FIELD GUIDE · Weather Basics
What Is a Heat Dome? Why Some Heat Waves Just Won't Break
What is a heat dome, and why does the heat last so long?
Every summer brings hot days. But occasionally a heat wave arrives that feels different — it settles in, gets worse by the day, and simply will not break. The temperature climbs, the nights stay warm, and a week later it's still going. That's usually the signature of a heat dome, and it's one of the most dangerous weather setups there is, precisely because it lasts.
You can watch one take shape on the LEV map using the Temperature and Pressure layers together — the heat below, and the lid of high pressure holding it down.
A heat dome is a lid of high pressure
The mechanism is simpler than the dramatic name suggests. A large, strong area of high pressure sets up over a region and then stalls there, sometimes for a week or more. That dome of high pressure acts like a lid on a pot.
Why a lid? Two reasons working together:
- High pressure makes air sink. And sinking air warms up as it descends and compresses — the same physics that warms a bicycle pump. So the dome is actively heating the air beneath it.
- High pressure clears the sky and stalls the wind. No clouds means the sun reaches the ground unfiltered all day. No wind means no fresh, cooler air gets pulled in to flush the heat away.
Trapped sun, sinking warm air, and no escape route: that's a heat dome.
Why it gets worse every day
The cruel part of a heat dome is that it compounds. Because nothing disturbs it, each day's sun bakes ground that's already hot from the day before. The land heats the air, the air can't escape, and the baseline creeps upward. Day one might be merely hot; day four is often the deadliest, because the heat has had days to accumulate with no rain and no fresh air mass to reset things.
This is the key difference from an ordinary hot spell. A heat wave is just the symptom — a run of hot days. A heat dome is the stubborn high-pressure cause that makes a heat wave severe, widespread and unbreakable. The dome is the lid; the heat wave is what happens underneath it.
The hidden danger: humidity and warm nights
Raw temperature is only half the threat. Your body cools itself by sweating, and sweat works by evaporating — but in humid air it can't evaporate efficiently, so cooling fails just when you need it most. Forecasters fold this into the heat index, the "feels like" number that combines heat and humidity.
Under a humid heat dome, the danger isn't only the afternoon peak — it's that the overnight low stays high. Normally a cool night lets the body recover. When the dome keeps nights warm too, there's no relief, and that relentlessness is what makes prolonged heat the deadliest weather hazard of all, especially for older people, young children, and anyone without air conditioning.
Seeing one on the map
A heat dome has a clear fingerprint across LEV's layers. The Temperature layer shows a wide blanket of extreme heat. The Pressure layer reveals the big, stable high sitting right over it. And — tellingly — the wind layer goes oddly calm across the whole region, because a dome strangles the wind. When you see all three at once, you're not looking at a passing hot day; you're looking at a lid that's going to stay.
There's an air-quality angle too: stagnant, sunny, windless air under a dome is exactly the recipe for ground-level ozone to build up, so a heat dome often arrives with a slide in the air quality index even far from any smoke.
The bottom line
A heat dome is a parked dome of high pressure that traps heat by making air sink, clearing the sky, and stalling the wind. It doesn't just make a day hot — it makes the heat build and linger, with warm nights that give no recovery. Spot the high pressure sitting over a pool of extreme heat on the map, and you've spotted a heat wave that isn't going anywhere soon.
Frequently asked questions
What is the difference between a heat wave and a heat dome?
A heat wave is the symptom — a stretch of unusually hot days. A heat dome is one common cause: a large, stubborn area of high pressure parked over a region that traps heat beneath it. Not every heat wave is a heat dome, but when a heat wave is severe, widespread and refuses to break for days, a heat dome is usually the reason. The dome is the lid; the heat wave is what happens under it.
Why does a heat dome make it hotter and hotter each day?
The high pressure makes air sink, and sinking air compresses and warms. It also clears the sky of clouds and stalls the wind, so the sun beats down unobstructed day after day onto the same ground. Each day the land and air bake a little more, and with no rain or fresh air mass to reset it, the heat accumulates. That compounding is why day four of a heat dome is often the most dangerous.
Why is heat dome humidity so dangerous?
When the air is hot and humid, your sweat can't evaporate efficiently, which is how your body normally cools itself. Forecasters track this with the heat index, which combines temperature and humidity into what it 'feels like.' Under a humid heat dome the overnight low stays high too, so the body never gets the cooling break it needs to recover — which is what makes prolonged heat waves so deadly, especially for vulnerable people.
How can I see a heat dome on a map?
Switch on the temperature layer to see the broad blanket of extreme heat, and the pressure layer to find the large high-pressure center sitting over it. A heat dome shows up as a wide, stable zone of high pressure with intense heat pooled beneath — and because the wind stalls under a dome, the wind layer will look unusually calm across the whole region.
SEE IT LIVE
Everything in this guide is on one real-time map.