## Thursday, April 25, 2013

### Grade comparison: Devil Mountain Double versus Terrible Two

Anyway, I got curious as to how the Devil Mountain Double course compared with the Terrible Two course in that regard. Which is steeper, and do both tend to follow the superposition-of-cosine-squared probability distributions I proposed?

In each case, I did the fits "by eye". I made no attempt to match the total climbing in the actual profiles with the total climbing from the analytic fits, except for a crude check on Devil Mountain Double due to a fit that wasn't as good as for Terrible Two (more on that a bit later). I smoothed the profile with a bi-exponential smoothing function of characteristic length 50 meters, then partitioned the profiles into 50 meter segments, and did a histogram of the grades from these 50 meter segments. These thus don't represent the maximum peak grades on the courses, for example at particular switchbacks, but rather the grades which are sustained over at least 100 meters or so.

For Terrible Two, I had previously done a crude fit to the grade distribution. I redid the fit more carefully here:

I modeled the grade for the Terrible Two course assuming a trimodal distribution: there's three types of roads:

1. 52% of the total distance is steep mountain roads, where the maximum grade is 18%.
2. 32% of the total distance is rolling roads where the maximum grade is 4%
3. 16% of the total distance is flat roads where the maximum grade is 2%.

The distribution is fairly symmetric, with the climbs similar to the descents.

In contrast, here's the result for the Devil Mountain Double course:

The first thing which you might notice relative to Terrible Two is the strong asymmetry here. The climbs are steeper, in general, then the descents. This is essentially due to the two climbs: Mount Hamilton and Sierra Road. For Mount Hamilton, the particular requirement that heavy hardware be hauled up to the summit for the creation of the Lawrence Livermore Observatory imposed an imperative on gradual grades on the western side (Mount Hamilton Road). The eastern side, free from such a requirement, was able to be built (as San Antonio Valley Road) taking a much more direct route up the hill. The other is Sierra Road. Sierra, the climb which follows the descent from Hamilton, is a steep climb which is followed by the more gradual Felter road descent. These two climb-descent pairs weight the distribution in favor of steeper climbs and more gradual descents.

I separated climbs and descents to yield the following:

1. 44% of the total distance is mountain descent, where the peak grade is 13%. Note the hump which rises from the shoulder of this distribution. That's Mount Hamilton Road, which has a particularly uniform grade for each of it's three primary descents. I did the fit as a compromise between the Mount Hamilton Road hump and the rest.
2. 7% of the total distance is essentially flat but descending, with a peak grade of 2%
3. 14% of the total distance is essentially slightly rolling but climbing, with a peak grade of 3%.
4. 35% is steep climbing, where the peak grade is 15.5%.

So with this approximation, 48% of Terrible Two is flat or rolling, while only 21% of Devil Mountain Double is. But the climbs and the descents of the mountainous portion of Terrible Two is steeper, with a maximum grade of around 18%, while the steep roads of Devil Mountain Double max out at "only" 15.5%, and the descents avoid major steepness with a max grade of 13%. The initial descent from Mount Diablo summit clearly peaks steeper, but it's so short that the rounding and interpolation scheme used to generate the plot reduces the peak a bit (the focus is on sustained grades, which are more significant).

The result? Devil Mountain Double ends up with more vertical feet, but the descents are faster (more gradual grade means less of the potential energy wasted in safety-motivated braking). And without the real leg-breaking climbs of Terrible Two, pacing on hills is easier to control. What isn't shown here is the wind generally blowing riders down the coast to Fort Ross in Terrible Two. This, combines with less total climbing, makes Terrible Two net faster.

murphstahoe said...

The thing that makes the Terrible Two faster is that you spend a *lot* more time in a paceline than you do at the DMD. The leadin to Diablo is only a few miles while the leadin to Trinity is long and the group generally stays together. Trinity is a shorter climb than Diablo and large groups form in Napa for the run to Calistoga, and reform for the run to the Geysers.

80 miles in and other than a 3 mile climb you are riding in large groups. At the DMD you spend almost no time in large groups - not to mention there are fewer riders overall

djconnel said...

That's an excellent point. And it's not just the position of the flat roads, but also their relative lack, in DMD. DMD has somewhat fewer riders, but they are additionally diluted by having two separate starts, the 5am and a 6am. I am planning on the latter since (1) it will be a better draft at the start, (2) warmer descending Diablo (3) Won't need to carry light up Diablo (not that big a deal, though).

Ygduf said...

and (4) I told you to!

I never did terrible two. The weekend is bad for me, but it always sounded harder. Steep climbing in the heat means nowhere to hide.

djconnel said...

I did DMD in 2000 (report), and froze descending Diablo, bonked on San Antonio Valley, but finished. In 2002 I did it again, fitter and more confident, but it was near-freezing on Diablo (data) and there was hail on Hamilton. Diablo I survived, but I turned back at Mines Road. I'm 2/3 on Terrible Two, dropping out once when I was sick and it was in the low 50's on the course. So I've had issues with the cold, but I always manage to deal with the heat. So you're right: weather is a big factor. Here I'm just looking at the road grade. I should run the courses through my bike speed model, but I'm fairly sure DMD will be slower due to longer distance and more climbing.

PaulS said...

It is also worth looking at the relative ambient temperatures. DMD is held late April whereas TT is mid-June.

Both courses feature long, exposed climbs. On hot, sunny days, thermo-regulation systems are stretched with a concomitant increase in rider heart rate.

If the average temperature of TT is hotter than DMD, this should be taken into account because its effect on heart rate is the same as making the climbing grades steeper.

Dirk dB said...

I remember lots of pacelining on TT, not just the Trinity approach but also on Silverado (towards the Geysers); and in a small group, the highway 1 section can indeed be ridden crazy fast.
For me this would probably somewhat be offset by the heat (I do much better in the cold than in the heat).
Have you done an analysis of Alta Alpina? I think it would be similar to DMD, though much more symmetric, and of course a bit slower due to altitude...