Per the discussion in the NNE Winter Thread at American Weather Forums last night, our most recent winter storm system started up yesterday afternoon. Snow levels were up above 1,000’ to start, but they gradually came down in elevation, and the valleys were reporting a mix of rain and snow in the evening. By 7:00 P.M. we started getting initial slushy accumulations on elevated surfaces down here at the 500-foot elevation, and it took a bit more time for the temperatures to drop below freezing, but within a couple of hours they’d fallen enough that the accumulations really started to take hold. Although we only had an inch or two of snow accumulation in total here at our site, we picked up 0.40 inches of liquid equivalent from the system, so the snow for the local mountains probably had at least a half inch of liquid in it. That’s definitely enough to get into the realm of a modest resurfacing.
When I saw Bolton Valley’s initial early morning report of 3 to 4 inches of snow, I decided that mid-fats were the practical play for today’s skis. Dylan had the day off from work, and I’d planned to get him up if the morning snowfall numbers were substantial enough, but 3-4” was modest enough that I decided to let him sleep in and I headed up by myself to sample what the storm had brought us. Heading up the Bolton Valley Access Road, the elevation dependence of the snowfall was stark: I had ascended above 1,000’ before there was really more than a trace of new accumulation in that area. And even after that, accumulations were slow to increase; it wasn’t until I hit the Bolton Valley Village at 2,000’ that I really felt the accumulation were substantial enough that they were going to make a big impact on the skiing.
I did find 3 to 4 inches of new snow at 2,000’ when I did some checks around the Village, so that was encouraging – if the main base had that much new accumulation at that point, it was likely going to be more in the higher elevations. The Wilderness Double Chair was scheduled to start running at 10:00 A.M., so my plan was to kick off the day’s ski session with some touring before Wilderness lift access was available. I ascended up to ~2,700’ to one of my usual transition points by the time lift-service was underway, so my initial descent was from there. My descent was via a combination of Cougar and Lower Turnpike, and the powder turns were excellent. On low-angle terrain, the new snow was substantial enough that it easily provided 100% bottomless powder turns, and on medium-angle terrain I’d say it was in the range of ~80% bottomless turns. The new snow was medium weight powder in probably the 8% H2O range, and just dry enough that you could keep moving fine on even low-angle terrain.
When I’d descended to the base of the Wilderness Chair it was one wind hold, and they suspected it would be about 30 minutes before it would be back up, so I checked out the other lift offerings. The Snowflake Chair provided some great turns with a few inches of powder over a groomed base on Sprig O’ Pine, and off the Mid Mountain Chair, Beech Seal had excellent natural accumulations that had resurfaced even the manmade snow on the skier’s left to a good degree. Off the Vista Quad Chair, Sherman’s Pass is finally open, so I used it to make my way back over toward the Wilderness terrain, which delivered great natural snow turns as usual. Riding the Vista Quad, I found that the winds were howling above 3,000’, and temperatures were dropping well into the 20s F. It was getting bitter up there.
In terms of snowfall and accumulations, there was at least light to moderate snowfall during my entire ski session, and it was pounding 1-2”/hour snowfall for a while just as I was starting the initial ascent of my ski tour. With continued snowfall and rates like that, it wasn’t surprising that accumulations had jumped up a bit from the initial morning report. Here’s the approximate snow accumulations profile I found from this event as of about midday when I was leaving the mountain:
340’: T
500’: T”
1,000’: T-1”
1,200’: 0.5-1”
1,500’: 1-2”
2,000’: 3-4”
2,500’: 5-6”
3,000’: 6-7”
It was really windy up at the Vista Summit, and I couldn’t get access to the usual protected spots I like to use to gauge depth, so what I’ve put down is my best estimate. Overall though, isolating depths for the snow from this most recent storm was relatively easy because we had some warmth earlier this week that consolidated the top of the snowpack. Like with the last storm though, it’s not a rock-hard subsurface – it’s a spongy interface and the new snow has bonded well to it, so that’s great for the skiing. For the elevations below 1,500’, those depths reported above are actually more than what was there when I initially ascended the access road in the morning, because the heavy snowfall during the morning had added accumulations there that hadn’t been present earlier. I was surprised that the base of Timberline at 1,500’ only had an inch or two of new snow, so even being where the precipitation fell as all snow wasn’t quite enough to get solid accumulations that would dramatically affect the resurfacing of the slopes; you really needed another 500 feet or so to get into the best stuff.
The continued snowfall today was definitely having an effect though, as evidenced by some of the midday updates to the Bolton Valley Snow Report:
10:30am Update: How’s about a couple of rope drops? Glades, Swing, Fanny and more have joined the ranks since we opened this morning, and the snow is still coming down.
12:15pm Update: The ropes keep dropping – we’re adding Bolton Outlaw, Peggy Dow’s, Cougar, Old Turnpike, and Lower crossover to the mix!
This storm was a great way to kick the conditions up some notches as we head toward Christmas, and with a couple more clippers on the way in the coming days plus cold temperatures for the foreseeable future, it looks like conditions will be improving throughout the coming week.
