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How does a heat wave happen?
Quick answer
A heat wave forms when a slow-moving high-pressure system traps air over a region. The sinking air is compressed and warmed, clouds are suppressed, and dry ground stops evaporation from cooling the surface. With little wind to move the mass, heat accumulates day after day until temperatures far exceed normal.
A heat wave happens when a large, slow-moving high-pressure system parks over a region and traps hot air near the ground for days or weeks. The sinking air compresses and warms, skies stay clear, and the ground keeps heating until temperatures climb far above normal.
Step by step
- A large high-pressure system builds and settles over a region, often linked to a stalled jet stream.
- Air inside the system sinks toward the ground, and the increasing pressure compresses and heats it.
- Sinking air dries out, so clouds cannot form and the sun heats the ground all day.
- Dry soil means little water evaporates, so solar energy warms the air instead of being used for evaporation.
- The slow-moving system keeps the hot air mass in place, and heat accumulates over several days.
- Temperatures peak until the high-pressure system weakens or moves away and cooler air arrives.
Key things to understand
- A strong high-pressure system, often called a heat dome, settles over a region and pushes air downward toward the ground.
- As that air sinks it is compressed by the higher pressure below, and compression raises its temperature.
- The sinking air also suppresses cloud formation, so sunlight reaches the ground almost unchecked all day.
- Dry soil and low vegetation mean less water evaporates, so more of the sun's energy goes into heating the air instead of cooling it.
- Because the high-pressure system moves slowly, the same hot air mass sits in place for days, letting heat build up.
Labelled diagram
- High pressure forms
A slow-moving high-pressure system settles over the region and begins to push air downward.
- Air sinks and warms
Compression from sinking raises the air temperature and dries it out.
- Clouds disappear
Dry sinking air suppresses cloud formation, leaving clear skies and strong sunlight.
- Ground heats up
Sun-baked dry soil releases little moisture, so heat stays in the air.
- Heat accumulates
The stalled system holds the hot air for days, pushing temperatures higher.
- System breaks down
When the high pressure weakens or moves, cooler air returns and the heat wave ends.
Real-world examples
- The 2003 European heat wave pushed temperatures above 40°C (104°F) in France and killed tens of thousands of people, many of them elderly.
- In May 2022, Jacobabad in Pakistan recorded around 51°C (124°F), among the highest temperatures ever measured in South Asia.
- The 2021 Pacific Northwest heat wave sent Lytton, Canada, to 49.6°C (121°F), a national record, before a wildfire destroyed the town.
- In 2015, a heat wave in Andhra Pradesh and Telangana, India, killed more than 2,000 people during a prolonged spell of 45°C-plus days.
Common mistake
✗ Myth: A heat wave is just a few unusually hot summer days.
✓ Fact: A heat wave is defined by unusually high temperatures relative to the local normal, sustained over several days and often nights. The duration matters because heat accumulates and the body gets no overnight recovery, which is what makes it dangerous.
People also ask
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Part of the guide: Water & Weather Phenomena →

