When convection is strong and the updraft intense, the rising air may intrude into the stratosphere, producing ____.
A)a shelf cloud
B)straight-line winds
C)a roll cloud
D)a gust front
E)an overshooting tip

Question

Quizplus · Accepted Answer

When convection is strong and the updraft intense, the rising air can push past the tropopause into the stratosphere, creating an overshooting top. This phenomenon is indicative of a very strong storm, often associated with severe weather. Overshooting tops are a sign of the strength of the updraft within a thunderstorm, as they indicate that the rising air has enough momentum to break through the stable layer of the tropopause.

When Convection Is Strong and the Updraft Intense, the Rising