Taking advantage of the October powder today at Stowe
Well, we definitely got to witness Mt. Mansfield flexing the snowfall muscles today – despite the fact that we know this mountain’s ability to reel in snow, it just never gets old. Stowe delivers. I’d certainly been contemplating some turns, but after catching Powderfreak’s comment this morning about how it was dumping at the ski area, and then checking the web cams myself to see snow falling hard and fast at the base, that sealed the deal. Ty has been chomping at the bit for some skiing, so he joined me and we headed out in the early afternoon. Temperatures were in the low 40s F in the valleys, and the precipitation was generally light rain. The Worcester Range was visible to the east, white with new snow, but off to the west, a white haze hung over the spine of the Greens and we could see that it was definitely still snowing up there. The precipitation remained rain as we headed up the Mountain Road, but at ~900’ elevation near Northern Lights Lodge, we started to see leftover snow accumulations along the sides of the road. The snow on the ground continued to build, and by the time we pulled into Stowe’s Midway Lot at ~1,600’, we found 2-4” of snow on the ground up on the grassy slopes above. The temperature had only dropped to 38 F, but the precipitation had changed fully over to a light snow comprised of small flakes.
“…despite the fact that we know this mountain’s ability to reel in snow, it just never gets old.”
We changed things up in terms of equipment today, and instead of Tele, we went with alpine gear using Alpine Trekkers for the ascent. I haven’t had the Trekkers out in a while, but it was time to bring them back into service; I’ve finally moved my old Volkl CMH Explosiv fat skis to rock ski status, and I was eager to try them out on one of these early days. My only Tele rock skis are my old skinny Rossignol Hellgates, and with a waist of just 70 mm, they’re really not a great tool for these early season powder days. Combining Tele + skinny + variable early season powder is certainly a recipe for challenge. Another reason to go with the Trekkers today was that Ty’s boots and bindings are now large enough to easily accommodate Trekkers. He’s not at the stage yet with his Tele skiing that he’s ripping up early season, potentially inconsistent powder with aplomb, so going alpine on the tour would be much more enjoyable for him. We decided to go with his carving skis instead of his powder skis for the setup, and fortunately we were able to get a good fit out of his skins from his Telemark skis.
As usual, the Trekkers were great on the ascent. Although going with alpine skis and Trekkers is notably heavier than Tele, it’s typically not a big deal unless you’ve got huge tours to do. My biggest issue was with my skins – I’m not sure if the old skins for my CMH Explosivs have lost their water repellency, but whatever the case, today’s conditions had them catching and carrying a bunch of snow at times. I’d have Ty clean the underside of the skins off for me when we stopped, but we could never quite keep them from re-accumulating a coating of snow. Fortunately, Ty’s skins had no issues in that regard. The snow on the ground was quite wet at the base, but it dried out substantially as our elevation increased. We ascended via a bit of Perry Merrill, and then Gondolier to the Cliff House, and we observed the following snow depths with respect to elevation:
Aside from Ty’s first chance to try out Alpine Trekkers another new addition on this outing was his own Measurement Ski Pole. I put together measurement poles for both Ty and Dylan this fall, and it was great having Ty reporting depths along the ascent – with two observers we were able to collectively decide on the best approximations of depths to create the list shown above. It also kept Ty very interested in going higher, even if just to see how much deeper the snow was going to get. Although Dylan didn’t go out to the slopes today because he was off with E doing some shopping, based on Ty’s experience I think he’s going to have a lot of fun with the measurements on our next outing.
A shot from up near the Cliff House
It was around 4:30 P.M. when we hit the top of the Gondola at ~3,600’, and the snow was coming down with some good intensity. It wasn’t quite inch an hour snowfall since the flakes were still fairly small, but it felt like it was somewhere between ½ and 1 inch/hr and it was quite impressive. We took shelter under the Cliff House to gear up for the descent because of the intensity of the snowfall, but there was almost no wind, so it was nice to hang out and watch the flakes pour down. With the late hour, thick clouds, and hefty snowfall, it had that dusky feel of December in the north. Ty and I discussed how it just as easily could have been December with all the snow. Another great milestone for Ty was the fact that this was his first full ascent to the Gondola, and it was nice to see that he still had plenty left in the tank at the top. We put a call in to Mom to let here know that we’d be descending soon, but also to let her know about Ty’s accomplishment.
Extolling October Snow
We fueled up with some food and drink, but didn’t loiter too long because we knew the light was going, and we had to get in some shopping for dinner on the way home. Soon, we headed off down Perry Merrill, and one of the more challenging aspects wasn’t the snow, but the intense snowfall and reduced visibility. I’d been sort of soured on my CMH Explosivs the last time I’d used them, because they felt heavy and long and I just didn’t want to push them around, but today I’d say there was a newfound love for them. For whatever reason, perhaps because we were out on open trails instead of tight places, they felt great today – fat and stable, and just what one needs for the inconsistent early-season snow. Ty had to work hard on his skinnier skis to handle the powder, but we worked on technique on the way down and he made some great turns. I told him that if he could ski the powder on these skis, he’ll be cranking away when he’s on his powder skis.
That more intense snowfall was with us on the entire descent, and the freezing line had gone down as well. Back at the car, heavy wet snow was falling, and the temperature was down to 35 F, three degrees below where it had been when we’d arrived. It was the sort of precipitation that soaked you very quickly once you were out of your Gore-Tex, and we both got pretty wet putting away the gear and switching out of clothing. The precipitation eventually changed back to rain as we dropped into the valleys on the drive home, but it was raining quite hard at times. There had already been some additional snow accumulations down to lower elevations by the time we were leaving, and the snow in some of the lower elevations actually looked better than it had on the way up due to some new covering. Overall the quality of the skiing was quite good, especially up high, and it could be even better tomorrow with more snow falling tonight.
Temperatures at the Midway area had dropped three degrees while we were out on our ski tour, and a driving, wet snow greeted us back at the car.
Waterbury snowfall for the 2012-2013 season – broken down by month
The last snowstorm of the 2012-2013 winter season extended all the way out to Memorial Day weekend to produce some great late season skiing, but now that we’re well into summer and all the snow has melted, we can look back at how the winter went down at our location in Vermont’s Winooski Valley. The main focus in the seasonal analysis below is on snowfall, but snowpack and temperatures will be discussed as well. In this post I’ve hit on some of the highlights that came out of the data, and attached our various plots and graphs, but to get to the full data set, you can use the following link:
Thankfully, this past season’s snowfall (144.2″) marked a notable increase over the previous season (115.3″), but the total snowfall for 2012-2013 was still less than 90% of average, so that’s not likely to lift the season into the category of “great” winters. In addition, the amount of snow on the ground at the house last season didn’t help to improve the winter’s standing. Using the value of snow depth days as an integrative way of representing the season’s snowpack, one finds the 2012-2013 winter season producing a value of 729 inch-days, less than half the average value, and right down there in the basement with the well below average 2011-2012 season (688 inch-days). And, if the overall snowpack depth hadn’t already undermined any chances of redemption to an average level, the 2012-2013 snowpack secured the season’s ignominy by reaching the lowest value we’ve seen in January and February (3.0″), and coming within a hair’s breadth of melting out in the area around our measurement stake at a record early date in mid March:
This past season’s rather meager snowpack at our location in Waterbury (red line) relative to average (green shading)
Often, each month of the winter/snowfall season has its own unique flavor with respect to the weather, so one method I like to use to get a feel for the winter is to look at it on a month-by-month basis. Again, the focus below is on snowfall at our location, but snowpack is also considered, as well as mountain snowfall/snowpack and the associated effect on the local skiing. I’ll have a separate 2012-2013 ski season summary coming up, so I’ve kept the ski discussion minimal here in anticipation of a more thorough discussion in that report. The month’s total snowfall is listed at the start of each section below for reference:
Snowfall: 0.1″ – October snowfall isn’t reliable enough down at our elevation to be factored much into the seasonal assessment, but this October was on the weak side, with just a tenth of an inch of snow, vs. the mean of roughly an inch. Regardless of this, there was still enough for the needs of companies like https://divisionkangaroof.com/areas-served/gainesville/ with the weight of the snow causing damage to some roofs. One small feather in the cap of 2012-2013 is the fact that the first accumulating snow fell on October 12th, which beats out 2010-2011’s October 15th snowfall by three days, and now represents the earliest measurable snowfall I’ve recorded here at the house since I started monitoring the weather in 2006.
Snowfall: 6.3″ – November snowfall came in just a bit below average this past season, so certainly not remarkable, but notable in that it was probably about as average a November as we’ve seen. November has typically been feast or famine when it comes to snow. We actually had a total of five snowstorms in November, but a small to moderate storm of 4.4″ at the end of the month contributed the bulk of the monthly total as well as some of the first great skiing of the season in the mountains.
Snowfall: 49.5″ – December held the first lengthy, redeeming snowfall period of 2012-2013. Although the first half of the month was extremely poor on snowfall (just 2.2″ of snow at the house), from the 16th of December onward, temperatures got cold and snow came in for a dramatic change; close to 50″ of snow fell on us in the second half of the month, and as a whole the month actually wound up several inches above average. Those in homes with faulty or no heating in place are likely to struggle with the crushing cold at this time of year which is why it’s so important to conduct regular maintenance on heaters so you’re not left to suffer over winter. Reaching out to the likes of these professionals could help with this – siriuspac.com/heating-repair-service/. A problem left unaddressed could snowball into substantial damage and become more costly to repair over time so it’s well worth acting on it as early as possible. We received our second (15.5″) and fourth (11.7″) largest storms of the season during that stretch, right near Christmas and just a few days apart, so needless to say, the snow was there to set quite the holiday mood in the valleys and up above on the slopes.
Snowfall: 21.9″ – January continued that good, snowy weather pattern in its first week, albeit to a lesser degree than December, but unfortunately that modest first week ultimately wound up representing roughly half of the month’s snowfall. The second week featured a couple of substantial thaws with no measurable snow, and in fact we received no accumulating snow at all for the period between January 7th and 16th, a very long stretch for the mountainous areas of Northern Vermont during the winter. The third week of January offered just a few small systems, and the fourth week was arctic cold with minimal snow. The final week attempted to recoup the losses with a modest half foot storm, but it was too little too late – the month ended with just 21.9″ of snow, by far the lowest January in my records. The combination of very low snowfall and two January thaws was very deleterious to the valley snowpack – after coming down from the depths achieved in December, the snowpack depth at our location never even reached 10 inches again during the month, and got as low as 3.0 inches. That is ridiculously close to losing the winter snowpack in January, definitely the closest we’ve come based on my records since 2006.
Snowfall: 31.4″ – February was again below average in snowfall, partly due to the continuation of the dry arctic pattern in the first week, and it wound up missing the mark for the lowest February in my data set by less than an inch. Although that persistent dry pattern didn’t make for a very snowy first half of the month, our third largest storm of the season (12.6″) hit in the second week. It was still a rather modest storm, but at least it did break that one foot mark for accumulation at the house. By the end of the third week of February, the snow depth at the Mt. Mansfield stake actually poked above average for the first time in about a month and a half – but it was only by a couple of inches, and it quickly went back below average as the snowpack sat there essentially stagnant for an entire month. On February 21st, the snowpack was at 65″, and roughly a month later on March 18th, it was still at 65″, without any major consolidation of more than a few inches. That’s stagnant. Our snowpack at the house languished similarly, never even getting above 10 inches of depth during that stretch – and that’s a time of year when it is usually building to its peak of the season. The carryover of the low snowpack from January also set the lowest mark (3.0″) for snowpack that we’ve ever seen in February.
Snowfall: 4.2″ – April was even a couple inches below average for snowfall, but temperatures stayed cool enough to keep the winter season rolling along, and that’s what really helped make the period wintrier. We didn’t have any notable April snow accumulations down at our elevation, just a couple of small ones on the 2nd, and again on the 12th – 13th, but the mountains continued to get fresh snow right into mid month to keep surfaces in great form and the Mt. Mansfield snowpack robust.
Snowfall: 0.0″ – There was no accumulating May snowfall down at the house this season, but that’s not too much of knock on the Month, because not getting snow in May is more the norm than actually getting snow. The mountains did get that beautiful Memorial Day weekend storm though, and the late season powder skiing was mighty fine. Although I can’t factor that directly into the analysis for the valley, it was quite cold in the valleys at the end of the month, and close to even snowing there.
There were a couple of other interesting notes with respect to snowfall this season:
1) Storm frequency and average storm size: Despite coming in below average for snowfall, the 2012-2013 season offered up a healthy 51 accumulating snowstorms, almost up there with the 53 storms we received in 2007-2008. Of course, to come in below average for snowfall with that many storms indicates that the average snowfall per storm was down, and indeed it was. At 2.8″/storm, 2012-2013 ranks down there with 2011-2012 (2.6″/storm), the only odd seasons out compared to the more typical seasons up near 4″/storm. For whatever reason, this season’s average came in on the low side. This is presumably due in part to many of the everyday events being on the small side, but also due to the lack of bigger storms, which is covered in point #2 below.
2) Storms with double-digit snowfall: It’s certainly an arbitrary and subtle distinction, but after looking through my data, I noticed an interesting trend with respect to each season’s largest storms for our location. In my season summaries, I always make a list of the top five storms of the season, and when the season seems to have gone well, all of those top five storms have been in the double digits for snowfall. In fact, the “best” seasons thus far have been able to surpass that five-storm threshold. For reference, here’s the top five list for this season, with the links to the detailed web pages for each storm:
Indeed, if we look at the number of storms with double-digit snowfall by the seasons, we see an obvious trend. With the number of double-digit snowfall storms listed in parentheses after the season, one notes those “good” seasons – 2007-2008 (6), 2008-2009 (7), 2010-2011 (7) seemed to find a way to exceed five double-digit storms, whereas the poorer snowfall seasons – 2006-2007 (4), 2009-2010 (2), 2011-2012 (3), 2012-2013 (4) just didn’t. Surely the law of averages comes into play here to some degree – seasons with patterns producing lots of snow likely have a greater chance of getting a big storm in here, but that’s not a given. It’s also very suspicious that those seasons that come in sort of in that middling ground like 2006-2007 and our season of interest for this summary, 2012-2013, fall just short of making the cut. I suspect this trend may be more intact in a location like ours because of the relatively high number of storms and snowfall, and upslope snow (which was on the low side this season) as an extra protection against huge snowfall variance, but this is going to be an interesting trend to follow into the future as a gauge of snowfall seasons.
In sum, while snowfall was certainly a bit below average, and snowpack was well below average, I’d still give the season a reasonable grade. If C is average, I’d go with a C- for 2012-2013, just a bit off from making the average. Were snowpack a more significant factor in my winter preferences, one could argue for going a bit lower, but at least minimal snowpack was maintained throughout the entirety of the winter to keep everything white. Overall it could have been a lot worse, and with the amount of snowfall we did get, it’s hard to drop the season into the D range, which, based solely on snowfall and snowpack at the house, is where I’d put a season like 2011-2012.
Snowfall: Compared to the snowfall-deficient 2011-2012 Ski Season, the 2012-2013 Ski Season was certainly a step up, but it was still generally below average for snowfall in the mountains of Northern Vermont. It was Bolton Valley that seemed to fare the worst of the northern resorts along the spine of the Green Mountains, perhaps due to their west slope location and this season’s dearth of upslope snow; they reported just 78.5% of their average snowfall. Heading northward, Stowe and Smugg’s fared a bit better at around 85% of average, and Jay Peak reported roughly average snowfall. Down at our house in the Winooski Valley, snowfall was 88.6% of average, so not too shabby by most accounts, but a bit below the mean like some of the local mountains. These past two seasons have actually been the first pair delivering back-to-back below average snowfall in our area since we started keeping track in 2006. Those numbers can be seen in both our Waterbury Winter Weather Summary Table, and the table of Bolton Valley annual snowfall below; this past season’s snowfall is highlighted in blue:
Low snowfall last winter meant back to back seasons with below average snowfall at Bolton Valley.
Snowpack: Aside from the spikes associated with a couple of early season storms, the mountain snowpack was below average going into mid December. That changed quickly though, with the onset of all that new snow during the second half of the month. The above average snowpack achieved during the holidays didn’t actually stay that way during January’s warmth and lack of storms. After consolidation, the snowpack generally trundled along at or below average through February’s continuation of relatively low snowfall. From mid February to mid March, the snowpack sat there essentially stagnant for an entire month; to wit, on February 21st, the snowpack was at 65”, and roughly a month later on March 18th, it was still at 65”, without any notable consolidation of more than a few inches. The late season stretch from mid March to mid April represented a nice rebound for the mountains however, with some quick gains from the big Northern New England March storm getting it above average, and the snow depth staying at least modestly above during the period.
Two periods stood out this past season for above average snowfall: The holiday period and mid-March through the end of April.
Tree Skiing: One metric used as a rough guide for the start of off piste skiing in the Northern Green Mountains is the point at which the snow depth reaches 24” at the Mt. Mansfield stake. For those unfamiliar with how this metric was established, it’s described in some detail in the 2011-2012 ski season summary. With the incorporation of this season’s data, the mean date remains at December 12th ± 19 days, with an average depth at the stake of 25.9 ± 2.7 inches. After the very slow start in 2011-2012, in which the 24” depth wasn’t attained until January 3rd (more than a standard deviation later than the mean), this past season was notably earlier. The plot below shows the date at which 24” was obtained for each season since 1954, with 2011-2012 shown in red, and 2012-2013 shown in green:
Each star marks the date of attaining a snow depth of 24 inches at the Mt. Mansfield stake, covering all years since 1954. Although still a bit later than average, reaching a depth of 24 inches at the stake this past season (green star – Dec 22) occurred much earlier than the previous season (red star – Jan 3). The mean date for attaining a depth of 24″ is marked by the large vertical bar in the center of the plot, and the smaller bars indicate the range of one standard deviation above and below that mean.
This past season, the date (December 22nd, Depth=28”, Green Star) was still later than average due in part to the slow first half of December, but unlike last season it was well within the 1 S.D. bars (thin vertical black lines). Note that the 24” mark is being used as an indicator of when the first forays into appropriate off piste/tree skiing terrain typically start in the Central and Northern Greens. In terms of empirical tree skiing observations, personal experience again lends some support to the use of 24” mark this season, as we began venturing into the trees the very next day on December 23rd at Bolton Valley. It should be noted though, that while the 24” mark was attained on December 22nd this season, the 40” mark was attained the very next day on December 23rd. The 40-inch rule (i.e. reaching a depth of 40” at the stake), is used as an indicator of when most off piste/tree skiing around here is ready to go. Although I haven’t looked into the data, this season has got to represent one of the quickest ascents from 24” to 40” – it’s interesting to note however that after rising to 42” of depth on December 23rd and 24th, the snowpack settled back to 36” for a couple of days before rebounding to 45” on the 27th.
Snow Quality: As an monitor of snow quality for the season, the chronological list of our ski outings has once again been compiled, with those days in which we were skiing powder indicated by a P, and those days in which powder skiing wasn’t available indicated by an X. The availability of powder suggests a fairly high level of snow quality, and the absence of powder generally indicates that temperatures rose above freezing at all elevations. Each listing below represents a link to the full report where images and more information from the outing can be obtained. Outings with an X may still be providing decent skiing such as wet snow, corn, etc. (or else skiing was typically avoided) but aside from the spring period, there’s going to be a price to pay in terms of snow quality associated with these episodes when temperatures eventually cool back down. The pattern of snow conditions in the Northern Green Mountains was fairly typical this past winter, with those days lacking powder skiing showing up in three distinct periods: 1) the early season with its usual temperature fluctuations, up through mid December before the weather pattern changed and the cold weather stabilized, 2) a thaw period in mid January, and 3) the period starting in mid March where spring weather began to make inroads. However, with the way the weather patterns this past spring continued to provide cool temperatures and snowfall, powder skiing generally dominated until mid April. Having analyzed the skiing in this way for the past three seasons, a surprising level of consistency is noted, with an overall average of close to four out of five days providing powder, despite notable differences in the demeanor of these recent ski seasons. The 2010-2011 season, which was above average in snowfall, provided powder on 78% of outings, the 2011-2012 season, which was well below average in many ways, revealed the same 78%, and most recently the 2012-2013 season, which was slightly below average in this area, produced a very similar 77% of outings with powder. The percentages don’t take into account differences in the number of outings each season, but with all three seasons falling into the range of 50 to 60 ski outings, differences in the sample sizes aren’t huge. The list of categorized ski outings with links to their full reports follows below:
The detailed month-by-month synopsis of the season is next:
October: It wasn’t an especially snowy October to kick off the season; we had five rounds of snow in the mountains, and the third one even dropped accumulations to the lowest mountain valleys, but none of the storms were huge dumps, and we had just a tenth of an inch of snowfall down at the house for the month. October’s first snowstorm started up on the 7th, with snowfall being reported at the top of the Mt. Mansfield Toll Road in the afternoon, and by the next morning Powderfreak sent along his picture of 4” of accumulation at the top of the Stowe Gondola. I also got a shot of Mt. Mansfield later in the day with its first accumulation of the season. It didn’t seem like quite enough snow to tempt me out to ski, but the FIS boys hit the snow and provided a thorough report of the turns. The second storm delivered some accumulation on the 11th, with a snow line up around the 3,000’ level and less than an inch of snow found up on Mt. Mansfield. The third storm was the one that finally touched the lower valleys with some minimal accumulations, but in terms of mountain accumulations, I don’t think it was anything more than junkboarding material. The 4th (on the 14th of the month) and 5th (on the 16th of the month) storms of October also appeared to be pretty minimal and generally flew under the radar in terms of discussion. So while it wasn’t a great October for natural snow skiing (with nothing like the back-to-back larger storms at the end of October during the previous season), some folks made some turns and there were several smaller rounds of snow to keep the peaks white.
April: Despite the somewhat slow increases in the snowpack during the heart of the winter, the gains made during the latter half of March meant that the snowpack was at least modestly above average heading into April, and it quickly reached a peak of 87 inches at the Mt. Mansfield Stake when the first storm of the month dropped a foot of snow at Stowe on April 2nd. I was up at Bolton Valley that day for a ski tour, and I got to witness some impressive snowfall rates as the storm crashed into the higher elevations. The alpine terrain above tree line on Mt. Mansfield was in good shape, consistently providing excellent outings during that first part of the month. Cool temperatures with additional snow meant that the snowpack stayed at an above average level right through the month, and another storm on the 12th saw Ty and I enjoying close to a foot of dense powder out in the Bypass Chutes at Stowe on the 13th. The skiing gradually transitioned to full on spring conditions after that weekend as the active pattern waned, and an impressively long stretch of clear weather moved in and stuck around well into May.
May: For most of May, there wasn’t much to talk about in terms of new powder, especially with the extended period of incredibly clear weather that carried over from the end of April and lasted a fortnight, finally ending on the 10th of the month. There was some mighty fine spring skiing right through that period with all the sun and warm weather, even if it did cause the snowpack to decrease a bit faster than it otherwise might have. The tranquil period of warm weather allowed the Mt. Washington Auto Road to open on the 10th of the month as well (definitely on the early side), but since unsettled weather had just returned at that point, we didn’t get to make our spring pilgrimage to the snowfields until the 18th. To really cap the month off well, Northern New England and the Adirondacks were rewarded with a Nor’easter over Memorial Day Weekend, which delivered roughly 3 feet of powder to Whiteface and nearly 2 feet to Mt. Mansfield. Excellent powder turns were made while the valleys were almost fully leafed out for the spring. We didn’t actually head out for any June turns beyond that, but the skiing over Memorial Day Weekend had been so good that it hardly mattered – it was just a few short months until the snows of fall would be returning.
So what about the overall feel for the quality of the ski season in Northern Vermont? Well, much like the snowfall numbers suggest, it feels like it came in a bit below average, even if not horribly so. The mountain snowpack (as gauged by what was seen at the stake on Mt. Mansfield) had its ups and downs, and on balance it probably gets rated in a similar manner to what the slightly subpar snowfall would suggest. Being frequent Bolton Valley skiers and living down below the mountain in the Winooski Valley, our perspective might be skewed a bit downward with the resort receiving just 78.5% of their average snowfall. Having the north miss out somewhat on a couple of big regional storms, while watching a horrid valley snowpack (see the 2012-2013 Winter Weather Summary for details) that kept ski routes to the lower valley bottoms essentially off the table, certainly didn’t win the season any extra points. It seems that 2012-2013 ultimately sits in the lower half of ski seasons and won’t be remembered as anything epic, but it also appeared to hold onto a decent level of powder availability (77%) based on our experiences, and that means there was still a pretty decent amount of good skiing. The fact that even the poor 2011-2012 Ski Season was able to hold onto a powder percentage in that range is also reassuring in that regard, suggesting that there is indeed a certainly level of reliability that can be expected in these seasons where snowfall/snowpack is below average.
We’re pleased to announce the completion of our Bolton Valley Photo Gallery for the 2012-2013 ski season. This year’s gallery is our largest to date, with over 270 images documenting this season’s ski adventures indoors and out, in the front, side, and backcountry, under blue skies and flake-dumping maelstroms at Vermont’sBolton Valley Ski Resort. Continue on to the thumbnail images below and browse away! Detailed reports are associated with every photograph in the gallery, so if you find a scene that sparks your interest, simply hover over the thumbnail image to get the date, and head to the archives on the right side of the page to read the full report. We’ve also got similarly extensive galleries from the past several ski seasons, representing nearly 1,600 photographs from around Bolton Valley, and these can all be found at our J&E Productions Photo Galleries Page. We’ll also have our full 2012-2013 Ski Season Summary coming out later this summer, so stay tuned for that update as well.
“…you didn’t have to worry about hitting anything underneath and you could just let it rip.”
Saturday arrived with a nor’easter developing just like the weather models had suggested. For folks that had outdoor, warm-weather plans for the big holiday weekend, you almost couldn’t find a nastier combination of weather. Temperatures were in the 40s F, and there was plenty of wind and rain. We wondered if we were going to have to turn the heat back on in the house. Reports began to come in about the snow in the mountains, and by mid afternoon, Whiteface was already reporting that they had received 18” of new snow. As the afternoon wore on, even valley temperatures fell down well into the 30s F in many places in New England, and fairly low elevation spots began to report snow mixing in with the rain. Although we weren’t getting any snow down to the low elevations in our area, we lost power from about 8:30 P.M. to 9:30 P.M. for some reason, so we headed off to bed early and decided to see how things were going in the morning.
Snow closed down the road through Smuggler’s Notch today.
I made my morning CoCoRaHS observations at 6:00 A.M., and after checking back in on the weather board and looking at some of the mountain web cams, I decided to head to Mt. Mansfield for a ski tour. I couldn’t tell quite how low the snow line had gotten, but it was still below freezing in the higher elevations, and the precipitation had continued through the night. There was a good chance that a nice shot of snow had accumulated on Mt. Mansfield. I didn’t try convincing E or the boys to try to join me, since they were all still in bed, so I got into my ski clothes, let E know that I was on my way, and loaded up the car with my gear. I don’t typically find the ski gear vying for space with the baseball stuff in the back of the car, but it definitely was today. I headed off to the mountain around 7:30 A.M. or so, and temperatures throughout the mountain valleys in the Waterbury–Stowe area were in the lower 40s F on my drive. The precipitation was generally light rain until roughly the point where the electronic sign indicates the status of Route 108 through Smuggler’s Notch, and not long after that, the rain became much heavier. The sign, by the way, read “NOTCH ROAD CLOSED… DUE TO SNOW”. The road through the notch tops out near 2,200’, so clearly the snow was accumulating at that elevation on paved surfaces. The temperature remained in the lower 40s F until that final rise above The Matterhorn to Stowe Mountain Resort, where they dropped into the upper 30s F.
“You could do laps up there from 2,500’ to 3,600’ and think it was midwinter.”
I parked at the Midway Lodge (~1,600’), where the temperature was in the mid to upper 30s F, and the precipitation was generally snow, but certainly some rain as well, and the snow that was falling was of course incredibly wet. It was pretty nasty at that point, with 25 MPH winds and driven wet snow/rain. The snow wasn’t quite accumulating there, but it was close, and you could see the accumulations just a few hundred feet up the trails. The weather was nasty enough that I left my lens hood on my camera in its protective orientation, even when it went back in my pack. I rarely feel the need to do that, and typically flip it back around for storage, but that speaks to just how wet and windy that snow was to make me take that extra step to minimize the amount of precipitation getting on the lens filter.
Snow line in sight on Nosedive at 2,100′
In the Midway parking lot there were a few dozen vehicles belonging to skiers, and most of the people were heading up Gondolier, but my initial ascent was via Nosedive; it’s often a good bet for decent snow coverage and preservation in these early and late-season storms. Also, based on what I saw in the report from AdventureSkier.com last Sunday, it looked like there would be some decent base snow left in case the new snow depths were marginal. The first traces of snow accumulation on the ascent were at 1,800’, by 2,100’ there was generally complete coverage of the trail, and by ~2,200’ the depth was a couple of inches and it was consistent enough that I switched from hiking to skinning. Even with those couple inches of snow, I was beginning to experience some occasional slipping as I hiked, so it was nice to get the skis off the pack and on the snow where the skins had beautiful traction. There was a faint skin track from an earlier ascender, but it was intermixed with some of the descent tracks of skiers and a bit hard to follow. I met up with another guy that was making the Nosedive ascent, and we chatted a bit about skiing as we made our way up the mountain. He was just hiking in his boots with his skis on his back, which seemed like a bit more work as the snow got deeper and deeper, but it didn’t appear to slow him down too much. Listed below are the snow depths I found on the ascent of Nosedive with respect to elevation:
We stopped our ascent at 3,300’ because as we approached the switchbacks at the top of the trail we got some beta from a couple of skiers coming down Nosedive – they indicated that everything above that elevation in the switchbacks was scoured and really not worth it, and indeed that was obvious once we got to the landing below that final switchback at 3,300’. I’m going to call the average snow depth there 10” to be on the conservative side, but there were plenty of areas with 12”-15” of snow; there was just variability due to the effects of wind deposition. I stuck my measurement pole right in the snow in the center of that landing, and found 15” of snow depth. The guy that had ascended with me headed up just a bit higher to catch some turns along a drift of snow, so I pulled out the camera and got some action shots as he made his way down.
I didn’t get his name, but he had quite a blast ripping up the powder on Nosedive today.
Before beginning my descent, I downed a packet of GU Energy Gel to see if it would provide that extra boost of energy to my legs to permit proficient and aggressive Telemark turns. I’ve noticed that after fairly long and/or quick ascents, my legs are often still recovering, and not to the stage where they can handle a lot of rigorous Telemark skiing right away. Alpine turns are typically no problem, since they’re easier and more stable to begin with, and after decades of alpine skiing, my muscles have the memory to really let them do it efficiently. But those Telemark turns take a lot more work, and it seemed like a little extra boost of quick energy would get me where I needed to be. So, I took a cue from the boys, who like to have a GU when they’re starting to fade while we’re biking or skiing – the Vanilla Bean flavor is a favorite among all of us. I usually don’t find that I need to worry about having enough energy on outings with the boys along; the pace is so slow that E and I usually don’t get drained. The boys certainly push themselves though, often needing some sort of recharge due to their smaller energy reserves, and when that’s the case, it’s GU to the rescue. On bigger, faster paced outings by myself though, I also feel the drain, and today I wanted to give a recuperative GU shot a try. I had the GU just a few minutes before my descent, and it absolutely worked. It helped give my legs that quick energy that they craved, and they had no trouble making Telemark turns. It was great having maximum powder to drive the legs, and while there’s no way to know exactly how my legs would have performed without the shot of GU, it was certainly my hero for today. I can still remember when I first learned about those energy gels back in the early 2,000s when Scott and Troy and their Dirtworld.com mountain biking team would use them. They’d strap them to their handlebars and down one on each lap to keep their energy up. With the way it performed today, I think a shot of GU before each earned descent is going to become part of the routine.
“There were plenty of
untracked lines to ski,
and it was dense, wall-
to-wall snow…”
As for the snow conditions, indeed there was some leftover base snow on Nosedive, and that offered up great turns, but the new snow itself was extremely dense (probably 12-14% H2O or so) and as long as there was enough of it, there was no need for previous base because it kept you off of anything below. I caught some beautiful bottomless powder on the skier’s left below the switchbacks, and then a lot more on the skier’s right along the edge of the trail. The Telemark turns were definitely flowing, and despite the fact that it was dense snow that could easily have been challenging to ski, it wasn’t. I immediately thought back to that storm last year on April 10th. Mt. Mansfield picked up more than two feet of dense snow that covered everything, but it was quite a challenge to ski on the Teles. Sometimes you would punch through the snow too far, perhaps with one ski, making lateral balance tough, and fore-aft balance was also extremely challenging. It’s possible that there was snow of varying densities in that storm, with some less dense snow underneath the topmost layer. That’s “upside down” snow, which is typically more challenging to ski. It was after that storm that I really decided that I wanted some fat, rockered Telemark skis for powder, and eventually got the Black Diamond AMPerages. I can only wonder how they would have performed in that storm – they would have been nice today, but being unsure of the snow depths I went with my older Atomic RT-86 midfats, and there were no issues. Really, the most challenging aspect of today’s skiing was negotiating areas of thinner snow as you dropped in elevation. I was actually quite impressed with the quality of some of the powder skiing on Nosedive today, but little did I know it wasn’t even going to hold a candle to what was in store over at the Gondola.
22″ of new snow up at the Cliff House today
I had no time limits, and plenty of energy left in the tank with the shortened ascent, so I skied down to the junction of Nosedive and Cliff Trail, and continued my tour by skinning up Cliff Trail. Within a few moments of starting my ascent, it was obvious that snow depths were substantially greater on Cliff Trail than they were on Nosedive at equivalent elevations. I wasn’t sure if it was because I was heading toward the Gondola, or because Cliff Trail offers better protection from the wind, but coverage was deep, wall-to-wall. Unlike what I’d seen on most of Nosedive, there were no signs of whatever lay beneath the snow. It wasn’t an illusion either; the depth at 3,000’ on Cliff Trail was 11”, vs. the 8” on Nosedive. The snow just continued to increase as I ascended toward the Gondola, there was 12”+ by the junction with Perry Merrill at 3,400’, and 12” – 15” easily up at the Cliff House. That’s on the conservative side for what you could find up there, and in general the snow depth was somewhat deceptive because you didn’t sink much into the dense snow. But right in the middle of Perry Merrill just beyond the Cliff House I measured 22” of new snow in flat terrain with no drifting. The usual measurement off the top of the picnic tables was deceptive as well – there was about a half foot of snow on the tables, but you could tell that the snow was much deeper because the table’s seats were just about buried. I measured in the open space between the tables and got a depth of 18”, so presumably the tops of the tables didn’t accumulate the snow well due to wind, melting, or some other effect. Here’s the summary of the depths I found on the Gondola side ascending via Cliff Trail:
“…at times it was dense enough that you’d be smearing turns right on the surface.”
I had another GU and got ready for my descent. Even that first steep pitch of Perry Merrill had great coverage comprised of that dense snow. Typically you’d sink in a few to several inches, but at times it was dense enough that you’d be smearing turns right on the surface. It took a moment to adapt when that was happening, but somehow the variability in the turns didn’t seem to disrupt the flow of the skiing – it was just really fun. I almost headed back down Cliff Trail since the coverage was so complete, but there were already a couple of tracks on it, and it’s fairly narrow, so I opted to check out Perry Merrill instead. I was hoping it would live up to the coverage I’d seen on Cliff Trail, and indeed it was just as good, if not even a bit better. There were plenty of untracked lines to ski, and it was dense, wall-to-wall snow, all the way down to 2,500’. You could do laps up there from 2,500’ to 3,600’ and think it was midwinter. The snow certainly wasn’t fluffy VermontChamplain Powder™, it was dense Sierra Cement, but it wasn’t wet or sticky. It made for plenty of base and just skied really well – it was right near the top on quality that I’ve experienced relative to many similar early and late-season dense-snow events. Sinking into the snow only a few inches or so was inconsequential compared to the fact that you didn’t have to worry about hitting anything underneath and you could just let it rip.
The view from white to wet
I stopped my descent at around 2,300’, as the snow was down to about 4” and it was getting notably wetter. You could probably go down to around 2,100’ easily if you had your rock skis. I hiked down the last 700’ back to the Midway Lodge, and the last vestiges of snow disappeared right around 1,800’ just like I’d seen over on Nosedive. The precipitation was snow down to just a couple hundred feet above the base, and back down at the lodge it was mostly rain with some snow mixed in at times. There were some really good bursts of snow on my descent, even in the lower elevations. The temperature had increased a few degrees to ~40 F at the base, but it was midday at that point, so that was still quite impressive.
Overall, I was really excited about how my equipment and supplies performed on this tour. My Gore-Tex did its job in keeping me dry, despite the driving rain and snow. My skins held like glue even in the wet snow, and hiking both up and down in my Telemark boots was a joy. I remembered to put them in walk mode for the walking sections (and put them back in ski mode for the descents) and it was almost like being in my hiking boots. And then there was the GU. It really quickened my recovery for the descents, and I’m going to be keeping that on the tour menu going forward. The boys won’t be able to borrow GU from me as easily though when they need it. While the GU certainly did its thing, I’m sure my stop off at Dunkin Donuts to fuel up before the tour also helped. I was feeling so great when I got home at midday, that I was ready to go for another round of skiing if E and the boys wanted to. It was still nasty and rainy outside, and not really conducive to doing too much else, but we had some fantastic winter powder skiing sitting up there in the high country. I couldn’t convince them to go though, so they unfortunately missed out this time. We did get some quality time indoors though, which I’m guessing a lot of families were doing this weekend. Ty, Dylan and I had a great round of “The Settlers of Catan” while E did a bit of shopping. It was quite a storm though, with Whiteface and other areas of the high peaks really cleaning up and putting out some amazing pictures.
…and this is what you get for Memorial Day
Monday update: The clouds cleared out today to produce crystal blue skies, and naturally that revealed some amazing vistas of the spring foliage and snow-capped peaks everywhere. Mt. Mansfield and Camel’s Hump were topped with white, shimmering in the strong sun of late May, and the high peaks of the Adirondacks were brilliant. We traveled around from Waterbury to Vergennes to Cambridge doing various activities, so we took in numerous vantages of the Greens and Adirondacks. It turned out to be a spectacular Northern New England Day for the holiday, almost as if Mother Nature was trying to strike as sharp a contrast as possible against the recently departed storm.
Using the Auto Road to gain access to Mt. Washington’sEast Snowfields is a convenient way to get to some fantastic spring skiing, but a number of factors need to align for an optimal outing to come together. First, the road has to open. One never knows exactly when that’s going to happen, since it depends on how much snow has to be removed, how fast it’s melting, how much road maintenance needs to be done, how often bad weather delays work, etc. Then, even once the road is open, weather can still play a factor. Although some folks might be inclined to head up into the alpine regardless of the forecast, I think most folks would agree that a calm, warm, clear spring day (or at least as close as you can get to that ideal) is the way to go. Those types of days can be rare on Mt. Washington, but they certainly happen, and they typically occur more frequently the farther one gets into late spring. While time might be on your side with regard to weather, it’s generally not on your side when it comes to snowpack. With each passing day of warmth, the snowpack melts a little more, and ski options diminish. Unlike when you get an iceland camper rental over there, the snow isn’t lasting quite so long these days over here. And, even if the stars align to create that perfect combination of access, weather and snowpack on the mountain, there’s everything else in life that has the potential to get in the way of letting you jump at the opportunity. Once in a while, things just don’t come together before the snow melts, but somehow, even with all those obstacles, we usually manage to get over to New Hampshire for some spring camping and skiing with the boys, and this year was no exception.
“We had the snowfield to ourselves the entire afternoon…”
For two weeks from the end of April through to the second week of May, we saw an incredible stretch of clear, warm spring weather with absolutely no measurable precipitation at our house in Waterbury. This period produced some great spring skiing, but the warmth and sun also accelerated the snowmelt to a rate that was a bit faster than usual. This period was great in terms of progress on clearing snow from the Mt. Washington Auto Road however, and it was open to the summit as of last weekend. The weather was unsettled for that first weekend though, so we opted to head down to the South Shore area and visit Erica’s mom for Mother’s Day, and keep our eyes peeled for a good weather window. After a couple more days of unsettled weather, the clear regime returned this week, and prospects for an Auto Road trip were looking excellent. This morning, the forecast called for decent weather with temperatures in the 40s F, and the morning shot from the Ravines Cam revealed crystal clear skies. It also showed that the east side ski options below the Mt. Washington summit are still quite plentiful, with many additional snowfields available along with the main one.
Presidential view
We were on our way to the mountain by mid morning, and views from the west side were already encouraging as we approached the Presidentials. When the west side still has skiable snow, you know the east side is going to have plenty of options. Steep lines with decent snow were even visible on the north side of the range as we passed by on Route 2, and on the ascent of the Auto Road we could see various snowfields in the peaks towering above the Great Gulf. In the proximity of the Auto Road itself, the first signs of snow were at roughly the 3,500′ elevation. As for the East Snowfields, the setup today was a lot like we encountered during our 2010 trip, in that the broad strip of snowfields was present off to the north of the main East Snowfield. A look at the availability of snow in 2010 shows an interesting distribution of snow – that strip of snowfields off to the north was very prominent, and the main East Snowfield was surprisingly small. The current snowpack is definitely different from what we had available on our 2011 and 2012 trips, where the skiing was essentially down to just the main snowfield.
“The snowfield held
beautifully flat and
pristine corn snow…”
With the lower snowfields in action, we decided to go with the approach applied in our 2010 trip, which is to use the parking area below the 7-mile post on the road, instead of the parking area at the top of the snowfields. Using this technique, one can tour out along the more northerly snowfields as far as they want, even hitting the main East Snowfield if they’d like. Then, to finish the tour, instead of having to hike back up to the parking area atop the East Snowfield, one can essentially traverse back along the base of the snowfields with minimal additional ascent. Along the way, you can make descents in the other snowfields as well, which often have untouched snow. They’re used much less than the main East Snowfield and we’ve typically found that we have them to ourselves with untouched corn snow. At the end of our 2010 trip, we also discovered a very efficient use of the mountain’s hiking trail network for this type of tour. We’ve started traversing on the Nelson Crag Trail before, but, it turns out that simply descending straight down from the lower parking area on the Huntington Ravine Trail drops you right onto the northern edge of the snowfields, so you can use the trail to get you right to the snow. You can’t really see the snow from above, so it’s not obvious unless you know what you’re doing, but as long as those northerly extensions of the snowfield are present, it’s a really sweet and efficient approach. Even though the distribution of the snow in the snowfields area is different each spring, it’s nice to be developing a knowledge of what works well for getting to the snow. We’re definitely starting to dial in a good understanding of how to best approach what we see on the Ravines Cam in terms of touring the snowfields. This year our goal was to tour out toward the main East Snowfield as described above, with the potential to ski there, but it would depend on how good the skiing was that found along the way, as well as time, and of course the boy’s attitude and morale, which can be extremely flighty on these outings.
As expected, taking the Huntington Ravine Trail got us to the snow in just a few minutes of hiking from the car, and Ty and Dylan were ready to just stop right there and start skiing. E and I explained to them that what they saw was just the tip of the iceberg in terms of snow, and that we would be traversing southward for some longer lines. The snowfield there was only about 50 vertical feet or so, but typically the priority for the boys is to minimize the amount of hiking they have to do in whatever way they can. The boys did have a bit more challenge this year, since they were both carrying their own skis on their packs for the first time. Fortunately, they had both decided to use their Telemark skis, also a first for them, so it’s nice that their Teles are lighter than their alpines. This also meant that they could simply wear their Telemark boots and hike like me and Erica in ours, since they are very flexible and have rubber soles. This meant we didn’t have any alpine boots to carry, although Tele boots still aren’t quite as easy for hiking as standard hiking boots, so that was a bit of a bump in challenge for the boys. For E, this trip was also a chance to carry her skis on the Dakine Women’s Pro II 26L ski pack that she got for Christmas. Although she used it on some backcountry outings this winter, we were always skinning, so there was no need to carry her skis on her back. This was her first opportunity to really put it to the test with skis on it, and she was very impressed. I wouldn’t have thought about it, except that she commented on how it didn’t even feel like she had skis on her back – that’s always good sign when it comes to a ski pack. She also mentioned how the diagonal carry is so superior to the A-frame style carry in terms hitting the backs of the skis with your legs. I’ve always been very impressed with the diagonal carry on my Dakine Sequence ski/photo pack, so I’m glad E is getting to make use of that system. Dakine definitely knows how to set up a ski carry system. The one issue I did notice with E’s pack is that since it has a helmet carrying system (very cook and I wish I had one) it gets a bit tight when the skis are on there in diagonal carry as well. Overall the skis and helmet were nice and snug there though, and E had no complaints. Our only lament heading outbound on the tour was that with our skis angled down to the right, it meant that they occasionally touched the rocks because of the direction of the side slope on our southward traverse. It was only an occasional inconvenience though, and I joked that we could always traverse around the entire Mt. Washington summit cone in the other direction if we really wanted to avoid that issue ;).
Time to hit the snow!
After only about ten minutes of southward traversing, we came to a substantial snowfield of about 250′ vertical or so, and we decided to do some skiing. We hit the snowfield about midway up, so I set in a boot ladder to the top. The snowfield held beautifully flat and pristine corn snow, aside from a couple of very faint tracks from a previous skier or two that must have been there quite a while ago. The snowfield was continuous, but did have a choke point about midway down along the left, so one had to take that route.
It was good that we’d reached at least an initial snowfield, because the boys were already getting grumpy. They really wanted to get on with the camping. They’d been planning that aspect of the trip for a long time, looking on sites like campingfunzone.com for handy tips and tricks which they were now dying to try out, so while they enjoy being out on the snow, getting them to thoroughly relish all aspects of earned turns is always a challenge. They got out their flashlights for hiking when it got dark, and loved the setup and maintaining the fire, and other tasks like that. Some days they enjoy the experience, or at least substantial parts of it, but other times it’s essentially putting up with Mom and Dad dragging them around to these snowy spots. We’ve learned that it’s good to have a “carrot” aspect of the trip as well, whether it’s a stop in a the Bryant Cabin on a Bolton Valley Backcountry Network outing or the swimming pool after, a chance to eat out somewhere once we’re done, or in this case, a chance to do some camping. We relayed to them that they were sitting on their own private snowfield with great temperatures, no wind, no bugs, beautiful snow, and even some sunshine. These aren’t things that you can get every day, but in their minds they were already off the mountain and down by the tent and campfire.
Getting after some of that smooth corn snow today
At the top of the snowfield, I hung out for a while and enjoyed the scene, while the boys did a bit of sliding on the snowfield, and E made the first descent. Her turns looked good, and it was amazing how fast she dropped that vertical. It seemed like she was down toward the flats of the Alpine Garden area in an instant, and she looked so far away. I skied a run next, and then we eventually got the boys to make some turns, even though they were being somewhat lazy and reluctant. They both put together some nice Telemark turns, even though the pitch of the snowfield was quite steep. E and I both made some additional turns, with me finishing off a run on the lower right of the snowfield while E shot some pictures. We had the snowfield to ourselves the entire afternoon, so even though it was only about half the vertical of what was available on the main East Snowfield, it was such good skiing that we never even continued over there. The boys were a bit too sour for that anyway, and really wanted to get on to the camping. We could hear that occasional shout from people on the main snowfield though, and I’m sure there were some great times going on over there.
Dylan out there carving some turns on the Telemark skis
The return traverse to the car was pretty quick, and E and I helped out the boys by each carrying a pair of their skis. For the extra set of skis, we went with a vertical carry, and E seemed to still be impressed with the stability and ease of her pack, even with the second set of skis on it. I made the lowest traverse, so that meant a few minutes of hiking back up the Huntington Ravine Trail at the end, but I was eager to test that out. It was nice to walk on an established trail, since the going was a big quicker than across the random jumbles of rocks that give the Rock Pile its name. While we were loading up the gear at the parking area, we had some inquiries about where we’d been skiing, and one guy was very intrigued to know that you could access the snowfield from that lower parking lot. He said he’d like to try it out in the future.
“…but in their minds
they were already off
the mountain and down
by the tent and campfire.”
Each year we like to try out a new campground on our visit to the snowfields, and this year I decided that we’d head south to Glen, New Hampshire. I’d found a couple of potential campgrounds there. The first was the Green Meadow Camping Area, but when we stopped in and found out that they weren’t opening until next weekend, we headed to the Glen Ellis Family Campground a couple of miles down the road. I’d put it as the second choice because it was a bit more expensive, but once we got there you could immediately tell why. The grounds are immaculate, and the building that functions as the main office and store was a beautiful building. Everything was first rate, and they’ve got a huge playground, basketball and tennis courts, and even a pristine baseball diamond. It’s certainly in that upper echelon of campgrounds.
Visitation was only modest since it’s no Memorial Day yet, so they gave us one of the riverside campsites. We thought that would be nice, but it wasn’t until we finally got to it that was saw how amazing it was – it was absolutely one of the coolest campsites we’ve ever had in either to Eastern or Western U.S. There’s a wooded section with the usual fire ring, picnic table, etc., but then that expands up onto a riverside area comprised of the rocks that are part of the riverbed, with a second fire ring. It overlooks a gorgeous stretch of the Saco River that made E and I feel like we were back in Jasper National Park. As soon as we saw that riverside section, we knew we were going to pitch our tent right up there. The boys headed off to the playground for a bit, we cooked up some hot dogs and beans for dinner, and finished things off with s’mores and lot of campfire time. There wasn’t actually anyone else camping out on the river since campground visitation was light, but I have to believe those riverside spots are pretty coveted on busy weekend. The fly fishing looked amazing, and we saw one guy out working the stream about a half mile downstream. That is a campsite that will not soon be forgotten, and it will definitely be on our list for the next time we’re in the area. Apparently their Laundromat is a big deal as well, because there are as many signs for that as there are for the campground itself!
The view from our campsite at the Glen Ellis Family Campground today
Sunday update: The evening sky had some on and off broken clouds and a nice moon, and I bet it dropped into the 30s F overnight because even with the rain fly on the tent, we were down to the mid 40’s F. After breaking camp, we decided to try out one of the local restaurants for breakfast on the way home, and found the Glen Junction Family Restaurant. It definitely seemed to be the hot spot for breakfast, and the menu was almost overwhelming with the variety of combinations of fresh toast, omelets, and most of the usual morning fare that you can think of. Not surprisingly with the junction location, the theme is trains, and they’ve got some fairly large-scale trains that circulate around the rooms up near the ceiling. The boys definitely enjoyed watching those, as did the numerous children that were there as well – especially the younger ones. Of course any adults like me would enjoy them as well. One of the specials had eggs Benedict on French toast, which was tempting, although I ended up making my own omelet which contained corned beef hash and spinach. The waitress said that was the first time she’d ever had anyone put together that specific combination, and it turned out great. Everyone liked their fare, and we even had some extra to take home as the portions are plentiful.
We got home today around noontime, after a bit of maintenance on the mowers, I was able to do the first lawn mowing of the season. It’s only about four short months until I’ll be on the last mowing of the season, and we’ll be thinking about the first snows, but there are plenty of summer activities to do in the meantime. In terms of skiing, we’ll have to see if we want to take a trip down to Killington for some turns in the next couple of weeks, since they’re apparently going for June this year just like old times.
High above the Spruce Peak Base and ready for some corn snow turns
Our stretch of incredible spring weather continues, and today was another clear one with temperatures in the 70s F. We had to head to Morrisville for a midday first communion mass, but we took along the ski gear in case we had the time to do some skiing on the way back through Stowe. After grabbing some subs in Morrisville, headed up to the resort and took a look around to assess the ski options. The most continuous snow is over on Mt. Mansfield, where the North Slope area is still looking very good, with no breaks that I could see even down to the lowest elevations. There’s still a good amount of snow over at Spruce Peak as well though, with a lot of continuous vertical over in the Main Street area, and even snow down by the Spruce Peak Base.
“I’d say it might be the best corn snow I’ve skied all spring.”
E and the boys weren’t up for skiing, but I was still looking to get in a quick run, so we decided to set ourselves up with some easy slope access right below Slalom Hill and West Slope. We had lunch at one of the tables on the back deck of the Spruce Camp Base Lodge, and while E and the boys were off on a bathroom break, I stuck around and enjoyed the view of the slopes. It has really been quite the run of clear spring days for us out here in the mountains – we’ve now gone 10 days without measurable precipitation at the house, and that’s very impressive for the land of upslope where Mother Nature can find a way to make some sort of precipitation more often than not. Even if the rate of snowmelt is a bit faster than usual, we’re enjoying it, and there’s more to come this week. After finishing up our lunch, E and the boys headed off to play some chess on the outdoor chess set, while I headed up for a run.
On the descent of West Slope
Although I put my ski pants in my pack, it was warm enough that I just threw on my Tele boots and hiked in my shorts. The effects of the continued warm and dry weather are very obvious on the slopes, as the areas without snow are essentially dry. That made the hiking very easy on the grassy terrain, and it was a quick ascent up to the top of West Slope. The views were excellent, and although I couldn’t quite make out E and the boys over by the Stowe Mountain Lodge, they said that they were able to see me. I took a line down the skier’s left of West Slope, and the snow was beautiful – it was smooth, with a couple inches of peel away corn snow on top. I’d say it might be the best corn snow I’ve skied all spring. It was also nice to be back on the Telemark skis – I decided to just stick with skiing in my shorts since it was a fairly simple run, and was rewarded with some nice corn spray on the knees along with some really glorious Tele turns. There was a final stretch of snow at the bottom of Slalom Hill, so I walked across the slope to connect to that, and it brought me right down to the car.
E and the boys timed their return to the car just right because they could see me on my descent, and when we met up I tried to tempt them into going for a run by letting them know just how great the snow was. It didn’t work, as they were all just a little too tired from the busy weekend. We’re watching the Mt. Washington Auto Road to see how things develop in the next couple of weeks. There’s still quite a lot of snow up there, and the sooner they open the more options there will be on the snowfields.
Last weekend I visited Bolton Valley for turns, but in general it’s been another week with day after day of sun and warm spring temperatures of 70-80 F for the valleys, so I suspect Bolton’s snowpack isn’t very continuous at this point. The Mt. Washington Auto Road opened to tree line today, but a full opening is required to use it for access to the snowfields, so local turns seemed to be on the menu again. Stowe has plenty of snow and is one of the closest options at this point, but once I found out that Sugarbush was offering free skiing this weekend in support of Vermont Land Trust’s preservation of the Bragg Farm, that jumped right up on the list.
I’d been tossing around different ideas about when to ski among other weekend chores and activities, but once I got the word that Sugarbush wasn’t going to be opening on Sunday, that sealed the deal on today’s trip. Ty was away at a friend’s house and E was busy with other things, but Dylan definitely needed to get out of the house, so I grabbed him in the early afternoon and we headed off to Sugarbush to make some turns. Dylan actually protested about today’s trip at first, and you could tell that there was a big activation energy required to get him moving, but even he realized that he needed to get his butt off the couch. We hadn’t been in the car long before his disposition started to change. With him and Ty, it’s often about that activation energy.
The main paved parking lot right below the Clay Brook Complex had a decent amount of cars in it, but it wasn’t chock full and there were plenty of available spaces right up front from people who had already left for the day. The mountain was requiring that everyone have free tickets, even with the free skiing, but the process was easy – we just stopped in the ticket building and they handed them over to us. You could make your donation to the Bragg Farm preservation project right there as well if you wanted. As we were walking over to the base of the lifts, my fired Chris spotted us from his seat outside at the Castlerock Pub, and he said to stop back after we’d done our skiing. The scene was lively outside at the pub, with live music from a guitarist going strong.
I was initially surprised when we walked up the steps and found that the Super Bravo Chair wasn’t running, and quickly realized that skiing was off the Valley House Double today. That’s a much slower and lower capacity lift setup, and meant that there was a decent queue of about 10 minutes or so to be able to load. The upside was that it probably helped to keep traffic down on the minimal terrain they had open – essentially Stein’s Run with the Coffee Run runout below that to get you back to the base of the lift. I wasn’t too excited when I’d initially heard that the skiing was only off Stein’s, since it never really seems to have any decent bump lines, just big, widely-spaced things, but at least it was warm enough out that its traditionally hard, manmade snow would likely soften. As we stood in the queue, Dylan was still a rather reluctant participant. He said, “Dad, I’ve got three things to tell you that I don’t like… one, it’s too hot out; two, this line is too long; and three, the snow is going to be sticky. Apparently his glass was well empty, but I did assure him that the snow wasn’t going to be sticky; it was definitely well-ripened corn snow and you could tell that even as we stood there at the base elevation.
The skiing turned out to be much better than I’d expected, not so much due to the snow, which I expected to be decently softened with temperatures in the 70s F, but the terrain setup. In this case, Stein’s tendency for those wide, spread out bump lines meant that there was actually some pretty smooth snow off to the sides where fewer people were skiing. It wasn’t totally flat, but the bumps were fairly scattered, so you could enjoy that area for smooth turns, and then move toward the middle of the trail for more bumps. Amazingly, even on such a warm day, Stein’s still found a way to have firm snow between some of the bumps. It’s almost hard to imagine that on such a day, but Stein’s is steep and it really faces north. Dylan worked on his pole technique and we both had some fun turns. I’d gone with alpine equipment, not wanting to deal with Telemark turns on the typical crazy assortment of bumps that can sometimes be found on Stein’s, but it turned out to be so much better than I’d expected; Telemark skiing would certainly have been fun as well.
The lift queue at Valley House had gone down somewhat by the time we finished our run, but I still couldn’t convince Dylan to do any more skiing. He did say that the skiing was better than he’d though it would be, so that was at least a bit of a positive note in his rather sour disposition. We met up with Chris down at the Castlerock Pub, where we had some nachos and root beers. We’d checked over at Timbers first, but they weren’t opening until 4:00 P.M., so it seemed like a perfect time to introduce ourselves to what to the pub had to offer. On such a gorgeous day, you could either sit inside and be just out of the sun but catching the cool breeze, or hang out on the patio and absorb some rays. We haven’t seen Chris since the Warren Miller movie in the fall, so we caught up with his latest exploits; he’ll be up in the area for some work in the next couple of weeks, so hopefully we’ll see him again.
At least Vermont’s Skier’s Highway has got it’s 15 requisite pieces of flair.
I’m really glad that Sugarbush offered the free day today, because in our case, it needed to be something pretty economical to make it worth it for the minimal terrain. Simply skinning for turns at a place like Stowe is pretty high on our list, but today’s skiing was definitely worth it for a nice change of pace. It’s been a couple of seasons since we’ve had the occasion to visit the ‘bush, so I’m glad that we snuck a visit in under the wire today.
Enjoying the descent of Spillway today in the afternoon sunshine
We’ve had some decent temperatures to get the corn snow cycle going over the past week, and this weekend has been much better than last weekend in terms of warming up the snow on the slopes. Yesterday was pretty nice in terms of weather, but today was even warmer, and the sky was crystal clear. In terms of the mountain snowpack, Stowe is looking great down to pretty low elevations based on Powderfreak’s latest pictures, but I know the snow at Bolton Valley isn’t going to last as long due to its western exposure and late-day heating. With that in mind, I decided to make it a Bolton tour today, and since I haven’t been up since my April 14th tour at Timberline, it was a good time to check on the snow situation at the local hill.
“I actually found some of the smoothest snow, or more accurately softest snow, on Beech Seal…”
I headed up in the late afternoon, with valley temperatures around 70 F. There’s no visible snow along the Bolton Valley Access Road until one reaches the 1,500’ elevation, where there’s a big patch at the base of the Timberline area. There’s really not much snow visible on the Timberline trails below the 2,250’ elevation though, and I suspect most of what is there is leftover manmade snow. After passing Timberline, I next saw natural snow appearing a bit below the 2,000’ elevation as I approached the Village. Temperatures were in the low 60s F up at the main base area, and on the slopes in that area there’s snow right down to the main base lodge, but it’s not continuous on all trails. I had to walk a couple hundred feet in the flats above the lodge before I could put on my skins and ascend Beech Seal. From there on up though, the snow is basically continuous on Beech Seal, Sprig O’ Pine, Sherman’s Pass, and Spillway right to the Vista Summit. I took the Sherman’s Pass ascent, and there is some pretty dirty snow in protected areas that haven’t seen much sun. That sun was glorious today though, and I definitely brought along the sunscreen because we’re talking about an August-like sun angle now. On the upper half of the mountain, there’s actually a good mix of manmade and natural snow options, although the trails that received manmade snow are the ones that will really give you those continuous runs with good snow coverage. I stopped my ascent at the Vista Summit right beyond the top of Spillway Lane, ripped off my skins, and got into descent mode. There was just the slightest breeze, but the wind turbine was making good use of it and spinning along.
There are some sun cups starting to form that make the snow surface uneven in spots, but Spillway has smooth options just about everywhere so you can get in some really nice turns. Spillway’s steep pitch felt good as usual, and the snow is indeed nice after this week’s corn cycling. I actually found some of the smoothest snow, or more accurately softest snow, on Beech Seal; perhaps the lower elevation let it warm a bit more than what’s up on Spillway. In any event, the softening was far superior to what we experienced last weekend on either Saturday or Sunday – those temperatures were just a bit to cool to get things to where I found them today at Bolton. At the bottom of my run, I took off my skis and threw them back on my pack to walk through the couple big broken patches of snow in the flats above the lodge, but you can essentially ski all of the ~1,000’ of vertical on the main mountain for now. There’s no snow or even cool temperatures in the forecast this week; it looks fairly mild and sunny, so I’m not sure what the situation will be on the mountain next weekend. There will still be snow for skiing, but I don’t think it will be continuous with the melting that could take place in the sunny, warm afternoons we look to have on tap in the coming days.
As usual, the Trekkers were great on the ascent. Although going with alpine skis and Trekkers is notably heavier than Tele, it’s typically not a big deal unless you’ve got huge tours to do. My biggest issue was with my skins – I’m not sure if the old skins for my CMH Explosivs have lost their water repellency, but whatever the case, today’s conditions had them catching and carrying a bunch of snow at times. I’d have Ty clean the underside of the skins off for me when we stopped, but we could never quite keep them from re-accumulating a coating of snow. Fortunately, Ty’s skins had no issues in that regard. The snow on the ground was quite wet at the base, but it dried out substantially as our elevation increased. We ascended via a bit of Perry Merrill, and then Gondolier to the Cliff House, and we observed the following snow depths with respect to elevation:
That more intense snowfall was with us on the entire descent, and the freezing line had gone down as well. Back at the car, heavy wet snow was falling, and the temperature was down to 35 F, three degrees below where it had been when we’d arrived. It was the sort of precipitation that soaked you very quickly once you were out of your Gore-Tex, and we both got pretty wet putting away the gear and switching out of clothing. The precipitation eventually changed back to rain as we dropped into the valleys on the drive home, but it was raining quite hard at times. There had already been some additional snow accumulations down to lower elevations by the time we were leaving, and the snow in some of the lower elevations actually looked better than it had on the way up due to some new covering. Overall the quality of the skiing was quite good, especially up high, and it could be even better tomorrow with more snow falling tonight.
