ATMOSPHERIC LAYERS SIMULATION

Pressure halves for every 5.5 km of altitude, which is why a breath on the summit of Everest holds only about a third of the molecules it would at sea level. From the ground up to 600 km there are five layers in sequence: past 12 km the clouds and weather end, 25 km is the ozone layer where temperature rises with height instead of falling, 80 km is where meteors burn up, and the ISS at 400 km is still inside the thermosphere rather than out in open space.

▸ Building the 5-layer atmospheric column…
▸ Loading temperature gradient (4 reversals)
▸ Computing exponential pressure fall-off
▸ Releasing meteors · aurora · ISS
▸ Calibrating the Kármán line at 100 km…
▸ Ready — Online. ✅
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⌂ Earth

Simulation room Atmospheric layers

Atmosphere Layers
Online
altitude · temp · pressure
Altimeter
🌤️ Current altitude
drag ⇅ on the scene to change altitude
Scenario—
Altitude—
Layer—
Temperature—
Pressure—
Phenomenon—
Notes
The atmosphere is NOT uniform: temperature reverses 4 times (fall–rise–fall–rise), dividing it into 5 layers. Pressure falls almost exponentially — halving every ~5.5 km.
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Drag the ⇅ cursor (or the Altitude slider) up/down to explore each layer · try the layer scenarios on the right · click a concept for details
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Temperature & pressure profile vs altitude (0–600 km) temperaturepressure %
About Atmosphere Layers

Pressure halves for every 5.5 km of altitude, which is why a breath on the summit of Everest holds only about a third of the molecules it would at sea level. From the ground up to 600 km there are five layers in sequence: past 12 km the clouds and weather end, 25 km is the ozone layer where temperature rises with height instead of falling, 80 km is where meteors burn up, and the ISS at 400 km is still inside the thermosphere rather than out in open space.

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