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Monte Zoncolan: the climb, its race history and records

Monte Zoncolan: each side of the climb, its passages in the big races since 1996 and the records, each figure with the source it comes from.

The climb

Friuli-Venezia Giulia, Italy

SideStartLengthElevation gainAverageMaxSummitHairpinsSource
OvaroOvaro9.8 km1206 m12.3 %23.3 %1730 m22climbfinder.com
SutrioSutrio13.2 km1183 m9 %21.1 %1731 m15climbfinder.com

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

Race history since 1996 9

YearRaceStageTypeStage winner or first over the topSource
2021Giro d'Italia14Summit finishLorenzo Fortunatoen.wikipedia.org
2018Giro d'Italia Women9Summit finishAnnemiek van Vleutenen.wikipedia.org
2018Giro d'Italia14Summit finishChris Froomeen.wikipedia.org
2014Giro d'Italia20Summit finishMichael Rogersen.wikipedia.org
2011Giro d'Italia14Summit finishIgor Antónen.wikipedia.org
2010Giro d'Italia15Summit finishIvan Bassoen.wikipedia.org
2007Giro d'Italia17Summit finishGilberto Simonien.wikipedia.org
2003Giro d'Italia12Summit finishGilberto Simonien.wikipedia.org
1997Giro d'Italia Women10Summit finishFabiana Luperinien.wikipedia.org

Records

RecordRiderTimeYearSource
Sutrio: fastest race ascent (watts2win segment 12.34 km, 8.65%)Egan Bernal0:37:572021watts2win.eu
Ovaro: fastest race ascent (watts2win segment 9.99 km, 11.77%)Chris Froome0:39:362018watts2win.eu

A time is listed only where the sources agree on it; where two sources give different times for the same ride, it is left out.

How long would it take you?

Your time up Monte Zoncolan 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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