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.