Doubt that. It’s still the very long range NAM so whether it’s showing beefy totals or nothing at all it shouldn’t be taken serious until we get inside 36-48 hours. It had a 1035 HP sitting further south closer to the US border so I think we are sitting pretty as of right now.The NAM looks like it’s coming in pretty beefy for western/central NC and the northern Upstate but it is warmer than the GFS suit and CMC suit this might be because the NAM’s hp is 2-3 mb weaker than those models. However it looked like it did increase QPF this run.
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What trend? Outside of the euro there isn’t a trend.Ballgame for upstate...trend has been less precip and warm. Only extreme north get anything other than cold ass rain!
Dewpoint. Another poster hit the nail on the head. These warm dews we experience anymore will do a number on what would have been a classic CAD even 5 years ago.Doubt that. It’s still the very long range NAM so whether it’s showing beefy totals or nothing at all it shouldn’t be taken serious until we get inside 36-48 hours. It had a 1035 HP sitting further south closer to the US border so I think we are sitting pretty as of right now.
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.
Really cool study from Sanders & Barjenbruch (2016) wrt ice liquid ratios that's worth reading imo.
https://journals.ametsoc.org/view/journals/wefo/31/4/waf-d-15-0118_1.xml?tab_body=fulltext-display
For ice radial accumulations, which are the standard for measuring freezing rain accumulation, they found that for every inch of radial ice accrual about 3-4" of liquid equivalent is measured (via ASOS).
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Thus, when you see maps like this, especially when there's a ton of QPF, it's usually a good idea to take ~25-33% of these 1:1 QPF-ice accumulations.
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Pivotalweather also now has an option for those w/ a subscription where you can select for the Freezing Rain Accumulation Model (FRAM) accumulations described in the aforementioned study & these are considerably more reliable than 1:1 QPF-ice accum model output. The FRAM model uses regression on modeled precipitation rate, wet bulb temperature, and wind speed to estimate ice accrual. It's certainly better than using straight 1:1 QPF-ice output, but I would still urge caution in using a product like this.
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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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cloudy miserable day. Some cold rain, any ZR or sleet probably last under 2 hours at onset. Patchy mix.What does the bird man think about Zebulon?
2m Temps, dew points have both trended warmer in my area of the upstate on the NamWhat trend? Outside of the euro there isn’t a trend.
It does which makes it’s temp profiles in the long range warmer. That’s something that switched on the nam from years past. That’s why the rule of thumb is to really not put much stock into the nam until you get inside 36-48 hrs.Doesn't the NAM have the same issue as the Euro of being overamped, especially in the long range?