The History of Southern California Snow Conditions chart is the best expression I've devised for displaying the range and incidence of snow conditions. In order to construct such a chart it is necessary to have week by week reports of conditions. First Tracks Online provides frequent enough reports from Vermont since 1999-2000 to create a chart for the past 9 seasons.

The focus of these charts is to show coverage of terrain and
frequency/consistency of packed powder snow that has not been
through a melt/freeze. The weekly grades
are not a measure of fresh powder, which cannot be predicted in advance
for a specific week. In 2008 I derived a method to estimate percent of
powder days from monthly snowfall. I now apply that percentage to all
weeks rated **A** or **B** and show that percentage and an adjusted
total grade at far right. For details, see What Is
the Probability of a Powder Day?

.

This chart is focused specifically on the highest snowfall areas ranging from Killington (250 inches) in the south through Sugarbush and Mad River to Stowe, Smugglers Notch and Jay Peak (300-325 inches). Where information is available the grade is based upon the best of those 6 areas, since some Vermont locals demonstrate the ability to pick the right area within this compact region based upon recent weather and conditions.

A: |

B: |

C: |

D: |

R: |

HISTORY OF VERMONT SNOW CONDITIONS | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||

Pwdr Adj | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||

Season/Month | October | November | December | January | February | March | April | May | June | July | Total | A | B | C | Pwdr | Total | ||||||||||||||||||||||||||||||||||||||||||||||||||

2016-17 | D | D | 0 | D | D | D | D | 0 | D | C | B | C | 4 | A | B | C | B | A | 11 | A | A | B | C | 9 | D | C | A | A | 7 | B | A | B | C | D | 8 | D | D | D | D | 0 | 0 | 0 | 39 | 7 | 13 | 19 | 16% | 47 | ||||||||||||||||||

2015-16 | D | 0 | D | D | D | 0 | D | D | D | D | 0 | D | C | B | B | B | 7 | C | B | B | B | 7 | B | C | C | C | 5 | D | C | D | D | 0 | D | D | D | 0 | 0 | 0 | 20 | 0 | 7 | 13 | 6% | 21 | ||||||||||||||||||||||

2014-15 | 0 | D | D | D | D | 0 | D | B | B | C | 5 | C | A | A | A | 10 | A | A | A | A | 12 | A | A | B | B | A | 13 | A | B | B | C | 8 | C | D | D | D | 1 | 0 | 0 | 49 | 11 | 17 | 21 | 11% | 56 | |||||||||||||||||||||

2013-14 | 0 | D | D | D | D | D | 0 | D | B | C | C | 4 | B | D | C | B | 5 | A | A | A | B | 11 | A | A | A | A | B | 14 | B | B | B | C | 7 | D | D | D | 0 | 0 | 0 | 41 | 7 | 15 | 19 | 11% | 47 | |||||||||||||||||||||

2012-13 | 0 | D | D | D | 0 | D | D | D | B | A | 5 | A | C | B | B | 8 | C | A | B | A | 9 | A | B | B | A | B | 12 | A | B | C | C | 7 | D | D | D | D | 0 | 0 | 0 | 41 | 7 | 15 | 19 | 12% | 47 | |||||||||||||||||||||

2011-12 | D | 0 | D | D | D | D | 0 | D | D | D | D | 0 | D | C | B | B | A | 8 | B | A | A | A | 11 | A | B | C | D | D | 6 | D | D | 0 | 0 | 0 | 0 | 25 | 5 | 9 | 11 | 10% | 28 | |||||||||||||||||||||||||

2010-11 | D | D | 0 | D | D | D | D | 0 | D | C | B | B | 5 | C | B | A | A | A | 12 | A | A | B | A | 11 | A | A | B | A | 11 | A | B | C | C | 7 | D | D | 0 | 0 | 0 | 46 | 10 | 16 | 20 | 16% | 56 | |||||||||||||||||||||

2009-10 | D | D | 0 | D | D | D | D | 0 | D | B | B | C | 5 | A | A | A | B | B | 13 | B | B | B | A | 9 | B | B | C | C | 6 | C | D | D | D | 1 | D | 0 | 0 | 0 | 34 | 4 | 13 | 17 | 10% | 38 | ||||||||||||||||||||||

2008-09 | 0 | D | D | D | B | C | 3 | C | C | A | C | 6 | C | A | A | A | A | 13 | B | C | A | C | 7 | B | B | B | C | 7 | C | C | C | D | 3 | D | 0 | 0 | 0 | 39 | 6 | 11 | 22 | 14% | 45 | |||||||||||||||||||||||

2007-08 | 0 | D | C | C | 2 | C | A | A | B | A | 12 | A | C | B | A | 9 | B | A | B | B | 9 | A | B | B | A | A | 13 | B | C | B | C | 6 | D | 0 | 0 | 0 | 51 | 9 | 18 | 24 | 17% | 62 | ||||||||||||||||||||||||

2006-07 | 0 | D | D | 0 | D | D | D | D | D | 0 | D | C | B | B | 5 | B | A | A | A | 11 | A | B | A | B | B | 12 | A | A | B | D | 8 | C | 1 | 0 | 0 | 37 | 7 | 14 | 16 | 14% | 44 | |||||||||||||||||||||||||

2005-06 | B | 2 | D | D | 0 | D | C | C | B | 4 | C | C | C | B | A | 8 | B | B | A | A | 10 | A | C | C | C | 6 | C | C | C | D | D | 3 | 0 | 0 | 0 | 33 | 4 | 9 | 20 | 14% | 37 | |||||||||||||||||||||||||

2004-05 | 0 | D | D | D | 0 | D | C | B | C | 4 | C | C | C | B | C | 6 | B | A | A | A | 11 | A | A | B | B | 10 | C | C | D | D | D | 2 | D | D | 0 | 0 | 0 | 33 | 5 | 10 | 18 | 13% | 37 | |||||||||||||||||||||||

2003-04 | 0 | D | D | D | D | 0 | B | C | B | B | 7 | R | C | C | B | 4 | B | A | A | A | B | 13 | C | B | A | C | 7 | C | C | C | D | 3 | D | D | 0 | 0 | 0 | 34 | 4 | 11 | 19 | 14% | 39 | |||||||||||||||||||||||

2002-03 | D | 0 | C | C | D | C | B | 5 | B | A | B | A | 10 | A | A | A | B | 11 | A | A | B | B | 10 | B | B | B | C | C | 8 | B | C | C | D | 4 | D | D | D | D | 0 | 0 | 0 | 48 | 7 | 17 | 24 | 11% | 54 | |||||||||||||||||||

2001-02 | 0 | D | D | D | D | 0 | D | D | D | C | C | 2 | B | A | A | B | 10 | C | C | C | C | 4 | C | D | C | A | B | 7 | B | C | D | D | 3 | D | D | D | D | D | 0 | 0 | 0 | 26 | 3 | 7 | 16 | 13% | 29 | |||||||||||||||||||

2000-01 | D | 0 | D | D | D | C | 1 | C | B | C | A | A | 10 | A | A | A | A | 12 | A | C | A | A | 10 | A | A | B | A | A | 14 | B | B | B | C | 7 | D | D | D | D | 0 | 0 | 0 | 54 | 13 | 18 | 23 | 21% | 70 | |||||||||||||||||||

1999-00 | D | 0 | D | D | C | D | 1 | D | D | C | C | 2 | C | C | B | B | A | 9 | A | A | A | B | 11 | B | B | B | C | 7 | C | B | C | C | C | 6 | D | D | D | D | 0 | 0 | 0 | 36 | 4 | 11 | 21 | 14% | 41 | |||||||||||||||||||

Averages: | 0.1 | 0.7 | 4.8 | 8.8 | 9.8 | 9.3 | 4.5 | 0.1 | 38.06 | 6.2 | 12.8 | 19.0 | 13.0% | 43.8 |

In comparison to Southern California these Vermont areas average twice as much natural snow but have as least as much difficulty preserving it. While warm weather and strong sun are the culprits in SoCal, rain is the bane of eastern skiing and is much more frequent as shown here . The icy surfaces about which many eastern skiers complain are mostly due to a hard freeze after it rains.

Historically snowmaking in Vermont began in October, but has more recently been curtailed for economic reasons. In any case, rain is frequent enough in November that it is rare for anyone to get as much as 50% open. The 2002-03 season was the conspicuous exception in staying cold more consistently in the early season. Natural snow was actually below average in 2002-03, but the season scores well because temperatures stayed below freezing until mid-March. Many would argue that the quality of eastern skiing is more temperature dependent than snowfall dependent.

For the Vermont areas analyzed here natural snow is a much more important part of the equation than elsewhere in the East. Off-piste glades become safely skiable on about a 40-inch base (usually attained early January through late March) and there is often ample powder skiing when it snows during this period. The scale of areas like Stowe and Mad River Glen (as well as the gladed terrain) is similar to SoCal's Mt. Baldy. But the higher average, and more important greater consistency of snowfall in Vermont results in many more powder days. The 2000-01 season, which averaged close to 400 inches in Northern Vermont and over 500 at Jay, is illustrative. The 13 Vermont weekends rated A in 2000-01 are nearly double the best seasons in Southern California and comparable to average years in Whistler or Colorado. The 2011-12 season had been the worst on this chart before 2015-16. Northern Vermont's natural snowpack was subpar but was never taken down by big midwinter rains and only collapsed during a record March heatwave. Elsewhere in the Northeast 2011-12 was comparable to the prior worst ever season in 1979-80. 2015-16 broke many of the record low snowfall records from 1979-80, and in addition was plagued with numerous rain and thaw episodes. There were no weekends with full operation on packed powder conditions in 2015-16, while all other seasons since 2000 had at least 3 such weekends.

In the late season the warmer weather and more frequent rain curtail Vermont skiing much faster than in the West. Even with the huge snowpack of 2000-01 or the big April dumps in 2007 the natural snowpack was marginal for skiing by early May. Overall this chart confirmed my gut feeling that "an average season in Vermont is comparable to a good season in Southern California," with a score of about 35 (before powder adjustment). But 35 is also the score of the worst ever seasons at Alta and Whistler. 2015-16 was the only season in Vermont comparable to a poor season in Southern California.

__Other Eastern Regions__

1) Snowmaking leaders with mostly intermediate runs, places like Hunter Mt.,
Okemo, Sunday River. Early season profile is similar to the chart.
Fewer A's midseason due to half as much natural snow, more limited
spring operation, average score probably around 30.

2) Upstate NY, New Hampshire and Maine areas with terrain similar to the charted
Vermont group, but snowfall is typically less than 200 inches,
examples Whiteface, Wildcat, Sugarloaf. Slower to get covered
early, harder to keep covered with less natural snow (or wind
exposure in the case of Wildcat), average score probably around 25.

3) Quebec has multiple regions. The Townships (Sutton, Orford) are
the extension of Vermont's Green Mountains though at lower
altitude. Snowfall around 250, probably scores 30-35. The
Laurentians (Tremblant) are colder than New England but get no more
than 150 inches natural snow. Likely score 25-30. The Quebec City
area (St. Anne, Le Massif) is equally cold but more snow, overall
200 inch average, likely score 30-35.

4) Southern New England and mid-Atlantic areas are lower and often
on the wrong side of a rain/snow divide. Average score at most areas no more than 20.
Snowshoe has high altitude for the East and a bit more natural
snow, probably scores at least 25.

__More Snow Conditions Charts__

Mammoth/Sierra Nevada

Fernie and Whistler

Utah

Colorado