Following on from some posts I made earlier, and given the frankly boring weather outlook, I thought I'd look into the death of my favourite weather phenomenon - the midwinter easterly. We've had easterlies in spring and autumn, but for the purpose of this post I'm concentrating on winter.
Living here in the southeast, near to (but not on) the coast, it's darned hard to get snow these days. I grew up in the 80s and my love of the weather was formed by watching the snow come down, year after year. My gran said to me that it doesn't snow every year, but I'd seen firsthand that it did... that is until winter 1987/8, which was indeed snowless here. After that I learned to treasure snowfall rather than expect it - but I knew that if we didn't get any it'd only be a couple of years until we did.
And so that held through the 90s, until January 1997. That was the last deep cold easterly and was the last time I saw powder snow, icicles, snow sublimating rather than melting, all the traditional bits of winter that I remembered. It was also my last year as a child, for I turned 18 that autumn.
I couldn't have known then that the following 19 years would be icicle-free and largely free of ice days. Little did I realise how frustrating it'd become as a snow fan down here - the former ally of snow (convection over the sea) would turn into the villain, raising temperatures just that bit too much for decent snow.
So, rose-tinted glasses or not? Let's look at some cold, hard data. Here's a chart showing snowfall days at Manston, together with ice days. Note that snowfall can include sleet, or just a flurry of snow - it doesn't mean heavy snow! Data is from Tutiempo, which goes back to January 1973. Note that the chart shows the December of a given year, plus the following January and February.

At first glance it may look like not much has changed. Look more closely though and you'll see a near complete absense of ice days since 1997. Many of the snow days have been sleet since then, whereas before then more of them were snow rather than sleet. (The data may well miss out a couple of days in before 1977, as figures were rounded to the nearest number. There were a few zeroes which may or may not have been ice days).
From this, it's clear that the climate of this part of the world has undergone a marked change in winter. Why is this?
The answer is the lack of midwinter easterlies. You see, down here we rely on easterlies (or NE'lies) for snow. Snow from the north or NW is rare, as we rely on an organised front making it this far. Even then, it's a hell of a job to get ice days from the north or NW.
The other way of getting heavy snow is via a frontal attack from the SW, but that's not only rare but fraught with danger; get it a bit too mild and you just end up with slush.
No, the reliable way is to get a deep cold pool advected from the east. The North Sea causes instability and as the air's really cold although it warms up it remains below freezing - the ideal recipe for heavy convective snow showers. Any troughs/fronts in the flow just add to the mix.
Ideally the cold pool would be modified as little as possible by the sea, which would require a strong easterly flow in order to speed its journey and minimise the modification taking place. A sharply defined cold pool is a bonus too, as the greater contrast seems to aid convective potential. Even without that though snowfall was possible or even likely if an easterly flow was sustained for more than a couple of days.

Here are three examples, excluding the obvious one (1987). In 1986 we had a slack pressure pattern, but that blob to the east contained some seriously cold air (<-20C at 850). 850s fell to -13C over Kent, low enough to trigger slow-moving snow showers.
In 1991 we had an upper cold pool move swifly westwards just to the south. 850s were -17C for a time over Kent, enough to cause persistent heavy, thundery snow showers.
At the end of 1996 a cold pool moved westwards over the southern UK, with -14C 850s accompanying it. At a time of minimum insolation, temperatures plummeted even at the coast and heavy convective snow was the order of the day. This was the last time a high of -1C or lower was recorded here, along with icicles etc.
Some would say these sorts of setups were never common and to be fair they weren't that common - you would expect 2 or 3 a decade in the 70s, 80s and 90s. However, even "near miss" setups would give snow, as conditions weren't as marginal as they are now. Indeed, many of the ice days in the Manston chart were from setups where the core of the cold didn't even reach us!
2005 was the last true easterly spell here, but it simply came too late. In addition, recycled air from the Med got caught up in the flow, diluting the 850s and meaning for most it was just raw drizzle rather than a winter wonderland.

Eventually (after another week of this!) some cold air did arrive - 850s fell to -14C briefly in Kent, but as it was under a ridge and light northerlies there was no convective activity. A pulse of milder air moved down from the north, which brought a return to some wet snow but with the loss of really cold air aloft it was again too little to sustain it - temperatures were above freezing and it just led to a slushfest.
So, with that in mind, there are several factors at work here.
- Synoptically it seems that easterlies of any type are rarer than they were before 1997.
- When we do get easterlies, any cold pools are ill-defined and lack contrast with surrounding air (compare 2005 with the others). This leads to greater stability of the air, reducing the "lake effect" of the North Sea.
- When air does move in from the east, it's not as cold as it was due to greater mixing out of the airmass. Or, to put it another way, something invariably fouls the flow to prevent a direct feed from Russia.
Add to that a general background warming and what was marginal is now rain, what was a safe snow event (-1C) is now marginal.
I've been scouring various archives to try and find what flipped in 1997. It's clear to me that something changed in our atmospheric circulation to prevent easterlies and to warm things generally. I looked at sunspots (not much correlation there, although 2010 did occur during a minimum). I looked at El Nino (inconclusive). I looked at sea temperatures - and found something that fits, namely the AMO.

This is the multidecadal Atlantic oscillation. As can be seen, it flipped from negative (cold) to positive (warm) around 1997 - and it's been warm ever since. As the Atlantic has such a large effect on our weather I wouldn't mind betting this is part of the puzzle - the extra warmth will have added more energy to our weather, promoting a stronger jet (due to greater contrasts between the Atlantic and the Arctic) and thus reducing the frequency of blocking episodes. Furthermore, the extra warmth would help turn what would have been marginal events into rain events, or snow events into sleet.
I don't know why it'd have the effect of reducing the depth of cold pools from the east (the few times they occur), but it could well be tied in to the lack of blocking generally allowing more mixing-out to occur.
This all sounds fine and dandy, now all we need is some weather data before 1963 or so... and, of course, we know all about 1962/3 and 1946/7, both of which were epic cold spells in the middle of a mild AMO. What about the rest of it?
Amazingly, some data from the 30s exists on TuTiempo for Manston. The winter of 36/7, for example, saw one snow day and no ice days. It was 5/0 for 37/8 and 8/5 for 38/9. And lo, 38/9 contained a textbook easterly:

There were others, too, during that period of positive AMO. So it's not the be-all-and-end-all.
However, I feel confident enough to draw some conclusions.
- The AMO has some effect on the UK and surrounding areas, possibly quite a big one. Easterlies and snow seem more common during negative phases.
- Something changed in 1997 to make easterlies of any type much rarer. It also coincided with a marked reduction in ice days.
- Since 1997 snowfall has become much more marginal, with some events which would have been snowfall now coming as sleet/rain instead.
- When the AMO flips back negative again we are likely to see more in the way of cold, wintry weather - however that isn't likely for some time.
This research is, of course, heavily biased to the SE - an area which has seen IMO one of the biggest changes since 1997. Areas which are less dependent on easterlies for snowfall (ie the Midlands north and west) won't have seen anywhere near as much of a change.