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Nonclassical Mesoscale Fronts Caused by Solitary Waves

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Presentation on theme: "Nonclassical Mesoscale Fronts Caused by Solitary Waves"— Presentation transcript:

1 Nonclassical Mesoscale Fronts Caused by Solitary Waves
1. Hydraulic Jumps 2. Bores 3. Density Currents

2 1. Hydraulic Jumps The dynamic upfold of isentropic surfaces at the location of abrupt mass flux convergence accompanying a local near-surface surge in mass.

3 2. Bores A shallow, intense, near-surface wave forced by an upstream or downstream mass impulse and very effective at forward downward momentum fluxes and rearward upward momentum fluxes.

4 3. Density Currents A local, near-surface density gradient typically preceding relatively cold air or a surge of mass flowing out of deep convection, down a mountain, parallel to a mountain or over a relatively smooth surface.

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7 Bore Genesis Supercriticality, Partial Blocking, Complete Blocking and Subcriticality all refer to the relative depth of the impulsive density current (Do) to the depth of the downstream inversion (Ho).

8 Bore Genesis Subcriticality: Ho >>> Do
Supercriticality: Ho >> Do Partial Blocking: Ho > Do Complete Blocking: Ho < Do

9 Velocity Equations 1. 2. 3. 4.

10 Density Current Depth

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