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weatherwiz

Meteorologist
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About weatherwiz

  • Birthday 10/28/1988

Profile Information

  • Four Letter Airport Code For Weather Obs (Such as KDCA)
    KBDL
  • Gender
    Male
  • Location:
    northeast Springfield (near Wilbraham line)
  • Interests
    Weather, sports, ?

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  1. Yeah I don't know what else to say. I mean December was not bad overall and it could have been worse. Sure I guess we could have had more snow given how cold it was and yes some areas got more than others, but it wasn't a shutout and nobody got shutout. Were people expecting 20-30"? We get snow...people complain because it wasn't enough, we don't get snow and people complain. People want snow and there are offerings of potential and people complain. I don't even know what the expectations are anymore lol
  2. It's definitely an extremely intriguing look and what I like about it is this type of pattern opens the door for some southern stream involvement and that would at least offer some potential for a bigger storm. But why I also love the Jan 10-15 period is we may see a relaxing NAO during that period, or the NAO becoming less negative and at the same time we're seeing variations within the state of the PNA. The pattern will not be void of energy and storm chances. If we want to add another layer to this is we will have the PV displaced on our side of the hemisphere.
  3. The overall look isn't terrible, in fact, it's probably better to see than these "great looking patterns" that haven't seemed to materialize the last few winters. There will be multiple storm chances over the next 2-3 weeks, probably on the order of one system every 6-9 days.
  4. I am pretty intrigued in the period of Jan 10-15. But we have a light snow event tomorrow, probably another one in a week, then there could be some room for a bigger storm moving towards mid-month.
  5. This isn't a terrible looking sounding on the Cape. Def unstable in the lowest 3km But can anyone say Martha's vineyard jackpot?
  6. Yup...great post. The environment isn't too terribly far off from what you would see with a LES environment. Should actually be some weak instability present...not sure if we're looking at enough to yield thunder potential but I could see a very narrow area of enhanced lift. Someone could def pull off 3-4" on the Cape
  7. Hey I'm with you...I have no doubt we will cone out of it and we will get smoked again. I get there is a luck factor in this and there are things we don't truly know or understand, but all we can do is try to use data and knowledge to further understand. At this point we are closer to getting out of this and I can't see us staying in this drought for much longer. It's more of a theory at this point so I don't have a ton of data or reanalysis maps I can throw into this...but would be a fun project to dig deeper. Anyways, we have to look at the jet stream on a global scale and all the influences which shape the jet stream structure, position, and strength. As you know, when the jet stream is faster, it becomes more difficult to really amplify the jet stream (not impossible but just more difficult). I just think that where we are positioned globally, we are in a spot in which the faster winds result in an increased probability for amplification to our west and then just to our east. Where I've started to develop this idea was based on some of the weather across the West the last few years. Remember a few years back the West was getting absolutely pummeled for a 6 week stretch which was something more akin to what you would see in EL Nino versus La Nina. The orientation and structure of the jet stream was not what you would typically see. This is all a ramble...but I will eventually get back to you with more coherent thoughts.
  8. It's not like it's just applicable to our area though, the concept would apply to other areas of the globe too. For us it's just a product of where we reside regionally.
  9. correct, and the faster (or slower) flows aloft play a significant role in where ridge/trough axes occur.
  10. Actually that would be incorrect. Fast flow doesn't necessarily inhibit storms from bombing out nor does changes in the size and structure of the Hadley Cell. They just influence the jet stream differently and shift around regions which are favorable for deep cyclogenesis. A faster flow makes it more likely for storms to bomb out farther to our west versus towards the coast and then for storms to bomb out as they move just off the coast towards Atlantic Canada.
  11. What a quiet year and really stretch we have been in for the severe weather department. Although I did get that gustnado back in April which was cool. That September 6 event was pretty crazy though
  12. I think the storm knocked out my internet. Been out for 3 hours. How am I supposed to watch hockey tonight???
  13. The observer must still be salty about the Bills going for 2 and not paying attention
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