My money is on Q being on queue - with a quantum of Siberian cold heading our way by the 10th March. The equinoctial effects on the cold makes it less stable, and more “slippery” and inclined to advection. Makes cold spells more likely but shorter than mid winter ones. So far it is modelled to just miss us - and I did not know this was due to influences of the PV in Canada and all that knock-on to do with Baffin...I would love to know a bit more how that works.
There are many games of consequences in weather modelling, just like the southerly pushing north on a stalling Atlantic front - if it reaches Svalbard it means a Scandi high forms, but if it doesn’t quite reach that far north, it means a high over Denmark or even Holland and we get dry cool weather...(in winter), so the Baffin factor is new to me.
Loved the diagram Q, but please could you put some meat on the bones?
There is something wonderful about spring snow events, when the uppers are really cold, because the snow is more sugar like, fluffy, white and more candle floss like. Strangely the rather wet and westerly 70s (after 1970-71 and before 1979 that is, the cold spells sometimes came later - one being the 25th of March: 2.5cm fell in my low lying Sussex home on 2 consecutive nights, to melt off during the day due to intense, sunny, blue sky days....real glad-to-be-alive days - with a touch of night-time magic - of intense alpine type snow-fests.
Brecklands, South Norfolk 28m ASL