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What is the Mean Shear Vector?

Published in Atmospheric Science 2 mins read

The mean shear vector is the vector difference between two points.

In meteorology and atmospheric science, shear refers to the change in the wind vector (both speed and direction) over a given distance, typically with height. The overall wind shear profile across multiple layers can be visualized using a hodograph.

While the shear vector itself represents the difference in wind between any two heights, the term "mean shear vector" is often used to describe the average shear over a specific layer or, as defined in the reference, specifically the difference between the wind vectors at the beginning and end points of that layer.

Here's a simple breakdown based on the definition:

  • Shear Vector: The difference in the wind vector between two different heights.
  • Mean Shear Vector: The vector difference between two specific points (representing the wind vectors at the lower and upper bounds of the layer being considered).

Understanding the mean shear vector for a particular layer is crucial for analyzing atmospheric conditions, such as potential for severe weather development, as it summarizes the overall change in wind velocity across that layer.

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