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CLIMATE/EARTH 401�Geophysical Fluid Dynamics�Dynamical Meteorology

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Vorticity 8: Scaling

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Vorticity and Divergence

  • Related to shear �of the velocity field.

∂v/∂x-∂u/∂y

  • Related to stretching �of the velocity field.

∂u/∂x+∂v/∂y

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Conservation of vertical component of vorticity

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Scale Analysis of the Vorticity Equation

  • Changes in relative vorticity are caused by:
      • Divergence
      • Tilting
      • Gradients in density
      • Advection
  • Which of these are most important for large-scale flows?
  • Back to scale analysis…

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Scale factors for “large-scale” mid-latitude

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Scale of relative vorticity

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Compare relative vorticity to planetary vorticity

Usually, planetary vorticity is larger than relative vorticity.

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Time rate of change of relative vorticity

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Remaining Terms

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Scale analysis of the vorticity equation

  • Divergence term largest, followed by horizontal advection and the local time rate of change of relative vorticity
  • Tilting term important where there is large shear and strong horizontal gradient in the vertical velocity (boundary layer, smaller scales)
  • Thermodynamic term important where there are strong density (temperature) gradients that intersect lines of constant pressure (sea breeze, fronts)

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Consider divergence term

  • This term scales larger than the other terms.
    • But, remember that the divergence of the horizontal wind is, in actuality, small compared to the change in wind with x,y

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Consider divergence term

Divergence scales as the scale of the �ageostrophic wind, so

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Consider divergence term

We saw that the relative vorticity is typically about an order of magnitude less than the planetary vorticity. So

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So for quasi-nondivergent (i.e., geostrophic) flow

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Compare relative vorticity to planetary vorticity and to divergence

Again we see the importance of the rotation of the Earth.

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Terms in Vorticity Equation

Time rate of change

Horizontal advection

Vertical advection

Divergence

Tilting

Planetary vorticity advection

Solenoidal term

Time rate of change

Horizontal advection

Divergence

Planetary vorticity advection

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Assume balance among terms of 10-10 s-2

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End: Vorticity 8: Scaling