TeamPlayersBlue wrote:1044 MB High in the E Pac? Wow.
Ive been racking my brain on the atmosphere lately, trying to figure out what is making this high stay parked off the West coast this season. What is the mechanism for this and why? This is an example of la nina i understand, also with its clockwise motion around the high, it will increase upwelling in the equatorial region of the E Pac (La nina) but where does it start? MJO? /headsabouttoexplode
From what I know one of the biggest influences of pumping up that high is via an active MJO (7-8-1 range). Tropical forcing sends deep low pressures to the Aleutians which in turn pumps ridges ahead of it (amplifying them). Also I think the high is always there in winter but where it is, can be influenced by El nino/La Nina.
Everyone is picking on the GFS for not being right but in this case we are not looking at specifics. It has trended nonstop for 3 days now with an EPAC ridge. The ensembles both GFS and Euro support as well as the Canadian. What really got me into buying is lately the MJO forecast has been changing for the better, no good MJO = no good ridge but the trend has been giving credence over the days. So far this season the high hasn't gotten help from the MJO so it hasn't been able to tug itself into Alaska, yielding to the Alaskan Low. You don't look at specifics long range, but you can look at the 500mb and see how models are trending. And this is why
Portastorm has been worked up!

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ImageShack.usTo add the MJO forecasting has been rough this year, so it doesn't mean the forecast will verify, just looking at the trends. At least it is leaving the center circle of death (weak) and finally doing something.