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The Midlatitude Cyclone

The Midlatitude Cyclone. Cyclone Development begins with a stationary front. Before Birth. Forecasting where on the Stationary front the development will occur is the tricky part!. Nascent stage of Cyclone Development. Birth and adolescence. Mature stage of Cyclone Development.

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The Midlatitude Cyclone

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  1. The Midlatitude Cyclone

  2. Cyclone Development begins with a stationary front Before Birth Forecasting where on the Stationary front the development will occur is the tricky part!

  3. Nascent stage of Cyclone Development Birth and adolescence

  4. Mature stage of Cyclone Development Adulthood

  5. Mature Wave Cyclone

  6. Typical Cold Front Structure • Cold air replaces warm; leading edge is steep in fast-moving front shown below due to friction at the ground • Strong vertical motion and unstable air forms cumuliform clouds • Upper level winds blow ice crystals downwind creating cirrus and cirrostratus. Note change in wind and temperature as front passes. • Slower moving fronts have less steep boundaries and less vertically developed clouds may form if warm air is stable

  7. Typical Warm Front Structure • In an advancing warm front, warm air rides up over colder air at the surface; slope is not usually very steep • Lifting of the warm air produces clouds and precipitation well in advance of boundary • At different points along the warm/cold air interface, the precipitation will experience different temperature histories as it falls to the ground

  8. The Partially Occluded Stage begins when the cold front starts to overrun the warm front Middle age

  9. Partially occluded wave cyclone • Cold-occluded front • Approach brings weather sequence like a warm front • Frontal passage brings weather more like a cold front • Warm-occluded fronts also possible Cold-occluded front

  10. Relationship between occluded fronts and Midlatitude cyclone development Mature wave cyclone Partially occluded wave cyclone

  11. The Occluded Stage is characterized by more warm air being pushed aloft and the size of the warm air wedge at the surface decreases significantly Over the Hill

  12. Relationship between occluded fronts and a Midlatitude cyclone Partially occluded wave cyclone Occluded wave cyclone

  13. The final decay stage of the cyclone. The warm air is isolated aloft with cold air beneath. Death

  14. The Wave Cyclone Model(Norwegian model) • Stationary Front • Nascent Stage • Mature Stage • Partially Occluded Stage • Occluded Stage • Dissipated Stage

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