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12/26-12/28 Potential Snow Threat


CooL

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Once again...not all of us live in Brooklyn. It's not over for Putnam/Orange/Rockland counties.

Don't forget Westchester.

I agree with Anthony that this threat is done for the City proper. Too much BL warming on southerly winds ahead of the primary, and 850s are marginal anyway. For the majority of posters on the board who live in NYC proper or in the suburbs immediately east/west of the City, you're not going to see anything from this system. Those of us who have some elevation in Westchester, Rockland, Putnam, Orange etc could still see snow.

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I'm somewhat surprised that most are writing this off given it's still at 84 hrs. We've seen significant changes up through 24-48 hrs before. Is it going to be a big snow for the coast? No, probably not. But I certainly wouldn't go calling off any snow at this time frame.

Absolutely, could not agree more. As it is, the Euro is currently showing the rain/ice/snow line only about 50 miles north of New York City, nearly 4 days away. As is, it might produce a few inches of snow in most of the north and west suburbs according to the Euro and possibly the JMA and the UKMET, and the GFS is not that far behind really. We still have more than 3 days and only 50 miles to go to make the difference between a big rainstorm and a really big snowstorm.

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Absolutely, could not agree more. As it is, the Euro is currently showing the rain/ice/snow line only about 50 miles north of New York City, nearly 4 days away. As is, it might produce a few inches of snow in most of the north and west suburbs according to the Euro and possibly the JMA and the UKMET, and the GFS is not that far behind really. We still have more than 3 days and only 50 miles to go to make the difference between a big rainstorm and a really big snowstorm.

I know it's the NAM at 84 hours. But shows frozen percip north and west of the city for at leadt several hours. Looks like ice really, but something to keep an eye on.

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Is anyone looking into the wind potential with this? I'm not an expert with forecasting wind gust potential although the NAM and GFS have a moderate LLJ with 925mb winds up to 60-70 knots along with the heavy rain:

post-1753-0-40932600-1356297741_thumb.pn

As long as the low level lapse rates are unstable (>7K/km) there will be no problem mixing down gusts close to 50.

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The 18z GEFS is a good 100 miles southeast of the operational run. Still not good enough for us, but it is closer. At 84 hrs the operational run has the low centered near State College, while the GEFS has the low centered near Philly. At 90 hrs. the operational run has the low centered near Binghamton, while the GEFS has the low centered near NYC.

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I was just looking at the NOGAPS and the Canadian in high resolution on the Wright-Weather website. I mean you almost forget about these models because they are simply not very good, but we are getting close enough in now that they are useful for something, especially when they seem so close to the JMA and the UKMET. BOTH the NOGAPS and the Canadian have what appears to be a very significant snowstorm for Northern, especially Northwest New Jersey on the 12z run. The JMA and UKMET we have to king of guess at because of the 24 hour intervals, but it is possible that they could also be a snowstorm just northwest of NYC from the looks of it. The UKMET and the JMA tracks seem to be very similar to the Canadian and the NOGAPS at 12z which definitely show a big time snowstorm just northwest of NYC. Is it possible that the Euro and the GFS are too far NW. I mean the UKMET is definitely not a bad model and the JMA is not horrible either. I was actually shocked at how both the Canadian and the NOGAPS had very similar solutions and honestly the UKMET and JMA look very similar as far as I can tell with the 24 hour time steps. This might get interesting for areas just northwest of NYC.

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The 18z NAM is close too. Northwest jersey stays frozen for at least 6 hours.

The models do not generally pick up on front end snows well here beyond 72 hours or so outside of cases with very strong cold air masses in place. I don't think there is any way NYC/LI/coastal CT see front end snows with the setup RIGHT NOW on most models but certainly HPN/POU/FWN/DXR/ would be prone in this setup.

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With the holiday I am off work and I have spent quite a bit of time analyzing things today. As of right now, it appears to me that the UKMET, the JMA, the Canadian, and the NOGAPS produce a significant if not major snowstorm for Northwest New Jersey as of the 12z runs. The NOGAPS just came in even about 25 miles further southeast than the 12z run, so it is even colder still. The GFS is pretty clearly the odd model out with its solution of the low sitting over State College and is therefore WAY too warm. The Euro is somewhere in between, producing 3-6 inches of snow in Northwest New Jersey on the 12z run. The Canadian and NOGAPS were nearly all snow for this storm in Northwest New Jersey, which I only realized after looking at them on Wright-Weather's high resolution website. On the other websites the Canadian looked like it would be too warm with the low further north, but in high resolution you can see that the low is centered more near Atlantic City on the 12z Canadian, as it is with the 12z and 18z NOGAPS. The UKMET also places the low near Atlantic City, so I can only assume this would also lead to a snowy solution in Northwest New Jersey. It appears that the JMA would have the same solution, but the 24 hr time steps make it difficult to see, but it definitely looks that way to me. So we have model number 1 (Euro) with 3-6 inches in Northwest New Jersey currently and 50 miles away from being all snow in our area, model number 2 (UKMET) highly likely showing a snowy solution in our area, model number 3 (GFS) out in la la land, and models number 4, 5, and 6 all showing a very snowy solution. Let's see where my hard work today takes us.

post-1914-0-84932900-1356308616_thumb.pn

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With the holiday I am off work and I have spent quite a bit of time analyzing things today. As of right now, it appears to me that the UKMET, the JMA, the Canadian, and the NOGAPS produce a significant if not major snowstorm for Northwest New Jersey as of the 12z runs. The NOGAPS just came in even about 25 miles further southeast than the 12z run, so it is even colder still. The GFS is pretty clearly the odd model out with its solution of the low sitting over State College and is therefore WAY too warm. The Euro is somewhere in between, producing 3-6 inches of snow in Northwest New Jersey on the 12z run. The Canadian and NOGAPS were nearly all snow for this storm in Northwest New Jersey, which I only realized after looking at them on Wright-Weather's high resolution website. On the other websites the Canadian looked like it would be too warm with the low further north, but in high resolution you can see that the low is centered more near Atlantic City on the 12z Canadian, as it is with the 12z and 18z NOGAPS. The UKMET also places the low near Atlantic City, so I can only assume this would also lead to a snowy solution in Northwest New Jersey. It appears that the JMA would have the same solution, but the 24 hr time steps make it difficult to see, but it definitely looks that way to me. So we have model number 1 (Euro) with 3-6 inches in Northwest New Jersey currently and 50 miles away from being all snow in our area, model number 2 (UKMET) highly likely showing a snowy solution in our area, model number 3 (GFS) out in la la land, and models number 4, 5, and 6 all showing a very snowy solution. Let's see where my hard work today takes us.

They added the J MA to the graphic LOL.

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With the holiday I am off work and I have spent quite a bit of time analyzing things today. As of right now, it appears to me that the UKMET, the JMA, the Canadian, and the NOGAPS produce a significant if not major snowstorm for Northwest New Jersey as of the 12z runs. The NOGAPS just came in even about 25 miles further southeast than the 12z run, so it is even colder still. The GFS is pretty clearly the odd model out with its solution of the low sitting over State College and is therefore WAY too warm. The Euro is somewhere in between, producing 3-6 inches of snow in Northwest New Jersey on the 12z run. The Canadian and NOGAPS were nearly all snow for this storm in Northwest New Jersey, which I only realized after looking at them on Wright-Weather's high resolution website. On the other websites the Canadian looked like it would be too warm with the low further north, but in high resolution you can see that the low is centered more near Atlantic City on the 12z Canadian, as it is with the 12z and 18z NOGAPS. The UKMET also places the low near Atlantic City, so I can only assume this would also lead to a snowy solution in Northwest New Jersey. It appears that the JMA would have the same solution, but the 24 hr time steps make it difficult to see, but it definitely looks that way to me. So we have model number 1 (Euro) with 3-6 inches in Northwest New Jersey currently and 50 miles away from being all snow in our area, model number 2 (UKMET) highly likely showing a snowy solution in our area, model number 3 (GFS) out in la la land, and models number 4, 5, and 6 all showing a very snowy solution. Let's see where my hard work today takes us.

It's true some of today's modeling was pretty snowy for far NW NJ. But with some models showing a strong warm layer above 850mb, and some showing warmth under 850, there could be a lot of sleet (or even ZR) with all of those solutions. I would hedge towards mixing unless and until the SLP gets east of a particular location.

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The H5 low treks essentially E/ENE upon reaching Ohio's latitude. What a difference in H5 evolution from the 18z run, and as I said before, I doubt changes are finished.

The potential track as progged reminds me of the Feb 14 2007 event, with a primary up to OH, secondary transfer which hugged the coast, and a pretty strong sfc high in sern Canada. The resultant weather was a widespread snowstorm for the interior Northeast and a lot of sleet/ice down to the coast. Not saying it'll be similar, just an observation as a potential track/synoptic analog.

Courtesy of Ray's site

358q71h.jpg

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The H5 low treks essentially E/ENE upon reaching Ohio's latitude. What a difference in H5 evolution from the 18z run, and as I said before, I doubt changes are finished.

The potential track as progged reminds me of the Feb 14 2007 event, with a primary up to OH, secondary transfer which hugged the coast, and a pretty strong sfc high in sern Canada. The resultant weather was a widespread snowstorm for the interior Northeast and a lot of sleet/ice down to the coast. Not saying it'll be similar, just an observation as a potential track/synoptic analog.

Courtesy of Ray's site

358q71h.jpg

Looking at the re-analysis on ewall its amazing that event stayed all frozen, it basically showed the same screaming SE flow this one does.

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Looking at the re-analysis on ewall its amazing that event stayed all frozen, it basically showed the same screaming SE flow this one does.

If I remember correctly, my forecast called for mostly rain/changeover to rain the night of the 13th, but I knew something was up when my winds remained NELY and surface temps flat-lined in the mid/upper 20s. What followed was an impressive ice/sleet event for my county. Problem this time around is I think the surface temperatures aren't as cold to start with, so it would be warmer given the GFS verbatim, and generally rain for the coast.

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Looking at the re-analysis on ewall its amazing that event stayed all frozen, it basically showed the same screaming SE flow this one does.

That was the storm the nam was off by 10 degrees. One big difference. That storm ran into a cold dome of air. If I remember right it was in the upper 20s the whole time. Ths time we start at 40

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