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Home » UPSC News Editorial » Tropical cyclones with increased intensity necessitate a new category.

Tropical cyclones with increased intensity necessitate a new category.

UPSC News Editorial: Tropical cyclones with increased intensity necessitate a new category.

Beyond Category 5: The Looming Threat of Super Cyclones and the Urgent Need for Adaptation

 

    • Tropical cyclones, colossal weather systems characterized by swirling winds, torrential rains, and storm surges, have long been a force of nature wreaking havoc on coastal communities. However, a new and terrifying chapter is unfolding – the rise of super cyclones exceeding the current classification system. This editorial dissects this intensifying threat, the urgent need for a Category 6 designation, and the critical steps needed to bolster coastal defenses.

 

A Growing Monster:

 

    • Tropical cyclones form over warm ocean basins where sea surface temperatures exceed 26.5°C. These storms typically originate in the North Atlantic, East Pacific, West Pacific, South Pacific, and the Indian Ocean. While historically, around 85 tropical storms formed annually, with about half intensifying into cyclones, a disturbing trend is emerging. Data suggests an increase in the frequency and intensity of these storms, particularly the most powerful ones.

 

The Saffir-Simpson Scale and its Limitations:

 

    • The current public warning system for tropical cyclones relies on the Saffir-Simpson Hurricane Wind Scale (SSHS). This scale categorizes storms based on their maximum sustained wind speed, with Category 5 representing the most destructive storms exceeding 252 km/h. However, recent research paints a concerning picture. Studies reveal that storms are exceeding Category 5 wind speeds with alarming regularity.

 

The Need for Category 6:

 

    • A 2023 study published in the Proceedings of the National Academy of Sciences highlights the urgency of revising the SSHS. The research suggests storms exceeding 309 km/h are becoming more frequent, with wind speeds potentially reaching even higher levels as global warming progresses. To reflect this reality and effectively communicate the escalating risk, the authors propose introducing a Category 6 designation on the SSHS.

 

Climate Change: The Fuel Behind the Fury:

 

    • The primary culprit behind intensifying cyclones is the relentless rise in global temperatures due to greenhouse gas emissions. Warmer oceans act as a supercharger for these storms, providing the energy required for rapid intensification, extended lifespans (like Cyclone Freddy’s record-breaking 37 days in 2023), and significantly higher wind speeds. With every degree of warming, wind speeds in the strongest cyclones increase by an estimated 12%, translating to a staggering 40% increase in destructive potential.

 

The Looming Threat for India:

 

    • While the North Indian Ocean currently experiences fewer Category 5 storms compared to other regions, the future remains uncertain. Continued unabated warming significantly increases the likelihood of a Category 6 storm striking India’s coastline. This necessitates immediate action to upgrade disaster management strategies and strengthen early warning systems to safeguard lives and infrastructure.

 

Building Resilience in the Face of Adversity:

 

    • The specter of super cyclones demands a multi-pronged approach. Revisiting and revising disaster management plans is crucial, with a focus on evacuation protocols, emergency shelters, and stockpiling essential supplies. Strengthening early warning systems using advanced technology like Doppler radar can provide vital lead time for evacuations. Investing in robust coastal defenses, including seawalls, dykes, and mangrove restoration projects, can act as a first line of defense against storm surges and coastal erosion.

 

Conclusion:

 

    • The emergence of super cyclones is a stark wake-up call. Ignoring this growing threat is not an option. By acknowledging the science, adapting our preparedness strategies, and prioritizing climate change mitigation efforts, we can build resilience and protect coastal communities from the devastating consequences of these monstrous storms. The time to act is now, before the fury of a super cyclone unleashes its wrath.

 

What are Tropical cyclones?

 

Nature’s Fury: Unveiling the Power and Peril of Tropical Cyclones

 

    • Tropical cyclones, also known as hurricanes or typhoons depending on their location, are swirling storms of immense power that form over warm tropical ocean basins. These destructive weather systems unleash a devastating combination of ferocious winds, torrential rains, and storm surges, posing a significant threat to coastal communities. Let’s delve deeper into the science behind these storms and understand their impact.

 

Formation and Fuel:

 

    • Warm Waters: Tropical cyclones thrive in warm ocean environments where sea surface temperatures exceed 26.5°C (80°F). This warm water acts as fuel, providing the energy needed for the storm to form and intensify.
    • Low Pressure Systems: These storms originate from pre-existing low-pressure systems over the tropics. As warm, moist air rises from the ocean’s surface, it cools and condenses, releasing energy that fuels the storm’s development.
    • Coriolis Effect: The Earth’s rotation creates a force called the Coriolis effect, which deflects winds and sets the storm on a rotating path. This rotation gives rise to the characteristic spiral structure of a tropical cyclone.

 

Structure and Intensity:

 

Explainer: The furious eye(wall) of a hurricane or typhoon

 

    • Eye: At the center of a tropical cyclone lies a calm, relatively cloud-free area called the eye. This is due to the sinking air in the storm’s center.
    • Eyewall: Surrounding the eye is the eyewall, a ring of intense thunderstorms with the highest wind speeds and heaviest rainfall.
    • Rainbands: Beyond the eyewall lie spiral bands of heavy rain and gusty winds extending outward from the storm center.
    • Saffir-Simpson Hurricane Wind Scale: This scale categorizes tropical cyclones based on their maximum sustained wind speed. Category 5 represents the most intense storms, with winds exceeding 252 km/h (157 mph). Recent research suggests the emergence of storms exceeding these limits, prompting discussions about a potential Category 6 designation.

 

Breakdown of Tropical cyclone formation:

 

Stage 1: Heating Up

    • Imagine a vast stretch of ocean in the tropics. The relentless sun heats the ocean surface, creating warm water (over 26.5°C or 80°F). This warm water acts like a giant fuel tank.

 

Stage 2: Rise and Twist

    • Warm air is lighter than cool air, so it naturally rises from the hot ocean surface. As this warm, moist air ascends, the Earth’s rotation gives it a spin, creating a swirling motion.

 

Stage 3: Low Pressure Party

    • As the warm air rises, it leaves a bit of a gap behind, creating a zone of low pressure at the ocean’s surface. Think of it like sucking on a straw – you create low pressure in your mouth.

 

Stage 4: Feeding the Frenzy

    • This low pressure acts like a vacuum, sucking in even more warm, moist air from the surrounding areas. This influx of air further fuels the rising and spinning motion, creating a cycle.

 

Stage 5: Birth of a Cyclone
    • As the warm air continues to rise, it cools down and condenses into clouds. The combination of this rising, spinning air, warm temperatures, and low pressure creates a swirling storm – a tropical cyclone.

 

The calm area in the very center of the storm, with clear or partly cloudy skies, is called the eye. This occurs because most of the rising and spinning air is concentrated in the outer eyewall of the cyclone.

 

Impacts and Threats:

 

    • Destructive Winds: Tropical cyclones unleash powerful winds that can cause widespread damage to buildings, infrastructure, and vegetation.
    • Torrential Rainfall: These storms produce massive amounts of rain, leading to flash floods, landslides, and riverine flooding, impacting lives and property inland.
    • Storm Surges: The combination of low pressure and strong winds associated with a tropical cyclone pushes a wall of seawater towards the coast, causing devastating inundation in low-lying areas.
    • Coastal Erosion: The powerful waves and storm surges associated with these storms erode beaches and coastlines, altering landscapes and threatening coastal infrastructure.

 

Preparedness and Mitigation:

 

    • Early Warning Systems: Implementing robust early warning systems is crucial for timely evacuation and minimizing casualties. These systems utilize weather monitoring technologies and communication networks to alert communities of impending storms.
    • Coastal Defenses: Investing in coastal defenses such as seawalls, dykes, and mangrove restoration projects can provide a vital first line of defense against storm surges and coastal erosion.
    • Disaster Management Plans: Developing comprehensive disaster management plans that outline evacuation procedures, shelter arrangements, and emergency response protocols is vital to ensure a coordinated response during cyclones.
    • Climate Change Mitigation: Addressing climate change by reducing greenhouse gas emissions is crucial for mitigating the long-term trend of intensifying tropical cyclones.

 

Conclusion:

 

    • Tropical cyclones represent a significant natural hazard for coastal communities worldwide. Understanding their formation, structure, and impacts is critical for preparedness and mitigation strategies. By investing in early warning systems, coastal defenses, and disaster management plans, we can build resilience and better safeguard lives and infrastructure from the wrath of these powerful storms. Remember, knowledge is power, and being prepared is the best defense against the fury of nature.
(Source: The Hindu)

Mains Questions:

 

Question 1:

Tropical cyclones are becoming a growing threat to coastal communities worldwide. Discuss the factors contributing to the intensification of these storms and the challenges they pose. Suggest suitable mitigation strategies. (250 words)

Model Answer:

 

Factors Intensifying Tropical Cyclones:

 

    • Warming Ocean Temperatures: Rising sea surface temperatures due to climate change provide the necessary energy for tropical cyclones to form and intensify.
    • Low Pressure Systems: Pre-existing low-pressure systems in the tropics become breeding grounds for these storms.
    • Reduced Wind Shear: Weakening vertical wind shear allows for more efficient storm development and intensification.

 

Challenges Posed by Tropical Cyclones:

 

    • Destructive Winds: High winds cause widespread damage to infrastructure, buildings, and vegetation.
    • Torrential Rainfall: Heavy rains lead to flash floods, landslides, and riverine flooding, impacting lives and property.
    • Storm Surges: Rising sea levels combined with strong winds cause devastating inundation of coastal areas.
    • Coastal Erosion: Powerful waves and storm surges erode beaches and coastlines, threatening infrastructure and altering landscapes.

 

Mitigation Strategies:

    • Early Warning Systems: Implementing robust weather monitoring and communication networks to alert communities and facilitate timely evacuation.
    • Coastal Defenses: Investing in seawalls, dykes, and mangrove restoration projects to provide a first line of defense against storm surges and erosion.
    • Disaster Management Plans: Developing comprehensive plans outlining evacuation procedures, shelter arrangements, and emergency response protocols.
    • Climate Change Mitigation: Reducing greenhouse gas emissions to address the root cause of intensifying cyclones in the long term.

 

Question 2:

The Saffir-Simpson Hurricane Wind Scale (SSHS) is being challenged due to the emergence of storms exceeding its highest category. Discuss the limitations of the SSHS and the need for potential revisions. (250 words)

Model Answer:

 

Limitations of the Saffir-Simpson Hurricane Wind Scale (SSHS):

    • Categorical Ceiling: The current scale only reaches Category 5, with a maximum wind speed of 252 km/h. Recent research suggests storms exceeding these limits are becoming more frequent.
    • Focus on Wind Speed: While wind speed is a crucial factor, the SSHS doesn’t fully capture the destructive potential of a cyclone, which also depends on storm surge, rainfall intensity, and size.

 

Need for Potential Revisions:

    • Introducing a Category 6: Considering the increasing number of storms exceeding Category 5 limits, a new category with a higher wind speed threshold might be necessary.
    • Holistic Approach: Exploring ways to incorporate factors like storm surge and rainfall alongside wind speed for a more comprehensive risk assessment.

 

  • These questions highlight the growing concern regarding tropical cyclones and the need for effective strategies to address them. By understanding the science behind these storms and their evolving nature, policymakers can develop better preparedness and mitigation plans to safeguard coastal communities.

 

Remember, these are just two examples of UPSC Mains questions inspired by the upsc current affair. Feel free to modify and adapt them further to fit your specific needs and writing style. Good luck with your preparation!

Relevance to the  UPSC  Prelims and Mains syllabus under the following topics:

UPSC Prelims:

    • Prelims (General Studies Paper-I): General Geography: This section might include a question on the basic formation and characteristics of tropical cyclones. It’s unlikely to go into great detail but could test foundational knowledge.

UPSC HPAS Mains:

    • GS Paper I – Geography: This paper delves deeper into the topic. You might encounter questions on:
      The geographical factors influencing the formation and intensity of tropical cyclones (e.g., sea surface temperatures, Coriolis effect).
      The impact of tropical cyclones on coastal communities (e.g., destruction of infrastructure, storm surges, landslides).
      Mitigation strategies for reducing the risks associated with tropical cyclones (e.g., early warning systems, coastal defenses).

 

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