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Stormchaserchuck1

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  1. July ECMWF run.. it has a warm bias but wow
  2. Science forum bro. I don't think a -EPO can't happen.. that's more possible than historical analog suggests, but +PNA has been really hard to come by in this peak decadal -PDO or whatever is going on.
  3. Finally! Let's see if it holds for more than a couple of days.
  4. ^I think it was you that made the good point that the S. Hemisphere Winter has high correlation, and a trough is usually dominant in El Nino's. We haven't seen that so far this year. An El Nino this strong should still show something vs recent climo imo.
  5. Hadley Cell contraction in July 1972, 1982, 1997. Not so much in 2015, 2023. We are still following closer analogs most closely
  6. Maybe a little bit of an extreme bias If we continue to see no Hadley Cell contraction that would really be something!
  7. That N. Pacific Low is in the perfect position for our historical analog snowstorms. And -NAO, just put a 50/50 low underneath like mitchnick said it would look really favorable. Unfortunately, seasonal models have a huge ENSO bias. We have not seen a North Pacific low for more than a few days since January, July will be the 6th month in a row of -PNA. Just not getting that pattern at all right now. In 2023 it was never occurring too, and seasonal models kept outputting the same default ENSO, which didn't verify.
  8. It would be nice to get a N. Pacific trough at all, for all the models showing this for the Winter
  9. I don't think a Winter -EPO El Nino is impossible. Further north it's more random than the mid-latitudes and the historical analog composite is probably biased to +epo (same with +ao and +nao of super Nino's). The warmth is definitely winning the battles in 2026 so far, however.
  10. El Nino who? ERA5 record highest 500mb height over the CONUS is 6027 gpm (21 Aug 2023)
  11. Northern Hemisphere pattern continues to disconnect from ENSO
  12. What's their all time high record low (anyone know?) Imagine if it was July 27!
  13. I don't think we've seen a North Pacific low anomaly for more than a couple days since the event began.
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