
A tropical cyclone is a storm system characterized by a large low-pressure center, a closed low-level circulation and a spiral arrangement of numerous thunderstorms that produce strong winds and heavy rainfall. Tropical cyclones feed on the heat released when moist air rises, resulting in condensation of water vapor contained in the moist air. They are fueled by a different heat mechanism than other cyclonic windstorms such as Nor'easters, European windstorms and polar lows, leading to their classification as "warm core" storm systems. Most tropical cyclones originate in the doldrums, approximately ten degrees from the Equator.
The term "tropical" refers to both the geographic origin of these systems, which form almost exclusively in tropical regions of the globe, as well as to their formation in maritime tropical air masses. The term "cyclone" refers to such storms' cyclonic nature, with anticlockwise rotation in the Northern Hemisphere and clockwise rotation in the Southern Hemisphere. Depending on its location and intensity, a tropical cyclone may be referred to by names such as "hurricane", "typhoon", "tropical storm", "cyclonic storm", "tropical depression" or simply "cyclone".
Types of cyclone: 1. A "Typhoon" is a tropical cyclone located in the North-west Pacific Ocean which has the most cyclonic activity and storms occur year-round. 2. A "Hurricane" is also a tropical cyclone located at the North Atlantic Ocean or North-east Pacific Ocean which have an average storm activity and storms typically form between May 15 and November 30. 3. A "Cyclone" is a tropical cyclone that occurs in the South Pacific and Indian Oceans.
Super Cyclonic Storm Amphan was an extremely powerful and devastating tropical cyclone that caused widespread damage in Eastern India, specifically in West Bengal and Odisha, and in Bangladesh, in May 2020. It was the strongest tropical cyclone to strike the Ganges Delta. It was the strongest tropical cyclone to hit India since 1999. It was a rare cyclone that lashed northern Bangladesh from Rajshahi to Rangpur in the early hours of 21 May with strong winds. It caused severe damage to mango production of Rajshahi and Rangpur. It was also the fourth super cyclone that hit West Bengal and Kolkata, causing at least 133 fatalities and forcing the evacuation of over 4 million people. The storm severely disrupted power and telecommunication networks, leaving Kolkata and surrounding rural districts (such as North 24 Parganas and South 24 Parganas) without electricity for over a week, while storm surges breached coastal embankments and caused extensive saltwater intrusion in the Sundarbans. Causing over US$15 billion of damage, Amphan was also the costliest cyclone ever recorded in the North Indian Ocean, until it was surpassed by Cyclone Senyar in 2025.
The first tropical cyclone of the 2020 North Indian Ocean cyclone season, Amphan originated from a low-pressure area persisting a couple of hundred miles (300 km) east of Colombo, Sri Lanka, on 13 May 2020. Tracking northeastward, the disturbance organized over exceptionally warm sea surface temperatures; the Joint Typhoon Warning Center (JTWC) upgraded the system to a tropical depression on 15 May while the India Meteorological Department (IMD) followed suit the following day. On 17 May, Amphan underwent rapid intensification and became an extremely severe cyclonic storm within 12 hours. On 18 May, at approximately 12:00 UTC, Amphan reached its peak intensity with 3-minute sustained wind speeds of 240 km/h (150 mph), 1-minute sustained wind speeds of 270 km/h (165 mph), and a minimum central barometric pressure of 920 mbar (27.17 inHg). The storm began an eyewall replacement cycle shortly after it reached its peak intensity, but the continued effects of dry air and wind shear disrupted this process and caused Amphan to gradually weaken as it paralleled the eastern coastline of India. On 20 May, 12:00 UTC, the cyclone made landfall in West Bengal, near Bakkhali, generating a storm surge of 2.5 to 5 metres (8.2 to 16.4 ft). At the time, the JTWC estimated Amphan's 1-minute sustained winds to be 175 km/h (110 mph). Amphan rapidly weakened once inland and dissipated shortly thereafter. (Full article...)

The radius of maximum wind (RMW) is the distance between the center of a cyclone and its band of strongest winds. It is a parameter in atmospheric dynamics and tropical cyclone forecasting. The highest rainfall rates occur near the RMW of tropical cyclones. The extent of a cyclone's storm surge and its maximum potential intensity can be determined using the RMW. As maximum sustained winds increase, the RMW decreases. Recently, RMW has been used in descriptions of tornadoes. When designing buildings to prevent against failure from atmospheric pressure change, RMW can be used in the calculations. (Full article...)


The 2020 Atlantic hurricane season was the most active Atlantic hurricane season in recorded history in terms of the total number of tropical and subtropical cyclones, with 31 such systems forming throughout the season and all but one becoming a named storm, breaking the previous record set in 2005. Of the 30 named storms, 14 developed into hurricanes, and a record-tying seven further intensified into major hurricanes. It was, after the aforementioned 2005 season, the second and final season to use the Greek letter storm naming system. 11 of the 30 named storms made landfall in the contiguous United States, breaking the record of nine set in 1916. During the season, 27 tropical storms established a new record for earliest formation date by storm number. This season also featured a record ten tropical cyclones that underwent rapid intensification, tying it with 1995, as well as tying the record for most Category 4 hurricanes in a singular season in the Atlantic basin. This unprecedented activity was fueled by a La Niña that developed in the summer months of 2020, continuing a stretch of above-average seasonal activity that began in 2016. Despite the record-high activity, this was the first season since 2015 in which no Category 5 hurricanes formed.
The season officially started on June 1 and officially ended on November 30. These dates, adopted by convention, delineate the period of the calendar year during which tropical cyclogenesis most often occurs. However, the formation of tropical and subtropical systems is possible at any time of the year, as demonstrated by the early formation of Tropical Storms Arthur and Bertha, on May 16 and 27, respectively. This was the sixth consecutive year with a pre-season system and the second of these seasons to have two, with the other being 2016. The first hurricane, Hurricane Hanna, made landfall in Texas on July 25. Hurricane Isaias formed on July 31, and made landfall in the Bahamas and North Carolina in early August, both times as a Category 1 hurricane; Isaias caused $4.8 billion in damage overall. In late August, Laura made landfall in Louisiana as a Category 4 hurricane, becoming the strongest tropical cyclone on record in terms of wind speed to make landfall in the state, alongside the 1856 Last Island hurricane and Ida. Laura caused at least $19 billion in damage and 77 deaths. September was the most active month on record in the Atlantic, with ten named storms. Slow-moving Hurricane Sally impacted the United States Gulf Coast, causing severe flooding. The Greek alphabet was used for only the second and final time, starting on September 17 with Subtropical Storm Alpha, which made landfall in Portugal on the following day. (Full article...)

Italicized basins are unofficial.
Last updated: 16:17, 24 October 2026 (UTC)

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The 1996 Atlantic hurricane season consisted of the events that occurred in the annual cycle of tropical cyclone formation over the Atlantic Ocean north of the equator. The official bounds of each Atlantic hurricane season are dates that conventionally delineate the period each year during which tropical cyclones tend to form in the basin according to the National Hurricane Center, beginning on June 1 and ending on November 30. However, tropical cyclogenesis is possible at any time of the year. Activity during the season was above average; thirteen named storms developed, with nine becoming hurricanes and six further strengthening into major hurricanes. The first system, Tropical Storm Arthur, formed on June 17; the last, Hurricane Marco, dissipated on November 26.
The season's most destructive storms were Hurricane Cesar, Hurricane Fran, and Hurricane Hortense. Hurricane Cesar (later known as Hurricane Douglas in the Eastern Pacific basin) was the deadliest storm of the season; it killed at least 51 people and caused severe damage in northern Colombia and southern Central America. Hurricane Fran caused $3.2 billion (1996 USD) worth of damage in the United States, mostly in North Carolina, and killed 26 people. Hurricane Hortense dropped torrential rainfall on southwestern Puerto Rico and the eastern Dominican Republic, killing 21 people and leaving behind $127 million (1996 USD) in damage. (Full article...)
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