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Slide 1

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Cylonogenesis As jet stream turns
towards pole it speeds
Jet stream slows down as Polar Maritime air up sucking air behind it
it turns towards the
equator causing air to sink
Mist cloud mist and fog develop.
Possibly some rain where warm air
starts to rise
Tropical Maritime air…read more

Slide 2

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Pm blowing
air across
Air…read more

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Slide 4

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Rossby wave develops further causing a
greater pressure difference
Cold front develops were cold air is sucked in to replace
rising warm air
Cloud development as
moisture for Tm air Winds start to develop in a
condenses as the air is circular pattern drawn in to the
forced to rise and cool area of low pressure
Gently sloping ward front develops
where warm air rises over cold air
Wave Depression…read more

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