E showing how its done in the powder at Bolton Valley today
An Alberta Clipper hit the New England region yesterday, dropping up to 10 inches of snow in Northern Vermont and continuing the process of covering up surfaces that were hardened by the big mixed precipitation event earlier this week. We had a couple additional rounds of light snow prior to yesterday’s storm, but there still hasn’t been enough new snow to resurface steep, icy terrain. As such, Bolton Valley only has their core set of trails open on the main mountain. I had fun on those trails on Saturday, but it’s still a limited number of options for runs, and with a good amount of new powder available, we decided to earn some turns and get some fresh tracks today. The Wilderness Lift isn’t running yet for the season, so we decided to pay that terrain another visit. Ty, E, and I had a great time there back on November 30th, and with the current firm, icy subsurface, we knew that the moderate pitches and relatively high elevation of the lower Wilderness area trails would be a good bet for powder skiing today.
Now that we’re back into a more consistently wintry weather regime, the Northern Greens snow globe has kicked in, and we’ve had a fairly consistent supply of light fluffy snows in the air. It’s not really substantiating the base snow, but it is creating quite the quintessential Vermont winter scene for holiday visitors, and it’s topping off the slopes with some serious softness. Another burst of flakes was just kicking off when we left the house to head up to the mountain today after lunch, and the snowfall intensity increased as we headed up toward the resort. Up in the Village we encountered temperatures in the low 20s F and steady light but accumulating snows. There were plenty of cars in the parking lots, but since spots were opening up with early afternoon departures, we secured a spot right at the north end of the upper lot.
“The descent was a peaceful glide through silky smooth powder, with only the occasional touchdown on the old base.”
We headed up to the landing on the northwest corner of the main Village complex, and got our gear ready. Quinn passed through and gave us a heads up on conditions – below the powder was a slick, icy base as we’d suspected. We followed a nice skin track up Lower Turnpike, and there were a few sets of tracks on the trail, but a lot of fresh snow remaining. A couple of guys came down the trail and let us know that the steep upper sections weren’t worth the effort because of the ice, right in line with what our beta was suggesting. Depth checks at the start of the ascent revealed 5-6” of powder, which represents the accumulations from this recent clipper and the couple of small bouts of snow that preceded it.
“…you could really feel the way the floatation afforded by our fat skis was letting us ride a bit higher and faster in the powder on those lower-angle pitches.”
We skinned up among steady flakes, enjoying the snowy views of evergreens around us, and when Dylan called for a break ,we stopped at the first crossover to the Wilderness Lift Line at 2,500’. I checked on the conditions on Wilderness Lift Line, and found that it had been hit with wind harder than our last visit – it was clear that although Turnpike had a few tracks, it was the better choice for snow quality. With Ty leading the charge, we continued on up to ~2,750’ before finally putting a halt to the ascent because we were getting into icy, scoured terrain. The snow depth up at the point had increased to roughly 7 inches.
The descent was a peaceful glide through silky smooth powder, with only the occasional touchdown on the old base. The pitch and powder were essentially perfect, although the powder was deep enough that Dylan would sometimes have difficulty keeping his speed up. Dylan’s Telemark skis (Völkl Gotama Juniors) are fairly wide, but nothing like the Black Diamond Elements and AMPerages that E and I were using, and momentum issues aside, you could really feel the way the floatation afforded by our fat skis was letting us ride a bit higher and faster in the powder on those lower-angle pitches. I was curious to see if E had noticed the effect, so I asked her how she felt about the speed of her skis on the descent. She initially thought that they were very fast, and figured it was because they haven’t been used for too many outings and had been waxed. I explained that a good part of that was actually from the floatation that the skis provided. Ty invented a new descent technique where he would kneel all the way on the tips of his skis with both knees, and in the powder it gave the illusion that he was just kneeling in the snow with no skis and flying down the mountain. We’ll have to get some video of that at some point, because it’s quite a hoot.
Ty dives in
We ended our descent back at the landing on the northwest corner of the Inn, and discovered that it’s a great spot to be if you want to catch up with what’s going on at the resort. After seeing Quinn at the start of our tour, we ran into Cam and later Josh at the end of the tour. We got to chat about the current state of the conditions, being happy that there are still great options out there for powder, but hoping that we can get some larger storms in here to start building the base. We’re in an OK pattern for maintenance over the next couple of days, and there’s a chance for getting in on snow from a coastal system as we head into Sunday night. We’re certainly a bit fat to the northwest to really jackpot with that storm, but if we can get some base-building synoptic snow out of it, it will really be a step toward terrain expansion.
Yesterday E had her training day for our school’s ski program at Stowe, and boy was it cold – it was below zero F for the entire morning. I’d sent E off with plenty of hand and foot warmers, and she made use of them. She actually cracked the lens in her goggles toward the end of the morning, but by then everyone was just about done anyway. I don’t think there were many takers for afternoon turns once the requisite training items were covered in the morning.
Things were a little different for my training day today – temperatures were rising through the teens F, and oh yeah, there was a bit of a snowstorm in the intervening period. This storm was one of those that comes out of the Ohio Valley and redevelops off the New England coast, and it brought up to 19 inches of new snow for the Vermont ski areas. Snowfall totals were a bit lower for the Northern Vermont ski areas, generally approaching a foot, but as my snow analyses had shown, there was plenty of liquid equivalent in the snow; as of this morning, we’d picked up close to ¾ of an inch of liquid in the snow and the density was close to 10% H2O. The snow was of course quite dry with the cold temperatures in the area, but it certainly wasn’t fluff that might be prone to blowing away.
“The snow depth at the Mt. Mansfield Stake isn’t quite to that 24” mark yet, but people are definitely starting to ski those areas of early season trees.”
For today’s training session, Claire assigned me to the level eight group, and when the instructors were dividing up the trainees in that group, they further broke them up by those who had already skied five days or more, and those who hadn’t. Although I’d yet to ride a ski lift this season, I’ve been out several times already, so I joined the former group, with Steve as our instructor.
“During today’s session, Steve brought us into Sunrise Glades, Birch Glades, and Lower Gulch Glades, and they were all in
pretty good shape.”
With all the new snow, Steve’s plan for the day was to let us ski a lot. Instead of working on drills, he wanted to work on group management (i.e., how do the coaches effectively manage their groups of students on the slopes) in between the skiing. This was actually a nice change of pace, since E and I have had plenty of sessions with drills for both us and the students over the past few training sessions. One new group management technique that I learned today was for brining the kids into new areas of trees. What Steve likes to do is to show the students the entrance to the glade, but instead of entering that first time, he goes around to the exit of the glade via the trails. That way, the students know what is in store, and are ready with a little more directional orientation for when they actually do ski the glade. We talked a lot about strategies to use when bringing the kids into the trees, and it was a good fit for the trainees in our group, because many worked with the advanced students and were indeed doing a lot of off piste skiing. Steve also worked on the partner strategy for ensuring that everyone is accounted for at each stop. We actually had a real-time demonstration of its effectiveness, since my partner John had misheard our lift destination on one run and ended up at the Gondola instead of the Fourrunner Quad. Since we knew he was missing, I was able to run over to the Gondola and retrieve him.
Grabbing the Tele boards for some afternoon turns
In terms of conditions, naturally they were best early on – we had a couple of great runs down Perry Merrill with good packed snow, and chowder and powder off to the edges. It was nice that Steve just let us rip it up. I generally found 12” of powder whenever I looked in undisturbed places, which is presumably the combination of snow from this storm and that frontal passage the other day. The snow depth at the Mt. Mansfield Stake isn’t quite to that 24” mark yet (22” as of this evening’s report), but people are definitely starting to ski those appropriate areas of early season trees. During today’s session, Steve brought us into Sunrise Glades, Birch Glades, and Lower Gulch Glades, and they were all in pretty good shape. If you were going for lines of fresh powder, you wanted to be on your guard a bit since there are still some obstacles about, but in many spots it was hard to tell that it was so early in the season. In areas that had seen skier traffic and had packed snow, you could just ski it and really didn’t have to worry about coverage issues. In any event, it was definitely nice to be back in the trees. Indeed those runs listed are the more moderately pitched, well maintained glades that are amenable to these earlier visits, but they’re very low on the mountain and that says a lot about the current state of the snowpack.
After some lunch and paperwork at the Great Room Grill, Steve said that we were done, but that anyone who wanted to could meet with him at 1:00 P.M. and work on identifying weaknesses in student’s ski technique and how to remedy the situation. Having done a lot of that over the past few sessions, I decided I’d just grab a pair of my Tele skis from the car and take a final run or two before heading home. I was just going to grab my mid fats and head back over toward the Chapel Glades, but then wondered if the Sensation Quad was open – if it wasn’t, it might be a nice place to earn some turns. With that in mind, I grabbed the fat boards off the rack, finding everything covered in a layer of new snow that had fallen during the morning. Once I checked in at the lift status board at the Spruce Peak Base, I saw that indeed the Sensation Quad was running. That meant that the terrain over there on Spruce would likely be pretty packed out, but I decided to just go for it instead of making yet another trip back to the car.
I took a trip up the Sunny Spruce Quad and made my way over toward the base of Sensation. There were actually very few people over in that area, but in terms of traffic, the damage had been done earlier in the day. There were still pockets of powder off to the sides of trials, but with Main Street closed for snowmaking, terrain was limited. Even the hiking terrain above the top of Sensation was tracked up, so people had clearly been doing what they could to get some powder with the limited acreage that’s currently available on Spruce Peak. In spots where the snow surface was down to manmade snow, the fat skis were definitely a poor tool for the job. I ended up just going with alpine turns in the areas where the snow was firm like that, because getting the fat skis on edge in a Telemark stance in those areas felt like trying to get a snowboard on edge on icy terrain. They’re just not meant to do that well. I will say that I notice the deficiencies of fat, rockered skis much less when I ski them alpine, so that may be one reason that so many people are willing to use them as more all around skis (or they just go in with the recent marketing trends and figure that’s the way it is). With my legs cooked from the morning’s runs, I was very ready to call it a day after that trip to the bottom. I really would have liked to venture over to the snowfields above Meadows for some powder, but they had that area roped off because of snowmaking below. It was looking so good in there with the tracks from when it had been skied – hopefully I can get in there on my next Stowe powder day.
Getting after some of that leftover Thanksgiving powder
For the valleys in Northern Vermont, our first big winter storm of the season hit the area this week, and it created some potential holiday travel woes because of its occurrence so close to Thanksgiving. The storm was essentially complete by the time we traveled on Thanksgiving Day, but with 8.2 inches of snow, and 1.62 inches of liquid equivalent, it had certainly bolstered the snowpack in the yard and changed the look of the landscape. While the storm did have some mixed precipitation and rain in the middle, it was quite a nice gain in snow for the mountains, with some of the ski areas in the Northern Greens picking up more than foot of snow. And, as is often the case, the final volley from the storm consisted of a good shot of dry powder that sat well atop some newly added dense base to create some great Thanksgiving Day skiing.
With our holiday traveling done, we finally had the chance to get out today and sample some of the new snow. Dylan was away at a friend’s house, but E, Ty, and I headed up to Bolton Valley to earn some turns. They had reported 9 inches of new snow for Thanksgiving morning, and as we headed up to the Village, we stopped in at the base of Timberline at 1,500’ to check on how the snow had settled in down at that elevation. The depth of the powder was 3 to 4 inches over a good base, and we could see that there had been plenty of ski activity on Timberline’s slopes. Continuing on up to the Village at 2,100’, we found that the snow had increased to 4 to 6 inches in depth.
“The powder skiing was every bit as good as what I’d experienced on Sunday…”
Having experienced some good snow on Turnpike on Sunday, I figured that we would check that out again today. Of course, with it being two to three days since the snow fell, plenty of skiers and snowboarders had been out on the trail, a lot more than the single track I’d seen on my last trip. We were treated to a nice skin track, but most of the powder was tracked out, so we definitely kept our eyes open on the ascent for lesser used options. We ran into Cam at the top of Lower Turnpike, and chatted about the mountain’s opening in a couple of weeks. If we can stick with the current weather pattern, things are looking quite good.
Like I’d done on Sunday, we stopped our ascent around 2,900’ on Turnpike since the terrain above that level was rather windswept, but snow depths had increased to roughly 6 to 8 inches, and combined with the base, there was easily over a foot of snow sitting there in many places. On the ascent I’d looked at the snow on Cougar and the Wilderness Lift Line, and I’d seen only a couple of tracks, so we worked those into our descent. The powder skiing was every bit as good as what I’d experienced on Sunday, and I was glad that we found plenty of untracked snow for Ty and E. Ty was putting together some great turns on his Teles, and I think his skiing was helped by the fact that he was in high spirits. E had her first chance to get on her Element skis with her new Telemark boots, and she definitely felt a big increase in control that she’d previously lacked with on her fat skis with her old boots.
E finding much more ability to drive her powder skis today with her new boots
Today was a great, mellow outing, just like you’d expect pre-season at Bolton Valley. Along with Cam, we saw a couple other pairs of skiers, and they all appeared to be experiencing that same vibe. We’ve actually got our next small storm coming through tonight, and it’s supposed to persist into tomorrow, so perhaps we’ll get a freshening of the powder that will set things up for more turns. It’s been a great November of skiing around here, and now it’s on to December – let’s hope it can follow suit.
Some of Bolton’s powder today, thanks to yesterday’s Alberta Clipper
I hadn’t yet been up to Bolton Valley for turns this season, because based on what the web cams have been showing for all the storms thus far, the slopes at Stowe have seen bigger accumulations and better coverage. This time around though, things seemed more equitable. I’d seen the general state of coverage at Stowe when I stopped there for a tour on Thursday, so I had a good idea of what was down after the additional 4 to 6 inches reported this morning due to the recent Alberta Clipper. I could see from the Bolton Valley Live Web Cam that, although there was definitely some wind pushing the snow around and scouring some areas, accumulations were at least in the same ballpark as what Stowe had seen. As long as I went for a protected section of the mountain, it looked like coverage was going to be sufficient for some good powder turns.
“If you’ve ever heard of the ‘no chain’ expression in cycling, for when the pedaling seems effortless, then the expression for today’s ski outing would be ‘no width’.”
I wasn’t initially sure if I’d want to head out to the slopes today, since just a few inches of snow were expected from the clipper, but more due to the fact that the coldest air of the season has moved in on the back of this storm. With significant winds as well, it sounded like it was going to be brutal out there on the mountain. The reality was though, that this was November cold, not January cold. When we were out in the yard early this afternoon taking some potential Christmas card photos, the temperature was in the low 20s F and it was reasonably comfortable. It was going to be colder and windy on the mountain, but it seemed like great weather for earned turns.
Village views of changing seasons on today’s ascent
I headed up to the mountain in the mid afternoon, made a quick Timberline stop at 1,500’ to measure the snow depths, finding 2-4”, and then parked in the top tier of the village lot around 2,100’. The temperature was in the mid teens F, and snow depths had increased to around 4-5”. After a conversation with Quinn subsequent to one of our recent October snowstorms, he’d mentioned going for an outing on the Turnpike trail, and with today’s accumulations and wind, that sounded like the perfect, protected option for an afternoon ski tour. I found a nice skin track that had been set in place by a prior skier, and it brought me up through some beautifully protected terrain. I think this was actually my first time ascending Turnpike on skins, and it is indeed a nice route. It’s got that type of modest pitch that makes you feel like you’re out for a stroll and hardly doing any work. The coverage was looking decent, and there was even a bit of old base snow that was initially sporadic, but increased as I got higher on the mountain. At 2,500’ I found snow depths in the 5-7” range, and I continued to follow the skin track up to around the 2,800’ mark, where it terminated. My plan was to ascend as high as the quality of the snow dictated, stopping when the winds or terrain outweighed the elevational increase in accumulations. Whoever had made that skin track had the right idea, because at 2,800’ it was starting to get to that point. I pushed on to 2,900’ at the top of Turnpike, and called it there because the next pitches on Peggy Dow’s were clearly steeper, rockier, and exposed to the wind. The snow had definitely been getting deeper though, and I’d say the depth of the powder up there was 7” or more.
Enjoying a snowy scene at the top of today’s tour
I was unsure exactly how the descent was going to go. I’d chosen Turnpike because it has that protection from the wind, but also a nice combination of blue/green pitch and a generally grassy, not rocky, surface. The new snow was quite dry, but I’d brought my fattest Tele boards, my AMPerages at 115 mm underfoot. I was banking on that width to keep me afloat. I dropped in for my first turns, and another aspect of the snow conditions quickly became apparent… the snow was indeed light and dry, but it was cold enough that it was also slow. I was worried that the lack of glide in the dry snow was really going to affect the descent, but as soon as I hit the first steeper pitch the turns started flowing. Coverage was definitely adequate, and I touched down on the old base or grass very infrequently. Turns were very smooth, and as I was gliding my way down, I was confident that I’d made the right ski choice for the day. In fact, it felt like the perfect ski choice, and amazingly, given the situation I think I would have gone even fatter with the skis.
Today’s snow offered up some great turns even on the bottom half of the mountain
People are always pushing the fattest skis for the deepest powder, and that definitely makes sense in terms of floatation, but they’re good for so much more. Indeed I find them absolutely horrible on firm snow; it’s a lot like trying to ride a snowboard on a hard surface. But today didn’t have anything to do with firm snow, it was all powder… light, dry powder, and the fatties shone in just modest depths in multiple ways because of their floatation. First, despite the airy snow, they were keeping me off the subsurface and allowing bottomless turns. Second, and this one was totally unanticipated prior to discovering how dry and slow the snow was, they were allowing me to plane at the more modest speeds attained on today’s moderate pitches. That kept me going on lower angle pitches, really enhancing the fun factor, and it’s been one of the few times when I’ve had the feeling that even wider skis wouldn’t have been overkill. If you’ve ever heard of the “no chain” expression in cycling, for when the pedaling seems effortless, then the expression for today’s ski outing would be “no width”. Even though it was all Telemark turns, in which transitions are much slower than alpine, things seemed to move effortlessly from edge to edge during the turns, and it all just flowed.
Looking ahead, we’ve got a small system expected to affect the area tomorrow night with some snow, and then a much more significant system as we move toward Thanksgiving. That one could be messy with some mixed precipitation, but hopefully we’ll get some snow out of it as well.
You had to hunt a bit more today due to skier traffic and wind, but great powder is still out there.
When it comes to the Northern Greens, it can be hard to know when a snowstorm is complete. Just when you think an event is finally winding down, these mountains can cause it to fire back up and dump another foot of snow. In this case, that’s just what happened. After Tuesday’s great outing on Mt. Mansfield, I figured there wouldn’t be enough additional snow to lure me back out on the slopes too quickly, but I was wrong. While people anticipated a couple of additional inches to fall as the event finished up, a foot of additional snow was reported at Jay Peak, and another half foot at Stowe. There was already plenty of base in place, so after hearing first hand reports from some of our students at UVM about the great skiing brought about by the additional snow in the mountains, and seeing pictures like the one Powderfreak posted from Jay Peak, I heard the slopes calling again.
A view on the Liftline ascent
So I headed out to Stowe for another early morning session, and the temperature was definitely warmer this morning than what I encountered on Tuesday – it was even a bit above freezing in some of the mountain valleys, and around the freezing mark at the Midway Lot (~1,600’). The snow was still dry, but what was immediately evident was that the snow conditions aren’t as pristine now as they were a couple of days ago. The decrease in quality I saw was due to a combination of skier traffic and wind, and in those areas that were affected, the fresh fluff that fell yesterday was beaten down into something much denser. Since the snow had that wind crust in areas, it was a little harder to efficiently probe the snowpack depths on my ascent, but in general nothing has really melted over the past couple of days, and the snow depths with respect to elevation seemed fairly similar to the numbers provided in Tuesday’s report. I went with yet another ascent route today, and ascended the skin track up Midway that continued on to Liftline. This is the route that I had used last November, and it was a little frustrating at that point because I was using skins cut to Atomic RT-86s that were a bit too narrow for my AMPerages. I’ve got full-width skins now, so the issues from that day were resolved, but I was still slipping a bit up part of the Liftline skin track, and I’ve decided that it’s due to the fact that people have put in a skin track that’s just a little too steep. People should incorporate a few more switchbacks on the Liftline route to get a more reasonable grade on the ascent; it typically ends up being more efficient in the long run.
In any event, while I’d seen some decent, soft looking snow on Midway, Liftline was exposed and was riddled with wind crust. I watched a group of three guys descending the trail, and it was obvious from how little they were sinking into the snow that the wind crust was indeed substantial. One of the three appeared to be an excellent Telemark skier, and at one point he went head over heels dealing with the challenging snow. Seeing that spectacle, I decided to go for something more protected, and Goat came to mind. Some wind had still gotten in there, but it was far more protected than Liftline. I’m more leery about trails like Goat in the early season, since it holds a lot of interesting rocks, but as I probed along the skier’s left of the trail, I found a solid two feet of snow. That definitely looked sufficient for skiing the trail.
“The farther down I went on the trail, the more protected and fluffier the snow was…”
With still a little trickiness to the snow, and the narrow, bumpy, rough and tumble nature of Goat, I found myself making plenty of alpine turns at first. I’ve got to say, I’d love to have another pair of these AMPerages mounted alpine, because they were a heck of a lot of fun in that snow – they created such a stable platform. The farther down I went on the trail, the more protected and fluffier the snow was, and I finished off with some beautifully soft turns on Lower National, which had seen a lot less traffic than the bottom of Lower Nosedive. Coverage remains quite good, and I even passed through some woods on my traverse to Lower National that could easily have been skied. That’s certainly consistent with the snow depth at the Mt. Mansfield stake hovering close to that 24” mark.
It was definitely warming up when I left, and I felt a little stickiness in the snow in the very lowest elevations (last couple hundred feet), so I’d say the snow down there will lose some of its fluffiness. There’s still plenty of snow out there for those that want to make turns, but you just have to pick the lesser used areas now if you want untracked snow. It also may mean going a bit higher to get into the winter snow, depending on how high the freezing line crept upwards today.
“If someone had asked me about ski choice for today, I would have just said to take your fattest skis, whether they’re brand new or not.”
The front came through overnight as expected, dropping about an inch of snow down at our house, and more in the higher elevations. Things seemed to have come together, so I decided to head out to Stowe for an early ski tour. Temperatures were generally in the mid 20s F as I traveled through the mountain valleys, and there were no issues with the roads until I started climbing up toward the mountain around 1,000’. Above that elevation I found enough packed ice and snow that it warranted a bit more cautious driving. At the Midway Parking Lot (1,600’), the temperature was 20 F and there was light snow falling. There was the usual crowd of early morning skiers heading out and returning from the slopes, and I suspected it would be easy to find a nicely established skin track on any of the typical routes.
Heading out from Midway for turns
Since our last outings a couple of weeks ago focused on the Gondola side of Mansfield, I decided to mix it up this time and took the well established skin track that headed up Nosedive. It was well packed, and made all the sweeter by the fact that for much of the ascent there was a parallel boot pack available for anyone hiking without skins. The snowpack increased very quickly with elevation on the bottom half of the mountain, and I found the following depths during my ascent:
1,600’: 4-6”
2,000’: 8-10”
2,500’+: 12-18”
Above ~2,500’, I was essentially well into the deep stuff, and the gains in snow depth weren’t huge beyond that. Of course, when you’re already talking 12-18” of snow with plenty of substance to it, the lack of additional increases isn’t a big deal. At the top of Nosedive, I continued my ascent up the Toll Road for a few more minutes to check in on the depth of the snowpack at the fabled Mt. Mansfield Stake. At ~3,700’, the stake showed at least 17” of snow, and I generally found 18-19” there when I probed on the edge of the Toll Road itself, so indeed the snow depth up there was right around a foot and a half.
It’s really a nice sheltered area up along the road by the stake, and since the snow wasn’t perturbed by wind, you could definitely get a sense for where the snow stood with respect to quality. Indeed that quality was looking very good. As one would expect with the latest round of fluff, the snowpack was right side up with the lightest snow on top, and it was primed and ready for some turns. Big, dendritic flakes were falling while I was there switching over for the descent, and I stood and savored the moment for a while before pushing off down the road. I crossed over toward the Fourrunner Quad, and the summit area was awash in manmade snow. I didn’t even see that many guns going up there – I think the resort has already been able to hammer that area with manmade snow with the cold temperatures we’ve had.
Hayride today
So now I’m left with just one more thing to discuss, the pièce de résistance for the day… the descent. While ascending Nosedive, it was clear that there had been a huge bolus of snow dropped above 2,500’, so coverage wasn’t going to be an issue. Temperatures were certainly not in question either, since it must have been somewhere in the teens F. That left the aspects of snow density and the effects of the wind, and based on the turns I was seeing by people descending Nosedive, it looked like the skiing was going to be fine, even if not sublime. But, I suspected I could do better. There had definitely been some wind on Nosedive that appeared to have packed out the snow a bit. With that in mind, I decided to roll the dice and check out another descent route – Hayride. I’d had good luck on Hayride back on April 10th of last year, when Mt. Mansfield got laced with over two feet of dense, resurfacing snow. It was actually the challenge of that snow on Telemark gear that was one of the final nails in the coffin in convincing me to finally get some fat, rockered skis for Telemark use. I could already tell that today’s snow conditions were nothing like what I encountered on that April outing – with the new fluff, this snow was notably drier. I hadn’t actually thought that it would be anywhere near the quality of what we had last November on the 30th, but after a few turns on Hayride I found that it was certainly in the same league. And indeed we’re talking quite the league – Hayride was sheltered from the wind, so turn after turn after turn I was able to push hard on the deep snow. It gave way, let you sink in, but pushed back with just enough force to keep you from getting to the ground. With 115 mm underfoot and judicious line choice, I think I touched down twice on something other than snow on the entire descent. Just like last November, the AMPerages were totally in their element, letting me play around in the deep snow on a remarkably stable platform. They helped out immensely with fore-aft balance, and I can recall some specific instances where I was saved from what easily could have been a face plant. If someone had asked me about ski choice for today, I would have just said to take your fattest skis, whether they’re brand new or not. Today, a combination of fat skis with the available snow would be plenty to keep you safely above most underlying obstacles. You’d probably end up having a heck of a lot of fun as well.
Taking advantage of the October powder today at Stowe
Well, we definitely got to witness Mt. Mansfield flexing the snowfall muscles today – despite the fact that we know this mountain’s ability to reel in snow, it just never gets old. Stowe delivers. I’d certainly been contemplating some turns, but after catching Powderfreak’s comment this morning about how it was dumping at the ski area, and then checking the web cams myself to see snow falling hard and fast at the base, that sealed the deal. Ty has been chomping at the bit for some skiing, so he joined me and we headed out in the early afternoon. Temperatures were in the low 40s F in the valleys, and the precipitation was generally light rain. The Worcester Range was visible to the east, white with new snow, but off to the west, a white haze hung over the spine of the Greens and we could see that it was definitely still snowing up there. The precipitation remained rain as we headed up the Mountain Road, but at ~900’ elevation near Northern Lights Lodge, we started to see leftover snow accumulations along the sides of the road. The snow on the ground continued to build, and by the time we pulled into Stowe’s Midway Lot at ~1,600’, we found 2-4” of snow on the ground up on the grassy slopes above. The temperature had only dropped to 38 F, but the precipitation had changed fully over to a light snow comprised of small flakes.
“…despite the fact that we know this mountain’s ability to reel in snow, it just never gets old.”
We changed things up in terms of equipment today, and instead of Tele, we went with alpine gear using Alpine Trekkers for the ascent. I haven’t had the Trekkers out in a while, but it was time to bring them back into service; I’ve finally moved my old Volkl CMH Explosiv fat skis to rock ski status, and I was eager to try them out on one of these early days. My only Tele rock skis are my old skinny Rossignol Hellgates, and with a waist of just 70 mm, they’re really not a great tool for these early season powder days. Combining Tele + skinny + variable early season powder is certainly a recipe for challenge. Another reason to go with the Trekkers today was that Ty’s boots and bindings are now large enough to easily accommodate Trekkers. He’s not at the stage yet with his Tele skiing that he’s ripping up early season, potentially inconsistent powder with aplomb, so going alpine on the tour would be much more enjoyable for him. We decided to go with his carving skis instead of his powder skis for the setup, and fortunately we were able to get a good fit out of his skins from his Telemark skis.
As usual, the Trekkers were great on the ascent. Although going with alpine skis and Trekkers is notably heavier than Tele, it’s typically not a big deal unless you’ve got huge tours to do. My biggest issue was with my skins – I’m not sure if the old skins for my CMH Explosivs have lost their water repellency, but whatever the case, today’s conditions had them catching and carrying a bunch of snow at times. I’d have Ty clean the underside of the skins off for me when we stopped, but we could never quite keep them from re-accumulating a coating of snow. Fortunately, Ty’s skins had no issues in that regard. The snow on the ground was quite wet at the base, but it dried out substantially as our elevation increased. We ascended via a bit of Perry Merrill, and then Gondolier to the Cliff House, and we observed the following snow depths with respect to elevation:
Aside from Ty’s first chance to try out Alpine Trekkers another new addition on this outing was his own Measurement Ski Pole. I put together measurement poles for both Ty and Dylan this fall, and it was great having Ty reporting depths along the ascent – with two observers we were able to collectively decide on the best approximations of depths to create the list shown above. It also kept Ty very interested in going higher, even if just to see how much deeper the snow was going to get. Although Dylan didn’t go out to the slopes today because he was off with E doing some shopping, based on Ty’s experience I think he’s going to have a lot of fun with the measurements on our next outing.
A shot from up near the Cliff House
It was around 4:30 P.M. when we hit the top of the Gondola at ~3,600’, and the snow was coming down with some good intensity. It wasn’t quite inch an hour snowfall since the flakes were still fairly small, but it felt like it was somewhere between ½ and 1 inch/hr and it was quite impressive. We took shelter under the Cliff House to gear up for the descent because of the intensity of the snowfall, but there was almost no wind, so it was nice to hang out and watch the flakes pour down. With the late hour, thick clouds, and hefty snowfall, it had that dusky feel of December in the north. Ty and I discussed how it just as easily could have been December with all the snow. Another great milestone for Ty was the fact that this was his first full ascent to the Gondola, and it was nice to see that he still had plenty left in the tank at the top. We put a call in to Mom to let here know that we’d be descending soon, but also to let her know about Ty’s accomplishment.
Extolling October Snow
We fueled up with some food and drink, but didn’t loiter too long because we knew the light was going, and we had to get in some shopping for dinner on the way home. Soon, we headed off down Perry Merrill, and one of the more challenging aspects wasn’t the snow, but the intense snowfall and reduced visibility. I’d been sort of soured on my CMH Explosivs the last time I’d used them, because they felt heavy and long and I just didn’t want to push them around, but today I’d say there was a newfound love for them. For whatever reason, perhaps because we were out on open trails instead of tight places, they felt great today – fat and stable, and just what one needs for the inconsistent early-season snow. Ty had to work hard on his skinnier skis to handle the powder, but we worked on technique on the way down and he made some great turns. I told him that if he could ski the powder on these skis, he’ll be cranking away when he’s on his powder skis.
That more intense snowfall was with us on the entire descent, and the freezing line had gone down as well. Back at the car, heavy wet snow was falling, and the temperature was down to 35 F, three degrees below where it had been when we’d arrived. It was the sort of precipitation that soaked you very quickly once you were out of your Gore-Tex, and we both got pretty wet putting away the gear and switching out of clothing. The precipitation eventually changed back to rain as we dropped into the valleys on the drive home, but it was raining quite hard at times. There had already been some additional snow accumulations down to lower elevations by the time we were leaving, and the snow in some of the lower elevations actually looked better than it had on the way up due to some new covering. Overall the quality of the skiing was quite good, especially up high, and it could be even better tomorrow with more snow falling tonight.
Temperatures at the Midway area had dropped three degrees while we were out on our ski tour, and a driving, wet snow greeted us back at the car.
Waterbury snowfall for the 2012-2013 season – broken down by month
The last snowstorm of the 2012-2013 winter season extended all the way out to Memorial Day weekend to produce some great late season skiing, but now that we’re well into summer and all the snow has melted, we can look back at how the winter went down at our location in Vermont’s Winooski Valley. The main focus in the seasonal analysis below is on snowfall, but snowpack and temperatures will be discussed as well. In this post I’ve hit on some of the highlights that came out of the data, and attached our various plots and graphs, but to get to the full data set, you can use the following link:
Thankfully, this past season’s snowfall (144.2″) marked a notable increase over the previous season (115.3″), but the total snowfall for 2012-2013 was still less than 90% of average, so that’s not likely to lift the season into the category of “great” winters. In addition, the amount of snow on the ground at the house last season didn’t help to improve the winter’s standing. Using the value of snow depth days as an integrative way of representing the season’s snowpack, one finds the 2012-2013 winter season producing a value of 729 inch-days, less than half the average value, and right down there in the basement with the well below average 2011-2012 season (688 inch-days). And, if the overall snowpack depth hadn’t already undermined any chances of redemption to an average level, the 2012-2013 snowpack secured the season’s ignominy by reaching the lowest value we’ve seen in January and February (3.0″), and coming within a hair’s breadth of melting out in the area around our measurement stake at a record early date in mid March:
This past season’s rather meager snowpack at our location in Waterbury (red line) relative to average (green shading)
Often, each month of the winter/snowfall season has its own unique flavor with respect to the weather, so one method I like to use to get a feel for the winter is to look at it on a month-by-month basis. Again, the focus below is on snowfall at our location, but snowpack is also considered, as well as mountain snowfall/snowpack and the associated effect on the local skiing. I’ll have a separate 2012-2013 ski season summary coming up, so I’ve kept the ski discussion minimal here in anticipation of a more thorough discussion in that report. The month’s total snowfall is listed at the start of each section below for reference:
Snowfall: 0.1″ – October snowfall isn’t reliable enough down at our elevation to be factored much into the seasonal assessment, but this October was on the weak side, with just a tenth of an inch of snow, vs. the mean of roughly an inch. Regardless of this, there was still enough for the needs of companies like https://divisionkangaroof.com/areas-served/gainesville/ with the weight of the snow causing damage to some roofs. One small feather in the cap of 2012-2013 is the fact that the first accumulating snow fell on October 12th, which beats out 2010-2011’s October 15th snowfall by three days, and now represents the earliest measurable snowfall I’ve recorded here at the house since I started monitoring the weather in 2006.
Snowfall: 6.3″ – November snowfall came in just a bit below average this past season, so certainly not remarkable, but notable in that it was probably about as average a November as we’ve seen. November has typically been feast or famine when it comes to snow. We actually had a total of five snowstorms in November, but a small to moderate storm of 4.4″ at the end of the month contributed the bulk of the monthly total as well as some of the first great skiing of the season in the mountains.
Snowfall: 49.5″ – December held the first lengthy, redeeming snowfall period of 2012-2013. Although the first half of the month was extremely poor on snowfall (just 2.2″ of snow at the house), from the 16th of December onward, temperatures got cold and snow came in for a dramatic change; close to 50″ of snow fell on us in the second half of the month, and as a whole the month actually wound up several inches above average. Those in homes with faulty or no heating in place are likely to struggle with the crushing cold at this time of year which is why it’s so important to conduct regular maintenance on heaters so you’re not left to suffer over winter. Reaching out to the likes of these professionals could help with this – siriuspac.com/heating-repair-service/. A problem left unaddressed could snowball into substantial damage and become more costly to repair over time so it’s well worth acting on it as early as possible. We received our second (15.5″) and fourth (11.7″) largest storms of the season during that stretch, right near Christmas and just a few days apart, so needless to say, the snow was there to set quite the holiday mood in the valleys and up above on the slopes.
Snowfall: 21.9″ – January continued that good, snowy weather pattern in its first week, albeit to a lesser degree than December, but unfortunately that modest first week ultimately wound up representing roughly half of the month’s snowfall. The second week featured a couple of substantial thaws with no measurable snow, and in fact we received no accumulating snow at all for the period between January 7th and 16th, a very long stretch for the mountainous areas of Northern Vermont during the winter. The third week of January offered just a few small systems, and the fourth week was arctic cold with minimal snow. The final week attempted to recoup the losses with a modest half foot storm, but it was too little too late – the month ended with just 21.9″ of snow, by far the lowest January in my records. The combination of very low snowfall and two January thaws was very deleterious to the valley snowpack – after coming down from the depths achieved in December, the snowpack depth at our location never even reached 10 inches again during the month, and got as low as 3.0 inches. That is ridiculously close to losing the winter snowpack in January, definitely the closest we’ve come based on my records since 2006.
Snowfall: 31.4″ – February was again below average in snowfall, partly due to the continuation of the dry arctic pattern in the first week, and it wound up missing the mark for the lowest February in my data set by less than an inch. Although that persistent dry pattern didn’t make for a very snowy first half of the month, our third largest storm of the season (12.6″) hit in the second week. It was still a rather modest storm, but at least it did break that one foot mark for accumulation at the house. By the end of the third week of February, the snow depth at the Mt. Mansfield stake actually poked above average for the first time in about a month and a half – but it was only by a couple of inches, and it quickly went back below average as the snowpack sat there essentially stagnant for an entire month. On February 21st, the snowpack was at 65″, and roughly a month later on March 18th, it was still at 65″, without any major consolidation of more than a few inches. That’s stagnant. Our snowpack at the house languished similarly, never even getting above 10 inches of depth during that stretch – and that’s a time of year when it is usually building to its peak of the season. The carryover of the low snowpack from January also set the lowest mark (3.0″) for snowpack that we’ve ever seen in February.
Snowfall: 4.2″ – April was even a couple inches below average for snowfall, but temperatures stayed cool enough to keep the winter season rolling along, and that’s what really helped make the period wintrier. We didn’t have any notable April snow accumulations down at our elevation, just a couple of small ones on the 2nd, and again on the 12th – 13th, but the mountains continued to get fresh snow right into mid month to keep surfaces in great form and the Mt. Mansfield snowpack robust.
Snowfall: 0.0″ – There was no accumulating May snowfall down at the house this season, but that’s not too much of knock on the Month, because not getting snow in May is more the norm than actually getting snow. The mountains did get that beautiful Memorial Day weekend storm though, and the late season powder skiing was mighty fine. Although I can’t factor that directly into the analysis for the valley, it was quite cold in the valleys at the end of the month, and close to even snowing there.
There were a couple of other interesting notes with respect to snowfall this season:
1) Storm frequency and average storm size: Despite coming in below average for snowfall, the 2012-2013 season offered up a healthy 51 accumulating snowstorms, almost up there with the 53 storms we received in 2007-2008. Of course, to come in below average for snowfall with that many storms indicates that the average snowfall per storm was down, and indeed it was. At 2.8″/storm, 2012-2013 ranks down there with 2011-2012 (2.6″/storm), the only odd seasons out compared to the more typical seasons up near 4″/storm. For whatever reason, this season’s average came in on the low side. This is presumably due in part to many of the everyday events being on the small side, but also due to the lack of bigger storms, which is covered in point #2 below.
2) Storms with double-digit snowfall: It’s certainly an arbitrary and subtle distinction, but after looking through my data, I noticed an interesting trend with respect to each season’s largest storms for our location. In my season summaries, I always make a list of the top five storms of the season, and when the season seems to have gone well, all of those top five storms have been in the double digits for snowfall. In fact, the “best” seasons thus far have been able to surpass that five-storm threshold. For reference, here’s the top five list for this season, with the links to the detailed web pages for each storm:
Indeed, if we look at the number of storms with double-digit snowfall by the seasons, we see an obvious trend. With the number of double-digit snowfall storms listed in parentheses after the season, one notes those “good” seasons – 2007-2008 (6), 2008-2009 (7), 2010-2011 (7) seemed to find a way to exceed five double-digit storms, whereas the poorer snowfall seasons – 2006-2007 (4), 2009-2010 (2), 2011-2012 (3), 2012-2013 (4) just didn’t. Surely the law of averages comes into play here to some degree – seasons with patterns producing lots of snow likely have a greater chance of getting a big storm in here, but that’s not a given. It’s also very suspicious that those seasons that come in sort of in that middling ground like 2006-2007 and our season of interest for this summary, 2012-2013, fall just short of making the cut. I suspect this trend may be more intact in a location like ours because of the relatively high number of storms and snowfall, and upslope snow (which was on the low side this season) as an extra protection against huge snowfall variance, but this is going to be an interesting trend to follow into the future as a gauge of snowfall seasons.
In sum, while snowfall was certainly a bit below average, and snowpack was well below average, I’d still give the season a reasonable grade. If C is average, I’d go with a C- for 2012-2013, just a bit off from making the average. Were snowpack a more significant factor in my winter preferences, one could argue for going a bit lower, but at least minimal snowpack was maintained throughout the entirety of the winter to keep everything white. Overall it could have been a lot worse, and with the amount of snowfall we did get, it’s hard to drop the season into the D range, which, based solely on snowfall and snowpack at the house, is where I’d put a season like 2011-2012.
We’re pleased to announce the completion of our Bolton Valley Photo Gallery for the 2012-2013 ski season. This year’s gallery is our largest to date, with over 270 images documenting this season’s ski adventures indoors and out, in the front, side, and backcountry, under blue skies and flake-dumping maelstroms at Vermont’sBolton Valley Ski Resort. Continue on to the thumbnail images below and browse away! Detailed reports are associated with every photograph in the gallery, so if you find a scene that sparks your interest, simply hover over the thumbnail image to get the date, and head to the archives on the right side of the page to read the full report. We’ve also got similarly extensive galleries from the past several ski seasons, representing nearly 1,600 photographs from around Bolton Valley, and these can all be found at our J&E Productions Photo Galleries Page. We’ll also have our full 2012-2013 Ski Season Summary coming out later this summer, so stay tuned for that update as well.
“…you didn’t have to worry about hitting anything underneath and you could just let it rip.”
Saturday arrived with a nor’easter developing just like the weather models had suggested. For folks that had outdoor, warm-weather plans for the big holiday weekend, you almost couldn’t find a nastier combination of weather. Temperatures were in the 40s F, and there was plenty of wind and rain. We wondered if we were going to have to turn the heat back on in the house. Reports began to come in about the snow in the mountains, and by mid afternoon, Whiteface was already reporting that they had received 18” of new snow. As the afternoon wore on, even valley temperatures fell down well into the 30s F in many places in New England, and fairly low elevation spots began to report snow mixing in with the rain. Although we weren’t getting any snow down to the low elevations in our area, we lost power from about 8:30 P.M. to 9:30 P.M. for some reason, so we headed off to bed early and decided to see how things were going in the morning.
Snow closed down the road through Smuggler’s Notch today.
I made my morning CoCoRaHS observations at 6:00 A.M., and after checking back in on the weather board and looking at some of the mountain web cams, I decided to head to Mt. Mansfield for a ski tour. I couldn’t tell quite how low the snow line had gotten, but it was still below freezing in the higher elevations, and the precipitation had continued through the night. There was a good chance that a nice shot of snow had accumulated on Mt. Mansfield. I didn’t try convincing E or the boys to try to join me, since they were all still in bed, so I got into my ski clothes, let E know that I was on my way, and loaded up the car with my gear. I don’t typically find the ski gear vying for space with the baseball stuff in the back of the car, but it definitely was today. I headed off to the mountain around 7:30 A.M. or so, and temperatures throughout the mountain valleys in the Waterbury–Stowe area were in the lower 40s F on my drive. The precipitation was generally light rain until roughly the point where the electronic sign indicates the status of Route 108 through Smuggler’s Notch, and not long after that, the rain became much heavier. The sign, by the way, read “NOTCH ROAD CLOSED… DUE TO SNOW”. The road through the notch tops out near 2,200’, so clearly the snow was accumulating at that elevation on paved surfaces. The temperature remained in the lower 40s F until that final rise above The Matterhorn to Stowe Mountain Resort, where they dropped into the upper 30s F.
“You could do laps up there from 2,500’ to 3,600’ and think it was midwinter.”
I parked at the Midway Lodge (~1,600’), where the temperature was in the mid to upper 30s F, and the precipitation was generally snow, but certainly some rain as well, and the snow that was falling was of course incredibly wet. It was pretty nasty at that point, with 25 MPH winds and driven wet snow/rain. The snow wasn’t quite accumulating there, but it was close, and you could see the accumulations just a few hundred feet up the trails. The weather was nasty enough that I left my lens hood on my camera in its protective orientation, even when it went back in my pack. I rarely feel the need to do that, and typically flip it back around for storage, but that speaks to just how wet and windy that snow was to make me take that extra step to minimize the amount of precipitation getting on the lens filter.
Snow line in sight on Nosedive at 2,100′
In the Midway parking lot there were a few dozen vehicles belonging to skiers, and most of the people were heading up Gondolier, but my initial ascent was via Nosedive; it’s often a good bet for decent snow coverage and preservation in these early and late-season storms. Also, based on what I saw in the report from AdventureSkier.com last Sunday, it looked like there would be some decent base snow left in case the new snow depths were marginal. The first traces of snow accumulation on the ascent were at 1,800’, by 2,100’ there was generally complete coverage of the trail, and by ~2,200’ the depth was a couple of inches and it was consistent enough that I switched from hiking to skinning. Even with those couple inches of snow, I was beginning to experience some occasional slipping as I hiked, so it was nice to get the skis off the pack and on the snow where the skins had beautiful traction. There was a faint skin track from an earlier ascender, but it was intermixed with some of the descent tracks of skiers and a bit hard to follow. I met up with another guy that was making the Nosedive ascent, and we chatted a bit about skiing as we made our way up the mountain. He was just hiking in his boots with his skis on his back, which seemed like a bit more work as the snow got deeper and deeper, but it didn’t appear to slow him down too much. Listed below are the snow depths I found on the ascent of Nosedive with respect to elevation:
We stopped our ascent at 3,300’ because as we approached the switchbacks at the top of the trail we got some beta from a couple of skiers coming down Nosedive – they indicated that everything above that elevation in the switchbacks was scoured and really not worth it, and indeed that was obvious once we got to the landing below that final switchback at 3,300’. I’m going to call the average snow depth there 10” to be on the conservative side, but there were plenty of areas with 12”-15” of snow; there was just variability due to the effects of wind deposition. I stuck my measurement pole right in the snow in the center of that landing, and found 15” of snow depth. The guy that had ascended with me headed up just a bit higher to catch some turns along a drift of snow, so I pulled out the camera and got some action shots as he made his way down.
I didn’t get his name, but he had quite a blast ripping up the powder on Nosedive today.
Before beginning my descent, I downed a packet of GU Energy Gel to see if it would provide that extra boost of energy to my legs to permit proficient and aggressive Telemark turns. I’ve noticed that after fairly long and/or quick ascents, my legs are often still recovering, and not to the stage where they can handle a lot of rigorous Telemark skiing right away. Alpine turns are typically no problem, since they’re easier and more stable to begin with, and after decades of alpine skiing, my muscles have the memory to really let them do it efficiently. But those Telemark turns take a lot more work, and it seemed like a little extra boost of quick energy would get me where I needed to be. So, I took a cue from the boys, who like to have a GU when they’re starting to fade while we’re biking or skiing – the Vanilla Bean flavor is a favorite among all of us. I usually don’t find that I need to worry about having enough energy on outings with the boys along; the pace is so slow that E and I usually don’t get drained. The boys certainly push themselves though, often needing some sort of recharge due to their smaller energy reserves, and when that’s the case, it’s GU to the rescue. On bigger, faster paced outings by myself though, I also feel the drain, and today I wanted to give a recuperative GU shot a try. I had the GU just a few minutes before my descent, and it absolutely worked. It helped give my legs that quick energy that they craved, and they had no trouble making Telemark turns. It was great having maximum powder to drive the legs, and while there’s no way to know exactly how my legs would have performed without the shot of GU, it was certainly my hero for today. I can still remember when I first learned about those energy gels back in the early 2,000s when Scott and Troy and their Dirtworld.com mountain biking team would use them. They’d strap them to their handlebars and down one on each lap to keep their energy up. With the way it performed today, I think a shot of GU before each earned descent is going to become part of the routine.
“There were plenty of
untracked lines to ski,
and it was dense, wall-
to-wall snow…”
As for the snow conditions, indeed there was some leftover base snow on Nosedive, and that offered up great turns, but the new snow itself was extremely dense (probably 12-14% H2O or so) and as long as there was enough of it, there was no need for previous base because it kept you off of anything below. I caught some beautiful bottomless powder on the skier’s left below the switchbacks, and then a lot more on the skier’s right along the edge of the trail. The Telemark turns were definitely flowing, and despite the fact that it was dense snow that could easily have been challenging to ski, it wasn’t. I immediately thought back to that storm last year on April 10th. Mt. Mansfield picked up more than two feet of dense snow that covered everything, but it was quite a challenge to ski on the Teles. Sometimes you would punch through the snow too far, perhaps with one ski, making lateral balance tough, and fore-aft balance was also extremely challenging. It’s possible that there was snow of varying densities in that storm, with some less dense snow underneath the topmost layer. That’s “upside down” snow, which is typically more challenging to ski. It was after that storm that I really decided that I wanted some fat, rockered Telemark skis for powder, and eventually got the Black Diamond AMPerages. I can only wonder how they would have performed in that storm – they would have been nice today, but being unsure of the snow depths I went with my older Atomic RT-86 midfats, and there were no issues. Really, the most challenging aspect of today’s skiing was negotiating areas of thinner snow as you dropped in elevation. I was actually quite impressed with the quality of some of the powder skiing on Nosedive today, but little did I know it wasn’t even going to hold a candle to what was in store over at the Gondola.
22″ of new snow up at the Cliff House today
I had no time limits, and plenty of energy left in the tank with the shortened ascent, so I skied down to the junction of Nosedive and Cliff Trail, and continued my tour by skinning up Cliff Trail. Within a few moments of starting my ascent, it was obvious that snow depths were substantially greater on Cliff Trail than they were on Nosedive at equivalent elevations. I wasn’t sure if it was because I was heading toward the Gondola, or because Cliff Trail offers better protection from the wind, but coverage was deep, wall-to-wall. Unlike what I’d seen on most of Nosedive, there were no signs of whatever lay beneath the snow. It wasn’t an illusion either; the depth at 3,000’ on Cliff Trail was 11”, vs. the 8” on Nosedive. The snow just continued to increase as I ascended toward the Gondola, there was 12”+ by the junction with Perry Merrill at 3,400’, and 12” – 15” easily up at the Cliff House. That’s on the conservative side for what you could find up there, and in general the snow depth was somewhat deceptive because you didn’t sink much into the dense snow. But right in the middle of Perry Merrill just beyond the Cliff House I measured 22” of new snow in flat terrain with no drifting. The usual measurement off the top of the picnic tables was deceptive as well – there was about a half foot of snow on the tables, but you could tell that the snow was much deeper because the table’s seats were just about buried. I measured in the open space between the tables and got a depth of 18”, so presumably the tops of the tables didn’t accumulate the snow well due to wind, melting, or some other effect. Here’s the summary of the depths I found on the Gondola side ascending via Cliff Trail:
“…at times it was dense enough that you’d be smearing turns right on the surface.”
I had another GU and got ready for my descent. Even that first steep pitch of Perry Merrill had great coverage comprised of that dense snow. Typically you’d sink in a few to several inches, but at times it was dense enough that you’d be smearing turns right on the surface. It took a moment to adapt when that was happening, but somehow the variability in the turns didn’t seem to disrupt the flow of the skiing – it was just really fun. I almost headed back down Cliff Trail since the coverage was so complete, but there were already a couple of tracks on it, and it’s fairly narrow, so I opted to check out Perry Merrill instead. I was hoping it would live up to the coverage I’d seen on Cliff Trail, and indeed it was just as good, if not even a bit better. There were plenty of untracked lines to ski, and it was dense, wall-to-wall snow, all the way down to 2,500’. You could do laps up there from 2,500’ to 3,600’ and think it was midwinter. The snow certainly wasn’t fluffy VermontChamplain Powder™, it was dense Sierra Cement, but it wasn’t wet or sticky. It made for plenty of base and just skied really well – it was right near the top on quality that I’ve experienced relative to many similar early and late-season dense-snow events. Sinking into the snow only a few inches or so was inconsequential compared to the fact that you didn’t have to worry about hitting anything underneath and you could just let it rip.
The view from white to wet
I stopped my descent at around 2,300’, as the snow was down to about 4” and it was getting notably wetter. You could probably go down to around 2,100’ easily if you had your rock skis. I hiked down the last 700’ back to the Midway Lodge, and the last vestiges of snow disappeared right around 1,800’ just like I’d seen over on Nosedive. The precipitation was snow down to just a couple hundred feet above the base, and back down at the lodge it was mostly rain with some snow mixed in at times. There were some really good bursts of snow on my descent, even in the lower elevations. The temperature had increased a few degrees to ~40 F at the base, but it was midday at that point, so that was still quite impressive.
Overall, I was really excited about how my equipment and supplies performed on this tour. My Gore-Tex did its job in keeping me dry, despite the driving rain and snow. My skins held like glue even in the wet snow, and hiking both up and down in my Telemark boots was a joy. I remembered to put them in walk mode for the walking sections (and put them back in ski mode for the descents) and it was almost like being in my hiking boots. And then there was the GU. It really quickened my recovery for the descents, and I’m going to be keeping that on the tour menu going forward. The boys won’t be able to borrow GU from me as easily though when they need it. While the GU certainly did its thing, I’m sure my stop off at Dunkin Donuts to fuel up before the tour also helped. I was feeling so great when I got home at midday, that I was ready to go for another round of skiing if E and the boys wanted to. It was still nasty and rainy outside, and not really conducive to doing too much else, but we had some fantastic winter powder skiing sitting up there in the high country. I couldn’t convince them to go though, so they unfortunately missed out this time. We did get some quality time indoors though, which I’m guessing a lot of families were doing this weekend. Ty, Dylan and I had a great round of “The Settlers of Catan” while E did a bit of shopping. It was quite a storm though, with Whiteface and other areas of the high peaks really cleaning up and putting out some amazing pictures.
…and this is what you get for Memorial Day
Monday update: The clouds cleared out today to produce crystal blue skies, and naturally that revealed some amazing vistas of the spring foliage and snow-capped peaks everywhere. Mt. Mansfield and Camel’s Hump were topped with white, shimmering in the strong sun of late May, and the high peaks of the Adirondacks were brilliant. We traveled around from Waterbury to Vergennes to Cambridge doing various activities, so we took in numerous vantages of the Greens and Adirondacks. It turned out to be a spectacular Northern New England Day for the holiday, almost as if Mother Nature was trying to strike as sharp a contrast as possible against the recently departed storm.
Now that we’re back into a more consistently wintry weather regime, the Northern Greens snow globe has kicked in, and we’ve had a fairly consistent supply of light fluffy snows in the air. It’s not really substantiating the base snow, but it is creating quite the quintessential Vermont winter scene for holiday visitors, and it’s topping off the slopes with some serious softness. Another burst of flakes was just kicking off when we left the house to head up to the mountain today after lunch, and the snowfall intensity increased as we headed up toward the resort. Up in the Village we encountered temperatures in the low 20s F and steady light but accumulating snows. There were plenty of cars in the parking lots, but since spots were opening up with early afternoon departures, we secured a spot right at the north end of the upper lot.
The descent was a peaceful glide through silky smooth powder, with only the occasional touchdown on the old base. The pitch and powder were essentially perfect, although the powder was deep enough that Dylan would sometimes have difficulty keeping his speed up. Dylan’s Telemark skis (Völkl Gotama Juniors) are fairly wide, but nothing like the Black Diamond Elements and AMPerages that E and I were using, and momentum issues aside, you could really feel the way the floatation afforded by our fat skis was letting us ride a bit higher and faster in the powder on those lower-angle pitches. I was curious to see if E had noticed the effect, so I asked her how she felt about the speed of her skis on the descent. She initially thought that they were very fast, and figured it was because they haven’t been used for too many outings and had been waxed. I explained that a good part of that was actually from the floatation that the skis provided. Ty invented a new descent technique where he would kneel all the way on the tips of his skis with both knees, and in the powder it gave the illusion that he was just kneeling in the snow with no skis and flying down the mountain. We’ll have to get some video of that at some point, because it’s quite a hoot.
