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Thermal Wind & Temperature Advection Concepts

Explore thermal wind, its balance with the atmosphere, temperature advection, and their effects on wind patterns and frontal zones. Learn how to interpret Doppler velocities for weather forecasting.

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Thermal Wind & Temperature Advection Concepts

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  1. Thermal Wind, Temperature Advection, and Doppler

  2. The Thermal Wind • The thermal wind, VT, is a vector defined as the difference between the geostrophic wind at two levels of the atmosphere. • The name is really a misnomer, not a wind, but a difference of the winds at two levels.

  3. Thermal Wind and Thickness • The thermal wind vector is parallel to thickness lines • The magnitude of the thermal wind vector is proportional to the horizontal gradient of the thickness lines (or the mean temperature gradient of the layer).

  4. You can convince yourself

  5. Believe it or Not! • Much of the atmosphere is in approximately thermal wind balance (follows the thermal wind equation). • Why? Because most the atmosphere is ~ geostrophic and in hydrostatic balance. • In most of the atmosphere, vertical wind shear is relative to horizontal temperature gradients.

  6. Temperature Advection • Vertical geostrophic wind shear is associated with temperature gradients. • But the fun doesn’t stop there. The turning of the geostrophic wind with height is related to temperature advection.

  7. Temperature Advection • Backing (counterclockwise turning with height) of the the geostrophic wind: cold advection • Veering (clockwise turning with height) of the the geostrophic wind: warm advection • Thus, if the actual winds are ~geostrophic (not bad assumption above boundary layer) one can determine temperature advection from a single sounding

  8. Does this make sense? Backing Veering

  9. Frontal Zones • In cold frontal zones winds back with height • In warm frontal zones wind veer with height • In areas of little temperature advection, there is little turning with height

  10. Warm Front Approaching UIL

  11. Cold advection sounding

  12. Weather Radar and Temperature Advection • You can tell whether warm or cold advection is occurring by looking at the Doppler Velocities • Specifically, the zero radial velocity line (usually gray)

  13. Radar Imagery is generally not for a level surface • Scans in azimuth ( 0 to 360°) at a series of increasing scan angles from the horizontal.

  14. Each radar elevation angle shown on a polar-type chart with range circles

  15. “ S “ shape: veering

  16. Backing: Backwards S

  17. Fronts and Wind Shear Example:January 11, 2014 Washington Coast

  18. Warm Front Approaching UIL

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