dBZ (meteorology)
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This article may be too technical for most readers to understand. Please help improve this article to make it understandable to non-experts, without removing the technical details. The talk page may contain suggestions. (July 2011) |
dBZ stands for decibels of Z. It is a meteorological measure of equivalent reflectivity (Z) of a radar signal reflected off a remote object.[1] The reference level for Z is 1 mm6 m−3, which is equal to 1 μm3. It is related to the number of drops per unit volume and the sixth power of drop diameter.
Reflectivity of a cloud is dependent on the number and type of hydrometeors, which includes rain, snow, and hail, and the hydrometeors' size. A large number of small hydrometeors will reflect the same as one large hydrometeor. The signal returned to the radar will be equivalent in both situations, so a group of small hydrometeors is virtually indistinguishable from one large hydrometeor on the resulting radar image.
A meteorologist can determine the difference between one large hydrometeor and a group of small hydrometeors as well as the type of hydrometeor through knowledge of local weather condition contexts.
One dBZ-scale of rain:
- >65 Extreme
- 46-65 heavy
- 24-45 moderate
- 8-23 light
- 0-8 Barely anything
dBZ values can be converted to rainfall rates in millimetres per hour using this formula:
[edit] References
- ^ NWS JetStream - Weather Glossary: D's
- ^ "NWS NEXRAD". http://www.desktopdoppler.com/help/nws-nexrad.htm#rainfall%20rates. Retrieved November 7, 2010.
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