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Hurricanes (Tropical Cyclones)
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Geography of storm names
Atlantic and eastern Pacific: “hurricanes” Indian Ocean and Australia: “cyclones” Western Pacific, N. hemisphere: “typhoons”
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Western Pacific typhoons, 2011
Season: June 1 – November 30
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Eastern Pacific hurricanes
Hurricane Linda Season: May 15 – November 30
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Atlantic hurricanes Season: June 1 – November 30
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Australian cyclones season Season: November 1 – April 30
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North Indian Ocean cyclones
Season: April – December
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South West Indian Ocean cyclones
Season: November 15 – April 30
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Origin regions: Requirements:
expansive surfaces of warm (>26⁰C), deep ocean waters no upper level wind shear Coriolis (therefore do not develop at the equator)
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Trade wind Inversion In an INVERSION, temperature increases with altitude Instead of the normal decrease with altitude Recall the Hadley Cell circulation: Descending air in subtropical Highs Creates a subsidence inversion Subsiding air warms Makes a layer of warm air over cold air
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Subsidence inversion
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Inversion is strongest at
Subtropical highs and weakens towards equator Inversion prevents tall clouds from forming Marine layer (beneath inversion) Trade winds equator subtropics
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Inversion is also lowest along eastern margins of oceans ,
Where upwelling and cold, ocean currents keep the marine layer cool. Inhibits vertical cloud growth. On western side of ocean basins, warm surface waters heat marine layer and it expands to a greater height . Tall cloud growth is possible.
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Therefore, hurricanes form in western portions of ocean basins.
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Ways that hurricanes begin:
1. as easterly waves (Hurricane Georges is an example) Requires spin Most Atlantic hurricanes begin in Africa
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Pacific High Azores Bermuda High Monsoonal Low
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NE Trades ITCZ Turned SW by Coriolis deflection equator ocean Africa SE Trades
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If storm moves off African continent towards Atlantic, becomes “easterly wave” (carried west by equatorial easterlies) Of approx. 100 each year, 6 become hurricanes
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60% of the Atlantic tropical storms and minor hurricanes originate from easterly waves
nearly 85% of major hurricanes have their origins as easterly waves nearly all of the tropical cyclones that occur in the Eastern Pacific Ocean can be traced back to Africa
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2. with wind shifts associated with fronts in the tropics
(Hurricane Arlene is an example) NE trades front S winds
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front
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Easterly wave moves across Atlantic as a small bunch of thunderstorms;
May become a tropical disturbance : disorganized group of thunderstorms that spin tropical disturbances disorganized groups of t-storms; some spin 90% fizzle out 2. tropical depressions : wind speeds 23 mph 3. tropical storm : wind speeds 39 mph (named) 4. hurricane : wind speed 74 mph
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Progression of storms to hurricane:
1. tropical disturbances disorganized groups of t-storms; some spin 90% fizzle out 2. tropical depressions : wind speeds 23 mph 3. tropical storm : wind speeds 39 mph (named) 4. hurricane : wind speed 74 mph
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Speed and direction in North Atlantic basin:
10 – 20 mph travel (NOT wind speed) Originally steered by easterly winds (trades) Are drawn into circulation around subtropical highs and are veered to the north (clockwise) When north enough, are steered by westerlies Details of paths are erratic Due to storm structure and interaction with environment
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Anatomy of a hurricane Spiral bands of thunderstorms
Strong central LOW Convergence at surface Moist warm air rising Condensation Upper level winds and cirrus clouds at top
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Eye and Eyewall Rising air causes crowding at top center
Causes a HIGH at top center HIGH at top and LOW at bottom makes air descend in center Descending air can’t make clouds Therefore clear EYE in center
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High Low Eye is clear, calm
Average : 15 miles wide; experienced on ground for approx. 1 hour High Low
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Eyewall: surrounds eye
High Low
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eyewall Greatest wind speed, thickest cloud cover; heaviest rain (100 in/day) Wind speeds strongest here due to conservation of angular momentum
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Hurricane hunter air flight
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