Published on 9 Feb 2015

Cloud trapped under high pressure: a weather forecaster’s nightmare

If you’ve looked at the weather charts for the coming days and seen the big area of high pressure across the UK, you’d probably think that us weather folk have got an easy ride this week.

However, the opposite is true! Cloud and moisture trapped under a big area of high pressure over the UK in winter can give some of the greatest challenges to weather forecasters, as well as the weather computer models that we use.

I can hear you thinking that this should be a really easy task with an expensive supercomputer churning out detailed weather information. However, there’s a bit more to it than that.northwales_cloudbreaks_g_wp

Weather computer models work by dividing our atmosphere into grid boxes, within which complex calculations are done to determine weather conditions at each point around the earth.

In simple terms, these calculations concentrate on the state of three fundamental elements that influence the weather on our planet: pressure, temperature and humidity.

Why are pressure temperature and humidity so important?

Air pressure is a measure of the weight of air above a particular location. If the pressure is high, then the air sinks and the highpressure_chart9thFeb_MO_wpweather is likely to be settled. If the pressure is low, then air rises and forms clouds, with unsettled weather more likely.

As well as affecting the nature of what falls from the sky, temperature also drives the jet stream. Contrasts in temperature horizontally and vertically in the atmosphere help create wind and transfer energy from one place to another.

Humidity is a measure of how much moisture is present in the atmosphere. Whilst for some parts of our planet, such as the tropics or deserts, it doesn’t change much over time, in temperate latitudes like ours, it varies a lot. This is what makes the weather across the UK some of the most changeable in the world.

Why do weather computer models struggle to get the cloud detail right?

Cloud cover in weather computer models is parameterised, which means that a number of assumptions and simplifications are made as to how cloud cover is worked out in each of the grid boxes I mentioned a little earlier.

world_grid_g_wpThe Met Office EURO4 model that covers the UK has grid boxes that are 4km by 4km in size.

In the current weather situation, there’s a lot of cloud in the lower part of the atmosphere and not much wind to stir things up. As are result, the computer models can have difficulty working out precisely what is happening with the cloud cover in each 4km by 4km grid box.

For example, the model may have worked out that in one grid box there’s full cloud cover, when in reality the cloud has broken up, leaving just 30 per cent cloud cover.

Amplified errors

This may not sound significant, but when an incorrect assumption is put into the bigger, evolving picture, it can cause errors to become amplified over time. This can give a very different forecast in comparison to what is happening in reality.

Interestingly, today, it has been ECMWF’s global weather computer model that has done the best job of predicting the sunny and cloudy areas – despite it having a much lower resolution than the Met Office’s EURO4, which has predicted way too much cloud in places where it’s sunny.

So, despite possible predictions of cloudy skies where you are for the days ahead, you could in fact wake up with the pleasant surprise of sunshine.

Don’t forget, you can get the latest forecast on the Channel 4 Weather website. I also post regular updates on Twitter – @liamdutton

Tweets by @liamdutton

3 reader comments

  1. Josie Msonthi says:

    I love Liam Dutton’s weather website, showing so much detail and explaining in such a way that as an enthusiastic weather follower amplifies understanding. Thanks.

  2. Duncan Wells says:

    Dear Liam,

    What I don’t understand is why there is any cloud trapped by the high pressure. We had pressure of 1040 or so at the weekend in Chalfont St. Peter and now we have 1028/30, so the pressure has dropped but with high pressure one has cold air falling and with low pressure one has warm air rising. So where has the warmer air which has risen to condense out as cloud and become trapped under the higher pressure, come from? Is it due to the sun heating the ground when there was cold air falling and a clear sky and that this warm air has risen, condensed and become trapped?

    All the best,

    D

    Duncan Wells
    RYA Instructor
    Principal http://www.westviewsailing.co.uk
    Author; http://www.bloomsbury.com/uk/stress-free-sailing-9781472907431/
    Creator; http://www.livesavers.co.uk
    Voiceover; http://www.duncanwells.com
    01753 890555

  3. ashley haworth-roberts says:

    Although pressure was high near the UK last week, was not the cloud (not convective cloud but low stratocumulus layers) probably dragged in by weak warm/occluded fronts from the north west or brought in from the east as light winds crossed a cold late winter North Sea (dull weather in north west England from the former, dull weather later on in the week in the south from the latter)? The question I think was whether sinking air and a probable temperature inversion might melt the cloud or not (for want of a more precise physical description).

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