Cumulonimbus clouds are tall, dense clouds associated with thunderstorms. They often have an anvil-shaped top and can produce heavy rain, lightning, and strong winds.
Infrared satellite imagery can be used to identify thunderstorms due to their distinctive cold cloud tops. Thunderstorms usually have high cloud tops that are colder than surrounding clouds, making them easily identifiable on infrared satellite images by their brightness and structure.
Seattle experiences thunderstorms on average of about 5 to 10 times per year. Thunderstorms are more common in the late spring and summer months due to warmer temperatures and increased atmospheric instability.
Cumulonimbus clouds are associated with thunderstorms.
Not all isolated thunderstorms develop into severe thunderstorms. Severe thunderstorms are characterized by specific criteria such as strong winds, large hail, and tornadoes, which may or may not be present in isolated thunderstorms. Factors like atmospheric instability, moisture content, and wind shear can contribute to the development of severe weather conditions.
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