
Nearly Live Weather Data from the Base of Stark Mountain, Brought to Us by Our Friends at
Magic Hat, Makers of Single Chair Ale:
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| Date | July 30, 2010 |
| Time | 11:50:00 AM |
| Temp | 62.7 ° F (17 ° C) |
| Wind | 2 mph (3 kph) from the West (bearing 281°) |
| Windchill | 62.7 ° F |
Mr Joshua Fox now has a MRG weather blog which he will be updating continuously concerning the weather at Stark Mountain. Click on the Fox Report logo above to access the Blog.
Also be sure to check out his pre-season predictions and see how accurate he is.
+ See Latest Forecast
Warm weather ends an uneven season
Uneven would be a generous way of putting it, disappointing might be the blunt way. There were some high expectations going into the year as it appeared we would have the right mix of high octane jet energy in the south and cold weather from the north to produce some big things. In fact, that is exactly what we saw, but all the fun was well to Vermont's south. The snow would have been more welcomed in our neck of the woods since it caused unprecedented disruptions in air traffic and costly clean-up projects in our major U.S. cities.
It is funny to look at the compiled data and how it illustrates how 2007-2008 got turned upside down thanks largely to a flip in the ENSO from La Nina to El Nino. Take a look at how we left 2007-2008 at the SCWB.
"Montreal, Quebec - 142 inches (169 % of average)
Burlington, VT - 100 inches (131 % of average)
Boston, MA - 51 inches (113 % of average)
Philadelphia, PA - 6 inches (25 % of average)
In the language of anomalies that is quite a contrast. In other words, some pain and suffering had to be endured by skiers/riders who stayed at Seven Springs or Snowshoe WV this year. Lattitude was key at we had it at MRG and this proved to save our season."
Pain and suffering is not the word to describe the season at Seven Springs or Snowshoe this past winter. Both mountains received over 200 inches of snow which in the case of Seven Springs was a record. Most importantly, the conditions were epic for the first three weeks of February in all of those locations as record snow was combined with consistent cold.
At Mad River Glen, we did not have a winter as futile as 2005-2006 or 2001-2002. We were pleasantly surprised early in the season as several storms pronged to move well to our south took an 11th hour turn northward to yield some powder. The mountain missed the Megalopitan storm "I" but did get a multi-day powder fest on New Years as a storm retrograted westward out of the Gulf of Maine. This was arguably the best event of the season for the mountain and was meteorologically fascinating since the event caused Champlain induced powder to fall over Burlington to the tune of 3 feet.
There was much anticipation after a quiet end to January since the pattern in early February looked as stormy as any I have ever seen in winter. The pattern was fueled by a plethora of blocking mechanisms across the high latitudes and an extremely energetic southern branch of the jet stream. The blocking was so ferocious that the storm track was forced unusually far to our south. Interestingly, so was the cold weather. Florida was not the place to visit during the winter as frequent outbreaks of intense cold resulted in the coldest winter in over 30 years. At Mad River glen, the cold weather never reached a level we would consider "intense" and although the winter was free of large scale "thaws" temperatures averaged above normal for the season. It was an unusual combination of circumstances to say the least but one that caused back to back major storms across the Mid-Atlantic States in early February. The seasonal snowfalls in cities like Baltimore, MD and Philadelphia climbed to 400 % of normal but much of Vermont continued to be plagued with a snow drought. Not only did MRG miss both Megalopitan events in February, but terrain induced events were non-existent as northern branch jet energy was locked up across Canada and southern branch energy was causing unprecedented snow farther south.
The big event of the winter at MRG occurred late in February. It was a very convoluted system flush with moisture but initially disorganized and ultimately quite mighty but very occluded. The initial burst of snow resulted in a swath of 50 inch totals up the spine of the Berkshires and Green Mountains but as the storm matured, it brought a conveyor of warmth into interior New England while cold advanced east into areas like Maryland, Pennsylvania and New Jersey. There were several hours during this event where you could've driven south on the New York State Thruway and the weather would have transitioned from heavy rain to heavy snow. In many ways it underscored the personality of the entire winter as an imaginary line within a few degrees of 40 north seemed to divide areas that received record snow from areas that consistently seemed to receive little snow. The storm in late February was a great one for MRG and would have been epic were it not for that warm intrusion which made conditions very changeable as you moved down the mountain.
In the end an El Nino of moderate strength such as the one that was present for much of the season, combined with the consistent presence of mid latitude cold are certainly the ingredients necessary for a winter such as the one we received. My conventional wisdom was perhaps wish casting for a winter more similar to 1992-1993 or 1977-1978 but the winter turned out to be a more exaggerated version of 1986-1987 or 1987-1988. The year perhaps most similar was 1957-1958. In that winter, record snow hit portions of Maryland and Pennsylvania late in the season in another year where the El Nino was very prevalent.
On a more personal note, I once again enjoyed the opportunity to talk weather to the greatest weather audience perhaps in the world. I felt the quality of the blog perhaps suffered at times since at times I found it challenging to combine my work load with blogging responsibilities. To make a long story short, it was easier to maintain the blog when you are unemployed and in search of things to do. I got a lot of emails, mostly positive and many I never got a chance to respond to. I appreciate the comments even if I never got a chance to craft a response. Enjoy the summer, stay safe think big snow for next winter.
-Josh Fox of the SCWB
NWS Forecast
Expires:201007302030;;462586
Fpus51 kbtv 301502
zfpbtv
zone forecast product for vermont and northern new york
national weather service burlington vt
1102 am edt fri jul 30 2010
vtz003-004-007-302030-
orleans-essex-caledonia-
including the cities of.Newport: Island pond. St. Johnsbury
1102 am edt fri jul 30 2010
rest of today: Mostly sunny. Highs in the upper 60s. Northwest
winds around 10 mph.
Tonight: Clear. Patchy fog after midnight. Lows 39-46. Light
and variable winds.
Saturday: Sunny. Highs in the mid 70s. Light and variable winds.
Saturday night: Clear. Patchy fog after midnight. Lows in the mid
40s. Light and variable winds.
Sunday: Mostly sunny. Highs in the upper 70s. Light and variable
winds.
Sunday night through tuesday: Partly cloudy. Lows in the mid 50s.
Highs in the lower 80s.
Tuesday night: Partly cloudy with a 30% chance of showers.
Lows in the lower 60s.
Wednesday: Mostly cloudy with a 40% chance of showers.
Highs in the upper 70s.
Wednesday night: Partly cloudy with a 30% chance of
showers. Lows around 60.
Thursday: Partly sunny. Highs in the upper 70s.
$$
Live Weather Pics

Canadian Radar, thanks to our neighbors to the north Environment Canada, has a more accurate view of both sides of the Green Mountains.
Remember, radar measures precipitation intensity. When looking at snowfall, two tenths of a centimeter (darker blue) per hour will bring a tenth
of an inch of snow, or just a dusting when air temperatures are just below freezing. However that same .2 of a centimeter will add more snow
when applied in colder temperatures.

This is a close up visual satellite picture as recently as 15 to 30 minutes ago. It is centered on Montpelier Vermont. After sunrise and
before sunset in clear conditions, local terrain will show up nicely while the sun will be casting long shadows. It has the effect of a
local relief map and can show lake effect plumes coming off Lake Champlain as streaks emanating downwind usually toward Boston.

This is a standard mosaic colorized winter radar. It uses the current National Weather Service Doppler radar network and is presented courtesy
of the Weather Underground. Under light snowfall conditions, there will be little radar return shown.

This is an image of the prevailing cloud cover currently over the Green Mountain region. Updated every 15-20 minutes.
This infra-red shot is like the visual version only is colorized. Typically shown is an orange or warmer color with black sources of water
i.e. ponds lakes showing up where skies are clear. Different scales of cloud temperature are colored to show different cloud levels.
Also during the day you can see the heating effects as the color changes, likewise cooling effects with arctic air and the like. Colder
cloud tops often mean heavier precipitation when associated with an ongoing storm.
Last modified January 06 2009 04:49 PM