Drag the aircraft upward. Pressure, density, and oxygen don't fall in a straight line — they drop exponentially.
A free density altitude calculator + a live atmosphere explorer. Watch thin air hit oxygen & SpO₂, horsepower, the power curve, and cabin altitude — built for pilots, students & AvGeeks.
The dots are illustrative; the real number density (from n/V = P/kBT) is below — and it's staggering.
2.55 × 1025 molecules/m³ · 100% of sea level
The S-curve. Above the cliff you're safe; past it, saturation falls off a ledge.
This view tops out at 65,000 ft — the Armstrong limit, where unprotected body fluids boil at body temperature. For perspective, the Kármán line (the conventional edge of space) sits near 330,000 ft / 100 km — roughly 5× higher than the top of this chart.
Density altitude is the altitude your aircraft thinks it's at. On a hot day at a high-elevation field, thin air robs lift, propeller thrust, and engine power — even though your altimeter reads field elevation.
Educational estimates only — not for flight planning, dispatch, or weight-and-balance. Always fly the numbers in your POH and current official weather.
Drag the chart to set temperature — at this field and altimeter, density altitude climbs about 120 ft for every °C above standard.
Thin air carries less oxygen for combustion, so a piston engine loses power as density altitude rises. Pick your aircraft and a density altitude to see the horsepower you actually have. ↑ use the density altitude from above
Educational estimates only — not for flight planning, dispatch, or weight-and-balance. Always fly the numbers in your POH and current official weather.
The power needed to hold altitude is drag × airspeed, and it's U-shaped: parasite power grows with the cube of speed, while induced power (the cost of making lift) falls as 1/speed. They balance at the bottom — the minimum-power speed. Slower than that, flying slower needs more power: the "back side of the power curve," the region of reversed command. Curves assume 1g level flight at gross weight — where the power-available line crosses the curve on the right is max level speed; the low-speed crossing is below stall (hypothetical, not a real flying speed). Drag the speed and watch it. ↑ use the density altitude from above
Educational estimates only — not for flight planning, dispatch, or weight-and-balance. Always fly the numbers in your POH and current official weather.
Pressurized aircraft don't hold the cabin at sea level — they maintain a maximum pressure differential (ΔP) between inside and outside. Pick an aircraft and cruise altitude to see the cabin altitude your body actually experiences, and the blood oxygen that comes with it.
Educational estimates only — not for flight planning, dispatch, or weight-and-balance. Always fly the numbers in your POH and current official weather.
Density altitude is pressure altitude corrected for non-standard temperature — the altitude at which the air density you're flying in would occur in the standard atmosphere. On a hot day at a high field, density altitude can be thousands of feet above your actual elevation, which is why aircraft climb and accelerate so poorly in those conditions.
First find pressure altitude: PA = field elevation + (29.92 − altimeter setting) × 1000. Then correct for temperature: DA = PA + 120 × (OAT − ISA temperature), where ISA temperature is 15 °C minus about 2 °C per 1,000 ft of pressure altitude. The calculator above does this for you.
As air pressure drops, the partial pressure of oxygen drops with it, so each breath delivers less oxygen to your blood. Hypoxia can begin degrading night vision as low as ~5,000 ft, and judgment well before you'd notice. Under FAR 91.211, U.S. pilots need oxygen above 12,500 ft cabin altitude (after 30 minutes), continuously above 14,000 ft, and must provide it to passengers above 15,000 ft.
For an unacclimatized person breathing cabin air, SpO₂ falls from ~97% at sea level to roughly 87% at 10,000 ft, ~72% at 18,000 ft, and ~50% at 25,000 ft. The drop accelerates because the oxygen–hemoglobin curve falls off a cliff once arterial oxygen pressure drops below ~60 mmHg.
A normally-aspirated piston engine loses power roughly in proportion to air density — about 3% per 1,000 ft of density altitude (Gagg–Ferrar). At 8,000 ft density altitude a 180 hp engine makes closer to 135 hp. Turbocharged engines hold rated power up to a critical altitude, then fall off the same way.
Yes — it's a myth that they don't. Jet engines produce thrust (not horsepower), and thrust falls as you climb because thinner air means less mass flowing through the engine — roughly in proportion to the ambient pressure ratio, so a turbofan at FL400 may make only a third of its sea-level static thrust. Turboprops produce shaft horsepower and are usually flat-rated to a critical altitude (like a turbocharged piston), then lose power as density falls. Jets cruise high not because they keep their power, but because drag drops even faster up there and fuel efficiency improves — so the reduced thrust carries them further per pound of fuel.
The fuselage can only hold a limited pressure difference (ΔP) between inside and outside. At cruise the system maintains that maximum differential, which works out to a cabin altitude near 8,000 ft for most airliners. Newer composite jets like the 787 and A350 tolerate a higher ΔP and target ~6,000 ft, which reduces fatigue on long flights.
Spotted a wrong number, an airport that won't look up, or a calculator you'd love to see? Tell me — it shapes what gets built next.
Built by Levan Sulakvelidze — an instrument-rated private pilot based at KMYF (San Diego) and trained at KGAI (Gaithersburg, Maryland). DensityAlt grew out of genuine curiosity about how the air, your blood oxygen, and your airplane's performance all thin out with altitude — and a wish for free tools that get the physics right.