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Running Tools

Altitude Calculator

How much slower is the same effort at altitude? Enter a pace and an altitude and this converts between the two, for every race distance from 1500 m to the marathon.

Calculator Mode

Enter the pace you hold at sea level and see what the thin air turns it into.

Units

Choose your preferred unit system for altitude and pace

Your Sea-Level Pace

The distance sets how long you are out there, and with it how much of the effort is aerobic — which is the part altitude takes away.

Altitude & Acclimatization

Height above sea level — not the climbing you do during the run. The model covers 0 to 3,000 m (9,843 ft).

Acclimatization gives some of the loss back, never all of it. VO₂max stays down for as long as you are up there; what recovers over two to three weeks is your submaximal performance.

⚠️ Important Notice

These are estimates for healthy runners going up to train or race, and the range is wide for a reason — the difference between two runners at the same altitude is larger than most people expect. Above about 2,500 m, altitude sickness becomes a risk in its own right (headache, nausea, broken sleep, breathlessness at rest) and no pace adjustment fixes that. Go up gradually, drink more than feels necessary, and treat the first two days as easy running whatever this calculator says.

About Running at Altitude

Air pressure falls with altitude, so every breath carries less oxygen. Your muscles still need the same amount, so the ceiling on aerobic power drops, and the longer the race the more of it sits under that ceiling. That is the whole mechanism — and it is why the correction here is not a single percentage but depends on the distance, on your fitness, and on how long you have been up.

Why Sprints Get Faster: Below roughly 800 m the sign flips. A sprint is almost entirely anaerobic, so the missing oxygen barely registers, while the thinner air genuinely reduces aerodynamic drag — and the runner goes faster. The 1968 Mexico City Olympics, held at 2,240 m, is the cleanest evidence there is: world records fell in every event up to 400 m and in the long jump, while the 5,000 m, 10,000 m, marathon and steeplechase were won in times well outside what those same fields ran at sea level. This calculator starts at 1500 m because that is the shortest distance where the aerobic loss reliably wins.

How the Correction Is Built: Four steps, in order. VO₂max falls with altitude — about 6.3% per 1,000 m for trained runners in the hypobaric-chamber measurements this uses (Wehrlin & Hallén, 2006), less for untrained ones. Only part of that reaches your race, because you race at a fraction of VO₂max and that fraction depends on how long the race lasts. Thinner air then returns a little through reduced drag. Acclimatization recovers part of what is left. The result is anchored to a measured performance rather than to theory: a 3,000 m time trial at 2,100 m runs about 9.7% slower than the same runners at sea level.

What Acclimatization Does and Doesn't Do: Two to three weeks high up raises red cell mass and restores much of your submaximal performance, but VO₂max at altitude stays down the whole time you are there — you do not get it back by staying. That is why the fully acclimatized setting reduces the cost instead of removing it. Coming back down, the benefit is real but modest, and it fades over two to three weeks.

Training by Effort, Racing by Numbers: Above about 1,200 m, run easy days on effort and let the pace be whatever it turns out to be. Sessions are what need real thought, and the recovery is what changes most — lengthen recoveries before you slow the reps down. If you train high and race low, the paces you hit up there are not the paces to plan a sea-level race around: convert them with the second mode of this calculator first, which is exactly what the coaching platform does automatically with every activity that syncs in.

Frequently Asked Questions

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