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Spring Temperature Fluctuations - Meandering Jet Causes Sudden Changes in Airmass

A look at why in Spring we often see big fluctuations in temperatures over a few days

Spring Temperature Fluctuations - Meandering Jet Causes Sudden Changes in Airmass
Blog by Nick Finnis
Issued: 30th March 2020 18:09
Updated: 30th March 2020 18:18

Over the last few weeks we’ve seen the temperature fluctuate quite a bit. The weekend before the weekend just gone saw high pressure over Scandinavia feed in a cold and dry easterly wind. Then early last week the wind switched to a milder southerly flow, allowing the temperature to climb 19.4C in north Wales. Then over the weekend, a record-breaking intense area of high pressure building to the west of Britain pulled in a cold and strong northerly wind, making the first day of British Summer Time on Sunday feel more like winter, with wintry showers falling as snow even in the south. The cold northerly eases over the next few days with the flow turning more westerly, so it will become less cold for a time, but cold arctic air looks like it will try and push south again later this week, bringing another cold snap by Friday – with sleet and snow showers for the north. However, there are signs that winds will switch to a milder south or southwesterly direction by Sunday, with temperatures reaching the mid-teens, perhaps the high teens early next week.

It’s quite common in spring to see big swings in temperatures over a few days. This is because the jet stream tends to weaken as we head through spring, meaning it meanders polewards and then equatorwards over adjacent areas of Europe – rather then moving west to east, so a slight shift in these meanders in the jet stream means the low-level wind we experience can switch from southerly to northerly or vice versa, so air of tropical origin is suddenly replaced by air of arctic origin and all that implies with temperature and weather conditions.

Weakened and meandering jet stream recently means changes in airmass over the space of a few days

We’ve seen these switches in wind direction within a few days over the past few weeks. These different wind directions have brought in quite different airmasses. There are basically 6 different airmasses that affect the British Isles and are shown on the Met Office graphic below.

Britain experienced a cold easterly wind via a Scandinavian high a few weekends ago, this brought a Polar continental (Pc) airmass – which in late autumn, winter and early spring tends bring cold dry air from eastern Europe and western Russia. As the dry air crosses the North Sea it picks up moisture and forms cloud – which can grow deep enough to bring showers which can fall as snow if the air is cold enough. Though in late Spring, summer and early autumn this airmass is often warm and dry – bringing settled, sunny and warm weather.

The easterly wind eased before a milder southerly wind developed early last week, this brought in a Tropical continental (Tc) airmass across England and Wales, a mild but dry flow originating from southern Europe so with some sunshine and some foehn effect to the lee of high ground temperatures reached 19.4C in north Wales. Though across Scotland and N. Ireland the airmass was more of Tropical maritime (Tm) flow off the Atlantic, bringing mild but cloudy conditions with some rain. A Tc airmass in summer that orginates from Spain or NW Africa can bring very hot weather with temperatures exceeding 30C.

Then this past weekend a strong and cold northerly wind developed to the east of an intense area of high pressure over the Atlantic centred to the south of Iceland. This northerly brought in an Arctic maritime airmass (Am) – feeding in cold air direct from the arctic. This Am airmass usually brings showers accompanied by below average temperatures throughout the year, in winter showers often falling as snow, in early/mid spring showers of a wintry nature too, sometimes falling as snow even to low levels in the south given how dry the air is (dew points below 0C) at the surface.

Over the next few days winds will back to a westerly direction as high pressure to the west relaxes, bringing in a returning Polar maritime (rPm) airmass which will be less cold but cloudier thanks to more in the way of moisture, the south staying dry but some showery rain possible in the north.

Arctic maritime (Am) airmass tries to push south again later on Thursday and on FrIday, there’s been some uncertainty how far south it will get, but it appears it will succeed briefly by early Friday, albeit more noticeable across the north, with snow showers possible for Scotland.

Then a change of airmass looks likely again as we head through the weekend, with winds switching to a southerly then eventually southwesterly direction through Sunday and into early next week. This will bring in a Tropical maritime (Tm) airmass that orginates from the sub-tropical area of the North Atlantic. This airmass can often be cloudy, particularly in the winter and around western coastal areas, but where the sun pops out, it could be pleasantly warm with temperatures reaching high teens.

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