STRESSORS INDICATORS

Precipitation

Latest Score:

4.6/5

in 2025

Weight: 9.1%
score trend is up over time

Water is essential to a healthy forested ecosystem, but excess water can lead to flooding and disease outbreaks, while a deficiency can lead to drought1. For example, extreme rain events can cause flooding in low-lying areas, but even upland forests may experience “overland flow”. This occurs when rainfall is so heavy that it cannot be absorbed into the soil. Aquifers are not replenished and soil erosion may happen, exposing tree roots and washing away nutrients. Fluctuations in rainfall above or below the long-term mean will lead to stressful conditions for some forest species while creating ideal conditions for other species. Trees are adapted to the long-term conditions they have experienced, therefore deviations in precipitation from the long-term mean (both above and below) could be problematic to forests. Ideally, a healthy forest ecosystem has water availability that remains consistent. Total annual precipitation is the sum of all water (in the form of rain, snow, or ice) that fell within a calendar year for Vermont.  A high score means that precipitation levels are near the long-term mean.

1Rustad, 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.

Total annual precipitation shapes the forest water balance, and both extremes are problematic — deficits bring drought stress while excesses bring saturation, erosion, and flooding. The leaf scores departure from the 1961–1990 normal, capturing "drought or deluge" symmetrically. The regional context supports this reading: the Northeast has become warmer and wetter with more frequent extreme precipitation events, so both the long-term shift and its growing variability move conditions away from the envelope forests are adapted to.

Interpretation provided by:

Rustad et al. 2012, GTR NRS-99 (warmer, wetter region; more extreme precipitation).

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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.

Annual total precipitation for Vermont is obtained from NOAA National Centers for Environmental Information. V5.0 processing uses the Vermont-only climate subset and the current precipitation field.

Precipitation is scored as two-sided consistency with the fixed 1961-1990 mean and standard deviation. Departures toward either unusually wet or unusually dry annual conditions lower the score using the smooth-decay function. The source is a single NOAA regional/state climate value for each year rather than a station sample maintained by FEMC, so no sampling uncertainty band is shown.

1 NOAA National Centers for Environmental Information. Climate at a Glance / climate divisional data. Available at: https://www.ncei.noaa.gov/access/monitoring/climate-at-a-glance/