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Col d'Aubisque: the climb, its Grand Tour history and records

Col d'Aubisque: each side of the climb, every Grand Tour passage since 1996 and the records, each figure with the source it comes from.

The climb

Nouvelle-Aquitaine (Pyrénées-Atlantiques), France

SideStartLengthElevation gainAverageMaxSummitHairpinsSource
LarunsLaruns17.1 km1202 m7 %13.8 %1709 m16climbfinder.com
Argelès-Gazost (via Col du Soulor)Argelès-Gazost29.7 km1409 m4.7 %9.4 %1711 m7climbfinder.com

Each side from one source, linked. A dash: the sources we opened disagree or give no figure, so we leave it out.

In the Grand Tours since 1996 14

YearRaceStageTypeStage winner or first over the topSource
2023Vuelta a España13CrossedMichael Storerfr.wikipedia.org
2022Tour de France18CrossedGiulio Cicconeen.wikipedia.org
2018Tour de France19CrossedRafał Majkaen.wikipedia.org
2016Vuelta a España14Summit finishRobert Gesinken.wikipedia.org
2012Tour de France16CrossedThomas Voeckleren.wikipedia.org
2011Tour de France13CrossedJérémy Royen.wikipedia.org
2010Tour de France16CrossedChristophe Moreauen.wikipedia.org
2007Tour de France16Summit finishMichael Rasmussenen.wikipedia.org
2005Tour de France16CrossedCadel Evansen.wikipedia.org
2002Tour de France11CrossedLaurent Jalaberten.wikipedia.org
2000Tour de France10CrossedJavier Otxoaen.wikipedia.org
1999Tour de France16CrossedAlberto Ellien.wikipedia.org
1998Tour de France10CrossedCédric Vasseuren.wikipedia.org
1996Tour de France17CrossedNeil Stephensen.wikipedia.org

How long would it take you?

Your time up Col d'Aubisque at a steady power, from a physics model.

Advanced: rolling resistance and drag

Estimate from a physics model (Martin et al. 1998), on the average gradient. Wind, surface, pacing and steep sections change the real time. More cycling tools

How this is calculated

P × 0.977 = ½ · ρ · CdA · v³ + v · m · g · (sin θ + Crr · cos θ), θ = arctan(average gradient), m = rider + bike, g = 9.81; solved for the speed v, time = length / v. Air density ρ: NASA GRC troposphere: T=15.04-0.00649*h; p=101.29*((T+273.1)/288.08)^5.256; rho=p/(0.2869*(T+273.1)); h = mean of start and summit altitude. Sources: Martin et al. 1998, J Appl Biomech 14(3):276-291 — https://collections.lib.utah.edu/ark:/87278/s6jd5f71; Defraeye et al. 2010, J Biomech 43(7):1262-1268 (upright position, cyclist+bike 0.270 m2) — https://lirias.kuleuven.be/retrieve/232736; NASA Glenn Research Center, Earth Atmosphere Model (metric) — https://www.grc.nasa.gov/www/k-12/airplane/atmosmet.html. Climb geometry: the side's source in the table above.

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