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Tulip Trouncer 5........The Comeback


Mr Torchey

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1.1" on the car top... Lawn whitened now in Ayer. trees turning cake white, too... Aggregate size has decreased - no longer any large "clumping", but individual hexagon plates are noted alone with smaller aggregate clusters. Plating with small stellular arms extending means it is cold aloft. This may earn me a hot dog but if you know your Meteorology, you can almost guess what the temperature is at 850 by whether you have needles/columns, plates, or true dendrites.

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Snowing good here. All non paved surfaces getting covered. Even the shady parts of my driveway are coated.

Final call:

MBY. 8.5"

ORH Will. 7.5"

KRAY. 5.0"

Dom. 11"

Sam. 12"

keV. 4"

Pete. 9.5"

Ginx. 3.5"

WeatherMA 4"

Scooter 1.5"

Dryslut 13.5"

Jayhawk 12"

Dendrite 14.7"

Gonna bust low me thinks.

1" on the grass so far, 33.1F, but not sticking on pavement so far. Hoping that starts soon...scooter.gif

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Scott sleet and snow much lighter.

Ruc kind of nailed this early band. Let's hope it's a little warm in error. 2.6 or 2.7....I expected zero. Cool stuff. Photos of flakes later some were enormous. I went out back to measure and it was the proverbial wall of snow falling.

I figured that was bright banding not s++.

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1.1" on the car top... Lawn whitened now in Ayer. trees turning cake white, too... Aggregate size has decreased - no longer any large "clumping", but individual hexagon plates are noted alone with smaller aggregate clusters. Plating with small stellular arms extending means it is cold aloft. This may earn me a hot dog but if you know your Meteorology, you can almost guess what the temperature is at 850 by whether you have needles/columns, plates, or true dendrites.

We had larger aggregates too when the heavier band came over, but flakes are smaller again now that its just back to moderate or high end light.

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That's obscene. I've never had to pay for a ticket at Stowe and at those prices I wouldn't. Not worth the price of admission. MRG at half that is unbeatable.

One of my students uses some Vermont value pass thing. He is addicted to VT skiing.

On a recent project he plastered it with Stowe and MRG logos

I show him Powderfreaks pics and he gets big eyed.

I still like my under $6 per visit WaWa deal. Wish it could go forever

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You should flip then as soon as that heavy band to the south moves north..maybe 20 mins? 31.8 and snow

Man this is where the hills really do matter. And its funny, these events seem to go "ok" for the coastal plain at low elevations, but they always blow goats in the larger, interior valleys. Growing up in the Hudson Valley like two towns over from Rick/Logan11, these spring events would always be rain/snow mix with 3" at 200ft, while there's 8-10" at 1,000ft blowing sideways off Rick's field. It was the same in the Champlain Valley... down at 200-300ft its a struggle the whole storm, while 1,000ft is ripping and sticking sideways to everything.

I'm not sure if the coastal plain is just closer to better dynamics, or if its that ENE wind causing some slight cooling from convergence as the wind hits land and gently sloping terrain... or if its the fact that the interior valleys need to downslope from somewhere regardless of what direction the wind comes from, and that slight downsloping component keeps things slightly more marginal than even a lower elevation on the coastal plain.

Either way, it sounds like the hills around the HFD-BDL area already have a 1"+ lead on the valley. That first inch is a biggie (what did she say?) because accumulations come easily on snow.

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Just grass/deck or is it sticking to pavement up there?

Its beginning to stick to the roads...but not in the middle...its at the stage where the sides of the road are getting accumulation but the middle is still mostly wet with maybe some transparent slush.

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Man this is where the hills really do matter. And its funny, these events seem to go "ok" for the coastal plain at low elevations, but they always blow goats in the larger, interior valleys. Growing up in the Hudson Valley like two towns over from Rick/Logan11, these spring events would always be rain/snow mix with 3" at 200ft, while there's 8-10" at 1,000ft blowing sideways off Rick's field. It was the same in the Champlain Valley... down at 200-300ft its a struggle the whole storm, while 1,000ft is ripping and sticking sideways to everything.

I'm not sure if the coastal plain is just closer to better dynamics, or if its that ENE wind causing some slight cooling from convergence as the wind hits land and gently sloping terrain... or if its the fact that the interior valleys need to downslope from somewhere regardless of what direction the wind comes from, and that slight downsloping component keeps things slightly more marginal than even a lower elevation on the coastal plain.

Either way, it sounds like the hills around the HFD-BDL area already have a 1"+ lead on the valley. That first inch is a biggie (what did she say?) because accumulations come easily on snow.

Not really. The hills west of here have virtually no accumulation. The precip just hasn't been that heavy here. We've only picked up a couple hundreths. Areas on the east side of the valley do have a jump start not so much because of elevation but because of heavier precip rates.

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Man this is where the hills really do matter. And its funny, these events seem to go "ok" for the coastal plain at low elevations, but they always blow goats in the larger, interior valleys. Growing up in the Hudson Valley like two towns over from Rick/Logan11, these spring events would always be rain/snow mix with 3" at 200ft, while there's 8-10" at 1,000ft blowing sideways off Rick's field. It was the same in the Champlain Valley... down at 200-300ft its a struggle the whole storm, while 1,000ft is ripping and sticking sideways to everything.

I'm not sure if the coastal plain is just closer to better dynamics, or if its that ENE wind causing some slight cooling from convergence as the wind hits land and gently sloping terrain... or if its the fact that the interior valleys need to downslope from somewhere regardless of what direction the wind comes from, and that slight downsloping component keeps things slightly more marginal than even a lower elevation on the coastal plain.

Either way, it sounds like the hills around the HFD-BDL area already have a 1"+ lead on the valley. That first inch is a biggie (what did she say?) because accumulations come easily on snow.

Absolutely true and this is why I usually do well, despite having 111' of elevation...there are no hills around me.

The rule is if you aren't IN the hills, then you want them nowhere near you.

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That's obscene. I've never had to pay for a ticket at Stowe and at those prices I wouldn't. Not worth the price of admission. MRG at half that is unbeatable.

Hey ya don't have to tell me twice, lol. I can never blame people for not wanting to pay that. They give me a pass and pay me to ski, haha, so I consider that a win. But the more mind-boggling thing is that during holiday periods and kids vacation periods, that place is packed to capacity. Literally filled parking lots, annoying lift lines (not as bad as Killington or S.VT), and just a lot of people (busy day is 9,000-10,000 people) everywhere. All at $84 lift tickets. That's a lot of revenue. And during vacation periods, supply and demand says ticket prices should be higher!

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