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Those Shifty Winds

Gemini Sparkle

Key Takeaways:

  • The article clarifies "veering" (clockwise wind change) and "backing" (counter-clockwise wind change), which are crucial for understanding wind shear caused by temperature advection (thermal wind) or friction.
  • Friction in the planetary boundary layer typically causes winds to decelerate and back as a pilot descends, an effect usually confined to the lowest few thousand feet of the atmosphere.
  • However, turbulence and chaotic mixing, especially from daytime heating, often overwhelm these predictable backing/veering patterns, making precise low-altitude wind behavior highly variable and difficult for pilots to anticipate.
See a mistake? Contact us.

An excellent article by editor Frank Bowlin on ILS technique appeared in the February issue. A small error led to some confusion, and IFR embarked on a quest for accuracy. That quest got stymied with some faulty background. We thank astute readers for returning us to the righteous path. I’ll now clear away all confusion and help you understand in great detail which way the wind shifts, and why.

Definitions
When talking about wind shear, it’s important to be thoroughly familiar with the terms “veering” and “backing”. Veering is a clockwise change in the wind direction, normally in terms of increasing height or with time. Good practice is to carefully qualify all measures of veering to avoid confusion. For example if the winds are from the south at the surface and from the west aloft, that’s described as a wind profile that “veers with height.”

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