Tilted updraft

A tilted updraft (also known as a tilted storm) is a thunderstorm which is not vertically erect.[1] This happens as a result of unidirectional wind shear, or a change in wind speed with height. In such an environment, the top of the updraft is pushed further downstream than the lower parts as a result of stronger winds pushing the top, as it is higher in the atmosphere. Storms that occur in environments with wind shear are more likely to be severe.[1]

References

  1. 1 2 Michael Branick (March 11, 2008). "A COMPREHENSIVE GLOSSARY OF WEATHER TERMS FOR STORM SPOTTERS". NWS - Norman. Archived from the original on 2008-05-01. Retrieved 2008-05-18.


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