Based on the quality of yesterday’s skiing, I was leaning heavily toward heading out for another tour today. The backcountry conditions around Bolton are already quite good, and they were reporting another 2 to 4 inches of new snow this morning, so that was a nice bonus. Temperatures were expected to be about the same as yesterday, which meant single digits F.
Ty was able to join me today, so it was great to have company, and we were able to get some actions shots in the powder. We did a tour somewhat similar to what I did yesterday, but we lengthened it out a bit more. Instead of heading up to Heavenly Highway and working our way down to North Slope, we went all the way up to Moose Glen and then wrapped around on a descent toward the glades around Snow Hole, which was roughly a four-mile tour. I chose that route to get us some relatively high altitude turns after observing the notable improvements in the overall snowpack above 2,500’ yesterday.
The number of visitors at the resort seemed a bit less today – there was no sign posted about the Village lots being full, and we easily grabbed a parking spot in the upper lot by the entry to the Backcountry Network. With cold temperatures preserving the snow, conditions were similar to yesterday with 1 to 2 feet of powder available wherever wind hadn’t scoured it to lower depths. Touring some of the higher elevation trails allowed us to see the various areas that had been hit by wind, and you just had to be cognizant of where winds had affected the snowpack to pick the lines with the best undisturbed powder. The middle elevations were much less disturbed by the wind, and you could pick just about line and get some great powder turns.
The models suggest we might have another long-duration system like this past one starting up tomorrow night and running right through the week, and I see that Winter Weather Advisories are already up for the Northern Greens in anticipation of some of that snowfall.
Our current storm cycle started up back on Wednesday, with low pressure deepening as it passed over southeast New England and up into Maine. It then headed on up into eastern Quebec, stalled there for a bit, and finally moved to northwest to James Bay, where it’s expected to sit until about Monday. While this isn’t a stacked low-pressure system sitting in the Canadian Maritimes feeding continuous 1+”/hr. snows into the Northern Greens, the broad cyclonic flow supported by the various positions of the low pressure has kept the area in a nice moist westerly/northwesterly flow that’s been feeding snow into the mountains. So, this isn’t a typical 24-, 48-, or 72-hour type of storm cycle; it’s a much more drawn-out sort of “cycle”. I wasn’t sure how the positions of this low would actually play out with respect to snowfall, but since well before the start of the storm the National Weather Service Office in Burlington has been on it – they felt that the potential was there for solid amounts of snow over the protracted period. And they certainly weren’t wrong. It’s been a little tough to total up the mountain accumulations for the full event because it’s already been going on for four days, and the resorts typically only report up to 48-hour accumulations, but it looks like anywhere from roughly 1.5 to 3 feet have fallen in the Northern Greens from the system as of today.
Bolton Valley was reporting 4 to 6 inches of new snow overnight on top of their previous accumulations from the system. I’d already been finding snow accumulations of 9 to 10 inches when I was out touring at Bolton on Thursday, so between whatever fell Thursday night into Friday, plus these additional Friday night accumulations, there seemed to be some good powder potential out there. Temperature forecasts for the mountains were in the single digits F today, so touring seemed to be the best option. E was initially going to join me for a ski tour, but after thinking about the temperatures for a bit, she ultimately decided to work out at home instead.
I headed up to the mountain a bit after noontime, and people certainly didn’t seem to care about the temperatures – the signs were up for visitors to park at Timberline because the upper lots were full. Being after noon, I knew I’d be able to get a spot from someone who was leaving for the day, so I headed up to the main base anyway. I still ended up getting a spot in the lowest tennis court lot though, and that changed up my touring plans a bit. I had initially planned to ascend at the start of the Wilderness Uphill Route and then make my way toward Gardiner’s Lane, but since I was parked right down by the Pond Loop area with easy access to the Bryant Trail, I ascended there instead. I had just planned to loop around Bryant Cabin and then head out to start my descent on North Slope, but the temperatures felt great while touring, so I continued on up to Heavenly Highway, topped out around 2,800’, and started my descent via the “Not a Trail” glade. From there I continued down North Slope and then made a second ascent to ski some of the glades in the Snow Hole area.
It was clear that powder depths had increased at the resort since I was last there on Thursday. Winds have died down substantially now, so measuring the snow is much easier, and right at the car at ~2,000’ I was getting 8-12” depths for the surface snow above the base. By 2,500’ the typical depths were in the 12-16” range, and around 2,800’ I’d say they were 12-18”. I’d still think that’s somewhat conservative though, because I was often finding powder depths of 24” up around 2,700’-2,800’. Right now, getting up above 2,500’ makes a real difference in the snow though, because those areas must have done really well during our previous warmup – the interface between the surface snow and the base has mostly disappeared by that point (making it harder to measure just the new snow), and the skiing is really good. Dropping into my initial descent, I could tell that the overall snowpack was really deep. Below that top 24” of powder there was substantial base, and I’d say the snowpack there has to be 40 inches. The snowpack at the Mt. Mansfield Stake was at 39” as of a couple of days ago, and it hasn’t been updated since then, but based on what I found out there today a few miles to the south, it’s got to be over 40 inches by now.
Anyway, I’d recommend doing most of your touring up in that 2,500’ to 3,500’ elevation range if you can – it’s just a notable improvement in the overall snowpack below 2,500’. It’s still nice skiing down there, but it’s sort of mid-fat powder conditions below 2,500’, and full-fat conditions above 2,500’. I toured on mid-fats today, but I was wishing I had fat skis in that deep snowpack above 2,500’. The powder is of medium weight, so there’s plenty of liquid equivalent in there to really keep you off the base. As of this evening we’re approaching an inch of liquid equivalent from this system at our site in the valley, so you know the mountains have had at least an inch of two of liquid equivalent from this system so far, and it definitely felt like it based on what I experienced above 2,500’ today.
With respect to the ongoing storm, there was generally light but consistent snow falling when I was out on the mountain today. The flakes were small, in the 1 to 2 mm range, so it was hard to gauge snowfall rates, but I had to clean a decent layer off my car when I got back to it after just an hour or two of touring. Toward the end of my tour, the flake size was picking up noticeably to roughly 2 to 8 mm flakes. Down here at the house, we’ve had light snow all day, but it’s picked up more this evening with larger flakes, especially when strong echoes come through as more pronounced shortwaves embedded in the overall cyclonic flow move through the area. Based on what we’ve been seeing here at the house this evening, there should be at least another few inches out there by tomorrow morning for the mountains.
Our anticipated long-duration storm system began in the area yesterday with some light snow accumulations for the mountains and valleys, but snowfall really picked up overnight, so I decided to head up to Bolton today for some turns. As of this morning, Bolton Valley was reporting 7 inches of new snow from the storm, and snowfall has continued today. Their reported storm total seemed like a good amount for some ski touring, so that was my plan if I was heading up to the mountain alone. Dylan didn’t work until the afternoon, so he was planning to head up for a morning lift-served session with his fried Parker, and E had the day off due to school closures from the storm and she was thinking of going as well. Those plans fell through though – the winds were so strong that the Vista Quad Chair was on wind hold before it ever opened, and even the Mid Mountain Chair quickly went on wind hold in the morning. The only chairlift running by mid-morning was the Snowflake Chair, and with most of the Snowflake terrain not open, we generally felt that it wasn’t worth heading up for such minimal terrain. That brought me back to my original plan of ski touring on Wilderness.
Down at our place in the valley we’d picked up 4 to 5 inches of snow from the storm at that point, but the contrast in accumulations was stark as I dropped down into Bolton Flats on my way to the mountain – the snow accumulation there looked like an inch at most. Accumulations were the same at the base of the Bolton Valley Access Road at 340’, and I had to get above 1,000’ before I really started seeing accumulations of at least a few inches. Up in the Village parking areas, it was impossible to find a sheltered spot to get a reliable measurement of accumulations at 2,000’, so I had to wait until I got into the relative shelter of the Wilderness Uphill Route to really check the snow depth. Once one the ascent though, I checked the snow depth along the sheltered edge of Wilderness numerous times, and the measurements were all between 8 and 9 inches, with one measurement of 7 inches. At 2,500’ I was measuring 9 to 10 inches of accumulation, and I never got any reliable measurements higher than that, even up above 3,000’. I stress “reliable” because the winds had wreaked havoc on the snow in many areas. Some spots were scoured down to the old base, and some places had 5-foot drifts. Up at the Wilderness Summit at 3,150’ the winds were absolutely howling – they had to be in the 50 to 60 MPH range at times. Finding a sheltered spot to pack up my skins was a huge challenge. Thankfully, temperatures were in the 20s F, so there wasn’t frigid cold to go with those winds. Photographs of gentled-settled powder snow were difficult to come by today, but if you wanted to get images of drifts… they were everywhere.
Here’s the snow accumulations profile I saw as of midday in the Bolton Valley area for this ongoing storm:
The skiing turned out to be excellent though. As long as you avoid any wind-scoured areas, there’s been a really decent resurfacing from this storm so far. We’ve picked up ¾” if liquid equivalent from the storm at our site down in the valley, and the mountains should have had at least that much, so an inch of new liquid equivalent up there seems very reasonable based on what I experienced today. The new snow our there certainly wasn’t fluff; with all the wind, it was actually feeling like typical 10% H2O synoptic snow, and out of the wind, the new snow was substantial enough to even resurface black diamond pitches. So, while it wasn’t sublime champagne powder, it was decent medium-weight powder, and it was much more what the slopes needed with respect to resurfacing.
We didn’t get too much accumulation (about an additional half inch) during the day today here at our house along the spine because as forecast, the Froude Numbers went well above 1.0, but they may have come back down a bit because we’re getting some decent accumulation this evening with these more recent bands of moisture pushing through.
Today the temperatures were still quite cold, so I again opted to stick to ski touring instead of riding the lifts, but it was a bit warmer than yesterday, and I decided to go a bit farther afield and higher in elevation. I set my sights on skiing in the Sterling Range, an area that has been on my list of ski touring spots for quite a while, but I just hadn’t gotten around to making the trip. A very convenient access point to the range is through the Sterling Forest area, and they have a really nice parking lot that’s maintained at the top of Sterling Valley Road.
I’d been up to the area in the warm season for mountain biking, but I haven’t been up there much in the winter. The snowpack around the houses up there is impressive, and you can tell that the area gets, and holds, a lot of snow. I guess it shouldn’t be too surprising with a number of houses that are well above elevations of 1,000’. Indeed there’s some good elevation there as you approach the Sterling Forest – the parking area is around 1,700’, which is 500’ higher than where I began my tour yesterday.
Most people I’ve talked to, as well as reports and videos I’ve seen, use the Upper Gorge Loop trail area as their main thoroughfare for touring. It serves as the approach and as a collector trail if you’re skiing the north side of the basin. For my approach I followed the northerly section of the Upper Gorge Loop Trail, which seemed to be the most popular based on the levels of traffic packing the snow. Following the trail, I began to see skin tracks branch off to head up the north side of the basin, but I continued on the loop trail until I hit its apex, just so I could get the lay of the land. I then skinned back a couple of minutes and took the highest skin track that was available. That brought me to the top of the ridge on the north side of the basin, and along the way I passed numerous open glades that had very few tracks and offered a lot of impressive skiing. I topped out around 2,900’ along the ridge, and descended through the glades back to the Upper Gorge Loop Trail.
Powder depths were very similar to what I found yesterday with respect to similar elevations. I was curious if there might be a difference in surface snow depths since I was about 12 miles farther north in the Northern Greens, but my measurements didn’t reveal any substantial differences. I did ascend substantially higher on this tour though, so it let me add on to what I’d found yesterday. The powder depth profile I found today was as follows:
There are other options for nice touring out there, such as dropping down the back side of the ridge into the next drainage, but the approach to the slopes in the main basin is already a couple of miles even before you begin the main ascent through the glades, so I couldn’t really tack on more with the time I had. It was a gorgeous midwinter day though, with lots of sunshine, and that definitely helped to bring the temperature up that extra notch relative to yesterday.
Since today’s forecast was in the single digits F, and there was the possibility of wind as well, ski touring seemed like the natural choice vs. riding the lifts. In addition, our current weather system, while certainly enough to freshen up surfaces, isn’t expected to be large enough to really reset the powder in areas that had been recently skied.
With the cold temperatures, and the way the depth and quality of the snowpack has been improving over the past week or two, I decided that I’d tour in some relatively low elevations nearby to see what potential they held. I started my tour at the Catamount Trail access area at roughly 1,200’ on the Bolton Valley Access Road, and did a ski tour up to the Buchanan Shelter near the 2,200’ elevation. That’s not a heavily used part of the Bolton Valley Backcountry Network, so I suspected that untracked powder would be relatively plentiful.
While I was out touring in the afternoon, light snow fell continuously, and throughout the tour I checked powder depths above the highest detectable subsurface layer in the snowpack. The powder depth profile I found with respect to elevation was as follows:
Even with cold temperatures, powder of the 3-4% H2O variety that we recently received from Winter Storm Heather can’t sustain that level of loft forever. Indeed, the powder I encountered today had settled down to something more in the 6-8% H2O range, so the numbers above are the depths to which the surface snow has currently settled. Obviously all these recent storms continue to push the useful snowpack to lower and lower elevations, so overall snowpack depth wasn’t an issue even down to the 1,200’ mark. It’s hard to get estimates of the total snowpack depth because the lower layers are so settled and thick, but the snowpack is maybe a couple feet deep down at 1,200’? While I don’t have an exact number, even if there was only a foot of base below the powder, it’s so consolidated and flush with liquid equivalent that it would easily do the job.
In terms of the skiing, the best turns were certainly up in the slopes just below the Buchanan Shelter where there is some solid pitch up into the black diamond realm. The approach portions of the tour have enough pitch to make a nice glide out and grab a few low-angle turns in certain spots, but with the current depths and density of the powder, descent speed is on the slower side right now. Also, cold temperatures like these reduce ski glide somewhat due to less melting, so that factors in as well. In the slopes up by the Buchanan Shelter I had the run of the area though in terms of fresh tracks. One person had recently skied back down the Beaver Pond Access Trail, but that was even a bit old, so it must have been from a couple of storms ago. Off in the trees, there were no prior tracks of any kind, so I had my pick of the most open lines, streambeds, chutes, etc. Fat skis were the call, and turns were definitely bottomless, but the best turns came from hitting those correct areas that appropriately accommodated the pitch, powder depth, cold snow, tree spacing, and all that. There were some excellent powder turns on the tour though, so even down to the lower elevations in the ~1,000’ range, the current snowpack is really delivering.
By observations time early this morning, the backside snows of Winter Storm Heather had departed and skies here at the house were partly cloudy. The clear skies didn’t really seem to jive with the imminent snow I saw in the forecast, but sure enough, clouds soon began to roll in, and within an hour, flakes were flying.
I decided to get in a quick morning session up at the mountain, and the snowfall continued to intensify as I ascended the Bolton Valley Access Road. Up in the Village there was steady snowfall, and while it wasn’t the pounding 1-2”/hour snowfall of yesterday, visibility dropped substantially and it felt like we were right back in the meat of the storm. It looks like today’s snow was rolling in from the lake effect snow event off to the west, so we thank our big friend Lake Ontario for that.
Wilderness was the hot ticket for skiing today, since the Wilderness Double Chair doesn’t run on Mondays and Tuesdays, and this was the first chance for lift-served access to all the recent snowfall from Winter Storm Heather. I decided to start off with a short workout ski tour using the Wilderness Uphill Route, then stuck around for a bit of lift-served skiing after that.
It’s getting a bit tougher to discern how much powder came specifically from Winter Storm Heather, since it’s just blending in with the layers below it as the subsurface is buried deeper and deeper, but the approximate powder depths I found today were as follows:
2,000’: 6-8”
2,500’: 8-10”
3,000’: 10-12”
There was definitely a bump in powder depths even compared to what we skied yesterday thanks to the additional overnight snow and the new snow that was falling. One obvious clue that depths had increased was the fact that the snow was now getting a bit too deep for low-angle terrain. Moderate angle and steeper terrain are now providing the best powder turns. I had a feeling we’d be getting to that point today, and indeed while I’d been on mid-fats for the past few days, today I bumped up to the fat skis and that was the correct call as long as you were skiing untracked snow.
Bolton Valley is indicating that they’ve picked up roughly 60 inches of snow since the start of the year, which is very solid snowfall total for the first half of the month. Heck, 60 inches of snow is respectable even for a full month’s total at many resorts.
It wasn’t even snowing this morning when Ty and I headed off to Burlington for an early appointment, so we knew we’d be giving Mother Nature some time to get rolling and freshen up the slopes. The snow from Winter Storm Heather started up a couple hours later, and by midafternoon we decided to head up to Bolton Valley for some turns.
We were happy to see that the Timberline Quad was running, so were able to park and start our session right there. Snow was simply pouring down at that point, and my initial measurements revealed storm totals of 4-5” at 2,500’ and 6-8” at 3,000’.
The snow was light and dry (my past couple of liquid analyses from down here in the valley averaged right around 4% H2O), so it was very high quality powder. With such cold smoke snow, you weren’t getting bottomless turns on steep terrain, but you could on low and moderate angle terrain, and the turns were great even if you were contacting the subsurface.
It was pounding 1-2”/hour snow the entire time we were on the mountain, so one could easily tack on another couple inches or so to the storm totals by closing time, and it even kept snowing into the evening.
In this morning’s update, Bolton Valley was reporting an additional 3-5” of snow from yesterday’s lake-effect snow and snow squalls. The other recent snowfall numbers they had in their report looked solid, with 12” in the last two days, 27″ since Tuesday night and more than 48” for the first half of the month. The season snowfall for the resort currently stands at 157”, and that’s very respectable since it’s already about half their annual snowfall average when we’re not even halfway through the snowfall season. What makes that pace more impressive is that they’ve had all that snowfall despite the second half of December being quite lean on snow. That really speaks to how much has been falling up there during the snowier periods.
There was no new snow falling today, which was somewhat notable because this morning’s snow report also indicated that if the current forecast for tomorrow’s snow comes through, they’ll be looking at 14 out of the first 16 days of 2024 with snowfall. With today’s break in the falling snow, I figured it was time to head out for a tour on the backcountry network as a reliable route to untracked powder.
I decided to head up the Bryant Trail to Bryant Cabin in the afternoon, and play it by ear with respect to lengthening my tour, depending on how my supply of daylight was looking. I was well ahead of sunset when I was up at Bryant Cabin, therefore I just continued on up to the Catamount Trail Glades so I could get in some turns in the higher elevations. Based on my recent outings at the resort, I knew that conditions improved a lot with elevation, so I wanted to get a good sampling of the powder up high. I topped out at an elevation of about 3,100’ on the back side of Bolton Mountain, descended through the Catamount Trail Glades, and then traversed back above Bryant Cabin and navigated a route through another half dozen different glades back to the base. Today definitely had a nice midwinter vibe, with bright afternoon sun, temperatures somewhere around 20 F, and great powder.
The surface powder and upper snowpack analysis was really interesting today. Starting my tour around 2,000’ in the Village, I found 4-5” of surface powder, and then there was a fairly solidified layer below it. That layer marks the wet snow that recently came from Winter Storm Gerri, which hardened up somewhat as temperatures dropped back below freezing. The surface snow above it is from the snow on the back side of the storm, plus the additional drier snows that have fallen over the past couple of days. As you ascend to higher elevations though, that firmer layer gradually begins to soften, and then above 2,500’ it starts to disappear altogether. At that point there is another substantial subsurface layer, which I suspect comes from Winter Storm Finn. So, monitoring the elevation profile for the depths of the powder was bit unusual. Compared to the 2,000’ elevation, I didn’t detect any notable increase in the powder depths at 2,250’, but at 2,500’ it finally started to deeper, and as I continued higher, I could still sort of detect an interface from Winter Storm Gerri, but it eventually became hard to discern. So, what I’ve done for the surface snow depth elevation profile below is to indicate those different layers, with the first depth being snow down to the dense layer from Winter Storm Gerri, and the second being the depth of the snow down to the dense layer from Winter Storm Finn.
At some point between 2,500’ and 3,000’ that first depth number sort of becomes moot, and you’re essentially skiing in the 8-16” of powder depending on elevation, so go I’d say go in with that mentality. In terms of getting out there in the backcountry around this part of the Northern Greens, I’d recommend touring above 2,500’ if you can for the best turns. I went with mid-fats on today’s tour, but you could easily go with fat skis if you’re going to spend most of your time above 2,500’. When I was up in the Catamount Trail Glades in the 3,000’ range, fat skis would have been nice, except in some of the denser areas of evergreens where they have trapped so much of the snowfall on their boughs, that you actually notice the deficiency of powder below.
The system that is expected to come into the area tomorrow is name Winter Storm Heather, and any snow from that should really be icing on the cake in terms of the ski conditions. Temperatures are forecast to stay cold, so you can pretty much take the powder depths I have above and then tack on whatever new snow comes next.
With the additional overnight snowfall, Bolton was reporting a total of 9 inches from Winter Storm Gerri as of their early morning report. And, since the Timberline Quad didn’t open yesterday due to winds, today would also be its inaugural run of the season. E and I figured the chance to visit the Timberline terrain that nobody has really skied at all up to this point was a nice bonus.
Based on the conditions I encountered yesterday, I really expected the main mountain to offer the best conditions today, especially above 2,500’ where the snow was never too wet. However, there was always the chance that the lower elevation Timberline terrain would still surprise us due to all the fresh snow. After our first lift ride on the Timberline Quad, the lift actually had to go off line for a time due to a mechanical issue, so heading to the main mountain turned out to be the appropriate option anyway.
Not surprisingly, there were a lot of fresh tracks to be had out there today, but I’d actually say the snow quality below 2,500’ was a notch beneath what it was when I was out yesterday afternoon/evening. Yesterday I was skiing in 6 to 7 inches of powder off Snowflake, but the bottom few inches of that snow must have still be fairly wet at that point because we found it had thickened up with today’s cooler temperatures. So, it meant that today we were only skiing in the top few inches of powder and contacting that denser snow below if we pressured our turns hard enough. As long as you had untracked snow, it was nice skiing, but it certainly wasn’t as bottomless as yesterday in those lower elevations. Areas with previous skier traffic ended up with uneven subsurfaces that definitely detracted from the quality of the turns. Thankfully, the dense snow didn’t form anything like a breakable crust, which would have made the skiing much more challenging. On our return trip to the Timberline Base, we did get first tracks down the lower half of Tattle Tale, and that was really sweet, even if the powder wasn’t as bottomless as it would have been yesterday.
Over the past week, the weather pattern has featured these larger systems with ample snow and moisture, and the most recent one in the series is Winter Storm Gerri. It moved into the area overnight in the wee hours with an initial burst of heavy snow. The front end snow in this case wasn’t as potent as it was with Winter Storm Finn that came through midweek, so when we saw that Bolton Valley was indicating only 2 inches of new snow in their early morning report, we knew there was no need to rush right up to the mountain.
We watched the Bolton Valley Base Area Webcam through the morning and could see that up at 2,100’, the precipitation was snow, and it was quite heavy at times. Dylan and Colin headed up to the mountain in the early afternoon, and we asked them to give us an update on what they found. Their impressions were that the snow surfaces were rather wet, and they said the precipitation was even mixed with rain in the lower elevations at times, so E figured that instead of skiing, she’d hold off until the snow got better. I took another look at the webcam feed and saw that there was heavy snow falling, and decided that it would definitely be worth it to head up for some lift-served runs.
Heading up the Bolton Valley Access Road, the precipitation switched over to all snow at roughly the 1,000’ elevation, and above that the road was quickly covered. The road conditions must have been getting a bit slick with the new snowfall because I had to drive around a van that was stuck trying to make it up the steep s-curve below Timberline. I had actually planned to park at Timberline and start my session there, but the Timberline Quad was apparently on wind hold, so I had to continue on up to the main base area. I arrived up in the Village to very heavy snowfall in the 1 to 2 inch per hour range, and with the intensity of that snowfall, there was just no way that the turns weren’t going to be great.
During my afternoon session I managed to get in runs on all the rest of the lifts, and heavy snow continued to pound the resort at all elevations. It was windy, especially at the Vista and Wilderness Summits above 3,000’, but thankfully the wind was from the west and at your back while you rode the lifts. After my first couple of runs, the lights were coming on, and I got to ski Spillway in night mode. I always find it exciting to be able to ski something that steep under the lights, and I knew that the conditions on Spillway were going to be really good because you couldn’t hear anything from the turns of the skiers and snowboarders below you as you passed over them on the Vista Quad. Indeed, my own experience on the trail revealed that the conditions on Spillway were simply fantastic; new snow was falling so heavily that it must have been covering up an slick spots faster than skiers could push the snow away.
I did notice that below the Mid Mountain elevations (~2,500’), the groomed/packed ski surfaces did have that “wet pack” feel that I’ve encountered in the lower elevations of Whistler Blackcomb. That’s usually a sign that some very wet snow has fallen and was packed by skier traffic. I could see what Dylan was talking about with respect to the wet surface conditions, but at the point that I was up there, those conditions were hard to find because temperatures were falling, and it was snowing so hard that those types of wet surfaces were covered up in all but the highest traffic areas. Some of the best turns I found were near the end of my ski session when I visited the Snowflake Chair. That area hadn’t seen much skier traffic, so I found a lot of fresh powder that skied beautifully. I did numerous depth checks and was consistently getting new snow depths of 6 to 7 inches. There was enough powder there that I questioned whether it was all from just this storm, but when Bolton’s afternoon snow update came in and they were reporting storm totals of 5 to 7 inches, that nicely corroborated my measurements.
All this new snow is a great addition to the snowpack, but even without it, one thing I noticed while out on the mountain today was the huge jump that the snowpack has taken since last weekend. I hadn’t been up to the mountain since Sunday, and at that time, patrol was just starting to open up more areas of natural snow terrain as coverage improved thanks to Winter Storm Ember. The contributions made by Winter Storm Finn must have been huge though, because the resort has now been able to open up just about everything, and everywhere I looked this evening, coverage felt like midwinter. As I look back now at my storm data, I guess I see the difference – Winter Storm Ember dropped 0.69 inches of liquid equivalent here at our site, while Winter Storm Finn dropped 1.99 inches of liquid equivalent. That’s almost triple the amount of liquid, and when you get up around 2 inches of liquid equivalent, that starts to become a serious resurfacing of the slopes. Winter Storm Gerri has already dropped about an inch of liquid equivalent here at the house, and the back side snow is still coming through, so that’s simply adding yet another great layer to the snowpack. All told, this past week of storms has dropped almost 4 inches of liquid equivalent here at our house in the valley, so it must have put down at least 4 to 5 inches plus of liquid equivalent for the mountains. When I look at the numbers, I realize now why the snowpack seems to have improved so much so quickly. When I was riding the Wilderness Chair today, I actually saw a ski patroller skiing the headwall of the Wilderness Lift Line to check the snow. You know the snowpack is getting decent when that headwall is even close to being skiable, so the fact that he was even testing it speaks volumes about how things have gone over the past week.