eduggs

Tue-Wed is super amplified. Big phase, neg titled trof, big QPF, and strong SLP. So we shouldn't really say it can't happen.

All guidance actually shows a pretty decent phasing event on Tue - Wed of this upcoming week. Pretty classic phase with the trof taking on a negative tilt and a strong surface SLP. Should be a big QPF maker and significant snowstorm for deep interior Ontario.

12z ICON, CMC, GFS, UK, and ECM all have a distinct (trackable!) wintry threat for Sat 3/8. Nice to see a sudden move towards model consensus. Too bad it's still 7+ days out.

I honestly thought JB would be unemployed and homeless by now. Surprised to hear his name mentioned... It was obvious to everybody about 11 or 12 years ago that he is a garbage meteorologist, a fraud, and an idiot.

I'm confident (though not certain) that you know less about fire prevention than experts whose job it is to know. The issue is likely a lot more complex than you indicate.

The averaged anomaly charts have been looking interesting most of the winter. But the actual realization of shortwaves has continuously materialized as not interesting.

How about we average every hour of the day instead of just the high and low? Then we would have a much better index of the temperatures on a particular day.

On the subject of temperature records... is anybody concerned about how temperature departures are calculated? Is averaging the daily high and low temperature even all that representative or comparable? Should it matter if a low temperature was achieved after a brief but precipitous drop vs. a constant temperature for 16 straight hours? All this fussing about reference periods and minor anomalies... when the method of calculation is hardly precise or rigorously scientific.

Apparently. I'm running behind all coastal regions from Cape May to Cape Cod since 2021.

Meh storm. Just a couple inches.

The Feb 28 - March 3 period is still worth watching. There's a tendency to amplify the flow for successive waves with marginal cold air and a modestly favorable longwave pattern. The 12z ICON, CMC, UK, and EC-AI show significant coastal storms during this period, though with mostly non-frozen precipitation. As usual, the nuances of wave interaction will be key to determining if we can sneak anything wintry out of it.

The Hudson Highlands area had an OK winter this year, especially when you factor in a few early season localized light/moderate events and the sustained snowpack. But I drove through parts of Orange and Putnam yesterday and there was a lot of bare ground on southerly, sun-baked aspects and the usual late-winter snowbanks on the sides of roads were largely missing. People were ice fishing out of the lakes, but the vibe was of a low-snow winter. Down in northern NJ this is the 3rd winter in a row essentially without snow, particularly east of the I-287 terrain boundary. It's been a miserable stretch for snow lovers.

Yup. Days and days of fairly steady modeling showing a miss despite an anomalous setup. Absent a few 5-7 days runs with coastal impact, this has been well telegraphed. You can't even hang your hat on any particular fantasy SREF member anymore as of 15z.

Japan has had a relatively warm winter. Despite that, some of the "heavy snow regions" have had a snowy winter... probably partly due to the warm anomalies in the Sea of Japan. Or are you referring to a different year?

NMB9 showing the extreme (weenie) solution.

A quick look at recent SREF members shows the kind of upper level evolution that would be required to get snow into our area from the coastal. The amount of modeled snow is closely correlated with the orientation of the height lines out ahead of the ULL (area highlighted below). In the very few members that show a few inches of snow for our area (from the coastal and not ULL pass), the 500mb height lines are oriented nearly south to north, indicating an ULL taking on a neutral or negative tilt. Note the 12z 12km NAM is on the more extreme end of the spectrum although not the most negatively tilted compared to the full 9z SREF suite. In the majority of members and models that show no snow from the coastal, the trof is positively tilted and height rises in this area are less pronounced. This connection is probably obvious to most. But I still find it somewhat illuminating to look at the individual SREF members since they show variation far outside the likely envelope of solutions.

The 12z RGEM actually made a similar shift to (/toward) the 12z NAM aloft in terms of adjusting the ULL position slightly west and raising heights out ahead. Unfortunately this only translates to a very slight northwestward shift in SLP and precipitation shield. But if you're tracking for the loooongshot chance of a big model bust, then you'd want to see a continued adjustment in this direction. The RGEM also has some snow with a norlun type feature as the ULL passes.

I think you discount the GFS slightly here because of the other guidance, but definitely not entirely. The GFS shows that if some aspect of this evolution is not favorable, the whole thing could fall apart. A miss southeast is still very much on the table. I'll be looking for run to run consistency from the other models in upcoming cycles; minimizing the variability will increase confidence. And of course any improvement in the GFS will be welcomed. But there could easily be occasional misses across guidance for the next few days. It is almost always like that at this range in advance of major storms.

As modeled on the 12z ECM, this is a 12-18hr event, depending on location across our area. Several of the individual members that gain more latitude also provide a longer duration event because we spend more time in the CCB as it pivots over our area.

And it's not like the GFS hasn't bit at all. The 0z was a significant snow event for DCA/Balt to PHL and major NYC to BOS. 6z was still significant for most of the corridor.

I don't have access to the individuals, but from the looks of it I'd estimate at least 25% of them would bring > 1.5" liquid to most of the area. Lots of high impact solutions there!... including several more intense than the operational. But the caveat is that individual ensembles cluster around the parent operational run. So the true chance of >1.5" liquid from this storm is probably less than indicated by the EPS spread.

It's a definite risk with a pinwheeling ULL pushing into confluence. If the complex is shunted east before mid-level lows mature, the magnitude of event collapses pretty quickly.

The low totals from the 12z ECM operational run are due to the SLP not gaining latitude. An ULL (offshoot of PV) forms off the coast and oozes eastward as the system stacks, pulling the whole system eastward. Great position for us, but not great for places further northeast. Many of the EPS individuals gain more latitude and would be great up and down the coast. But a slide east either with a modest event or a complete miss are still very possible.

The 12z ECM is obviously great, but we gotta watch that eastward slide at the end. The relatively low snow totals in SNE are a small red flag. I'd prefer this to tuck into RI and stall then to slide east so quickly. We're good for now but if the eastward pull happens earlier we get the SNE modeled snow. Then again other guidance (e.g., UK, CMC) hammers SNE.

I've heard that. But I don't believe it's true. The GFS OP is run at a higher vertical and horizontal resolution and also uses the observed initial state and boundary conditions. The individual ensemble members are run at a lower resolution with perturbed (adjusted) initial conditions. If you move far enough out in time horizon such that the resolution and data advantage of the OP run is minimized, I suppose the accuracy of any single individual member might approach the accuracy of the OP run. I'm thinking probably out beyond day 10. But at closer ranges the superior resolution and more accurate initial time steps of the OP should make it superior.