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Wind shear

Difference in wind speed or direction over a short distance

Wind shear is a difference in either wind speed or direction over a fairly short distance in the atmosphere. Wind shear can be divided into two different types: horizontal and vertical wind shear.

NASA schematic of the downward motion of the air until it hits ground.

Contents

When wind shear is observedEdit

Weather situations when the Wind shear is observed happen:

  • At weather fronts when the temperature difference across the front is 5 °C or more, and the front moves at 15 kt or faster.
  • At low level jets when a significant low level vertical wind shear can develop near the lower portion of the low level jet.
  • At mountains when winds blow over and create vertical shear on the lee side.[1]
  • At inversions when on a clear and calm night a radiation inversion is formed near the ground.
  • At downbursts when an outflow boundary moves away from a thunderstorm.
  • At sailing when wind shear affects sailboats by presenting a different wind speed and direction at different heights along the sailing mast.

Related pagesEdit

NotesEdit

  1. National Center for Atmospheric Research. T-REX: Catching the Sierra’s waves and rotors Retrieved on 2006-10-21.

Other websitesEdit