There are two changing influences on the North Atlantic jet stream that are having opposite effects, but taken together may partly explain what is going on regarding increased summer rainfall in NW England and SW Scotland and reduced summer rainfall and higher temperatures in SE England:
1) Poleward expansion of Hadley cell ie tendency for Azores High to extend slightly further North than previously
2) Arctic amplification(*) causing the Jet Stream in the North Atlantic to be further South than previously in summer
I posted several weeks ago that 4 out of the last 5 Junes feature in the top 20 wettest Junes in the NW England rainfall series [length of record = 148 yrs]
It is possible that (1) + (2) taken together are causing summer low pressure systems to follow a narrowed path, providing other factors align - ie there will still be occasional variations from this such as June & July 2018.
* Arctic amplification is a term used referring to the fact that the arctic is warming faster than the rest of the world
Funny you should mention the Hadley Cell, I was just thinking of that as I read through this thread from the start.
Last month caught my attention with respect to that. There was predominantly very low atmospheric angular momentum due to a developing La Nina event, which usually corresponds to more rainfall than usual right down into France (with temps varying around the average).
Yet, the southern reach of anomalously wet weather was southern Wales eastward and it was actually drier than usual in the far south (I saw about half the usual rainfall here).
An outcome that fits the notion of Hadley Cell expansion well.
Your suggestion regarding Arctic amplification, I'm less sure about. Arctic amplification is likely weakening the polar jet stream (on average, across the weeks and months), but that doesn't necessarily mean it moves southward. In fact, as amount of cold air the Arctic can support reduces, there ought to be an overall northward shift as the colder 'pool' shrinks in spatial coverage.
This, I believe, is where the North Atlantic sea surface temperatures are taking the wheel to steer things the other way. The central North Atlantic has been persistently cooler than its surroundings, often by several °C, for nearly all of the the past 5 years. This is likely to do with freshwater influx from Greenland ice melt interfering with the Atlantic Meridional Overturning Circulation (AMOC), of which the surface component is the Gulf Stream.
This has shifted the warm/cool boundary southward in the North Atlantic.
The outlook for the next decade is likely to be one largely decided by the Hadley Cell expansion and Arctic amplification competing with that. There are striking possible outcomes of the battle - the southward-shifted North Atlantic polar jet may become more restricted to over the ocean, leading to an increased incidence of troughs west of Europe working in tandem with highs over Europe to bring high-end heatwaves.
Perhaps, the rapidly developed, yet intense hot spells of 2019 & 2020 are demonstrations of that starting to become a feature already.
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