CYCLONES IN INDIA
Cyclone Name | Location | Landfall Date | Impact and Path |
Cyclone Jasper | Northeastern Australia | December 13, 2023 | - Damaging winds and heavy rainfall leading to flash flooding. - Thousands of homes and businesses without power. |
Cyclone Michaung | Andhra Pradesh, India | December 5, 2023 | - Strong winds and heavy rainfall causing damage to infrastructure and loss of lives. |
Cyclone ‘Midhili’ | Bangladesh coast | November 17, 2023 | - Made landfall with heavy rain and winds. - Impact includes inundation of villages and disruption of services. |
Cyclone ‘Hamoon’ | Southeastern coast of Bangladesh | October 25, 2023 | - Evacuation of thousands due to severe weather conditions. - Raised concerns about climate change impacts. |
Cyclone Tej | Arabian Sea, potential impact on Mumbai, Pune | Forecasted around October 21, 2023 | - IMD issued a cautionary notice about a potential cyclonic storm. - Uncertainty about evolution into a cyclonic storm. |
Cyclone Biparjoy | Gujarat, India | June 15, 2023 | - Landfall with strong winds and heavy rains causing casualties and damage to infrastructure. |
Cyclone Fabien | Southeast of Diego Garcia | April 17, 2023 | - Tropical cyclone with significant wind speeds and gusts. - Movement towards the southwest direction. |
Cyclone Mocha | Bay of Bengal, landfall in Bangladesh | May 14, 2023 |
- Very severe cyclonic storm causing widespread damage and casualties in Bangladesh and Myanmar.
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Cyclone Mandous | Andaman and Nicobar Islands, Chennai coast | December 14, 2022 |
Severe cyclonic storms hit coastal areas, causing disruptions and damage.
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Cyclone Sitrang | Assam, Odisha, West Bengal, Andaman and Nicobar Islands | October 22-25, 2022 |
Weak tropical cyclone impacting multiple states with heavy rains and localized damage.
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Cyclone Asani | Andhra Pradesh, Tamil Nadu, Karnataka, Odisha | May 7-12, 2022 |
The first cyclonic storm of 2022 caused severe rainfall and flooding in several states.
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Cyclone Jawad | Odisha, Andhra Pradesh | Expected, Not Yet Landfall |
The deep depression over the Bay of Bengal likely to intensify into a cyclonic storm, causing potential disruptions and evacuations.
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Cyclone Gulaab | North Andhra Pradesh, Odisha coasts | September 25, 2021 |
Impacting coastal regions with warnings issued by IMD for precautionary measures.
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Cyclone Tauktae | Southern Gujarat, Saurashtra | May 17, 2021 |
Very Severe Cyclonic Storm causing significant damage and casualties across Gujarat and neighbouring states.
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Cyclone Yaas | West Bengal, Odisha coasts | May 2021 |
Cyclonic storm hitting coastal areas with preparations and evacuations conducted beforehand.
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Cyclone Nisarga | Alibag, Mumbai | June 2020 |
Impacting Mumbai and surrounding areas, causing deaths, injuries, and infrastructure damage.
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Cyclone Amphan | Odisha, West Bengal | May 2020 |
Super cyclone causing widespread destruction in Odisha and West Bengal.
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Cyclone Kyarr | Western India, Oman, UAE, Socotra, Somalia | October 2019 |
Strong tropical cyclone affecting multiple countries in the region.
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Cyclone Maha | Gujarat, Indian coast | November 2019 |
Extremely severe cyclonic storms affect coastal areas with strong winds and heavy rainfall.
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Cyclone Vayu | Gujarat, Maldives, Pakistan, Oman | June 2019 |
Very severe cyclonic storm causing moderate damage in Gujarat and other regions.
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Cyclone Hikka | Oman, Arabian Sea | September 2019 |
Intense cyclonic storm impacting Oman and regions along the Arabian Sea.
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Cyclone Fani | Odisha, West Bengal, Andhra Pradesh, East India | May 2019 |
The strongest tropical storm affected Odisha and surrounding states, causing widespread destruction.
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Cyclone Bulbul | West Bengal, Bangladesh | 09 NOV 2019 |
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Cyclones, also known as hurricanes or typhoons depending on the region, are powerful tropical storms characterized by low-pressure centres, strong winds, and heavy rainfall. These storms form over warm ocean waters near the equator and are fueled by the heat and moisture from the ocean surface.
- Cyclones typically form over warm ocean waters with sea surface temperatures of at least 26.5°C (79.7°F). As the warm, moist air near the surface rises, it creates an area of low pressure. This low-pressure system then draws in more warm air from the surrounding area, causing the air to spiral upward and form clouds.
- Cyclones consist of several key components, including the eye, eyewall, and rainbands. The eye is a circular area of calm and relatively clear skies at the centre of the storm. Surrounding the eye is the eyewall, which contains the strongest winds and heaviest rainfall. Rainbands extend outward from the eyewall and produce additional rain and wind.
- Cyclones are classified based on their maximum sustained wind speeds. The Saffir-Simpson Hurricane Wind Scale is commonly used to categorize cyclones into five categories, ranging from Category 1 (winds of 74-95 mph) to Category 5 (winds of 157 mph or higher).
- Cyclones can have devastating impacts on coastal areas and inland regions. The strong winds, heavy rainfall, storm surges, and flooding associated with cyclones can cause widespread damage to infrastructure, homes, and crops. They can also result in loss of life and displacement of populations.
- Cyclones typically occur during specific seasons in different parts of the world. For example, the Atlantic hurricane season runs from June 1 to November 30, while the Pacific typhoon season generally occurs from May to October. In the Southern Hemisphere, cyclone seasons often occur during the summer months.
- Meteorological agencies use satellites, radar, and computer models to track the formation and movement of cyclones. Advanced warning systems allow authorities to issue alerts and evacuation orders to help communities prepare for and respond to cyclone threats.
- There is evidence to suggest that climate change may influence the frequency, intensity, and distribution of cyclones. Warmer ocean temperatures can provide more energy to fuel cyclone development, potentially leading to stronger storms. However, the relationship between climate change and cyclones is complex and subject to ongoing research.
3. Causes of Cyclones in India and Worldwide
- Cyclones are often triggered by unstable atmospheric conditions. When warm, moist air rises rapidly, it creates an area of low pressure at the surface. This instability can lead to the formation of convective clouds and thunderstorms, which are the initial stages of cyclone development.
- Wind shear refers to the change in wind speed and direction with altitude. Low wind shear allows cyclones to maintain their structure and intensify. Vertical wind shear, where winds change significantly with height, can disrupt cyclone formation and weaken existing storms.
- Cyclones draw their energy from warm ocean waters. Sea surface temperatures of at least 26.5°C (79.7°F) are generally needed to fuel cyclone development. Warmer waters provide more moisture and heat to the atmosphere, enhancing the instability that drives cyclone formation.
- Cyclones often originate from pre-existing disturbances, such as tropical waves or areas of low pressure. These disturbances can evolve into organized systems under favourable atmospheric conditions, leading to cyclone formation.
- The Coriolis effect, caused by the Earth's rotation, plays a crucial role in cyclone formation. In the Northern Hemisphere, the Coriolis force deflects moving air to the right, creating cyclonic circulation around areas of low pressure. In the Southern Hemisphere, the deflection is to the left.
- High humidity in the lower to middle levels of the troposphere contributes to cyclone development. Moisture-laden air rising from the ocean surface cools and condenses, releasing latent heat and further fueling the storm's convective processes.
Understanding these key factors helps meteorologists predict and monitor cyclone formation, providing valuable information for disaster preparedness and response efforts in vulnerable regions like India and around the world.
4. Types of Cyclones
Tropical Cyclones
Tropical cyclones are intense low-pressure systems that form over warm ocean waters near the equator. They are characterized by strong winds rotating around a central eye, with a well-defined circulation pattern. Tropical cyclones are further categorized based on their intensity.
- Tropical cyclones are characterized by rotating clouds and thunderstorms over tropical or subtropical areas.
- They have very high wind velocity and heavy rainfall.
- Movement is directed from east to west.
- Form only overseas with temperatures above 26-27 degrees Celsius and dissipate upon reaching land.
- Duration typically lasts 5-7 days.
Extratropical/Temperate/Frontal Cyclones
Extratropical cyclones, also known as mid-latitude cyclones or temperate cyclones, form outside the tropics, usually in higher latitudes. They derive their energy from temperature contrasts between air masses rather than warm ocean waters. Extratropical cyclones often bring heavy precipitation, strong winds, and temperature changes.
- Also known as Midlatitude Cyclones, these cyclones originate from temperate and high-latitude regions within 30 to 60 degrees.
- Characterized by cold fronts, warm fronts, and occluded fronts.
- Move from west to east.
- Air velocity is comparatively lower compared to tropical cyclones.
- Form over both land and sea.
- Duration typically lasts for 15-20 days.