I've been doing quite a bit of reading into the interference patterns seen this year and as far as I can see, the most similar historical years for this are 1995 and 2002.
So not surprising to see 2002 in the 7s club for the Feb CET.
So, feasibly, this month's super-mild outcome could have been foreseen if it had been possible to have much confidence in whether the interference pattern would give way or not.
Therein lies a huge problem; anticipating how that will unfold requires dependable projections for tropical phenomena such as the MJO, and we simply don't have those to hand.
This past week presented a clear example of the poor reliability; GEFS/GFS was very insistent on an extremely powerful tropical Pacific WWB across the Dateline that would have likely taken apart the Nina-like tendencies in the subtropics, but the actual outcome has been an only modestly strong event and not only that, but one centred more in the S Hemisphere than the N Hemisphere - focusing impacts on the wrong side for us.
EPS/ECM had a weaker WWB but still stronger than observed so it was not providing enough of a counter-signal to be able to make a confident decision one way or the other.
The same issues have plagued long-range guidance providers throughout this winter. The Nina-like interference (anomalous westerlies being deposited onto the northern flanks of the subtropical highs, making them stronger) has, it turns out, persisted most of the time, but there were a lot of occasions when the modelling was suggesting that developments would occur that could break it down, and not enough evidence to support contradicting those models. So, all that could be reasonably done was to take the modelling guidance, factor in the most similar historical cases in which the tropics behaved as the models predicted at the time and the relevant theory, and hope for the best.
I have a feeling climate change has, via expanding the Hadley cell and hence strengthening and inflating the subtropical highs northward, increased the readiness at which the atmosphere can take on this state by increasing the baseline westerly flow on the northern flanks of the subtropical highs.
I really hope I'm missing something there, because I don't fancy taking on many more seasons in which this interference pattern is playing havoc with the atmosphere! On the other hand, it's a great ingredient to have in play when it comes to fine summer weather in this country... you lose some, you win some! Hmm I'm definitely going to be missing something now aren't I?
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