5: Extratropical Cyclones Flashcards
Direction of cyclones in Northern hemisphere. Where does it develop?
- Surface winds blow counterclockwise and go inwards towards the low pressure center
- Develops in mid to high latitudes from warm and cold front working together
What is the Cyclone Life Cycle (Just brief, main purpose). Image
- Incipient cyclone: intensification of horizontal pressure gradient
- Wave cyclone: comma cloud formation
- Beginning occlusion: pressure drops
- Bent back occlusion: cyclone slowly dies as pressure drops
Image 1
Term for the birth of a cyclone
Cyclogenesis
Incipient Cyclone
- first step in cyclone life cycle
- Strong horizontal divergence develops east of an upper level trough which leads to the intensification of surface low
- Intensification of horizontal pressure gradient at the lower troposphere results in cyclonic circulation
- HIgh and low pressure and fast and slow wind speed alternate
- 1a
Wave Cyclone
- second step of cyclone life cycle
- front bends and form a wave like pattern
- upper level trough (low pressure) deepens
- central low pressur ~990mb
- Comma cloud formation
- 1b
Comma cloud
- formed in wave cyclone step
- Comma head: surface low
- Comma tail: surface cold front
- Dry slot behind tell: descending cold air
- image 2
Beginning Occlusion
- third step of cyclone life cycle
- Comma cloud will intensify
- Pressure drops to ~985mb
- Cold front catches warm front and occlusion begins
- Closed circulation above the surface low and descending dry air behind the cold front
- 1c
Bent Back occlusion
- last step of cyclone life cycle
- Cikd front will eventually overtake warm front and cyclone will die
- Central low pressure drops to ~980mb
- North Atlanta and North Pacific Occeans origin of intense cyclones
- 1d
Airflow in Cyclone Model
- Called conveyor belt model
- Warm moist air stream is ascending
- Dry air stream is descending
- Cold moist air stream is ascending
- image 3
wind direction in northern hemisphere
always west to east
Cyclone Characteristics like wind, temperatue, clouds and precipitation, and pressure
- image 4
- Wind: 4a, know it. counterclockwise and inwards
- temperature: 4b. Warm front is to the right of low pressure center and cold front is south of it. Behind the cold front and in front of the warm front is cold air mass. The warm air mass is between the cold and warm air mass, in front of the cold front an dbehind the warm front.
- Clouds and precipitation: know 4c. right in front of warm front is fog and drizzle, and as you go up is rain. The snow is more NW of th low pressure center. Ahead of the cold front are thunderstorms
- Pressure: 3d. Rising presure behind the cold front and falling pressure in front of the warm front
Principal Cyclone Tracks in Canada
- Storm travels eastwards and as it goes through water bodies it will carry lots of moisture –> results in huge amount of precipitation in the east coast (cyclones end in the Canadian Maritimes: Newfoundland)
- East Gulf Cyclone track is most common with most intense cyclones
- Many cyclones start in the lee of the Rocky Mountains
Lee Cyclogenesis for Alberta winter storms
- Cyclonic spin weakens as air ascends the western slopes of Rockies (horizontal divergence)
- Cyclonic spin strengthens as air descends the leeward slopes of Rockies –> smaller radius so faster (horizontal convergence)
- Conservation of angular momentum
- image 5
What is conservation of angular momentum
- smaller radius means faster
- Formula given: radius x velocity = new velocity
What is a Cyclone Bomb and other type of Bomb
Cyclone Bomb: cyclone whose central pressure falls by ≥ 24mb/24hrs rapidly
ERICA: Experiment on Rapidly Intensifying Cyclone over the Atlantic
* ERICA bomb: cyclose whose central pressure falls by ≥10 mb/6hrs