One Hour Precipitation
Just as the name implies, this is an image (right) of the estimated precipitation during the previous hour. But also as in the case of other Doppler radar images, there needs to be some caution in viewing this image as there are two main factors to consider. First, while the radar does a great job at correcting itself, there are times when the radar will be out of calibration. If the radar is “hot” (reporting echoes too strong) then the rainfall estimates will be an overestimate. Conversely, a “cool” radar will underestimate the precipitation. Always check nearby radars to see if they are reporting similar information to what is viewed by your local radar. Second, hail makes an excellent reflector of energy. Thunderstorms with hail will overestimate the amount of precipitation and the larger the hailstones, the greater the overestimate. Besides estimating rainfall, both the static and looping One-hour Precipitation images can provide other useful information. This is a good way to track individual storms. The first thing to notice is storms DO NOT always move parallel to the upper level winds. Some storms can move left, or right, of the upper level flow. Thunderstorms also do not always move in straight lines. Sometimes they curve as in the case of the two small storms to the right of #2. This is valuable information as storms that tend to move right of the main airflow, either in a straight line or curved path, are often capable of producing severe weather. These “right movers” may be difficult to see on looping Base Reflectivity images but the rainfall pattern they leave behind can be invaluable in knowing which storms require extra attention.