I’m not sure exactly when the snow from Winter Storm Quest started up around here, but it was well into the overnight hours, and I’m not even sure if I saw any accumulation before midnight. So, waking up this morning to find over 8 inches on the boards for 6:00 A.M. CoCoRaHS observations meant that the snow must have been coming down in the 1 to 2 inch per hour range. There were plenty of large flakes falling at that point, and this morning’s liquid analysis revealed that the water content in the snow was 8.5%, or a snow to liquid ratio of approximately 11 or 12 to 1.
Ty and I got up to the hill just about the time of the opening of the Timberline Quad, and had a great bunch of runs while we waited for Dylan and Colin to join us. During those morning runs, it was quickly obvious that the new snow that had fallen had laid in a massive resurfacing of the slopes. The snow was actually on the dense side due to fairly small flakes up at Bolton Valley, and I’d say it was running a bit above 10% H2O up there. The snow was dense enough that you wanted terrain on the steeper side to really have a good flow on the descent, and that was fine, because in terms of sufficient coverage of the base snow and any underlying obstacles, it didn’t matter how steep the terrain was. On piste, off piste, it didn’t matter; just pick the steepest lines you could find, ski as aggressively as you wanted, and you weren’t hitting the subsurface. We tested many of the steepest lines available on Timberline like the Spell Binder headwall and the Tattle Tale Headwall, and they skied beautifully. We hit steep off piste lines that I don’t usually find to be that great because their pitch is often too much for the quality of the snow or achieving bottomless skiing, and it just didn’t matter.
In terms of surface snow depths, our checks in the 1,500’ to 2,500’ elevation range were about 15 inches if we had to pick a best estimate, but it was really hard to tell exactly how much snow came from just this storm. The new snow was sitting atop snow from other recent storms, and it all just continues to stack and set up excellent surfaces. It snowed all morning, so that kept piling on new snow to the accumulations as well. Total snowpack depth is 40 inches or more above 2,500’, and the snowpack depth at the Mt. Mansfield stake being over 60 inches speaks to that.
Later in the morning we finally met up with Dylan and Colin, and we just went around hitting some of our favorite steepest off piste lines all over the mountain. Timberline had no lift queue for essentially the whole morning, but after about midday, the temperature at those lowest elevations seemed to creep up toward freezing and the snow became even a bit denser. It was somewhat subtle, but you could tell when you skied a run that the powder in the lowest elevations was a bit thicker than it was above 2,000’. After most of the morning at Timberline, we focused on the main mountain for the early afternoon where everything was above 2,000’, just in case Timberline continued to warm and the powder got wet.
We joined up with Parker and his dad for a final run on the main mountain before making a big long run all the way down from the Vista Summit to the Timberline Base. Temperatures clearly hadn’t gotten too high to really ruin the powder because it was still fine all the way to the Timberline Base at 1,500’. Ty, Dylan, Parker and I finished off our day around midafternoon with a visit to the Timberline Base Lodge and some great food from El Gato, and we definitely felt like we’d earned a good meal with the energy we’d put into the day’s skiing.
It continued to snow most of the day, and after a bit of a lull around midday, the snowfall picked right back in the afternoon to the level it had been in the morning. So, we knew there was definitely more accumulation on the way. Back down at the house at 500’ that afternoon we could see that temperatures had definitely gone above freezing because some of the new snow had settled, but the mountain elevations seemed to fare quite well with respect to any melting or settling.