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wxmeddler

Meteorologist
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Everything posted by wxmeddler

  1. Just saw the 12z GFS and came in to say that whenever you have 3 streams/waves interacting, the results are either explosive or disappointing. And 90% of the time, it's the latter. Stay full-hearted weenies. The overall pattern is good and we're entering peak season.
  2. Sure, you could have the low stack stall out just off the coast producing a longer duration storm. In my mind, we would need that southern stream s/w to not eject or get so strung out that it gets folded into the oncoming impulse from the dakota's but I'm not holding my breath on that. But... This is a triple phase setup, so things usually get messy.
  3. Yeah. We're not really setting ourselves up for tapping as much moisture as we could be for storms this time of year. The unusual part of this pattern is really the ridge over the PacNW. I don't recall seeing a 588dm high over Nor-Cal this time of year. We're just seeing the downstream effects of that which includes cold air intrusions coming straight south from Hudson Bay.
  4. Regarding the moisture issue: Yeah, that's not going away. The positive tilt of the trough at H7 and H85 ahead (1) of the synoptics getting in line for us is not great for folding the sub-tropical air back up into our area (2). The leading s/w that kicks out from the sub-tropical jet (3) is a kick in the pants.
  5. In a relative vorticity framework you get positive vorticity by either curvature (around a low) or by a positive change in wind speed to the right of the vector. Vort "lobes" tend to be produced by the curvature in, or in advance of a low, and the "ribbons" tend to be from areas of high wind shear across a horizontal distance. Look at an H5 wind map, then look at at an H5 Rel. Vort map, then flip them back and forth. You'll see it.
  6. Can't be upset with this at 5 days out. Not worth worrying about about the details (temps, banding, etc) now.
  7. Agreed. The tough issue with this potential that can't be changed is the approach of the pacific s/w. Normally, I like the "ribbon" coming through the Yellowstone region in a ESE direction. With the ridge so firmly anchored over Northern California, we're dealing with a wave diving out from the Dakotas to the SSE. But there's more than one way to bake a cake, and this seems to be one of them. Whatever works. lol
  8. The s/w coming through the Dakotas is slightly deeper, good sign
  9. I'm looking forward to the rain tomorrow.
  10. I plotted it out graphically. Ouch. N 125 Mean 21.4 Median 21.7 Std. Dev 4.1
  11. Assume no snow until overwhelming evidence proves otherwise is my mantra. 60 percent of the time... it works... every-time.
  12. Got a sudden and rude awakening by the WEA from my NYE stupor. My guess is that there are going to be many an upset person after that one. Thankfully it didn’t awaken the wife. Patiently awaiting the squall.
  13. Up-slope with diving mid-continent polar air masses are putting in the work. Pick the highest latitude / altitude combo.
  14. Sugar grain snow? Doesn't look like dendrites.
  15. The snow squall on Thursday pre-sunrise looks legit. Might have to set up an alarm for that one.
  16. It's not in Thurmont. The station is at Camp David which is at nearly the highest point in the Catoctins. https://www.weather.gov/wrh/timeseries?site=KRSP
  17. The front is fun. 10 deg drop in 8 min and a gust to 42 at Thurmont currently.
  18. Yes, the hodographs, as taken by themselves, are prime tornadic hodographs. However, the reason why they are like that is due to the surface inversion. If the surface inversion was mixed out then the 0-1 length would be shorter, but still capable of causing trouble.
  19. LWX is confident too much sfc stability, but I’m not so sure we don’t get some sort of dynamics that could break through. Won’t be widespread.
  20. I have a sneaking suspicion looking at satellite that places in N Baltimore and higher elevations of Harford co are plummeting right now.
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