STRESSORS INDICATORS

Climate Extremes

Latest Score:

3.5/5

in 2025

Weight: 9.1%
score trend is down over time

Changes in the proportion, extent, and severity of extreme weather events are an indication of a volatile and changing climate. Not only are extreme events stressful to forests, but they can cause significant problems for our infrastructure and health. NOAA National Centers for Environmental Information (NCEI) computes a regional Climate Extremes Index (CEI) based on the monthly maximum and minimum temperature, daily precipitation, and monthly Palmer Drought Severity Index1. The CEI is a combination of the proportion of the year and the area in the region that has experienced an extreme event for these three indices. The long-term variation or change in the CEI represents the tendency for extremes of climate to either decrease, increase, or remain the same1. Here, we set the target for the dataset as the long-term mean with the understanding that climate extremes are a natural phenomenon, but that changes away from this baseline may pose threats to both forests and humans. A High score means that there is a high number of extreme events in a given year.

1NOAA National Centers for Environmental Information. 2018. Climate Extremes Index. https://www.ncdc.noaa.gov/extremes/cei/

The Climate Extremes Index summarizes the proportion of the region and year experiencing extreme temperature, precipitation, and drought conditions. Unlike temperature or precipitation, this is a stress index rather than a natural climate variable: fewer extremes than the historical normal is simply good, not a sign of instability, so the leaf is scored one-sided, with only above-baseline extremeness lowering the score. Regional syntheses document an increase in extreme events over recent decades, consistent with the expectation that climate change brings more frequent extremes capable of stressing forests beyond their historical tolerance.

Interpretation provided by:

Rustad et al. 2012, GTR NRS-99; NOAA NCEI Climate Extremes Index documentation.

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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) - one-sided. Scored on how far the value rises above a calm-year anchor (one standard deviation below the fixed baseline); years at or below the anchor score highest. The baseline mean itself reads about 3.7 of 5.

Target value

Fixed 1961-1990 reference period (mean and standard deviation of that window); the top score is anchored one standard deviation below that mean.

Directionality of scores

Years at or below the calm-year anchor (one standard deviation below the fixed baseline) score highest; values above it score lower.

Minimum value used in scoring

Not applicable - values at or below the calm-year anchor all score highest.

Maximum value used in scoring

Not applicable - scored by departure above the fixed baseline.

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.

The NOAA National Centers for Environmental Information Climate Extremes Index (CEI) measures the fraction of the Northeast region experiencing unusually extreme temperature, precipitation, and drought conditions in a given year. V5.0 automates retrieval of the Northeast annual all-steps CEI record directly from NCEI and rebuilds the full historical series each update.

Climate Extremes uses a fixed 1961-1990 baseline but is scored one-sided because fewer climate extremes than the historical normal are not considered a stressor. The top score is anchored one standard deviation below the baseline mean. Values at or below that calm-year anchor receive the highest score, while increasing extremeness above the anchor lowers the score using the smooth-decay form; a year at the baseline mean scores approximately 3.7 of 5. Because CEI is a constructed index, no sampling uncertainty band is shown.

1 NOAA National Centers for Environmental Information. U.S. Climate Extremes Index. Available at: https://www.ncei.noaa.gov/access/monitoring/cei/