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Stuffing and Snow - Late November Banter and Obs


HoarfrostHubb

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Nice looking cold shot next weekend.

Very transient look for now though as it sweeps seaward quick with ridging coming in on the backside right away.

Just my opinion but feel like we have a ways to go yet before we truly settle in to a consistently cold pattern...2-3 weeks from now or so?

I think this pattern may be good for the interior, but I'm still thinking more into the 1st week of December in general for many. There are still some things I don't like and if you look at the GEFS...they are all over the place. That might be "muting" the cold shots which I agree with....but also indicate not every storm may be white. However, if we can keep that thumb look of ridging into Greenland or Davis Straits, that wil greatly help out.

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I think this pattern may be good for the interior, but I'm still thinking more into the 1st week of December in general for many. There are still some things I don't like and if you look at the GEFS...they are all over the place. That might be "muting" the cold shots which I agree with....but also indicate not every storm may be white. However, if we can keep that thumb look of ridging into Greenland or Davis Straits, that wil greatly help out.

GFS ensembels keep the favorable pattern relatively temporary. I'm not sure if that verifies but something to think about it. In the other thread you mentioned the 50mb polar vortex anomalies. Why is it important that the wave breaking reaches up there when it's above the trop? Is it because the lower stratospheric circulation will reassert itself after the Wave 2 forcing decreases?

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I think this pattern may be good for the interior, but I'm still thinking more into the 1st week of December in general for many. There are still some things I don't like and if you look at the GEFS...they are all over the place. That might be "muting" the cold shots which I agree with....but also indicate not every storm may be white. However, if we can keep that thumb look of ridging into Greenland or Davis Straits, that wil greatly help out.

Yeah I could see the interior and/or NNE having some wintry weather. Sort of climo favored areas anyhow.

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Kinda surprising to be -2.7 for the month of November and only have a trace to show for it. At least there's some chances the last week of November to throw some measurable on the board.

I know you know but it's been a funky way to run low departures. This airmass thats been stuck here this week for example is not "cold" in the traditional sense.

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GFS ensembels keep the favorable pattern relatively temporary. I'm not sure if that verifies but something to think about it. In the other thread you mentioned the 50mb polar vortex anomalies. Why is it important that the wave breaking reaches up there when it's above the trop? Is it because the lower stratospheric circulation will reassert itself after the Wave 2 forcing decreases?

Well the whole topic is about the stratospheric vortex. Around the vortex you have the polar night jet which develops from relative warm lower stratospheric air to the south as compared to the very cold lower stratosphere air near the pole. The whole idea is for this wave breaking to add warmth, ozone, and potentially less westerly momentum to this vortex. If you warm the vortex, you lose the temp gradient causing the strong polar night jet. In some stronger cases, the winds could reverse because now the air near the poles at this level is warmer than the lower stratospheric air to the south. Even though we have the tropopause separating the troposphere from the stratosphere, there is some exchange within these levels simply because they are so close to each other. So the idea of a strong lower stratosphere vortex tied to a stronger vortex in the upper troposphere seems to be valid. Same with a warming vortex creating that top down method of warming and then raising heights in the upper reaches of the troposphere. HM was saying that the circulation still appears to be strong when you move higher up in the stratosphere and that is a potential issue if this wave 2 does not significantly disrupt the vortex. It may build back down. I do see what he means in my limited knowledge.

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Well the whole topic is about the stratospheric vortex. Around the vortex you have the polar night jet which develops from relative warm lower stratospheric air to the south as compared to the very cold lower stratosphere air near the pole. The whole idea is for this wave breaking to add warmth, ozone, and potentially less westerly momentum to this vortex. If you warm the vortex, you lose the temp gradient causing the strong polar night jet. In some stronger cases, the winds could reverse because now the air near the poles at this level is warmer than the lower stratospheric air to the south. Even though we have the tropopause separating the troposphere from the stratosphere, there is some exchange within these levels simply because they are so close to each other. So the idea of a strong lower stratosphere vortex tied to a stronger vortex in the upper troposphere seems to be valid. Same with a warming vortex creating that top down method of warming and then raising heights in the upper reaches of the troposphere. HM was saying that the circulation still appears to be strong when you move higher up in the stratosphere and that is a potential issue if this wave 2 does not significantly disrupt the vortex. It may build back down. I do see what he means in my limited knowledge.

okay...that's kind of what I was thinking, cool.

It definitely disrupts the vortex into the upper levels of the trop/lower stratosphere but it appears above 70/50mb is still left in tact.

At least from the EC model forecasts.

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Yeah it's this rotting airmass with colder NNE winds and limited mixing. The airmass aloft is not cold at all.

Yeah... the inversion has been impressive. The summits have all been between like 28-36F consistently this week, while down in the mountain valleys we are hitting the teens nightly with freezing fog and light rime at times.

To have 4,000ft hitting highs in the mid 30s, usually means 50F+ down below 1,000ft with standard 5F/1000ft or 15F/3000ft afternoon lapse rate.

If one just looks at H85 temps, you would think all of New England below 1,000ft should be maxing in the 50s, not 40-45F.

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Yeah... the inversion has been impressive. The summits have all been between like 28-36F consistently this week, while down in the mountain valleys we are hitting the teens nightly with freezing fog and light rime at times.

To have 4,000ft hitting highs in the mid 30s, usually means 50F+ down below 1,000ft with standard 5F/1000ft or 15F/3000ft afternoon lapse rate.

If one just looks at H85 temps, you would think all of New England below 1,000ft should be maxing in the 50s, not 40-45F.

Yeah which is why people saying the cold is "overperforming" are not exactly correct. If we had west winds with this airmass we'd all be playing hackysack, but nobody wants to hear that....they only care about cold.

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