The Midlatitude Cyclone

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The Midlatitude Cyclone

Transcript of The Midlatitude Cyclone

Page 1: The Midlatitude Cyclone

The Midlatitude Cyclone

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Cyclone Developmentbegins with a stationary front

Before Birth

Forecasting where on theStationary front the developmentwill occur is the tricky part!

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Nascent stage ofCyclone Development

Birth andadolescence

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Mature stageof Cyclone Development

Adulthood

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Mature Wave Cyclone

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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 andcirrostratus. Note change in wind and temperature as front passes.

• Slower moving fronts have less steep boundaries and lessvertically developed clouds may form if warm air is stable

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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 inadvance of boundary

• At different points along the warm/cold air interface, the precipitationwill experience different temperature histories as it falls to the ground

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The Partially OccludedStage beginswhen the cold front starts to overrun the warm front

Middle age

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Partially occluded wave cyclone• Cold-occluded front

– Approach bringsweather sequencelike a warm front

– Frontal passagebrings weather morelike a cold front

• Warm-occludedfronts also possible

Cold-occluded front

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Relationship between occluded fronts and Midlatitude cyclone development

Mature wavecyclone

Partially occludedwave cyclone

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The Occluded Stageis characterized bymore warm air being pushed aloftand the size of thewarm air wedge at the surface decreases significantly

Over theHill

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Relationship between occluded fronts and aMidlatitude cyclone

Partially occludedwave cyclone

Occluded wavecyclone

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The final decay stageof the cyclone. The warmair is isolated aloft with cold air beneath.

Death

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The Wave Cyclone Model(Norwegian model)

• Stationary Front

• Nascent Stage

• Mature Stage

• Partially Occluded Stage

• Occluded Stage

• Dissipated Stage