WEATHERDUCK

A plain-English guide

What is a cloud inversion?

A cloud inversion is when a layer of warmer air traps cold, damp air in the valleys below it. The trapped air turns into fog or low cloud, and if you’re on a hill above it, you look down on a sea of cloud with clear sky overhead.

Joss standing on a stony summit above a sea of cloud at dawn, with fells rising through the cloud behind
Me, above the cloud at dawn.

How it forms

How does a cloud inversion form?

It takes a clear, calm night and three things happening in order.

  1. The ground cools after dark

    On a clear night the ground loses heat quickly and chills the air just above it.

  2. Cold air drains into the valleys

    Cold air is heavier than warm air, so it slides downhill and collects in valleys and hollows, a bit like water.

  3. A warm lid holds it in place

    A layer of warmer air above acts like a lid. If the trapped air is damp enough it turns into fog or cloud, and there it sits until the sun breaks it up.

Cross-section of a cloud inversion: cold, damp air trapped under a warm lid fills the valley with fog, while two summits rise above the cloud top into clear sunlit air.
Normally the air gets colder as you climb. In an inversion a warmer layer sits on top, trapping the cold, damp air and its cloud underneath. Any summit above the cloud top is in clear air.

Grey below, sunny above

Why is it grey in the valley and sunny on top?

If you’ve ever driven out of fog on the way up a hill and into bright sunshine, you’ve been through an inversion. The warm lid keeps the damp air and its cloud in a shallow layer near the valley floor, so the valley stays cold and grey while the air above is drier and clear.

The cloud has a flat top because it can’t rise through the lid. That’s what gives you the sea of cloud look, with hills poking through like islands. When there’s no lid and the cloud just keeps going up, you get an ordinary grey day however high you climb.

Panorama of sunrise over a sea of cloud filling the valleys, seen from a stony summit ridge
Sunrise over a full valley inversion, December 2021.

Know what you’re looking at

Is it a cloud inversion or just fog?

From inside the murk they all feel the same. What matters is what’s happening above your head.

What you’re looking at What’s happening Any good for a view?
Valley fog Cold air has pooled overnight and its moisture has condensed. Yes. This is what you want to see below you.
Radiation fog The same process over wider low ground after a clear, calm night. Often. It tends to burn off as the morning warms up.
Hill fog Cloud sitting on the high ground itself. No. The summits are inside it, not above it.
Haar or sea fog Damp air drifting in from the coast on an onshore breeze. Sometimes. The top is often ragged and it moves about.
Freezing fog Any of these in air below freezing, coating everything in rime. Only from above it. Take care on paths inside it.

The quick test is the cloud top. A real inversion has a clear ceiling with drier air above it, and the summits sit above that ceiling.

When to look

When do cloud inversions happen in the UK?

Mostly in autumn and winter, around dawn, after a clear and calm night. For our UK Cloud Inversion Report we scored 662 mornings in a row at 15 places around the UK. These are forecast scores rather than photographed inversions, but the season stands out.

6.9%
of October mornings reached our Likely band, the best month in the archive
3.9%
of December mornings, with November close behind at 2.8%
0%
of June mornings reached Likely, at any of the 15 places

They’re not impossible in summer, just rarer. We caught good ones in Scotland and Wales in July 2026. And no two seasons are the same: October 2025 was far busier than October 2024.

Read the UK Cloud Inversion Report

What a good night looks like

  • Clear skies overnight, so the ground can cool
  • Light winds, so the cold air settles instead of mixing
  • Damp air in the valleys, so it can turn into fog
  • Settled high pressure, which often brings all three
  • Sunrise, when the cold pool is usually at its deepest

Where to go

Where can you see a cloud inversion in the UK?

You need low ground below you and a hill that rises above the cloud. These are the places people ask about most, each with its own 24 hour forecast.

Somewhere else in mind? Check the forecast for any UK location

Seen for real

Real inversions we forecast in advance

I save every forecast before dawn, then check it against dated photos of what actually happened. Here are the latest ones.

Saved forecast map for 09:00 on 4 October 2026 with Glyder Fawr on the edge of a Likely cloud inversion area over Eryri.
Likely Forecast 12 hours ahead

Glyder Fawr to the Bannau, Wales

Glyder Fawr was on the edge of a Likely area the night before, and Very likely by morning. The webcam was stuck in cloud, but Morgan and Neil were up above it.

Read the forecast check
Map from the Yr Wyddfa report showing the cloud inversion outlook across Wales.
Likely Forecast 31 hours ahead

Yr Wyddfa, Wales

By the night before, Yr Wyddfa was Very likely. The summit webcam and a first-hand report both show it above a cloud sea across Eryri.

Read the forecast check
Map from the Highlands report showing the cloud inversion outlook over the Eastern Highlands.
Very likely Forecast 46 hours ahead

Torridon to Tap o’ Noth, Scotland

The Very likely area over the Highlands held right up to the final update. Walkers at Tap o’ Noth, Torridon and Loch Quoich found cloud below them at dawn.

Read the forecast check

Misses and uncertain calls get published too, as the record grows.

Browse all forecast checks

Quick answers

Cloud inversion questions

Is a cloud inversion the same as a temperature inversion?

Not quite. A temperature inversion is the warmer layer of air sitting on top of colder air, and on its own you can’t see it. A cloud inversion is what you get when the cold air underneath is damp enough to turn into fog or low cloud, so the inversion becomes visible.

What time of day is best for a cloud inversion?

Usually the hour or two around sunrise. The cold air has had all night to settle into the valleys, and the wind is often at its calmest. Once the sun gets going it warms the ground and stirs the air up, and the cloud tends to thin or lift through the morning.

How high do I need to climb to get above the cloud?

Above the cloud top, and that changes every time. Some mornings a low hill is enough, other mornings the cloud sits higher than most summits. The WeatherDuck forecast gives an estimate of the cloud top where it can, so you can pick a hill that should clear it.

Are cloud inversions dangerous?

The view isn’t, but getting to it can be. You’ll often walk up through thick fog in the dark, and in winter that fog can be freezing. Take a head torch, warm layers and a way to navigate in poor visibility, and check the mountain forecast for wind and ice before you go.

Can you predict a cloud inversion?

Yes, with a bit of honesty about the odds. The clues are a clear, calm night, damp air in the valleys and warmer, drier air above. WeatherDuck checks those for any UK location and gives each morning a band from Unlikely to Very likely. It’s a guide, not a promise, so it’s worth checking again before you set off.

Why are cloud inversions more common in autumn and winter?

Longer nights give the ground more time to cool, so more cold air collects in the valleys. The sun is weaker too, so it takes longer to break the layer up. Settled high pressure in autumn is the classic setup.

Before you set the alarm

Will there be a cloud inversion near you?

WeatherDuck checks for one every night, for any UK location. The 24 hour forecast is free, and a free account gets you an email when one looks likely.

Check the cloud inversion forecast Get a free alert