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Everything posted by RitualOfTheTrout
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Yeah... This winter is a total disaster dumpster fire. I know you're just kidding, so am I. If we bust on these next 2 storms hard to be bitter over it given totals to date even if we don't see another flake til next season. I don't think this shifts much more one way or another now. I'd guess 50-75 miles, if it's all further NW we see more sleet and rain then dry slot, the other way and its more snow, I think either option is still within the model error at this time.
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Yeah this is my thought too, nobody should jump off the ledge over the NAM the same way you shouldn't be dropping the "It's Happening Meme" when it bullseye's you. Now if other 00z guidance follows then backs it up at 12z tomorrow that's when I'll start to be concerned. Need to see at least 2-3 runs to establish a trend vs a wobble one way or the other.
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I won't feel good till I see 35dbz radar returns over my house Monday night lol. No, but really all the guidance has the storm and show a narrowing goal post, so I'm starting to have confidence but models have relatively dramatic changes over shorter leads than we are used to due to handling of the PV etc. thus far this season.
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I agree, it has the same general idea / track the GFS had. Also, PARA GFS looks pretty similar to the OP. Given how quick the storm is moving though and the threat of sleet / mix I think it's going to be tough to get 10-12 inches even in a perfect track scenario, but plenty of time to see how it plays out.
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I'm sure I'm going to oversimply or partially misstate something here, but an area of high pressure in and of itself will not necessarily "block" a storm from cutting into it. Now if it's strong enough and has a solid depth of cold air with it that will offer some resistance and will help to funnel cold air down into the storm possibly extending the amount of time an area stays frozen. The other thing to look at is how blocked the flow is, if you have a ball of low pressure stuck under a block at the 50/50 Longitude / Latitude (What some refer to as a 50/50 Low) that also helps slow the flow down so a high will have more staying power. The other than that really matters though is to look at 500, to block a storm from cutting you want confluence and you want the trough to not go negative to far to the West. So in the 500mb map below, the green circle you can see a piece of energy swinging by pushing the height lines in a more West to East (Compressing the flow between that and the ridge in the SE), that would imply once a storm gets to that point it's going to feel pressure to either move in a more Easterly direction or jump to the coast. The area circled in blue is the trough orientation, in this example its positive (height lines lean towards the right) This is indicative of a more progressive system still at that point and it would be less likely to cut and pump heights and subsequently flood us with warm air. As those lines become more straight up and down with a deepening storm, that's referred to neutral, and if they band to the left negative tilted trough. Also, pay attention to the colors, dark red would indicate there is a lot of energy in the trough, then do comparisons to previous runs to see if as we get closer in time there is more or less energy to discern a trend. In a simplified way, just imagine those lines as like a roadway or path of least resistance, and that is the track a storm will want to take. Looking at this level of the atmosphere its really interesting and obvious how other down / upstream features will effect the track of a storm.
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18z uses the 6 hour forecast from the 12z run as the initial data point, likewise 6z uses 00z 6 hour forecast for it's initialization where as 12z / 00z use fresh data from observations for the initialization. I thought though that the off hour runs get some new data, but I can't say for sure as it's been awhile since I looked into this and things may have changed.
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It's a message board for discussing weather, I never understood why people get so emotional over snow maps being posted. Use at your own risk, but they are like the cliff notes if I don't have time to look into things closer. Most should know they aren't to be trusted verbatim. Plus who doesn't like seeing that bright pink over your house?
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Looks like this one is wrapping up. One band to the north that should pivot South overnight but I think the bulk of our accumulating snow is about done for the city and north. Saturday keeps trending East with one low and the northern energy looks to barely hit us. Hopefully another 1-2 type deal at least but will have to see how it look once in the short range.
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LaNina typically favors cold out west / central US due to tropical forcing that favors SE Ridge. The models want to push it East but as we get closer the effects of the ridge are better resolved. By all rights a Nina Feb is usually warm, but we have the extreme blocking and piece of the PV squishing the ridge keeping us in the game.
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That's been the theme this winter though, more NS interaction, only to see less as we near in time.That said can't dismiss out of hand GFS depiction, but I'd hedge towards some sort of compromise between GFS / CMC solutions following the seasonal trend until proven otherwise. Agree with analyzing thermals at this juncture, if you do it's for pure entertainment purposes. The Euro depicting zr with temperatures in the low to mid 20s is not something we see around these parts very often so I thought it was interesting to point out.
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The Monday night into Tuesday storm Euro is showing about .7 qpf, but it all falls with 2m temperature between 17-26 degrees. Verbatim it would be snow to sleet to freezing rain, and it would be legit freezing rain at those temperatures especially when you consider the ground will already be well below freezing with snow cover and its happening very early morning. I'm not a big ice storm fan, but if your going to do it.. do it right lol
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It will depend on which layers of the atmosphere go above freezing. Models won't have a good handle on this until short range. This graphic helps visualize it: So even if the 2M temperature is 17 you could still see sleet or freezing rain if there is a warm nose somewhere in the column. A lot goes into this though, say you have a high to the north funneling in low dew point air, during heavy precipitation maybe you can wet bulb the column to 0 and get all snow, then during lulls you get drizzle / sleet. There are a lot of variables that go into figuring out p-type and snow ratios. You can't just say it's 20 degrees so ratios will be 15:1 (Not saying this is what you were implying just pointing it out.)