Potential for a little September snow in the Northern Greens?

It’s that time of year again when we start to think more about the colder weather, and for the past few days our NWS point forecast for Waterbury has shown sub-freezing low temperatures at the end of the week.  Talk about the first snowfall of the upcoming season, has already begun – over in the New England forum at Americanwx.com, Dryslot pointed out the potential snow showers and frost in the forecast from the National Weather Service office in Portland, Maine.  This morning I saw that there is a cold weather update at the Famous Internet Skiers website, and on SkiVT-L, there was a visit from Roger Hill, who threw out the potential for a little snow accumulation at Jay Peak.  Although it doesn’t seem to be the case this time, I’m certainly reminded of a couple of seasons ago when some September snowfall actually produced enough snow to get in some skiing.  The past couple of days have been pleasantly summery, even up here in Northern Vermont, but it sounds like the crisp feel of autumn is on our doorstep.

June upslope rain, with some snow for the mountains

After drying out to amazing low humidity on Wednesday, temperatures got really cool on Thursday and we got into a classic Northern Vermont upslope flow.  There was actually some snow falling in the highest elevations of the Greens, and certainly over in the Whites.   There were just a few spits of rain in Burlington when I left yesterday afternoon, but of course I got to the house and it was a steady light rain with a tenth or two of an inch already in the gauge.  This morning the gauge contained 0.27” of liquid in it and I thought, heck, that’s a half foot of upslope snow right there when the temperatures are appropriate.  I was looking at the radar image posted by Powderfreak at Americanwx.com and could see how at one point it exploded with 35 db and even a few 40 db echoes over our area at the junction of I-89 and the Chittenden/Washington county line, and then dissipated on the east side of the mountains once it dropped its payload:

Radar image of upslope precipitation
June upslope rain and snow hitting the Northern Green Mountains

When I submitted my report to CoCoRaHS this morning, I took a quick look at what some of the other stations had reported.  I sorted the list below from around 7:00 A.M. by total precipitation, but even without that, it was pretty easy to see the locations that got the liquid:

CoCoRaHS reports from the morning of June 3rd, 2011

I haven’t been able to check out the local peaks to see if they have any white on them because they’ve been socked in, but Mt. Washington got some new snow and they must have been whitened.  It’s 26 F up there now with freezing fog and 50+ MPH winds.  With such a good-looking forecast for tomorrow, we may head over for some turns, but these past couple of days certainly should have been good for snow preservation.

Thunderstorms and some heavy rains overnight

It didn’t seem like it rained a lot last night, but I found 1.63” in the gauge this morning, so it obviously added up.  We had some losses of power similar to what Powderfreak noted – a couple short ones in the evening, and then it went back out again around 8:00 P.M. and it was gone for the night.  It came back on early this morning at some point.  I didn’t stay awake for it, but apparently we had thunder and lightning pretty continuously through about 2:00 A.M.  This morning I was surprised to see the Winooski way back up to a level even with our local V.A.S.T. bridge and hogging almost the entire valley in our area, just like back in mid April when the snowpack was starting to melt.  I think it may have even been a bit higher this time, as the typically flooded residences and farmland west of the Cider House seemed quite inundated with water.  The water was probably the closest I’ve seen it to washing over Route 2 in that area – I think another foot of depth and there would have been water on the road.  I was surprised it got so high relative to the amount of water I recorded in the gauge, but then I checked the CoCoRaHS maps and saw that one observer over in Caledonia County reported 3.66” of water with this event.  I don’t think they are actually in our drainage, but clearly someone out to our east got a load of water from these storms overnight.  Our bus was late this morning due to road closures in the Montpelier area, so things have certainly been disrupted by the water.  I added an image of the VT CoCoRaHS table of Daily Precipitations Reports as of ~7:30 A.M. this morning, and it indicates that someone over in Danville got over 4 inches of liquid from these storms, so there are reports of some large amounts of liquid coming in from Caledonia County.

Table of rain totals from CoCoRaHS, May 27th, 2011
Some Vermont rain totals from the thunderstorms that came through the area overngight - some areas of Caledonia County to our east had over 4 inches of rain

Snow line around 1,500′ this morning

It was ~41 F at the house this morning, so I suspected that the snow level was still a bit high for new powder in the easily accessible elevations, but I checked in at Bolton on the way in to Burlington this morning to get a handle on where things were at in terms of base and new snow.  I could tell that it wasn’t yet a huge hit below 2,500’ yet because the cars coming down the road didn’t have snow on them, but the precipitation certainly looked like snow up high.  Here’s the vertical temperature profile I observed on the Bolton Valley access road around 7:00 A.M. with comments on the precipitation/accumulation; hopefully it will be useful for other mountain recreationalists:

340’:  41F (light rain)
950’:  40F (light/moderate rain)
1,100’:  39F (moderate rain)
1,500’:  38F (moderate rain/snow)
1,800’:  37F (moderate snow)
2,000’:  36F (moderate snow)
2,100’:  35F (moderate snow, accumulating)

As you can see from the above list, snow wasn’t accumulating until I reached the village at 2,100’, but it seemed to be accumulating on most surfaces other than the pavement, and there was probably ¼ inch down when I was there.  Skier’s left of Beech Seal showed a couple of breaks in coverage, as I suspected it would based on my Sunday observations, but it was still pretty close to continuous.

Even back down in the valley, there were some bouts of moderate precipitation, so hopefully that continues to hit the mountains.  Roger Hill was thinking that the snow level would rise a bit during the day today, so that may have to be factored in as well.

Heavy rainfall and more high water today

I haven’t seen any snow with this system, but last night’s precipitation seems worthy of note because we had 2.30 inches of liquid and the Winooski is back up even with our local VAST bridge as it was on the 11th, despite the fact that most of the snow has already melted in the lower elevations.  Some area schools are closed due to road access issues with this event.  I just summed my CoCoRaHS numbers for April and with this latest event the total liquid is right at 8.00 inches for the month thus far.  While I had that open I grabbed a few additional liquid numbers.  For the 2011 calendar year up to this point at my reporting location the liquid precipitation is at 20.46 inches, for the 2010 calendar year the total was 54.17 inches, and for the ’10-’11 snowfall season as it currently stands (October 15th, 2010 – April 16th, 2011), the total was 28.09 inches.

The snow in the yard has melted

The last of the snow in the yard melted today, so I can finish off that portion of my seasonal snowfall numbers.  The data for the last of the snow melting out in the yard (as of this season the mean date is April 15th ± 10 days) is actually something I’ve recorded all the way back since our first winter here (2006-2007) and April 24th is one day later than the previous record I had down (April 23rd, 2007).  This puts the continuous snowpack season in the yard at 141 days, which is exactly the same number recorded for ’06-’07.  Both of those seasons had slow starts with poor November snowfall, and snowpack that did not become established until early December, so they are well behind the highest value of 152 days recorded for the 2007-2008 season.  The next benchmark I’ll monitor will be when the last of the snow melts out in our neighborhood, which tends to be about a week beyond when the snow melts out at the house.

As I was skiing at Bolton yesterday I was reminded of some outings in April ’07, and realized that while the snowpack is in excellent shape this spring, the skiing this month has really paled in comparison to the equivalent period back in ’07.  Even down at this elevation we had almost two feet of snowfall in April ’07, and this season we’ve had just 4.4 inches.  I’m not sure what the mountains have had this April, but in ’07 it was measured in feet; I skied one day mid month on the mountain where I found up to 19 inches of new snow, and that was for just one of the storms.  The reading from the Mansfield stake on Friday was certainly respectable at 82 inches, but for the same date in ’07 it was actually at 84 inches.  It’s really been just an issue of the storm track this April; the moisture has been there, but the track has been too far to the north/west to get into the appropriate combination of precipitation and temperature.  With a good track over the past few weeks we probably would have had another April 2007 on our hands.  I think that the past couple of springs have been so poor in the snowfall department that some perspective has been lost on April’s potential, this one is good in terms of base/snowpack, but I’d say subpar for snowfall (we’re still below average by a few inches at the house).

Snowpack has reached zero at the back yard stake

Waterbury, Vermont 2010-2011 snowpack plot
The snow depth went to zero today at our back yard stake in Waterbury. (Click on the image for the full size plot)

As of this morning, the depth of snow at our back yard stake has reached zero, so I’ve updated my Waterbury snowpack plot and included it in this post.  This means that the last day with snow at the stake was 4/12, and the average I have for that value is 3/27 ± 14 days, so this season is a couple of weeks later than that average.  The next benchmark I’ll monitor will be when the final snow in the yard is gone, and based on data I have from ’07-’10, that average date is 4/12 ± 10 days, so roughly a couple of weeks later than when the snow has melted out at the stake.  As of today, the yard snowpack has been around for 130 days, but that is actually still below average (138 ± 14 days) because of the late start to the season; the start of continuous snowpack this season was on the later side at 12/5 vs. an average of 11/27 ± 9 days.  Unless the rest of the snow in the yard melts unusually fast however, the end result of the snowpack season will probably be somewhere around that average value.

I’d say that winter temperatures were more consistent than usual this season, so it’s a little easier to see the steady climb in snowpack from a value of 0″ on 12/4 through the value of 39.5″ on 3/8.  The average rate of increase during the period was 0.42″/day.  This was a decent snowpack season, with snow depth days from my stake coming in at 2,227 depth-days vs. the average of 1,812 ± 741 depth-days.  However, the combination of the rather late start and long stagnation through mid January (visible on the plot) while the storms were going south, meant that it certainly wasn’t up where the ’07-’08 season was at over 2,500 depth-days.

High water on the Winooski at the VAST snowmobile bridge

Image of high water on the Winooski
Melting snow from warm temperatures caused the Winooski to rise today - our local VAST snowmobile bridge was basically floating on the river.

With the recent warm temperatures melting some of the snowpack, the Winooski was quite high today, so I’ve added a couple of pictures of our local VAST snowmobile bridge.  The bridge was refurbished in the fall, and from the pictures one can see that the boards are still pretty light in color.  Normally the bridge is 5 to 10 feet above the river, so that provides a sense of the rise of the water level due to the melting snow, and with the fields off to the south taken over by water (visible in the background) the Winooski was several times its normal width. 

Close up image of the VAST snowmobile bridge at high water
A close up view of the south side of the VAST bridge and the flooded fields beyond

100 Inches

Mt. Mansfield and Waterbury Vermont snowpack plot for April 5th, 2011
The snowpack at the Mt. Mansfield stake hit 100 inches after yesterday’s snowfall – click for the full size plot
The snowpack at the Mt. Mansfield stake has been flirting with the 100-inch mark for several weeks, but thanks to yesterday’s snow, the afternoon reading indicated that we’d finally hit the century mark.  A depth of 100 inches at the stake is a nice benchmark indicating an excellent snowpack in the Northern Green Mountains, so the base depths for skiing should be decent for quite some time.  Down in the valley, the snowpack at our house in Waterbury was at 16 inches as of this morning’s reading.  I’ve added my latest plot for the Mt. Mansfield and Waterbury snow depths in this post.

Thursday afternoon NWS snow accumulations forecast update

BTV NWS Storm Total Snow Forecast map
The Thursday afternoon update for the Storm Total Snow Forecast map from the National Weather Service in Burlington - click for the full size image

The afternoon update to the Storm Total Snow Forecast map from the National Weather Service in Burlington suggests a few inches less accumulation all around.  A comparison to the previous map is in my afternoon post to the Northern New England thread at Americanwx.com.