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CAPE

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    NW of Greensboro, MD

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  1. The ring around the moon- its proven bigtime snow is on the way when you see that.
  2. Dumping snow ahead of the transition to sleet. Cool if that's real.
  3. No one checked the Spire Global Weather Basic? I hear its even more reliable than the Panasonic. Yeah baby!
  4. His record and accomplishments are comparable to Harbaughs- almost uncanny how similar. So if Harbaugh was a hot commodity immediately upon being fired, its kind of odd this guy has been available and teams haven't seem interested. Part of it is his persona i guess- just a bit boring. He is a very solid coach though. Look at the numbers- that's really all that matters.
  5. Snow melts efficiently here regardless, because most of the time we are above freezing a day or 2 after. If we get a 6" snowstorm in early March and temps are in the mid 20s with sun the next day, a good amount of it will still be otg.
  6. Workin on it, but just remember, if the storm is a coastal scraper I'm good with it. Also.. Why does this weekend 'hurt'? Gonna be the best storm you have seen in years. Get over the fact that it won't be all snow.
  7. The snow part depends on how hot and heavy it is at the beginning. We need it to come in and go moderate to heavy pretty quickly, and for the snow to last several hours. That's our chance to pick up 5 or 6" before the sleet takes over. As for freezing rain, it looks like there is a decent chance for you and I to pick up a quarter inch of ice, then maybe ending as plain rain with a temp of 33-34. Closer to the coast there will be a a longer duration of rain, and little to no zr.
  8. And that is largely a function of h5 shortwave interactions. As I have said- say it with me- all our hopes and dreams are determined by random wave interactions and timing.
  9. More phasing/amplification allows the primary low to track further north with a later transfer to the coast- and the developing coastal low is tucked. Earlier runs were less amped/ w flatter flow, a weaker primary with earlier transfer further south and the coastal low tracking ENE off the coast- this setup spares the area from too much warm air moving in aloft and at the surface in the vicinity of the coastal low. The warming is temporary as the colder air comes back in afterwards.
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