STRESSORS INDICATORS

Drought

Latest Score:

3.8/5

in 2023

Weight: 9.1%
score trend is down over time

While mild, short-term droughts are not an uncommon event in Vermont, with higher temperatures resulting from continued climate change, we may see more severe or longer duration droughts. Lack of water, particularly during the growing season, can result in short-term changes in our forests, for example, a tree will halt photosynthesis and growth until there is sufficient water. But droughts can also result in more serious consequences to forests, like lack of a viable seed crop or large die offs of vulnerable species, locations, or age classes. Seedlings are particularly vulnerable to drought due to their shallow root systems. Further, droughts can increase the chance of forest fire -- to which many of our tree species are not adapted. Insect pest outbreaks can also be more destructive when they occur with or following drought. Here, we used an index of drought called the Standardized Precipitation Evapotranspiration Index (SPEI), which incorporates both rainfall, temperature, and plant water requirements1,2. We set the target for the dataset as the long-term mean with the understanding that droughts are a natural phenomenon, but changes in the frequency or duration of seasonal droughts could pose serious threats to forests. A high score means drought severity is not deviating from historical patterns.

1Vicente-Serrano S.M., Beguería S., López-Moreno J.I., 2010: A Multi-scalar drought index sensitive to global warming: The Standardized Precipitation Evapotranspiration Index – SPEI. Journal of Climate 23(7), 1696-1718, DOI: 10.1175/2009JCLI2909.1. Available at: http://digital.csic.es/handle/10261/22405.
2Vicente-Serrano S.M., Beguería S., López-Moreno J.I., Angulo M., El Kenawy A. (2010) A global 0.5° gridded dataset (1901-2006) of a multiscalar drought index considering the joint effects of precipitation and temperature. Journal of Hydrometeorology 11(4), 1033-1043, DOI: 10.1175/2010JHM1224.1. Available at: http://digital.csic.es/handle/10261/23906.

"(Warming and reduced snowpack interact to) increase drought risk and put stress on forest ecosystems." — USDA Northern Forests Climate Hub, drought synthesis
Interpretation provided by:

Vicente-Serrano et al. 2010, *J. Climate* (SPEI method); USDA Northern Forests Climate Hub drought 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.

Drought is assessed using the Standardized Precipitation Evapotranspiration Index (SPEI), which combines precipitation supply with atmospheric water demand through evapotranspiration. The Dashboard uses a six-month SPEI spanning April through September to represent moisture conditions during the functional growing season.

V5.0 scores drought as two-sided consistency with the fixed 1961-1990 reference period. The baseline mean and standard deviation are held fixed and annual scores use the smooth-departure function; both unusually dry and unusually wet growing seasons therefore represent departures from the historical climate regime. SPEI is a deterministic constructed index rather than a sampled mean, so no uncertainty band is shown.

1 Vicente-Serrano, S.M., S. Beguería and J.I. López-Moreno. 2010. A multi-scalar drought index sensitive to global warming: the Standardized Precipitation Evapotranspiration Index. Journal of Climate 23(7):1696-1718.