30 July 1994  0517 UTC  NOAA 11
Northwest France



















Another example of a morning storm with plumes above. Notice the oval cloud above the point where the two plumes meet. As can be easily seen from the shadow width, the oval cloud seems to be significantly higher than the plumes (rough computations indicate that the oval cloud is about 300 m above the anvil top, while the height of the plumes is about 50 m).