even with a strong high in decent position the cold air push isn't what it should be. Even the NAM is very borderline which is telling to me. Anywhere south of 74 in NC is on the outside looking in if you ask me.
Probably anticipating the lull in precip (as seen in a lot of guidance) could easily send temps up a few degrees. Doesn’t help that overall qpf is going down either.Sorry if this doesn't belong here but something I don't get is how TWC and other met forecasts have highs in the lower 40s for the CLT metro area when even the warm Euro has us at the upper 30s at the warmest and the GFS keeps the area in the mid 30s.
Are they anticipating a weaker CAD?
Right now I would have to agree with you. Still time for the models to trend a little better. Still a few wild cards out there; like snow cover up over the western sections of the MA. Maybe this could help. RAH currently has slightly colder temps forecasted over the Triangle area. They're usually conservative (but very good) so they may be thinking a slightly colder solutions will win out. But I would say a win for us would be a few hours of ice in the trees on Wednesday morning. Here's my grid forecast:These elevated dews we've been having the last few years is gonna make this another cold rain for RDU.
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What does the bird man think about Zebulon?If there’s any weenies out there that want to see onset sleet I bet it occurs very far south (North half of Georgia, upstate South Carolina, Charlotte, NC) before the warm nose takes over to liquid. But may have to stay up overnight. I’m not sure about Raleigh as it’s so Far East and less favorable timing.