The Extreme Precipitation Monitor displays the climatological significance of the precipitation forecasted by the Weather Prediction Center (WPC). The climatological significance is represented by Average Recurrence Intervals (ARIs) of precipitation estimates from the NOAA Atlas-14, NOAA-40 and Atlas-2.

ARIs describe the expected amount of time (e.g., years) between periods of rainfall exceedances (usually in inches) at a given location. ARIs are approximately inversely related to the Annual Exceedance Probability, which describes the probability of a particular event occurring at any one location in any given year. For example, precipitation thresholds that have a 100-yr ARI have a 1-in-100 chance (i.e., 1% AEP) of occurring in any given year. The following table shows the equivalent AEP to ARIs ranging from 1-100 years.

This product is generated with WPC's Days 1-3 Quantitative Precipitation Forecasts (QPFs) for each 6- and 24-hour period. In the national mosaic, each contour level represents an ARI forecasted to be exceeded for the given time period. If the QPF for the given period is not expected to exceed the 1-yr ARI anywhere in the domain, the text at the center of the graphic will read "WPC-QPF NOT EXPECTED TO EXCEED THE 1-YR ARI". The value in recasting the QPF in the context of each ARI is that it allows the user to measure the climatological significance or "rarity" of a forecasted or observed rain event for any location. Furthermore, precipitation ARIs are used in the design of hydrologic and flood-control structures, so they are more relatable to emergency managers and key decision makers rather than absolute rain estimates alone.

Users should be aware that this product does not consider antecedent conditions and should not be used as a sole indicator for impacts from flooding. The severity of flooding is also dependent geographic location (urban vs. rural), antecedent conditions (e.g., soil characteristics and terrain), and total areal rainfall coverage. In general, large urban dams and levees are designed to withstand precipitation greater than the 100-yr ARI. Once the 100-yr ARI has been exceeded, these structures can fail and risk for damaging impacts to life and property is substantially increased.

The NOAA Atlas 14 data is available through the Precipitation Frequency Data Server, which provides point-based estimates of rainfall for ARIs between 1 and 1000 years for rainfall durations ranging from 5-mins up to 60 days based on a 90% confidence interval. Because the NOAA Atlas-14 update has not been completed for the pacific NW or Texas, the DOC Tech Paper 40 (1961) was used for TX, and the NOAA Atlas-2 (1973) was used for the Pac NW. These data were "stitched" together with the Atlas-14 data (courtesy of Dr. Russ Schumacher and Greg Herman).