Jump to content

weatherwiz

Meteorologist
  • Posts

    81,170
  • Joined

  • Last visited

2 Followers

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, ?

Recent Profile Visitors

40,518 profile views
  1. To our west but also within CT along the warm front during the afternoon with potential for supercells/isolated tornado risk. Then a line moving through during the evening with localized wind damage threat
  2. An unseasonably strong shortwave trough amplifies as it swings across the Great Lakes region on Saturday as it advances towards the Northeast Saturday evening/overnight. As it does so, a cold front will push across the Great Lakes region during the day with a warm front lifting across the Northeast during the day on Saturday ushering in a warmer and more moist low-level airmass. Ahead of the trough features 40-45 knots of westerly mid-level flow with 30-40 knots of southwesterly flow in the lower-levels of the atmosphere which will contribute to 30-40+ knots of bulk shear, sufficient for storm organization. With the warm front approaching and a relatively uncapped airmass, extensive cloud cover along with scattered showers and thunderstorms are expected throughout the day and this does raise concerns about how much surface heating can occur and how much instability can build. Secondly, the timing of the rain and thunderstorms associated with a pre-frontal trough will be during the early evening, after peak heating. While instability would be a concern moving out of peak heating, as the warm front continues lifting through the region, the advection of higher theta-e air should help maintain what instability we have in place or even boost instability values a bit. CAMS are rather bullish in developing multiple rounds of thunderstorms across NY and PA with potential for multiple and concentrated swaths of damaging wind gusts and even potential for a few tornadoes given high helicity values. CAMS weaken this activity as it propagates across New England during the evening, however, given strong dynamics, increasing height falls, and at least weak instability (MLCAPE ~1000 JKG), localized damaging wind gusts and perhaps even an embedded tornado would remain possible as this activity crosses the region. As usual, the best potential for damaging winds or a tornado would be western sections. If instability turns out greater than forecast, there would be potential for a greater damaging wind threat across western MA and western CT.
  3. Should be. Overall best severe threat will be off to the west but should still see some localized wind threat across the region during the evening.
  4. Certainly may be a brief window for something to become a bit organized before shear increases some
  5. Understanding smokes impact on convective potential is extremely complicated. If you're talking about convective potential which is extremely dependent on instability, then smoke is going to have a large negative impact on convective potential because its going to inhibit the convective temperature from being reached and of course lead to a reduction in instability. If you have a setup though in which forcing and dynamics are strong and you don't have to rely on large CAPE, smoke is probably not going to inhibit convection from developing (but of course may negatively impact strength). In the case of what happened across western Maine the other day, you already had capping in place from a stout EML so the dense smoke further enhanced capping and of course prevented convective temperature from being reached. Forcing for any afternoon storm development was always weak, which also increased tornado potential. So adding smoke into things just add another level of complexity but the impact of smoke on potential is going to vary based on the mechanisms involved in convective development.
  6. Nastiness moving through tomorrow night. Probably some violence western areas
  7. Pretty crazy how this happens. There is research too about damage paths in the South contributing to local enhancement of thunderstorm activity because of the temperature gradient which becomes established between the vegetation and the damage path. I think even some research with burn scars in the West with rain/storms
  8. but is that a snap shot from a general pattern or is that a pattern post front? If the formal, then yeah I would tend to agree.
  9. that looks probably isn't terrible for severe wx potential...would probably mean strong fronts moving through with good shear...probably not good for EML potential
  10. No EMLs but outside of Saturday night, Tuesday looks decent too for storms. Good shortwave and shear...just have to see how timing works out and what instability is like
×
×
  • Create New...