Hurricanes Doc
Hurricanes, Cyclones, Typhoons Structure
The eye of a hurricane has a radius of 15 to 25 km.
The eye mostly features clear skies and is a region of intense low pressure.
Conditions and Formation (Cyclogenesis)
Location and Temperature: Hurricanes typically form within or near the Intertropical Convergence Zone (ITCZ) over oceanic surfaces with temperatures exceeding 27°C.
Rising Air: The hot ocean heats the air above, causing it to rise and creating a circular area of low pressure at the ocean's surface.
Invitation of Moist Air: The low-pressure area attracts moist air, which rises, expands, and cools adiabatically, leading to condensation and the formation of cumulonimbus clouds.
Cloud Growth: Substantial convectional uplift within the clouds allows them to grow to significant heights, signaling the birth of a hurricane.
Perpetuation Factors:
Condensation in cumulonimbus clouds produces latent heat of vaporization, warming the air and promoting further cloud growth.
Heat from condensation can increase the ocean's surface temperature, further reducing pressure and pulling in more moist winds.
The quickly rising air within the cloud is diverted outward at the tropopause, aiding the system's ability to take in more air and fuel further growth.
Maturity of the Hurricane
Clouds organize into spiraling bands towards the center due to the Earth's rotation, giving the cyclone a westward motion. Once wind speeds reach 33 m/s (120 km/h), the storm is officially classified as a hurricane.
The eye has a diameter of about 30 km, with descending air experiencing adiabatic warming, creating a self-perpetuating heat engine.
Decay of the Hurricane
Land Interaction: Moving over land deprives the storm of its moist air supply, leading to decay.
Cold Water Impact: Transitioning over colder waters reduces available heat.
Physical Disturbance: Friction from mountains can disturb the cloud arrangement, contributing to decay.
Hurricane Categories
Hurricanes are categorized using the Saffir-Simpson Hurricane Wind Scale, ranging from Category 1 to Category 5, primarily based on wind speed and potential damage.
Category 1 Hurricane
Winds: 118-152 km/h.
Potential Damage: Some damage to frame homes, older mobile homes destroyed; power outages likely.
Examples: Hurricane Dolly (2008), Hurricane Sandy (2012).
Category 2 Hurricane
Winds: 152-176 km/h.
Potential Damage: Extensive damage to homes, risk to life from debris; potential long-term power loss.
Example: Hurricane Frances (2004).
Category 3 Hurricane
Winds: 178-206 km/h.
Potential Damage: Devastating damage to homes and infrastructure; significant blockages from uprooted trees.
Example: Hurricane Wilma (2005), Hurricane Katrina (2005).
Category 4 Hurricane
Winds: 208-250 km/h.
Potential Damage: Catastrophic damage; widespread destruction to buildings and infrastructure, long-term power outages.
Example: Hurricane Harvey (2017).
Category 5 Hurricane
Winds: greater than 250 km/h.
Potential Damage: Incredible destruction; substantial disruption of life and infrastructure; very few historical landfalls.
Examples: Hurricane Andrew (1992), Hurricane Camille (1969).
Hurricane Formation Basins
Atlantic Basin: Season runs from June 1 to November 30; peak season from mid-August to late October.
Affected areas: Bermuda, eastern Canada, U.S. East Coast, Central America.
Eastern Pacific Basin: Season starts May 15 to November; most active in early September.
Storms can also affect the USA's western coastline and Hawaii.
Western Pacific Basin: Runs from July 1 to November; peaks in early September.
Affects southern Asia, China, and Japan.
Indian Ocean: Northern Indian season is April to December; southern starts October to May.
The Bay of Bengal sees severe cyclones.
Tropical Storm Hazards
Flooding: Heavy rainfall can exceed local river discharge, causing catastrophic flooding, especially in areas like Mozambique.
Tidal Waves: Strong winds cause tidal waves up to 8m high that can devastate coastal areas, notably in Bangladesh.
Wind Damage: Steep pressure gradients create dangerous winds, causing structural failures and fatalities.
Debris Flows: Torrential rains facilitate landslides; incidents have occurred in Hong Kong due to typhoons.
Lightning and Hail: Lightning causes electrocution and fires, while hail can destroy crops.
Mitigation Attempts for Hurricanes/Typhoons/Cyclones
Weather Satellites: Geostationary satellites track cyclone development; they provide continuous imagery for monitoring.
RADAR Systems: Utilized for tracking rain and storm systems; provide early warnings.
LIDAR Equipment: Detects electrical activity within cyclone clouds; effective for long-range forecasting.
Numerical Forecasting: Uses mathematical models to predict cyclone behavior, though affected by observational network limitations in some regions.
Community Preparedness: Evacuations and shelter strategies are crucial during cyclone threats.
Hurricane Katrina
Characteristics
Third strongest hurricane recorded in the U.S. (based on barometric pressure).
Sustained winds of 201 km/h at landfall.
Movement
Initially made landfall in Florida, became a tropical storm, then regained strength in the Gulf of Mexico to reach Categories 4 and 5.
Landfall in Louisiana as Category 3 on August 29.
Effects
1,833 deaths; severe flooding in New Orleans.
80% of the city flooded post-storm, with 100,000+ homes lost.
Measures Following Hurricane Katrina
Flood management improvements initiated post-storm due to levee failures and suboptimal engineering practices.
A new system implemented at a cost of $14.5 billion aims to protect the city from future storms.