I had enough extra time today, so I headed back out to Stowe for a hike and some more turns. Based on what I’d seen on Spruce on my last outing, as well as the views across to Mansfield at that point, I decided it was time to check out something by the Mountain Triple. There’s some easy access snow right down to the base over there, and that fit the time I had.
As I walked along past the Triple, I surveyed the snow situation and headed toward Lower Standard, which seemed to have the best coverage. That area makes for a pleasant stroll because it’s generally quite grassy with modest pitches. Somebody had built the shape of a heart out of rocks on the ground near the ropes course, so that was kind of a nice accent to the area. The snow on Lower Standard is definitely more broken up than what it was a week earlier, and there are a couple of gaps near the bottom that are really best walked vs. trying to skip across on your skis.
That afternoon we had thunderstorms in the area, and as usual, there were some great views surrounding the resort and toward the Notch as the peaks worked their magic and forced the clouds around. While I was hiking I started to hear thunder to the east and northeast, off past Spruce Peak and over toward Madonna and Sterling. Eventually I started to see some tendrils of virga over there, and the thunder was becoming more expansive. I was just getting up toward the Crossover elevation, which was about where I was going to stop anyway because the snow petered out there, but the timing seemed good with the thunder building. I started seeing the first visible flashes from lightning just as I was getting back to the car, and the first drops of rain began to fall, so that timing really did work out well. I would have stayed around for some lightning photography over toward the Notch, but none if was producing visible bolts, it all seemed to be well up in the clouds or too distant.
Another spring storm moved into the area on Wednesday, and it resulted in a protracted period of precipitation that started to change over to snow yesterday afternoon into the evening. It was snowing at our house this morning with a bit of accumulation, and the visible snow line here in the Winooski Valley reached down to around 1,000’. The views from the Bolton Valley Main Base Webcam showed the slopes covered in a fresh coat of white, so I decided to get a bit of exercise and headed out for a morning ski tour.
As soon as I left the house and rounded the first corner on Route 2, I was shown a bright visage of white-covered peaks across the valley. These elevation-based snowstorms typically produce some great views, and the accumulations from this one varied a bit with aspect, so that made for some exciting scenery as I headed through the Winooski Valley.
Once I was on the Bolton Valley Access Road, the first traces of white appeared at roughly 900’, and the accumulations slowly increased to 2-3’ at the Timberline Base, and 3-4” in the Village. Temperatures were below freezing from probably 1,000’-1,500’ on up, so the new snow above that point was dense, but dry. There was a notable jump in accumulations just above 2,000’ or so as the profile below shows. Above that though, there wasn’t a lot of increase, so presumably the snow line crashed down to that ~2,000’+ level pretty quickly without spending a lot of time at 3,000’+.
Here’s the accumulations profile observed on this morning’s outing:
“I’d planned on a quick tour over in the lower elevations of the Wilderness area, but once I was over there out of the wind, I saw that the accumulations were solid enough to warrant a more extended tour into the higher elevations.”
I’d planned on a quick tour over in the lower elevations of the Wilderness area, but once I was over there out of the wind, I saw that the accumulations were solid enough to warrant a more extended tour into the higher elevations.
As mentioned, the snow was dense but dry, so it skied fairly well. On 115 mm fat skis I was typically sinking in a couple of inches, and there was a surfy consistency to the setup that really let you have some fun and smear your powder turns easily if you wanted. The snow provided plenty of cushion for low to low/moderate-angle terrain, and up above 2,800’ or so, old snow and snow bridges were still in place, so that made any water bars less of an issue.
“As mentioned, the snow was dense but dry, so it skied fairly well. On 115 mm fat skis I was typically sinking in a couple of inches, and there was a surfy consistency to the setup that really let you have some fun and smear your powder turns easily if you wanted.”
There were a few folks out and about in the Village, but out on the mountain itself it was pretty quiet. All I saw was a red fox that ran in front of me on Lower Turnpike, and a guy on a fat bike up near the summit. I was surprised to see him up at that point because there was a half foot of snow, and due to their weight those fat bikes are total dogs with respect to climbing, so I’m sure he’d put in plenty of work. There were some packed areas of snow due to resort operations traffic and wind scouring, so I’m guessing he made good use of that.
We’ve had a few nice snowstorms over the past few weeks, and this latest one was a nice way to kick off the month of May with a ski tour.
This latest winter storm sort of snuck up on us. Our local forecast at home did indicate the chance for a touch of snow during the overnight, but I was well into the wee hours before we’d expected to see anything. Yesterday afternoon though, it was pouring rain down here in the Winooski Valley, and with temperatures in the 30s F, it seemed suspiciously cool. Around 5:00 P.M. I decided to check on a couple of the local webcams at the resorts, and was surprised to see that it wasn’t just snowing at elevation, but in line with the pouring rain down in the valleys, intense snowfall was occurring in the mountains. It looked like the snow line was somewhere around 2,000’.
“I’d say fat skis were the way to go today, and indeed turns up high were bottomless and smooth, with little need to worry about hitting the base.”
By 8:00 P.M. we’d picked up about an inch of snow at the house, and with continued snowfall in the valleys, it seemed very likely that the mountains were going to have a solid new accumulation by the time the night was over.
In the Bolton Valley area this morning, there were accumulations all the way down to the base of the access road at 340’, and the accumulations slowly increased as one headed up to the resort. The snow depths started to increase more rapidly around the elevation of the resort Village, with 3 to 4 inches there, and those totals doubled by the 2,500’ elevation. Essentially all the snow above 1,500’ was winter-dry, and temperatures were still in the 20s F this morning from probably 1,500’ on up. I’ll have to look back at all the April and May storms we’ve had this season, but this was some of the driest/wintriest snow I can recall in the past few storms.
I’ve got the elevation profile for new snow accumulations below, and as you can see, the largest increases in depths indeed came from a bit below 2,000’ up to about the 2,500’ range before the rate of increase tapered down:
The storm was probably mostly snow above 2,500’, and with 1.21” of L.E. down here at the house, it was a decent resurfacing above 2,000’, and a very solid, “no worries” type of resurfacing above 2,500’. I’d say fat skis were the way to go today, and indeed turns up high were bottomless and smooth, with little need to worry about hitting the base. Indeed, midwinter-style powder is always appreciated in May.
While the upper elevation snowpack here in Northern Vermont got a bit of a boost from the snowstorm we had earlier in the week, the snow in the lower elevations is getting rather sparse. So while there’s still plenty of snow available in the local mountains overall, it’s not easy to head out on a tour that will let you ski right back to the base elevations. At the end of my tour on Tuesday though, the gentlemen I’d met out on the trail told me that there was still an impressive amount of snow available over by the Sunrise area of the resort. The terrain in that area really isn’t visible from Stowe’s webcams, or from the valley in general for that matter, but when the clouds started to rise away from the peaks this afternoon, I decided it looked nice enough for a quick ski tour and I decided to see what the area had to offer.
As soon as I walked up the access road from the Mansfield Base Lodge to the bottom of the Mountain Triple Chair, the possibilities were looking promising. A nice thick blanket of snow stretched right down to the base of the Standard trail, and coverage looked to continuous as far up the slope as I could see. There was enough open ground that I decided to simply hike vs. trying to skin, so I walked up the essentially snowless Lower Gulch as it paralleled Lower Standard. I did have to walk on snow at times as I got higher up the mountain and stuck more to Standard itself, but there were plenty of dry options as well if I’d wanted to take another route. I had only a certain amount of time, so I stopped my ascent after about 1,000’ of vertical near the top of Standard. There was plenty of snow to continue upward though for those interested in a longer descent.
“A nice thick blanket of snow stretched right down to the base of the Standard trail, and coverage looked to continuous as far up the slope as I could see.”
On the lower mountain it’s really the Standard trail that has the nearly continuous snow cover. The resort clearly made a lot of snow there this season, no doubt due to supporting the terrain park that occupies the trail. The snow cover isn’t quite 100% continuous throughout the entire length of the trail, but the only gaps are a couple of rather small ones that can be safely traversed without taking off your skis as long as you’re comfortable stepping across the ground slowly. There are a couple more spots that will likely open up soon, so watch for that if you go over the course of the next week. I do enjoy how every spring is a bit different with the trails that offer the best skiing, so being over on that side of the resort was a nice change of pace from the usual Nosedive options. The snow on Nosedive is still holding out well of course, but it doesn’t offer the same level of coverage right to the base that you can get on Standard right now, so the terrain off the Mountain Triple Chair could be a good option for touring if you’d like to check it out. It worked quite well for me, so hats off to the gentlemen I met on Tuesday who gave me the advice about the solid coverage on that side of the resort.
It turns out that we likely get a substantial May snowstorm here in the Northern Greens about every other year on average. It probably feels like May snowstorms are rarer than that, maybe because, well… it’s May. By this point in the season it typically hasn’t snowed in a few weeks, we’ve had some warm weather, Memorial Day is approaching, and people are well along into thinking about spring and summer. But I felt as though I’d been out on fresh snow several times in May since we’ve been back in Vermont over the past decade or so, and being curious about the actual numbers during the lead up to our current storm, I checked my ski report archives to see. Indeed, with today’s storm that makes at least five significant May snowstorms in the past decade. Here in the Northern Greens we also don’t catch the brunt of every May snowstorm that hits the Northeast, especially with the Presidentials in the mix, so I suspect that for the region as a whole the frequency of May snowstorms averages out to somewhere around a storm each season.
“…we likely get a substantial May snowstorm here in the Northern Greens about every other year on average.”
As expected, it was a cool, borderline wintry morning as I made my way to the mountain. Temperatures were in the upper-30s F in the mountain valleys, and mid-30s F at the resort base. I’d seen on Stowe’s web cams that the North Slope area had its typical late season residual snowpack, so I chose that for my ascent route. By the time I got out on my tour, the snow level was certainly rising relative to its lowest point overnight or this morning when there were more optimal temperatures and snowfall rates. New snow accumulations varied considerably depending on the underlying surface, with the best accumulations and retention found atop the existing snowpack.
“The amount of dense snow up high meant that you had plenty of cushion for some nice powder turns.”
Continuing up from the North Slope area, I headed through the Fourrunner Quad Summit and up the Toll Road past the Mt. Mansfield Stake to the Mansfield Summit Station at around 3,850’. Precipitation was snow at all elevations on my ascent, and it was fairly light for the most part until I got to the Summit Station along the Mansfield ridgeline. While I was hanging out there refueling and changing over for the descent, the intensity of the snowfall ramped up somewhat, with lots of tiny flakes at first. Eventually though, the snowfall picked up to a pounding of much larger flakes. There was definitely a lot of liquid coming out of the sky at that point, and my Gore-Tex® was getting a workout.
Observing the new snow accumulations along my ascent, the big jump in depths really seemed to happen between 2,000’ and 3,000’. Above 3,000’ I didn’t really see too much with respect to additional accumulation, so presumably temperatures were sufficient down to 3,000’ to maximize the snow from the available moisture right from the get go yesterday.
Here’s the elevation profile for the accumulations I found this morning:
The amount of dense snow up high meant that you had plenty of cushion for some nice powder turns. Of course, the density also meant that the snow was Sierra Cement/Cascade Concrete and you had your work cut out for you with respect to getting those powder turns. I had my midfat Telemark skis, and let’s just say that the Tele turns in today’s snow were a lot of work. It is mid-May though, so even dense powder turns this time of year are always a treat, and getting the workout is a big part of the experience anyway.
“…you had your work cut out for you with respect to getting those powder turns. I had my midfat Telemark skis, and let’s just say that the Tele turns in today’s snow were a LOT of work.”
In some cases it wasn’t just the descent that added an extra challenge due to the dense snow. I followed a pair of skin tracks on my ascent and noticed that in some spots the new snow had stuck to their skins. I wasn’t having that issue with my skins, but I eventually caught up to the gentlemen who were making the skin tracks, and they said for them it was an issue when they traveled over areas without an existing snowpack. I was able to pay them back for their helpful skin track by setting the track for the second half of the ascent, and while I didn’t see them on the descent, I saw them back at my car and at Edelweiss Deli where I grabbed a sub for lunch (great minds think alike) and it sounds like they had a great tour.
Wintry conditions in May are typically quite ephemeral, so I guess we’ll be back to spring skiing soon, but these late season powder days are always a treat. There’s a certain mystique with these late season elevation snow event because it feels like you were in another world when you get back to the strong sun, spring warmth, and rapidly emerging greenery in the valleys.
I looked out my office window at some point earlier this week and saw that there was quite a bit of white still visible on the slopes of Bolton Valley. So, when I had a bit of time with decent weather this afternoon, I decided to head up for a ski tour to see just how much skiing was still available.
On the drive up the Bolton Valley Access Road, the first signs of snow didn’t appear until about 1,500’ elevation near the base of the Timberline area. I was surprised to see that there were even skiable lines farther up on Timberline. Up at the main mountain, snowpack starts right at the base.
“I’m not sure if it was the hearty snowpack we had this winter, the amount of snow the resort made, the lack of any hot spells this spring, or a combination of these factors, but Bolton definitely has a solid amount of snow on the ground for this far into May.”
I was expecting to make some turns up on Spillway today, since that’s the area that tends to melt out last with respect to fairly lengthy ski lines, but there’s far more snow available than just the typical late season Spillway stuff. Multiple trails on the upper mountain have skiable snow, and the Bear Run/Sprig O’ Pine area on the lower mountain has quite solid coverage. Starting from up near 3,000’ on Spillway, I was able to ski almost continuous snow to the main base. There were a few small breaks in the snowpack, but nothing that required taking off my skis. That wouldn’t be too surprising on the eastern slopes of the Greens this time of year, but that’s quite impressive for the western slopes. I’m not sure if it was the hearty snowpack we had this winter, the amount of snow the resort made, the lack of any hot spells this spring, or a combination of these factors, but Bolton definitely has a solid amount of snow on the ground for this far into May.
In terms of the snow quality, it’s now has gone through numerous spring temperature cycles and is well consolidated into corn. The texture of the snow is excellent, with a couple to a few inches of loose snow peeling away from the surface. The only issue is that melting has creating an inconsistent surface in many areas that results in bumpy snow. The surfaces would actually benefit from a bit of skier traffic to smooth things out, so hopefully a few folks will get out there to enjoy it before it’s gone.
It’s always fun each spring to see just how the snowpack finally melts out on Mt. Mansfield. There are certainly those reliable, well-protected spots like Nosedive that hold snow well into the spring, but between the variability in natural snow deposition and snowmaking, you never quite know what areas are going to offer the best turns for your effort as we get farther into the spring. I headed out for turns this afternoon expecting to make a traditional Nosedive run, but upon appraising the availability of continuous lines and low-elevation snow, it was actually Liftline that seemed to be the best bet.
“I only had time to head to the top of that large section of snow (~2,300’), but it offered up some nice steep turns and the corn snow was in excellent shape.”
I once again parked in the new lot by the Midway Lodge just as I’d done for my outing last week, and headed up the Crossover trail until I encountered Sepp’s Run with substantial snow right down to the bottom at ~1,700’. I knew there was a break in the snow up toward Liftline, so I hiked until I hit the more substantial snow on there and then switched to skinning. I only had time to head to the top of that large section of snow (~2,300’), but it offered up some nice steep turns and the corn snow was in excellent shape. That section is one of the steepest of Liftline, so the skinning was a challenge without the ability to really spread out the switchbacks on the ascent, but it was doable with good support from my poles and ensuring that my skins were secure with each step.
On my descent I ran into Scott Braaten out for an afternoon tour, and then Jumpin’ Jimmy and I believe Aaron Lavallee as well, so it was quite the SkiVT-L reunion! We’re certainly past the point where you can easily skin up and get 2,000’ of continuous vertical feet of snow at Stowe, but we’re not too far off from continuous skiing from the top of the Fourrunner Quad from what I heard, so there’s definitely a lot of good skiing to be had. Jim said that the snow in the next section above where I’d stopped was really good, so if I get a chance it would be nice to get up there and make some turns before the snow melts out.
We had some great weather for skiing last weekend, but I was fighting a cold and decided to recuperate vs. pushing myself too hard with a tour. The great weather has continued this week though, with a simply amazing stretch of sunny spring days, and this morning I had a bit of time to get out for a ski tour at Stowe.
These recent days of warm weather have been eating away at the snowpack of course, and on my trip to the mountain I didn’t encounter any snow until the resort’s main base elevations around 1,500’. I parked by Midway, and similar to about a half dozen or so other cars I saw, I was able to use the nice new parking area the resort has added just below the Midway Lodge. I’d never even noticed that parking lot before because it’s usually covered with snow, but it’s got some nice clean asphalt that makes it a very nice spot for changing gear and clothing well away from any spring muck.
Nosedive still has coverage right to the bottom at the Crossover trail, so I started skinning from there at ~1,650’, and made my way up to the junction with Cliff Trail at ~2,700’. Nosedive has continuous coverage all the way up to that point, and although I didn’t continue higher on Nosedive itself, I’d be surprised if there were any breaks in the snowpack at the higher elevations. For my tour, I decided to continue on toward the Cliff House because I saw that Perry Merrill looked to have almost continuous coverage, and the skiing there will typically run out before Nosedive. I had to take off my skis and walk for a couple hundred feet because that junction area of Cliff Trail with Nosedive has melted out, but after that I was able to skin all the way up to the Cliff House. The resort’s been clearing out some of the work roads as they get ready for summer, and that really transformed the area up near the Cliff House with massive snow piles on the sides of the trail and nothing in the middle.
“The snow quality overall was excellent though, as we’ve obviously had plenty of freeze-thaw cycles by this point and the snow if very much in prime “corn” form.”
For my descent I continued on to the other side of the Cliff House and hit Upper Gondolier, then connected onto Perry Merrill lower down. Perry Merrill has just a couple of breaks in the continuity of its snow, although one is about 100 feet long and is best navigated by taking off your skis. The snow quality overall was excellent though, as we’ve obviously had plenty of freeze-thaw cycles by this point and the snow if very much in prime “corn” form.
As the spring semester winds down, many of our graduating biochemistry majors here at UVM have been getting out to enjoy the remaining snow in the mountains of both New Hampshire and Vermont. I’ve been hearing some fun reports, so when Rob invited me to join one of their Mt Washington adventures, I was definitely interested. His plan was for the Tuesday of senior week, weather permitting of course. My schedule looked good, so I was hopeful for the chance to commune with some of the seniors in the great outdoors before they’d begin departing after graduation.
“We could see that there had been some sloughing there due to the new snow, but the lower areas we could see looked quite settled and stable, and there had already been plenty of skier traffic in the gully.”
Mother Nature threw some rather interesting weather into the mix ahead of the planned trip, with Mt Washington picking up almost 3 feet of new snow at summit elevations over the past couple of days, and over a foot down at Hermit Lake. That was a lot of new snow, and the avalanche report suggest that northerly winds would be loading the more southerly-facing gullies and cross-loading the east-facing ones. Temperatures were expected to rise significantly today, which we knew would result in plenty of settling depending on elevation. There seemed to be enough potential to find at least some level of safe skiing, so we decided that we’d check with the staff on scene in the Hermit Lake area, and the trip was on.
Only Rob and Emily ended up being able to make the trip, but I met them at the Pinkham Notch Visitor’s Center, and after getting our gear together, we were on our way. I’ve hiked up to the Tuckerman Ravine area many times, but with the new snow I decided to try a gear setup that I’ve never used before. Instead of brining two pairs of boots (hiking boots and ski boots), I wanted to just wear my mid-weight Telemark boots for everything, hiking and skiing. It turns out that the setup worked great; my Garmont Gara boots have got rubber Vibram soles so they were plenty comfortable and pliable on the ascent through a lot of dry, rocky terrain. Ascending from Pinkham Notch at ~2,000’, we saw our first signs of snow at 2,650’, and at around 3,400’ the snow cover was continuous enough that I was able to start skinning there and made it right up to Hermit Lake. The new foot or so of snow had certainly helped with the potential for skinning – coverage would have been somewhat less continuous on that last part of the ascent without it.
We assessed the snow/ski terrain situation from there, and while most of Hillman’s was visible with clouds just skimming the upper reaches, Tuckerman Ravine was generally socked in. After consulting with the staff at Hermit Lake, and using what we could see, we decided that Hillman’s Highway was the way to go. Most skiers we encountered seemed to be making the same decision. We could see that there had been some sloughing there due to the new snow, but the lower areas we could see looked quite settled and stable, and there had already been plenty of skier traffic in the gully.
Emily and I skinned up the first part of gully, but around halfway it was just getting too steep and we had to switch to hiking. Thankfully there was a nice boot ladder already in place on climber’s right. I stopped around mid-gully where I figured I’d still get plenty of descent, and set myself in a good position with my camera. Emily and Rob headed up to where the gully splits into a Y, and went a little farther up the climber’s right option before settling down in a sheltered area of rocks. Above that point the snow hadn’t been skied and was a little questionable, and in that regard they were on the same page as other folks skiing in the area.
The best skiing was in areas where there had been some skier traffic that got down to the older corn snow surface, and the toughest turns were in the mush that had settled down near the bottom of the gully. The Sherburne Ski Trail had actually opened back up a bit with the new snow, and we were able to ski about a third of it before we had to cut back to the hiking trail. After that the descent was quick, and we were back at the cars saying our goodbyes.
The new snow is going to get even better with a couple of freeze-thaw cycles, and it’s certainly bolstered the snowpack somewhat in the higher elevations. Although they were in and out of the clouds, the summit snowfields looked really nice, so there should eventually be some excellent skiing up there with easy access as soon as the road opens back up.
The best weather in this weekend’s forecast appeared to be this morning, so I took advantage of the window and headed off to Mt. Mansfield for some skiing. The temperatures been fairly cool this week, so the snow cover on Nosedive hasn’t actually changed a lot relative to what can happen during some warm weeks. Coverage is still essentially continuous, but there’s a point in the middle that will create a gap soon. The snow was a bit softer this time compared to my last outing on Sunday, so that made for some really smooth turns. There are some areas with moguls, and plenty with smooth, skier-groomed snow to give you quite a variety of terrain. While I had actually hoped to ski Cliff Trail as a change of pace, it’s disconnected from Nosedive now so I stuck with the continuous coverage of Nosedive.
It looks like we’ve got some warmer weather coming this week, so we’ll have to see where the snowpack at Stowe will stand by next weekend.