The local ski resorts hadn’t picked up too much more than we had, but totals in the 6 to 10” range seemed typical, and that was certainly enough to entice me out for some early season turns. With that in mind, this morning I decided to head up to Bolton Valley to get in a ski tour and check out the new snow. With the fairly fluffy nature of the snow and based on what we’ve seen at the house over the past couple of days, I’m sure there had been some settling since it fell, but here’s the snow depth/elevation profile of what I found from the base of the Bolton Valley Access Road up to the local summit areas:
I started my ski tour around midday, when temperatures were just edging a bit above freezing at our house down in the valley, but above 1,500’, and certainly above 2,000’, temperatures never got above freezing so the snow was all winter consistency.
In terms of the skiing, it was undoubtedly early season, and rock skis would be your best bet if you’re going on anything with substantial pitch. I actually found the skiing better on the lower half of the mountain because there was a bit of a base there – I think more of the snow down in those elevations was melting on contact with the ground to create that dense layer. Up higher, the consistency of the snow was more straight fluff from top to bottom. As is often the case, most water bars had reasonable crossings at least at one point, but a few were dicey and took some extra navigation. There’s still running water in plenty of spots, and ponding in some flat areas. On my descent it was obvious that my skis got in contact with at least traces of that moisture, because about halfway down I had to pull out a credit card and spend probably 10 minutes doing a scrape down on the ski bases to really get things back in shape for gliding.
That effort was worth it though, because for the bottom half of my run I was on Lower Turnpike, and that offered what was unquestionably the best skiing of the tour. The combination of that bit of dense snow that accumulated as some base down in those elevations, plus some skier traffic packing down areas of the new snow as well, clearly created the best subsurfaces I encountered. On top of that you’ve got the fact that Lower Turnpike is essentially all grassy terrain, and it has a pitch that isn’t really overbearing for the amount of snowpack we’ve got, and it comes together for real winning combination. Even with some skier traffic, there was still plenty of powder to play around in throughout the trail, so that was a great way to finish off my run.
For anyone heading up, you may still want to hit the summit areas to check things out and get the exercise from a more substantial tour, but if you’re just looking to get out from some quality turns, Lower Turnpike is probably going to get you the most bang for your buck. It’s one of the designated ascent routes anyway, so there’s a nice skin track and it’s an efficient way to in some nice turns on the new snow.
I just got an alert on my phone this morning that we’re under a Winter Storm Watch in association with the next system. This one looks more substantial than this past one, but we’re still a day or two out so we’ll need to watch for any final refinements to the forecast.
One approximate measure of when the potential natural snow/off piste skiing begins each season here in Northern Vermont is the date when the snowpack at the Mt. Mansfield Stake reaches 24 inches. This is by no means an exact date, especially since it’s possible to get great turns on just a few inches of snow if the snow is dense and the underlying surface is grass instead of rocks. You can indeed get by with much less than 24 inches of snowpack if the snow is very dense, but not if it’s all Champlain Powder™ fluff. Based on empirical observations and reports from skiers in the area each season though, hitting the 24” mark is reasonable for most situations.
With that preface, let’s take a look at where last season sits with regard the start of the natural snow/off piste skiing around here. By most accounts, last season started off with bang. Even in the local mountain valleys, the winter snowpack started as early as November 10th. That’s very early for the valleys, and when the valleys are doing well, the mountains certainly are too.
The updated plot for the 60+ seasons in the Mt. Mansfield Stake database is below, with last season represented by the red star:
Before I add a bit of context to last season’s start, here are the stats for the data set:
Mean: Dec 12th
Median: Dec 9th
Mode: Dec 16th
S.D.: 18.8 days
Entry of this year’s data point had no effect on the mean, mode, or S.D. (within a tenth of a day), but it did drop the median by one day from Dec 10th to Dec 9th.
The plot would suggest a reasonably good start, but nothing outrageous: last year’s 24” date was Nov 27th, which is only 0.78 S.D. ahead of the mean, so well within 1 S.D. That puts it in roughly the top 22% of seasons, so about 1 in 5 seasons will have a similar or earlier 24” date.
While the 24” date is a nice snapshot for the start of the natural/off piste season, there are of course a number of other factors to take into account that made last November more impressive than that number alone:
1) Near miss: If you look at the raw November stake depth data (posted below), you can see that the snow depth at the stake reached 23” on Nov 21st. That’s as close of a miss as you can get to hitting 24”, so even as of the 21st of the month, the snowpack had essentially hit that two-foot level. Getting to that level by the 21st brings a season past 1 S.D. and into that top ~15% of seasons. That’s not a huge bump in this regard, but having nearly an extra week of borderline two-foot snowpack at that part of the season could easily mean an entire additional weekend of natural snow skiing potential.
2) No going back: This is a much bigger feather in last season’s cap. Even from about mid-month, the snowpack never really took a major hit, and once it did hit that 24” mark on Nov 27th, there was really no going back. It sailed past 24” and just kept climbing as you can see in the numbers at the end of the month. I haven’t added the December numbers below, but even with the lackluster December we had, the snowpack never dropped below ~40”. That can’t be said for all of the seasons on the left side of the plot (certainly not Mr. October out there in front, which was the 2006-2007 season – he was back to 0” at the stake by mid-November).
3) Snow-depth days: I haven’t calculated this for any November with the stake data, but it will obviously be a good integrative measure of how much snow was on the ground for the start of the season. I’m sure last November would have a solid ranking if I put those data together.
So, if we look into that left side of the plot, do we have any other recent seasons in there that we can use for comparison to last season?
Actually, that lone star (Nov 25th) just to the left of the red star for last season is for 2007-2008. We know that was a solid season around here. The snowpack began building in the first week of November, and there was really no going back there either. Unlike this past season, that solid November was followed up by a stellar December (almost 70” of snow here at the house) and the Mansfield snowpack was hitting five feet by the holidays. With a solid December, last season certainly would have given 2007-2008 a run, but instead it was languishing at around 40” at the stake during the holiday period.
With regard to some of the other stars up at that end of the plot:
The two compatriots of last season on the plot, those other two stars on Nov 27th, are 1997-1998 and 1977-1978. 1997-1998 looks pretty solid with a snowpack start in the first week of November, and snowpack at about that five-foot mark by the holiday period. There’s also a nice-looking bonus stretch of snow at the end of October, with snow at the stake for almost the last third of the month, and the depth peaking at 16”. Checking my archives, I actually went for some lift-served skiing at Sugarbush on Oct 28th, so that speaks to that period snow being a bit of something special. 1977-1978 was before my time around here, but it looks a bit tamer. There was nothing in October, then snowpack began to build around mid-November and was getting around the four-foot mark by the holidays.
The two stars right at Nov 20th are interestingly, back-to-back seasons of 1967-1968 and 1968-1969. Both had a little October snow, and then a snowpack start in the first week of November. Both had pretty steady climbs right through November and December, with 1967-1968 getting to around 40” for the holiday period, and 1968-1969 hitting a very robust 6+ feet of snowpack for the holidays. I guess that shouldn’t be too surprising, as that was just the start of a season that would become legend.
The star at Nov 18th is 1965-1966, and the progression looks sort of like 1967-1968. That’s quite a 4-year stretch of good early seasons from ’65-’66 to ’68-’69 with those three solid starts.
The star at Nov 16th is 1980-1981. That season is interesting in that the snowpack started building on Oct 20th and sailed right into November without ever going back to zero. Snowpack was 4+ feet for the holidays, but the rest of the season looks modest (relatively speaking) with the snowpack depth never getting above 6 feet.
The star on Nov 14th is for something more recent: 2003-2004. I was out in Montana for that one, but snowpack started building in the second week of November, it was 4+ feet at the holidays, and hit the 100” mark in March.
The star on Nov 13th is for 1976-1977. That looks like an impressive start, with snowpack taking hold in the second half of October, climbing right through November, and hitting roughly the 4-foot mark for the holidays. The stake didn’t quite top out at 100” that season, but it did pretty well topping out at 94”.
The final early star I haven’t mentioned yet is the one on Nov 11th, that’s for the 1990-1991 season. It seems like the only other boom and bust start to go with Mr. October (2006-2007). There was a little inkling of snow at the end of October and start of November, but snowpack started building at the end of the first week of the month and topped out at a very impressive 45” on Nov 14th! It was a downhill slide after that though. The snowpack never went lower than 9” but there were only 12-18” on the ground for the holiday period, and on Dec 30th it dropped from 18” to 13”, so that must have been quite a dagger in the holiday week (I guess that depends on whether it was a nice spring skiing day or a nasty rainstorm). The rest of that season seemed pretty blasé because the snowpack never even hit 5 feet. I don’t recall much about that season, but I’m assuming there was nothing too remarkable.
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.
This weekend we took advantage of the great off-season rates and stayed slope side at the Stowe Mountain Lodge, which I learned has now been renamed “The Lodge at Spruce Peak”. My sister and her family were in the area and staying at the Lodge for a couple of days, so this gave us a chance to catch up with them as well stay right by the slopes for some easy access to skiing on Mt. Mansfield.
We arrived at the Lodge yesterday afternoon, dropped off the car, and then got settled into our room while we caught up with my sister’s family. This time we tried out one of the one bedroom suites, similar to what we’ve had in the past at places like the Tram Haus Lodge. It’s definitely nice to have a bit more space and the multiple rooms, especially now that the boys are older (and bigger). The additional space was also convenient for when my sister’s family came over to visit. During the evening we generally relaxed, the kids headed to the pool/hot tub area for a bit, and we all had a great dinner at the Hourglass Lounge. There was snowfall all the way down to the base elevations in the evening, and as we had dinner we’d occasionally see windy whiteouts from all the blowing snow. It looked quite wintry, but temperatures were fairly marginal at the base elevations, so there was really only a trace of accumulation visible by morning.
I was the only one planning to ski today, so after we checked out of our room and had breakfast at Solstice, E and the boys dropped me off at the Midway Lodge. There were probably two to three dozen cars in the Midway parking lots, and people were heading out from there for ski tours along various routes. Chin Clip Runout looked pretty quiet, and it, along with Switchback is one of my favorite ascent routes, so I headed that way and started skinning.
On my ascent, I observed that additional snow accumulations seemed rather minimal below about 2,500’ – there was a windswept inch or two that was really scattered around atop the old base, and much of that was probably there from Saturday’s snow. The new snow had collected in pockets here and there, but I didn’t really see any substantial consistency until I started getting into the upper half of the terrain. Around the 3,000’ mark I started getting some solid 6 to 7 inch depths of reasonably dense, dry snow along the climber’s right of Perry Merrill. I saw some folks continue their ascents up above the Gondola into the alpine via Cliff Trail Gully, but I was a bit leery of what coverage would be like with the new snow over previous melting among the rocks. If the new snow depths continued to increase above the 3,600’ range then it could have been quite nice up there.
“The deepest accumulations I found were up around 3,500’ along the skier’s right of Perry Merrill, where 7 to 9 inches was pretty typical in undisturbed areas.”
Being underwhelmed by the accumulations I’d seen on my ascent of the main Gondi terrain, I headed toward Cliff Trail for my descent. The deepest accumulations I found were up around 3,500’ along the skier’s right of Perry Merrill, where 7 to 9 inches was pretty typical in undisturbed areas. That was really nice, and while the depth gradually decreased as I headed down Cliff Trail, the skiing there was quite good throughout. There were a few tracks on the trail, but only a handful of skiers had been down at that point. I’d say that the junction with Nosedive at around 2,700’ was right about where the best snow petered out. The elevation was part of it, but the change to Nosedive with its more open nature and higher levels of skier traffic made for a very obvious break in the availability of the new snow. That would have been an excellent spot to stop a descent if one was looking to lap the best snow up high.
We’ve got some fairly cool days coming over the next week, so the new snow should stick around for a while up high, although the quality may deteriorate somewhat from the typical spring temperature cycling.
After watching it snow all morning on the Bolton Valley Web cam, I decided to head up for a ski tour around midday to see how the new snow was settling in over the old snowpack. Similar to our house, the precipitation was rain and there was no snow at the base of the Bolton Valley Access Road, but driving up I encountered residual winter snowpack starting at ~1,400’. The rain changed over to snowfall right after that, around the Timberline Base at 1,500’.
I found a couple inches of new snow as I parked the car in the Bolton Valley Village around 2,000’, and that depth only increased slowly to roughly 3 inches at the 2,500’ level. I noticed a bit of a jump in depths when I hit the 2,600’ to 2,700’ range though, so that seemed to be a threshold of sorts for accumulations during this storm. .
Here’s the new snow depth profile with respect to elevation based on my observations from today’s tour:
“…with the dense snow there were actually plenty of nice bottomless turns available out there.”
On the ascent I was a bit worried that the snow was going to be sticky with respect to turns, but the temperature up top around 3,000’ was roughly 30 to 31 F. So it was certainly below freezing up there, and the new snow was dense, but definitely dry enough for some nice powder turns. I only found sticky snow to be an issue during the final couple hundred feet of descent to the main base area at 2,100’. I made my initial descent down Alta Vista, then worked my way over toward Wilderness, and with the dense snow there were actually plenty of nice bottomless turns available out there. Powderfreak reported some nice turns today at Stowe as well, and he found similar accumulations to what I encountered on my Bolton Valley tour.
The models and forecasts suggest that after a lull this afternoon, there’s a chance for more snow tonight into tomorrow as the back side of the system comes through. We’re planning to stay at the Lodge at Spruce Peak tonight, so hopefully I’ll have a chance to head out for some turns on Mansfield tomorrow.
It’s March, and the snowpack is deep here in Northern Vermont, so we planned to take a trip down the Bruce Trail today during our BJAMS ski session. E had recently been chatting with Brian and Joe in the program, and they were both interested in taking their kids on the Bruce, so we all joined together as a group for the run.
Knowing the round trip would take most of the afternoon, we started right off heading over to Mansfield and up the Fourrunner Quad. I brought everyone up for the requisite visit to Old Nosedive to enjoy the views and add a bit of bonus vertical to the run. Old Nosedive was packed with snow from our recent storm. It was dense powder similar to what we experienced yesterday at Bolton, but it skied quite nicely.
“The Bruce is in simply fantastic shape. That’s not surprising with over 10 feet of snowpack at the Mt. Mansfield Stake, so even the Bruce’s steep, south-facing slopes that lose coverage first are covered with literally feet of snow.”
The Bruce is in simply fantastic shape. That’s not surprising with over 10 feet of snowpack at the Mt. Mansfield Stake, so even the Bruce’s steep, south-facing slopes that lose coverage first are covered with literally feet of snow. The snow consistency varied from dense powder and skier-packed powder up high, to thick creamy snow in the middle elevation trees, to more spring-like snow in the lower elevations. The powder in the lower-elevation hardwoods was definitely getting a bit sticky with sun and warming temperatures, but it still skied quite well in all but the very sunniest spots. Even in the lowest elevations down near 1,000’ on the Nordic area terrain, the snowpack is substantial. Crossing over the bridges along the Nordic trails we found the snowpack to be at or above the level of the bridges’ railings – which are four to five feet tall! You can literally stand on the railings simply by moving to the edges of the snowpack.
The spring snow made the final part of the Bruce descent through the Nordic areas a bit slower than when the snow is more winter-like, but we all simply took our time and enjoyed the casual pace along the meanderings of the Ranch Brook on such a glorious late winter/early spring day. We had plenty of time for snacks while we waited for the Mountain Road Shuttle, so we made ourselves some seats in the snowbanks near the Notchbrook General Store and soaked in some rays as we waited for the bus and discussed our day’s adventure.
Well ahead of our current winter storm, the weather models were predicting it to be quite a whopper of a system. Multiple upper-level lows were expected to consolidate over the area, then a low pressure center would move up the coast and into Northern Maine before finally departing. Low pressure systems in that area are in a very sweet spot for our local mountains, since it’s excellent positioning to allow Atlantic moisture to be grabbed and wrapped around to the north until it slams into the Green Mountain Spine. It wasn’t surprising that storm totals were expected to approach 30 inches in the mountains. Indeed the local peaks got pounded with snow yesterday and overnight, and when the reports came in this morning, storm totals reached and even exceeded 30 inches.
Our plan was to head up to Bolton for some turns today, but all the lifts were initially on wind hold except the Mighty Mite, so we packed Tele and alpine gear and were all set to skin at Timberline until they started running things. By midmorning though, the resort was announcing openings of the Mid Mountain Chair and the Timberline Quad, so we’d be able to start lift-served skiing once we got there. Unfortunately, they were still plowing out the Timberline parking lot and asking people to park up at the main base. This meant connecting over from the main base to ski Timberline, however the Snowflake Chair, which is the best way to connect over, was down for maintenance. This made for a big line at the Mid Mountain Chair, and that connection still requires a short hike anyway, so we made the hike up Villager to get over to Timberline. We chatted with a patroller coming down Villager, and he wasn’t thrilled about our hike because it wasn’t a designated uphill route, but he understood under the circumstances. He just reminded us to stay to side, well out of the way of any resort vehicles that might be using the trail. It’s not really a long hike, but it did have the benefit that we got in some of our cardio today even though we didn’t end up skinning.
“Indeed the local peaks got pounded with snow yesterday and overnight, and when the reports came in this morning, storm totals reached and even exceeded 30 inches.”
In terms of the skiing, I’d say that the quantity of the new snow was absolutely there – it was a fantastic resurfacing and the groomed slopes were skiing as beautifully as one could imagine. The powder skiing definitely left something to be desired relative to our typical off piste conditions from a storm though. The snow was quite dense, and often windblown. We found that the trees offered some protection from the winds, so we typically got our highest quality turns there, but it was still Sierra Cement/Cascade Concrete type stuff and it would toss you around easily if you weren’t on your game or as it became more chopped up. It actually looked like a nice day to be on a snowboard with the dense snow. The skiing was still awesome of course, but it was just surprising that the backside champagne never developed enough to set the impressively right-side-up turns we’d anticipated. Presumably the parameters for optimal snow growth didn’t come together everywhere as the storm was finishing up
“I found several inches of new snow and bottomless turns along the trees to the skier’s right of Upper Meadows on my snowboard, so things were definitely looking up.”
This morning revealed a storm total of 3.3 inches of snow at the house, and 4 to 5 inches at the local resorts of the Northern Greens. We were eager to find out how well the new snow had covered up the old base as we headed off to out afternoon session at Stowe, so as soon as I’d grouped up with Molly and Dylan, we took a quick run off the Meadows Quad to get a sense for the conditions. I found several inches of new snow and bottomless turns along the trees to the skier’s right of Upper Meadows on my snowboard, so things were definitely looking up. I could see that snow options must have been pretty nice in the morning when the trails were relatively untracked, but there was definitely enough snow for use to head over to the Toll House terrain and surf some of the new powder on the boards.
E was potentially going to join us on her snowboard once she’d taken care of ensuring everyone was in their ski groups, so our group picked up Molly’s friend Julia on her skis and did a quick run off the Adventure Triple to take in some of the powder that remained below the lift. We all got together with E, and immediately made our way over to the Mountain Triple Chair on Mansfield to take in what we hoped to be a nice long run full of surfy powder turns down to the base of the Toll House Lift. I was a little leery of brining everyone into the Sunrise Glades because I wasn’t sure about their comfort level in the trees on their boards, but once we got past the Stowe Mountain Chapel and could see all the untracked powder in the various Toll House trees, everyone just dove right into the woods. There were a good 3 to 5 inches of powder with few if any tracks, and with that amount of cushion, I had no concerns about people’s ability to make turns or experience the tumbles we would all inevitable take. We rode the usual assortment of trees down much of the length of Toll House, and everyone had a great time surfing their way along. The moderate pitches there were just what the doctor ordered for the amount of powder we had available, and the exploration and practice riding in the trees made the experience a huge hit. We wouldn’t have been in there riding that fresh powder if it hadn’t been for the overnight snow.
We worked our way back to the Spruce Peak Village to end the day with a food break, and another one of my old straps on my snowboard broke, so that made for an adventurous return trip. I really do need to invest in some new bindings since mine are 20+ years old and the plastic is obviously getting brittle. Perhaps I’ll find an end of the season deal on something. I wouldn’t mind some of those Burton Step On® bindings – I’m so sick of dealing with those snowboard binding buckles, especially my broken ones!
I was planning to head to Bolton Valley for a bit of touring this morning, but when I saw they were reporting about 4 inches overnight, whereas Stowe had early reports of 8 or 9 inches, I switched up my plans and decided to do a few lift-served runs at Stowe instead. My snow analyses from the morning indicated that the new snow had come in around 5% H2O, which was a setup for some great powder turns.
I had a bit of interesting serendipity on this morning’s outing. I parked in the upper Gondi lot, planning to do most of my skiing there, but I had a pass issue that required me to head over to Spruce. Once I’d gotten things straightened out with my pass, I decided to just roll with it and catch some runs while I was over there. I headed out to the lifts and noticed something surprising – the Sensation Quad was running, but the Sunny Spruce Quad was down. The reverse is common if there are wind issues, but certainly not the combination they had today (it turns out it wasn’t a wind issue, it was mechanical I guess). Anyway, with Sunny Spruce down, it was pretty much country club powder skiing on that terrain for the few folks that felt like accessing it. I did an initial run on Sensation, which was pretty quiet aside from the NorAm races, and got some of the first tracks down Spruce Line. After that I did a couple of laps on the vacant Sunny Spruce terrain, running a circuit with the Meadows Quad and Sensation Quad, and of course including a hike to the top of Spruce Peak each time to get in that extra powder and make up for the fact that I was riding lifts instead of skinning.
“It was skiing much deeper than a foot at times, and doing some checks I was getting powder depths of 22 to 24 inches.”
It was snowing nice fat flakes all morning, and the increases in snowfall intensity were often quite notable as you headed up in elevation. It typically wasn’t an intense pounding snow, but often nice and steady, and sometimes you’d have that fairly decent snowfall with sunshine at the same time. There were a couple of times with the perfect simultaneous combinations of flakes and sun that I had to stand there in awe and soak in the mountain scene. And it was all gorgeous upslope flakes – the 5% H2O I’d found in my morning snow analyses was probably about what we had where the snow wasn’t affected by any wind. It was simply great snow quality with some good right-side-up nature to it thanks to some dense snow that had fallen at the beginning of the storm cycle.
Most off piste (and even some on piste) terrain I encountered was definitely delivering that 48-hour total of 13” that I’d seen in Stowe’s snow report. My first depth check of the day was in the Meadows East Glades, and my measurement came right in at 12 inches. I checked in spots off Upper Sterling and was typically getting 12-14”. I eventually got back over to the Gondola terrain and was really impressed with the skiing in the Bench Woods. It was skiing much deeper than a foot at times, and doing some checks I was getting powder depths of 22-24”. I did push through some sort of slightly thicker layer in those measurements, but it must not have been too sturdy because I was definitely skiing a lot of lines where the snow had that “up to the thighs” feeling. That’s typically in the two-foot realm vs. the one-foot realm. I found a sign I’d never seen in that area that said “Bob’s Rash”, and I have no idea how much of the terrain that sign was meant to cover, but the lines below it were beautifully steep and loaded with the kind of powder that billows up above your waist.