About the Tool
With this tool you can explore what an extreme precipitation event looks like by providing estimates of intensity and frequency of extreme precipitation events. The tools and visualizations allow you to examine how extreme precipitation events are likely to change in a warming climate over locations of interest to you.
By default, Cal-Adapt calculates extreme values of precipitation over a 2-day period, and defines an extreme event as the lowest value from Annual Maximum values in the historical period (1961–1990). Users can override these defaults by selecting a new “event duration” (number of days over which precipitation accumulates), or by selecting a different “threshold“ value that corresponds to either the 90th, 95th or 99th percentiles. The tool displays the extreme events that exceed the threshold in different ways. The Intensity chart shows the estimated intensity of precipitation events (Return Level) for a selected period (Return Period) and how it changes over the historical period (1961–1990), mid-century (2035–2064) and end-century (2071–2099). The other charts display the frequency of these events, the timing of these events and the longest stretch of consecutive extreme events.
What is a Threshold value?
The extreme threshold sets the conditions for which a precipitation event is considered “extreme“. By default, the threshold is set to the lowest annual maximum precipitation accumulation in the historical record (1961 to 1990). Other alternative threshold values (90th, 95th and 99th percentiles) are based on commonly used quantiles over the historical record. Selecting too high a threshold (in arid locations) or too low a threshold can decrease the reliability of the estimates.
What is an Event Duration?
Event duration is the number of days over which precipitation falls that contribute to a single event. Changing this value will change the extreme threshold.
What is a Return Period?
The return period estimates the average time between extreme events. This is sometimes worded as a “1 in x years” event.
What is a Return Level (Estimated Intensity)?
The return level is the estimated amount of precipitation that would be expected to be exceeded once every return period. Effectively it is the inverse of the return period. Instead of wondering how often an extreme precipitation event will occur, we are instead considering once in any given time period what would extreme precipitation event look like? The return level is similar to the accumulated precipitation threshold, but is estimated from the underlying statistical distribution of modeled precipitation data in future climate scenarios. By contrast, accumulated precipitation threshold are calculated from historical observed values.
Extreme Value Theory (EVT) is a statistical methodology used for describing rare events. There are several ways to apply EVT to precipitation data inlcuding fitting a Generalized Extreme Value distribution (GEV) over block maxima (annual maximum value) and the Peaks-Over-Threshold (POT) approach where probability distribution of exceedances over a pre-defined threshold are modeled using a generalized Pareto distribution (GPD). This tool explores extreme events in California using a POT approach.
Data values that exceed a high predefiend threshold, by default the lowest value from Annual Maximum values in the historical period (1961–1990), are extracted from a 30 year daily time series. If there are any back-to-back events only the largest such event is included. A generalized Pareto distribution is applied to this partial duration time series. Shape and scale parameters for the distribution are estimated using the Maximum Likelihood method. Return levels for selected Return Periods are estimated from the fitted model. Confidence intervals at the 95% level for each return level are estimated using the Profile Likelihood method, where sufficient (n > 100) events exist.
User Advisory: The Extreme Precipitation Tool is designed to broadly inform potential changes in extreme precipitation intensity and frequency across a wide range of environments and climate zones in California. On a local scale different statistical assumptions (i.e. using annual maximal values rather than partial duration time-series, fitting techniques for distribution parameters and choice of extreme value distribution) may be more appropriate. We encourage users to ensure the empirical fit of the applied distribution is acceptable to their end use before using estimates produced from this tool for planning purposes.
Update (Feb 20, 2022): Based on feedback from users, we have updated the tool to use the average of precipitation values from all intersecting grid cells for a polygon boundary before calculating intensity estimates. An earlier version of this tool used the maximum values from all intersecting grid cells which resulted in very high intensity estimates. Values using the average method more closely align with precipitation intensity estimates provided by NOAA.
- Wilks, D. (2011). Statistical methods in the atmospheric sciences (3rd ed.). Oxford ; Waltham, MA: Academic Press.
- Gilleland, E. (2015). Introduction to Extreme Value Theorem Analysis. National Center for Atmospheric Research.
- Coles, S. (2001). An introduction to statistical modeling of extreme values. London: Springer-Verlag. ISBN: 1-85233-459-2.
The following list of datasets were used to create this tool. Download data visualized in the charts by clicking the Download Chart button. For more download options follow the links below.