In both cases, there is still an area of radar echoes somewhere nearby. The second image shows that this happens when strikes originate in the anvil of the thundercloud (top part blown ahead of the cumulonimbus cloud by upper winds) or on the outside edge of the rain shaft. Lightning may be also located outside the precipitation recorded by radar. Lightning detectors do not suffer from a masking effect and can provide confirmation when a shower cloud has evolved into a thunderstorm. It is not always clear from early returns if a shower cloud will develop into a thunderstorm, and weather radar also sometimes suffers from a masking effect by attenuation, where precipitation close to the radar can hide (perhaps more intense) precipitation farther away. The cloud must develop to a certain vertical extent before lightning is produced, so generally weather radar will indicate a developing storm before a lightning detector does. Eventually the mass of rain drops is too large to be sustained by the updraft and they fall toward the ground.Condensation occurs and radar detects echoes above the ground (colored areas).Air is moving upward due to instability.The first image on the right shows the life cycle of a thunderstorm: Both phenomena are associated with thunderstorms and can help indicate storm strength. Lightning detectors indicate electrical activity, while weather radar indicates precipitation. Lightning detectors and weather radar work together to detect storms. weather radar A thunderstorm life cycle and associated reflectivities from a weather radar Distribution of electric charges and lightning strikes in and around a thunderstorm
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