Looks like a 'switch-flip' coming up mid-next week as AAM tendency heads sharply negative for a time but set against a high starting AAM anomaly; this is GWO stage 7-8 and corresponds to sluggish N. Atlantic westerlies but low heights to the W of the UK maintaining far enough north to prevent the resulting blocking high locating NW of the UK. A key difference to the typical Jan-Mar response, and something GFS took until today to fully adapt for.
Blocking NE or E of the UK with troughs out west struggling to make inroads, just doing enough from time to time to destabilise conditions with showers or thunderstorms the main source of rainfall in the UK (especially England).
That's the typical weak El Nino 'base state' from mid-late April to early-mid July. If it weren't for the complications that tend to arise, we'd be able to predict a warmer but not necessarily drier than average summer with good confidence for 2019.
From the evolution of that pattern, the latest two GFS runs give me final CET estimates of 8.9*C and 9.4*C, the former (06z) held back by a few more chilly nights (mins 2-5*C widely) managing to take place even as the warmer air established aloft.
Thinking longer-term again, I'll be really interested in how much we see the Azores High link up with the Scandinavian High this summer; ordinarily a Nino base state means a weak Azores High that has little direct influence, but there's an increasing amount of research pointing toward the reduced equator-pole temp gradient brought about by anomalously low low Arctic sea ice leading to a stronger Hadley cell, hence Azores High, and the sea ice area and extent is at record lows currently. Not only this, but low sea ice shows some (ancient) historical relationship with a stronger Scandinavian High too.
Last year we benefited from a super-strong Azores High regularly linking up with Scandinavian highs, thanks to low sea ice extent forcing combining with weak La Nina forcing; they both bring about the same response in the Azores High, and the low sea ice likely helped the Scandinavian highs to develop and persist too.
So what happens when it's a weak Nino pattern in place? Does the Azores High feature more than usual for the Nino base state and if so, does it work with, or against, the Scandinavian High which in theory should be exceptionally strong and persistent this May-July?
I look forward to finding out .
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