STRESSORS INDICATORS

Maximum Temperature

Latest Score:

2.8/5

in 2025

Weight: 9.1%
score trend is down over time

As our climate changes, it is predicted that there will be greater variability in annual temperatures, as well as warmer maximum temperatures in the summer. Higher summer temperatures can lead to drought and heat stress to forests, resulting in declines in tree health and tree mortality1,2,3. Here, we assess the change in maximum annual temperature in Vermont. Tree are adapted to the long-term conditions they have experienced, therefore deviations in maximum temperature from the long-term mean (both above and below) could be problematic to forests. A high score means that the maximum temperature is close to the long-term mean.

1Anderegg, W.R., Kane, J.M. and Anderegg, L.D., 2013. Consequences of widespread tree mortality triggered by drought and temperature stress. Nature Climate Change, 3(1), pp.30-36.
2Williams, A.P., Allen, C.D., Macalady, A.K., Griffin, D., Woodhouse, C.A., Meko, D.M., Swetnam, T.W., Rauscher, S.A., Seager, R., Grissino-Mayer, H.D. and Dean, J.S., 2013. Temperature as a potent driver of regional forest drought stress and tree mortality. Nature Climate Change, 3(3), pp.292-297.
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.

"The climate of the region has become warmer and wetter." — Rustad et al. (2012), USFS GTR NRS-99
Interpretation provided by:

Rustad et al. 2012, GTR NRS-99 (NE / eastern-Canada climate–forest synthesis).

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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.

Mean annual maximum temperature for Vermont is obtained from NOAA National Centers for Environmental Information. V5.0 processing uses the Vermont-only source subset and the current maximum-temperature field.

The annual value is scored against the fixed 1961-1990 mean and standard deviation using the two-sided smooth-departure function. Both unusually warm and unusually cool annual maximum temperatures are departures from the historical climate reference. No sampling uncertainty band is shown because the source provides a single regional/state climate value per year.

1 NOAA National Centers for Environmental Information. Climate at a Glance / climate divisional data.