Cyclones
Topic 11: Cyclones - Nature’s Deadliest Storms
Definition of Tropical Cyclones
Tropical Cyclone: A cyclonic low-pressure system occurring in the tropics with sustained winds of 119 km/h (74 mph) or greater.
Characterized by counterclockwise rotation around the region of low pressure (in the Northern Hemisphere).
Names for Tropical Cyclones
Different names based on geographic location:
Hurricane in North America.
Typhoon in Southeast Asia.
Cyclone in countries bordering the Indian Ocean.
Tropical Cyclone in Australia.
Page 2: Air Movement within a Hurricane
Eye: Center of the hurricane, characterized by the lowest pressure.
Eyewall: Region around the eye with the fastest winds and heaviest rain.
Contains the most severe weather conditions.
Rain Bands: Spiraling bands of thunderstorm activity surrounding the eyewall.
Page 3: Hurricane Strength
**Key Factors Influencing Strength: **
Amount of water vapor condensing to liquid; condensation releases latent heat, creating positive feedback.
Requires warm water (about 26°C) for evaporation.
Little to no wind shear is needed to prevent disintegration.
Stages of Hurricane Growth
Progression of tropical cyclones:
Tropical Disturbance → Tropical Depression → Tropical Storm → Hurricane.
Tropical Storm: Defined as a tropical cyclonic storm with sustained winds between 63 and 118 km/h.
Categories of hurricanes based on wind speed.
Page 4: Saffir–Simpson Hurricane Wind Scale
Ranks hurricanes based on highest wind speed averaged over a one-minute interval, measured at 10 m above the surface.
Page 5: Tropical Cyclone Geography
Location: Hurricanes are confined to tropical oceans.
Subtropical Highs: Guide the paths of hurricanes.
Restricted from forming within about 5° latitude of the equator due to lack of Coriolis force.
Page 6: Hurricane Hazards
Impact: Hurricanes are the leading meteorological killer worldwide.
Coastal Storm Surge: Most dangerous aspect of a hurricane, characterized by a rise in sea level due to strong winds and low atmospheric pressure.
Particularly threatens the Indian Ocean region due to high coastal populations and poverty limiting evacuation.
Page 7: Extratropical Cyclones
Midlatitude Cyclone: A large cyclonic system occurring at mid to high latitudes, also known as depressions or low-pressure systems.
Anatomy of a Midlatitude Cyclone
Composed of:
Cold Front: Cold air advances on warm air.
Warm Front: Warm air flows over cooler, denser air.
Page 8: Cyclogenesis
Definition: The process of midlatitude cyclone formation occurring mainly from fall through spring in areas between approximately 30° and 70° N/S.
Key Locations for Formation:
Downwind of mountain ranges.
Areas with warm water downwind of cold water or land surfaces.
Page 9: Effects on Weather
Midlatitude cyclones cause stormy conditions in regions like the U.S. and Canada from fall to spring.
Weather Associations:
Warm Fronts: Linked to steady precipitation and nimbostratus clouds.
Cold Fronts: Associated with short bursts of rainfall and cumulonimbus clouds, leading to severe weather events.
Page 11: Lifecycle of a Midlatitude Cyclone
Growth, maturation, and dissipation cycle lasts 1–2 weeks.
After passing over Great Lakes, can induce lake-effect snow:
Lake-effect Snow: Heavy snowfall when cold air moves over warm waters.
Nor’easter: A specific type of midlatitude cyclone famous for its blizzard conditions impacting the Mid-Atlantic states and New England.