Meteorological history | |
---|---|
Date | 20–21 May 2020 |
Very severe cyclonic storm | |
3-minute sustained (IMD) | |
Highest winds | 155 km/h (100 mph) |
Lowest pressure | 960 hPa (mbar);28.35 inHg |
Category 2-equivalent tropical cyclone | |
1-minute sustained (SSHWS/JTWC) | |
Highest winds | 175 km/h (110 mph) |
Overall effects | |
Fatalities | 98 |
Damage | $13.5 billion (2020 USD) |
Areas affected | West Bengal,Odisha,Bangladesh |
Part of the 2020 North Indian Ocean cyclone season |
Cyclone Amphan was the costliest tropical cyclone ever recorded in India and the North Indian Ocean,and the strongest cyclone ever since the 1999 Odisha Cyclone. It was the first storm,and strongest of the historic 2020 North Indian Ocean cyclone season,the costliest recorded cyclone season. It made landfall in West Bengal with 100 mph winds. Within India,the storm killed 98 people,and caused $13.8 billion (2020 USD). Amphan produced extremely high winds that ripped roofs off houses and uprooted trees,and storm surges of 15 ft (4.6 m) in areas like Digha,West Bengal. [1] [2]
During 13 May 2020, an area of low pressure developed over the Southeastern Bay of Bengal about 1020 km (635 mi) to the southeast of Visakhapatnam in the Indian state of Andhra Pradesh. [3] [4]
Over the next couple of days, the system became more marked as it gradually consolidated further, with bands of deep atmospheric convection wrapping into the system's low-level center. [5] [6] During 16 May, the India Meteorological Department (IMD) reported that the area of low pressure had developed into a depression and designated it as BOB 01 while it was located about 1,100 km (685 mi) to the south of Paradip in the Indian state of Odisha. [7] Moving northwards, the depression continually organized and became a cyclonic storm a few hours later, receiving the name Amphan. Due to conductive environments., Amphan underwent rapid intensification into a severe cyclonic storm, with the JTWC assessing an increase in winds from 140 km/h (87 mph) at 12:00 UTC to 215 km/h (134 mph), the equivalent to a Category 4 hurricane on the Saffir–Simpson scale (SSHWS), just six hours later. [8] Furthermore, the IMD upgraded Amphan to an extremely severe cyclonic storm on their cyclone intensity scale. [9] The broad storm was characterized by a cloud shield extending more than 1,110 km (690 mi) and a sharply-outlined 10 nautical mile-wide eye. [10]
On May 18, the IMD classified Amphan as a Super Cyclonic Storm, with 3-minute sustained winds of 240 kph, reaching its peak intensity later that day. [11]
Early on May 20, Amphan went through an eyewall replacement cycle. [12] Amphan was on a weakening trend. [13] Around 5:30 p.m. IST (12:00 UTC), Amphan made landfall as a Very Severe Cyclonic storm near Bakkhali, West Bengal with winds of 155 km/h (96 mph). [14] As it moved further inland, Amphan rapidly weakened. Just six hours after landfall, the JTWC downgraded the storm to a Category 1-equivalent cyclone and issued its final warning on the system, as it became disorganized. [15] On 21 May, Amphan dissipated into a well-marked low pressure area.
The government of Odisha directed the magistrates of four districts on 15 May to establish shelter homes for possible evacuees. [16] Odisha Chief Secretary Asit Kumar Tripathy initially identified 403 possible cyclone shelters in areas potentially impacted by Amphan, though 105 served as temporary medical centres for quarantines associated with the concurrent COVID-19 pandemic. [17] Shelters could only be filled to one-third capacity to maintain social distancing guidelines due to the pandemic. [18] [19]
Social distancing restrictions in West Bengal reduced evacuation capacity in shelters from 500,000 people to 200,000 people. [20] The Kolkata Municipal Corporation located schools and community centres for possible use as temporary shelters to augment evacuation capacity. [21] [22] At least 1,704 shelters were ultimately established in Odisha and more than 2,000 were used in West Bengal, including schools and public buildings. [23] The government of West Bengal planned to evacuate 200,000 people from their homes by 18 May; [24] nearly 300,000 people evacuated in total from the state, including 200,000 from North 24 Parganas district and more than 40,000 from Sagar Island. [25] [26] [27]
The coastal districts recorded an estimated gusts of 180 km/h (110 mph). [28]
In Kolkata, reports of car being overturned, trees uprooted and downed power lines caused into havoc. Some parts of the city remained without power. The streets were waterlogged and trees blocking the roads. Some districts got power in the middle of the night after the storm had passed. The airport was remained shut and became waterlogged, many structural damages were reported. [29] Chief Minister Mamata Banerjee even stated that "a bigger disaster than Covid-19". [28] Netaji Subhash Chandra Bose Airport, Kolkata, recorded highest wind speed of 133 km/h on 20 May 2020. Other parts of Kolkata experienced wind speed of 110–130 km/h. [30]
Although the state have escaped the worst part of the cyclone, it caused significant impact in the Odisha–West Bengal border districts. It affected 4.5 million people in the state. Due to high gust winds and intense rainfall, districts like Bhadrak and Kendrapara suffered especially for the paddy farmers since the paddy fields became unsuitable for paddy cultivation which was inundated by saline water due to storm surge. According to the Odisha Government, 3 million people remained without power due to power outage and it took a while to return to normalcy whereas the roads were being cleared by the National Disaster Response Force (NDRF). In Mahakalapada and Rajanagar, around 500 acres (200 ha) of lands were destroyed also because of saline water ingression and hundreds of acres of rabi crops were destroyed in Balasore and Bhadrak district. [31]
In the Dharma Port, an estimated wind speed of 120 km/h (75 mph) were recorded while Paradip recorded only 100 km/h (60 mph). [32]
Rains and strong winds from Amphan swept across many districts in Kerala beginning on May 16. [33] Thunderstorms associated with Amphan caused severe coastal erosion in the Valiyathura suburb of Thiruvananthapuram, damaging roads and destroying homes and threatening to displace over a hundred families from their homes. [34] Strong winds inflicted severe damage in Kottayam district, especially in Vaikom taluk, where homes and temples were impacted and trees and electric poles were downed. [35]
A ₹1.47 billion (US$19.3 million) damage toll resulted from the destruction of 16 homes and the partial damage of 313 homes. [36] A high school used as a homeless shelter collapsed, causing minor injuries. [35]
Tamil Nadu faced some impact from the cyclone. Heavy winds damaged at least 100 boats anchored in the Ramanathapuram district. [37] Coastal erosion from rough seas generated by Amphan led to the collapse of three houses at Bommayarpalayam in Viluppuram district. [38] Roughly 35 acres of banana crops around Gandarvakottai and Aranthangi were destroyed. [39] Northern areas of the state have heatwave-like conditions for a week because Amphan took all of the area's moisture. [40]
In Sooradapeta, near Kakinada in Andhra Pradesh, rough seas destroyed 35 homes and damaged several others. [41]
German NGO Welthungerlife released 100,000 Euro to fund Cyclone Amphan relief efforts. [42]
On 22 May, Prime Minister Narendra Modi conducted an aerial survey over Kolkata, along with Chief Minister Mamata Banerjee. [43] Modi announced a ₹10 billion (US$132 million) immediate relief package for West Bengal and ₹5 billion (US$66.2 million) in relief for Odisha. [44] [45] In advance, Modi announced that ₹200,000 (US$2,650) would be provided to the next of kin of people who died during the storm, and ₹50,000 (US$660) would be given to each injured person. [44] West Bengal CM Banerjee stated that it would take three to four days to assess the damage. [46] Twenty disaster relief teams were dispatched by the Indian Coast Guard to begin search and rescue operations. [46] Ten teams were sent to West Bengal to aid recovery, in addition to the NDRF teams pre-positioned there before Amphan's passage. [47] Also since most of the water pumps are operated in electricity and due to no electricity, several district suffered from water shortage which caused additional protest. [48] Approximately 1,000 ground teams worked to restore infrastructure and services in West Bengal after Amphan, though only 25–30 percent of workers were staffed due to the COVID-19 pandemic. [49] The resulting slow restoration of power sparked protests across West Bengal aimed primarily at electricity company CESC. [50] Some restoration efforts were disrupted by these protests. [51] The Home Department of West Bengal requested additional crews from railway and port interest, while five brigades from the Indian Army were deployed in Kolkata and the 24 Parganas districts to support recovery efforts. [47] [50] The government of Odisha sent 500 members of its disaster rapid action force and fire service to West Bengal. [47]
The European Union stated that it would initially provide €500,000 (US$545,000) for those affected by the storm in India. [47]
Additional assistance was requested from Jharkhand and Odisha. [49] Odisha Chief Minister Naveen Patnaik performed an aerial survey of the damage in his state following Amphan. [52]
In the Indian Ocean north of the equator, tropical cyclones can form throughout the year on either side of the Indian subcontinent, although most frequently between April and June, and between October and December.
The 2005 North Indian Ocean cyclone season caused much devastation and many deaths in Southern India despite the storms’ weakness. The basin covers the Indian Ocean north of the equator as well as inland areas, sub-divided by the Arabian Sea and the Bay of Bengal. Although the season began early with two systems in January, the bulk of activity was confined from September to December. The official India Meteorological Department tracked 12 depressions in the basin, and the unofficial Joint Typhoon Warning Center (JTWC) monitored two additional storms. Three systems intensified into a cyclonic storm, which have sustained winds of at least 63 km/h (39 mph), at which point the IMD named them.
The 1992 North Indian Ocean cyclone season was unofficially the most active year on record for the basin, with 10 tropical storms developing, according to the Joint Typhoon Warning Center (JTWC). There are two main seas in the North Indian Ocean – the Bay of Bengal to the east of the Indian subcontinent – and the Arabian Sea to the west of India. The official Regional Specialized Meteorological Centre in this basin is the India Meteorological Department (IMD), while the JTWC releases unofficial advisories. An average of four to six storms form in the North Indian Ocean every season with peaks in May and November. Cyclones occurring between the meridians 45°E and 100°E are included in the season by the IMD.
The 2006 North Indian Ocean cyclone season had no bounds, but cyclones tend to form between April and December, with peaks in May and November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean.
Extremely Severe Cyclonic Storm Sidr was a tropical cyclone that resulted in one of the worst natural disasters in Bangladesh. The fourth named storm of the 2007 North Indian Ocean cyclone season, Sidr formed in the central Bay of Bengal, and quickly strengthened to reach peak 1-minute sustained winds of 260 km/h (160 mph), making it a Category-5 equivalent tropical cyclone on the Saffir–Simpson scale. The storm eventually made landfall in Bangladesh on November 15, 2007, causing large-scale evacuations. At least 3,447 deaths have been blamed on the storm, with some estimates reaching 15,000.
The 2000 North Indian Ocean cyclone season was fairly quiet compared to its predecessor, with all of the activity originating in the Bay of Bengal. The basin comprises the Indian Ocean north of the equator, with warnings issued by the India Meteorological Department (IMD) in New Delhi. There were six depressions throughout the year, of which five intensified into cyclonic storms – tropical cyclones with winds of 65 mph (105 km/h) sustained over 3 minutes. Two of the storms strengthened into a Very Severe Cyclonic Storm, which has winds of at least 120 km/h (75 mph), equivalent to a minimal hurricane. The Joint Typhoon Warning Center (JTWC) also tracked storms in the basin on an unofficial basis, estimating winds sustained over 1 minute.
The 1995 North Indian Ocean cyclone season was below-average and was primarily confined to the autumn months, with the exception of three short-lived deep depressions in May. There were eight depressions in the basin, which is Indian Ocean north of the equator. The basin is subdivided between the Bay of Bengal and the Arabian Sea on the east and west coasts of India, respectively. Storms were tracked by the India Meteorological Department (IMD), which is the basin's Regional Specialized Meteorological Center, as well as the American-based Joint Typhoon Warning Center (JTWC) on an unofficial basis.
India is a country in the north of Indian Ocean that is the most vulnerable to getting hit by tropical cyclones in the basin, from the east or from the west. On average, 2–3 tropical cyclones make landfall in India each year, with about one being a severe tropical cyclone or greater.
The 2002 West Bengal cyclone was a deadly tropical cyclone that affected India and Bangladesh in November 2002. The sixth tropical cyclone and fourth cyclonic storm of the 2002 North Indian Ocean cyclone season, it developed in the Bay of Bengal northeast of Sri Lanka on November 10, as a tropical depression. After tracking northeast, the system strengthened into a cyclonic storm on November 11, as maximum sustained winds exceeded 65 km/h (40 mph). On November 12, it further intensified into a severe cyclonic storm. Later that day, the storm made landfall on Sagar Island in West Bengal with winds of 100 km/h (60 mph). After moving inland, it rapidly weakened and dissipated over Bangladesh on November 12.
The 2017 North Indian Ocean cyclone season was a below average yet deadly season in the annual cycle of tropical cyclone formation. This season produced only three named storms, of which one only intensified into a very severe cyclonic storm. The North Indian Ocean cyclone season has no official bounds but cyclones tend to form between April and December with the two peaks in May and November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. The season began with the formation Cyclone Maarutha on April 15 and ended with the dissipation of a deep depression on December 9.
The 2018 North Indian Ocean cyclone season was one of the most active North Indian Ocean cyclone seasons since 1992, with the formation of fourteen depressions and seven cyclones. The North Indian Ocean cyclone season has no official bounds, but cyclones tend to form between April and December, with the two peaks in May and November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean.
The 2020 North Indian Ocean cyclone season was the costliest North Indian Ocean cyclone season on record, mostly due to the devastating Cyclone Amphan. The North Indian Ocean cyclone season has no official bounds, but cyclones tend to form between April and November, with peaks in late April to May and October to November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. The season began on May 16 with the designation of Depression BOB 01 in the Bay of Bengal, which later became Amphan. Cyclone Amphan was the strongest storm in the Bay of Bengal in 21 years and would break Nargis of 2008's record as the costliest storm in the North Indian Ocean. The season concluded with the dissipation of Cyclone Burevi on December 5. Overall, the season was slightly above average, seeing the development of five cyclonic storms.
Extremely Severe Cyclonic Storm Fani was the worst tropical cyclone to strike the Indian state of Odisha since the 1999 Odisha cyclone. The second named storm and the first severe cyclonic storm of the 2019 North Indian Ocean cyclone season, Fani originated from a tropical depression that formed west of Sumatra in the Indian Ocean on 26 April. Vertical wind shear at first hindered the storm's development, but conditions became more favorable for Fani on 30 April. Fani rapidly strengthened, peaking at Category 5-equivalent intensity with winds of 280 km/h, tying with Cyclone Mocha as the strongest storm on record in the north Indian Ocean, in terms of 1-minute sustained winds. Fani slightly weakened before making landfall, and its convective structure rapidly degraded thereafter, degenerating into a remnant low on 4 May, and dissipating on the next day. It was succeeded by Cyclone Amphan in 2020 which caused a greater overall damage.
Cyclone Matmo–Bulbul is the unofficial collective designation given to both Severe Tropical Storm Matmo and Very Severe Cyclonic Storm Bulbul, which were a pair of destructive tropical cyclones that tracked in the Western Pacific Ocean and the North Indian Ocean in October and November 2019 respectively, killing 43 people and inflicting about US$3.537 billion in damage. Matmo was the 41st tropical depression and the 22nd named storm of the 2019 Pacific typhoon season, while Bulbul was the 9th depression and the 7th named storm of the 2019 North Indian Ocean cyclone season. The cyclone formed on October 28 in the South China Sea and intensified into Tropical Storm Matmo, as named by the Japan Meteorological Agency (JMA). On October 30, the storm made landfall in central Vietnam, causing flooding. Matmo weakened while moving westward across Mainland Southeast Asia, before degenerating into a remnant low later that day. The remnants of Matmo emerged into the Bay of Bengal, redeveloping into a depression on November 5. Late the next day, it strengthened into a cyclonic storm, renamed Bulbul by the India Meteorological Department (IMD), although the JTWC continued to refer to it as Matmo. The storm peaked on November 8, with maximum sustained winds 140 km/h (85 mph) estimated by the IMD. On November 9, the cyclone made its final landfall in the eastern Indian state of West Bengal, and around that time the storm turned to the northeast, moving into Bangladesh. The system degenerated into a remnant low two days later, over northeastern India.
Super Cyclonic Storm Amphan was an extremely powerful and catastrophic 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 also the fourth super cyclone that hit West Bengal and Kolkata since 2015 as well as being one of the strongest storms to impact the area. Causing over US$13 billion of damage, Amphan is also the costliest cyclone ever recorded in the North Indian Ocean, surpassing the record held by Cyclone Nargis of 2008.
Severe Cyclonic Storm Nisarga was the strongest tropical cyclone to strike the Indian state of Maharashtra in the month of June since 1891. It was also the first cyclone to impact Raigad & Mumbai since Phyan of 2009. The third depression and second named cyclone of the 2020 North Indian Ocean cyclone season, Nisarga originated as a depression in the Arabian Sea and moved generally northward. On 2 June, the India Meteorological Department (IMD) upgraded the system to a cyclonic storm, assigning the name Nisarga. On the next day, Nisarga further intensified to a severe cyclonic storm and turned to the northeast, ultimately making landfall approximately 95 km (60 mi) south of Mumbai. Nisarga rapidly weakened once inland and dissipated on 4 June.
Very Severe Cyclonic Storm Titli was a deadly and destructive tropical cyclone that caused extensive damage to Eastern India in October 2018. Titli was the twelfth depression and fifth named storm to form in the 2018 North Indian Ocean cyclone season. Titli originated from a low pressure area in the Andaman Sea on October 7. With warm sea surface temperatures and low wind shear, the low developed into a depression on October 8 in the central Bay of Bengal. It was tracked and followed by the India Meteorological Department (IMD), which also issued warnings and notices for the public. Titli continued to intensify at it moved toward the southeast Indian coast, becoming a very severe cyclonic storm, equivalent to a minimal hurricane on the Saffir–Simpson scale. It attained the intensity at the same time Cyclone Luban in the Arabian Sea was at the same intensity, marking the first instance since 1977 of simultaneous storms. The IMD estimated peak winds of 150 km/h (95 mph), while the American-based Joint Typhoon Warning Center (JTWC) estimated peak winds of 195 km/h (120 mph). Late on October 10, Titli made landfall in Andhra Pradesh, and it quickly weakened over land as it turned to the northeast. It degenerated into a remnant low on October 12.
The effects of the 2020 North Indian Ocean cyclone season in India was considered one of the worst in decades, largely due to Super Cyclonic Storm Amphan. Throughout most of the year, a series of cyclones impacted the country, with the worst damage occurring in May, from Cyclone Amphan. The season started with Super Cyclonic Storm Amphan, which affected East India with very severe damages. 98 total people died from the storm. Approximately 1,167 km (725 mi) of power lines of varying voltages, 126,540 transformers, and 448 electrical substations were affected, leaving 3.4 million without power. Damage to the power grid reached ₹3.2 billion. Four people died in Odisha, two from collapsed objects, one due to drowning, and one from head trauma. Across the ten affected districts in Odisha, 4.4 million people were impacted in some way by the cyclone. At least 500 homes were destroyed and a further 15,000 were damaged. Nearly 4,000 livestock, primarily poultry, died. The cyclone was strongest at its northeast section. The next storm was a depression that did not affect India. Then Severe Cyclonic Storm Nisarga hit Maharashtra, with high damages. Nisarga caused 6 deaths and 16 injuries in the state. Over 5,033 ha of land were damaged.
Very Severe Cyclonic Storm Yaas was a relatively strong and very damaging tropical cyclone that made landfall in Odisha and brought significant impacts to West Bengal during late May 2021. The second cyclonic storm, second severe cyclonic storm, and second very severe cyclonic storm of the 2021 North Indian Ocean cyclone season, Yaas formed from a tropical disturbance that the Indian Meteorological Department first monitored on May 23. Conditions in the basin favored development as the system became a deep depression later that day, before intensifying into a cyclonic storm on the next day, receiving the name Yaas. The system further intensified as it turned to the northeast, becoming a severe cyclonic storm on May 24 despite moderate wind shear. Marginally favorable conditions further continued as Yaas accelerated northeastward, strengthening to a Category 1-equivalent tropical cyclone and to a very severe cyclonic storm on May 25. Yaas crossed the northern Odisha coast around 20 km south of Balasore at its peak intensity as a very severe cyclonic storm on May 26. Upon landfall, the JTWC and IMD issued their final advisories as Yaas further weakened inland while turning north-northwestwards.
Cyclonic Storm Jawad was a weak tropical cyclone that caused disruptions over the East India and Bangladesh while bringing heavy rainfall and strong winds over these states as a weakened system. The tenth depression, sixth deep depression and fifth cyclonic storm of the active 2021 North Indian Ocean cyclone season, its predecessor was first tracked by Joint Typhoon Warning Center (JTWC) in the South China Sea as an area of low pressure. It then moved west-northwestwards into the Gulf of Thailand, where it crossed into the Andaman Sea by December 1. Near midnight of that day, the JTWC issued a TCFA on the system and on the next day, the India Meteorological Department (IMD) upgraded the system to a depression after passing through the Nicobar Islands. Further intensification ensued as the depression tracked through environmental conditions favorable for strengthening, and the system was upgraded into a deep depression on December 3 and into a cyclonic storm by 06:00 UTC that day, with the IMD naming it Jawad. However, this intensification was short-lived, as the system weakened to a deep depression back due to wind shear.