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Pattern looks improved for possible KU event 2/18-2/25 time range


Mikehobbyst

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A track maybe 50-100 miles east of the 12z GFS track would be awesome for everyone. I definitely agree there's a threat, but so much to be worked out that it's impossible to get excited yet. I would certainly like the confluence in SE Canada to hold steady, otherwise this cuts west.

Agreed. Luckily we're still in the "correcting" stage, while will likely continue through Friday. The GGEM being offshore suggests the out to sea solution is still a possibility. The UKIE being more amped up suggests to me that the Euro will probably be more amped than its 00z run as well.

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If we had some arctic or even polar air to work with, more of the storm would be snow on the 12z GFS. But b/c we're dealing with such a marginal airmass, the coast waits until the sfc low falls sub 990mb to start changing to snow. Normally in February you can get accum snow out of a relatively weak low, but this is akin to a late March type set up.

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The GFS still has almost 1" of liquid that falls as frozen QPF for the suburbs of NYC per the stormvista maps. Around 0.8" for the city itself.

Some areas of Northern NJ receive almost 1.3" liquid as frozen QPF.

BUFKIT doesn't seem to agree (shows 0.4" as snow for Morristown after receiving hour after hour of rain/sleet mix.

The actual 2m temp isn't that warm (mid 30s) but the 0C isotherm is up at 950mb for most of the storm for the northern half of NJ.

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We shouldn't be concerned about the rain/snow line this far out in my opinion. I'm just happy to see some more amped up solutions.

yes we should. there is almost no wiggle room for the city in this setup... no blocking, no confluence, fast flow, no source of cold air, low pressure over the great lakes

the negatives outweigh the positives

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Im not goin to entertain a rain - snow line out 4 days out , I am way more excited that the surface feature looks like it wants to repsond to the upper air pattern - we just watched a storm meander 200 miles east this past wknd from its prog 24 to 36 hr ealrier .

The models have plenty of wiggle room to figure outthe true trough axis .

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yes we should. there is almost no wiggle room for the city in this setup... no blocking, no confluence, fast flow, no source of cold air, low pressure over the great lakes

the negatives outweigh the positives

I guess my point is that I don't think it will be this close to the coast in the end. A track a bit offshore and we are all good.

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yes we should. there is almost no wiggle room for the city in this setup... no blocking, no confluence, fast flow, no source of cold air, low pressure over the great lakes

the negatives outweigh the positives

For the most part, this is true, but I do think there is some degree of confluence - look at the jet streak in northern New England. The 50/50 low, albeit weak, is doing something.

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I guess my point is that I don't think it will be this close to the coast in the end. A track a bit offshore and we are all good.

the factors i mentioned are allowing the storm to come west. there is almost nothing to stop the storm from coming west (assuming it phases and amplifies)

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the factors i mentioned are allowing the storm to come west. there is almost nothing to stop the storm from coming west (assuming it phases and amplifies)

Yes there is...there is a collapsing ridge out west which is going to stop the amplitude of the entire pattern to the east as it bulges east. The flow over Canada is pretty fast too so I highly doubt this storm is going to amplify enough to cut inland.

The problem we might have is that the northern stream isn't dropping far enough south. Last nights 00z GFS had a piece of the northern stream swing south and underneath our area. Today it remains over the Great Lakes which gives us a warmer boundary layer flow even initially.

Once the phase occurs over New England the cold air becomes entrained in the storm system.

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Yes there is...there is a collapsing ridge out west which is going to stop the amplitude of the entire pattern to the east as it bulges east. The flow over Canada is pretty fast too so I highly doubt this storm is going to amplify enough to cut inland.

The problem we might have is that the northern stream isn't dropping far enough south. Last nights 00z GFS had a piece of the northern stream swing south and underneath our area. Today it remains over the Great Lakes which gives us a warmer boundary layer flow even initially.

Once the phase occurs over New England the cold air becomes entrained in the storm system.

There is a 150 knot jet streak running west to east in northern New England - that's a very fast flow and makes me believe that the OP GFS is as far west as this thing can go.

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Yes there is...there is a collapsing ridge out west which is going to stop the amplitude of the entire pattern to the east as it bulges east. The flow over Canada is pretty fast too so I highly doubt this storm is going to amplify enough to cut inland.

The problem we might have is that the northern stream isn't dropping far enough south. Last nights 00z GFS had a piece of the northern stream swing south and underneath our area. Today it remains over the Great Lakes which gives us a warmer boundary layer flow even initially.

Once the phase occurs over New England the cold air becomes entrained in the storm system.

100 perc agree - We ve been watching a progressive pattern here for the last 2 months .

The models continue to advertise energy getting to the west coast at this time . the response downstream will set up your resistance or lack there of .

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