Tropical Storms and Climate Change
Tropical Storms
- Definition: Tropical storms are intense low pressure weather systems characterized by heavy rain and strong winds spiraling around a central eye.
- Common Names: They are referred to as hurricanes, typhoons, or cyclones depending on the region.
Development of Tropical Storms
- Conditions for Formation:
- Requires sea temperature of 27 °C or higher.
- Occurs between 5° and 30° north and south of the equator.
- Low wind shear in the atmosphere.
- Process of Development:
- Warm surface water evaporates, rises, and condenses into clouds releasing large amounts of energy.
- Rising air creates an area of low pressure, increasing surface winds.
- Tropical storms are pushed towards the west by easterly winds.
- Coriolis Effect:
- The storms spin due to the Coriolis effect, caused by the Earth’s rotation.
- Energy Source:
- Wind speeds increase as storms move over warm water. They weaken over land or cooler water due to a loss of energy.
- Seasonality:
- Most storms occur in the northern hemisphere from August to October; in the southern hemisphere, they occur from December to April.
Extreme Weather Conditions Associated with Tropical Storms
Extreme Winds
- Characteristics:
- High wind speeds can exceed 250 ext{ km/h}.
- Cause significant damage to buildings, vegetation, and can transport loose objects.
Extreme Rain
- **Heavy Precipitation: **
- Tropical storms can bring immense amounts of rain rapidly, leading to flooding.
- Mechanism:
- Warm, moist air is drawn into the storm, rising and cooling, releasing rain as it condenses.
- Consequences:
- Can result in extensive flooding and landslides.
Distribution and Frequency of Tropical Storms
- Distribution: Most occur between 5° and 30° latitudes. Fewer storms form closer to the equator due to insufficient warm water.
- Frequency Trends:
- Storm frequency varies annually; an increase observed in the Atlantic since 1984, but no significant trend over the last 130 years.
Case Study: Typhoon Haiyan (2013)
- Details:
- Made landfall in the Philippines on November 8, 2013; winds reached 314 ext{ km/h}.
- Severe rain and a storm surge caused waves up to 5 ext{ m}.
- Primary Effects:
- 8000 people died, over 1 ext{ million} homes destroyed, heavy flooding over 600 ext{ 000 hectares}.
- Secondary Effects:
- Landslides blocked roads, businesses destroyed leading to $5.6 ext{ million}$ workers jobless, disease outbreaks due to contaminated water.
Responses to Typhoon Haiyan
- Warnings: PAGASA warned 2 days prior, evacuating 800,000 residents.
- Emergency Declarations: The Philippines declared a state of emergency enabling aid to flow.
- International Help: Charities provided food, shelter, and sanitation facilities.
Long-Term Responses
- UN Appeal: More than 300 ext{ million} sought for rebuilding efforts.
- Reconstruction of Homes: Charities built hurricane-resistant houses.
- Tourism Promotion: Encouraged visits to unaffected areas to aid economic recovery.
Climate Change Impact on Tropical Storms
- Global Temperature Increase: Average sea surface temperatures increased by 0.9 °C since 1880, leading to more powerful storms.
- Forecast Changes in Storms: Rising sea temperatures may allow storms to form in new areas or increase their frequency and intensity.
UK Weather Hazards
- Diverse weather hazards include strong winds, heavy rainfall, droughts, and heatwaves, impacting economies and infrastructure.
Management of Tropical Storms
- Prediction and Monitoring: Utilizing technology to predict paths and allow for timely evacuations.
- Planning and Design: Buildings constructed to withstand storms, flood defences installed, communities trained for emergency responses to improve preparedness.
Conclusion
- Understanding the mechanisms and consequences of tropical storms is crucial for risk management and disaster preparedness, especially in regions prone to such severe weather events.