STRESSORS INDICATORS

Snow Cover

Latest Score:

3.8/5

in 2025

Weight: 9.1%
score trend is flat over time

Snow cover is projected to decrease in depth, duration, and extent under climate change. Lack of sufficient snow cover can make tree roots vulnerable to freezing damage and cause nutrients to be leached from the soil1,2,3. Also, the melting of snow in late winter can provide a steady supply of water to trees when they are preparing for bud break. Snow cover fluctuations above or below the mean may result in undesirable conditions for native forest species. Here, snow cover is defined as the number of days with snow cover greater than 1” in depth for Vermont. As trees are adapted to the conditions they have experienced, deviations in snow pack from the long-term mean (both above and below) could be problematic to forests. A high score means snow cover is near the long-term mean.

1Decker, K.L.M., Wang, D., Waite, C. and Scherbatskoy, T., 2003. Snow removal and ambient air temperature effects on forest soil temperatures in northern Vermont. Soil Science Society of America Journal, 67(4), pp.1234-1242.
2Groffman, P.M., Driscoll, C.T., Fahey, T.J., Hardy, J.P., Fitzhugh, R.D. and Tierney, G.L., 2001. Colder soils in a warmer world: a snow manipulation study in a northern hardwood forest ecosystem. Biogeochemistry, 56(2), pp.135-150.
3Rustad, L., Campbell, J., Dukes, J.S., Huntington, T., Lambert, K.F., Mohan, J. and Rodenhouse, N., 2012. Changing climate, changing forests: The impacts of climate change on forests of the northeastern United States and eastern Canada.

"(Reduced winter snowpack and increased soil freezing) could reduce forest growth rates in the northern hardwood forest region by 20 percent." — Reinmann & Templer, Hubbard Brook snowpack research
Interpretation provided by:

Reinmann & Templer (Hubbard Brook snowpack–growth experiments); Contosta et al. 2024, *PLOS Climate* (56-year Northeast snowpack trends); Huntington et al. 2004 (proportion of NE precipitation falling as snow).

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The score is calculated using a target value and the historical range of the the entire long-term dataset. The higher the score, the closer this year's value is to the target.

Once the score is computed for each year, the trend in scores over time is calculated. If the trend is significantly positive or negative, the long-term trend is marked as increasing or decreasing respectively.

Component Description
Scored as

Category 2 (consistency with a reference matters) - two-sided. Scored on how far this year's value departs from a fixed historical baseline; values close to that baseline score highest, and departures in either direction score lower.

Target value

Fixed 1961-1990 reference period (mean and standard deviation of that window).

Directionality of scores

Values near the fixed baseline score highest; departures in either direction score lower.

Minimum value used in scoring

Not applicable - scored by departure from the fixed baseline, not a range endpoint.

Maximum value used in scoring

Not applicable - scored by departure from the fixed baseline, not a range endpoint.

The Annual Variability badge shows whether this indicator's measured values move smoothly or jump from year to year. It compares the typical squared change between consecutive years (the mean successive squared difference, MSSD) against the variation of the whole record, computed from the raw data, not the score.

Low, Medium, and High are fixed thresholds shared by every indicator. A ratio below 1 reads Low: changes between years are small relative to the record's overall variation, the signature of a smooth or steadily trending series. A ratio near 2 is what random year-to-year scatter produces. Above 2 reads High: the series see-saws, reversing direction faster than chance would. Because the ratio is unit-free, the badge is comparable across indicators with very different units. It describes year-to-year behavior and does not affect the score; indicators with short records show no badge.

Snow Cover is the number of days with snow depth of at least 1 inch, from NOAA Global Historical Climatology Network Daily (GHCN-D) records at long-running Vermont weather stations1. For each station, the monthly day counts are summed over the snow year (October through the following May); a station-year missing any of those eight months is excluded. Stations differ considerably in their typical snow-cover duration because of elevation, latitude, and local climate (Vermont station averages range from roughly 80 to 200 snow-days), and the set of stations reporting changes from year to year, so a simple average of raw totals partly tracks which stations reported rather than the snow itself.

V5.0 therefore averages station departures2. Each station-year total is expressed as a departure from that station’s own long-term average, the departures are averaged across the stations reporting that year, and a single fixed constant (the mean of the included stations’ long-term averages) is added back so the indicator still reads in snow-days. V5.0 also expanded the Vermont station list from two to twelve long-running stations; a station needs at least 15 complete snow-years to establish its long-term average, so eleven are used. Stations with shorter records have long-term averages drawn from more recent winters, so their departures can understate part of the long-term decline; the approach is therefore conservative.

The score uses a fixed 1961-1990 baseline mean and standard deviation, calculated from the departure-based series, and the two-sided smooth-departure formula. This replaces the former moving long-term mean, so the reference does not shift as newer winters are added. Because the annual value is an average of station departures, the dashboard displays the standard error of that mean departure as a confidence interval; years with more reporting stations generally have tighter intervals.

1 NOAA National Centers for Environmental Information, Global Historical Climatology Network Daily (GHCN-D).
2 Brown, R., Derksen, C., & Wang, L. 2010. A multi-data set analysis of variability and change in Arctic spring snow cover extent, 1967–2008. Journal of Geophysical Research: Atmospheres 115, D16111. https://doi.org/10.1029/2010JD013975