The listing broker’s offer of compensation is made only to participants of the MLS where the listing is filed. Listing Information presented by local MLS brokerage: Zillow, Inc., REALTOR®- Lauren Buttazzoni - (313) 479-2702 The data relating to real estate properties on this website was last updated as recently as 06:06:54 PDT All information should be independently verified. The accuracy of all information, regardless of source, is not guaranteed or warranted. IDX information is provided exclusively for consumers' personal, noncommercial use and may not be used for any purpose other than to identify prospective properties consumers may be interested in purchasing. via Zillow, Inc and MLSĬopyright 2023 Realcomp II Ltd. Since hail can cause the rainfall estimates to be higher than what is actually occurring, steps are taken to prevent these high dBZ values from being converted to rainfall.IDX provided courtesy of Realcomp II Ltd. Hail is a good reflector of energy and will return very high dBZ values. These values are estimates of the rainfall per hour, updated each volume scan, with rainfall accumulated over time. Depending on the type of weather occurring and the area of the U.S., forecasters use a set of rainrates which are associated to the dBZ values. The higher the dBZ, the stronger the rainrate. Typically, light rain is occurring when the dBZ value reaches 20. The scale of dBZ values is also related to the intensity of rainfall. The value of the dBZ depends upon the mode the radar is in at the time the image was created. Notice the color on each scale remains the same in both operational modes, only the values change. The other scale (near left) represents dBZ values when the radar is in precipitation mode (dBZ values from 5 to 75). One scale (far left) represents dBZ values when the radar is in clear air mode (dBZ values from -28 to +28). Each reflectivity image you see includes one of two color scales. The dBZ values increase as the strength of the signal returned to the radar increases.  So, a more convenient number for calculations and comparison, a decibel (or logarithmic) scale (dBZ), is used.  Reflectivity (designated by the letter Z) covers a wide range of signals (from very weak to very strong). 'Reflectivity' is the amount of transmitted power returned to the radar receiver. The colors are the different echo intensities (reflectivity) measured in dBZ (decibels of Z) during each elevation scan.

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