Meteorological history | |
---|---|
Formed | May 17,2010 |
Dissipated | May 21,2010 |
Severe cyclonic storm | |
3-minute sustained (IMD) | |
Highest winds | 100 km/h (65 mph) |
Lowest pressure | 986 hPa (mbar);29.12 inHg |
Category 1-equivalent tropical cyclone | |
1-minute sustained (SSHWS/JTWC) | |
Highest winds | 120 km/h (75 mph) |
Lowest pressure | 974 hPa (mbar);28.76 inHg |
Overall effects | |
Fatalities | 65 total |
Damage | $117 million (2010 USD) |
Areas affected | Sri Lanka,India |
IBTrACS | |
Part of the 2010 North Indian Ocean cyclone season |
Severe Cyclonic Storm Laila was the first cyclonic storm to affect southeastern India in May since the 1990 Andhra Pradesh cyclone. The first tropical cyclone of the annual season,Laila developed on May 17,2010 in the Bay of Bengal from a persistent area of convection. Strengthening as it tracked northwestward,it became a severe cyclonic storm on May 19. The next day,Laila made landfall in Andhra Pradesh,and it later dissipated over land. It caused flooding and damage along its path. Laila is an Urdu/Arabic name,meaning Night. It was the worst storm to hit Andhra Pradesh in the last 14 years.
In the middle of May 2010, an area of convection, or thunderstorms, persisted about 865 miles (1400 km) south of the Indian city of Kolkata (formerly Calcutta) in the Bay of Bengal. It was initially disorganized, although satellite imagery indicated a mid-level circulation. [1] After a few days, the convection began consolidating around a developing low-level circulation, and rainbands became evident. With low amounts of wind shear in the region, the Joint Typhoon Warning Center (JTWC) assessed its chances of development as fair. [2] The official warning agency in the basin – the India Meteorological Department (IMD) – classified the system as Depression BOB 001 at 0900 UTC on May 17. [3] About three hours after the depression was first classified, the IMD upgraded the system to a deep depression, indicating sustained winds of at least 34 mph (55 km/h). [4]
Late on May 17, the JTWC classified the system as Tropical Cyclone 01B, based on further organization. By that time, it was located about 485 miles (780 km) east-southeast of Chennai, Tamil Nadu, and was moving westward due to its position southwest of the subtropical ridge. [5] The IMD upgraded the deep depression to Cyclonic Storm Laila early on May 18. [6] With further consolidation of the convection throughout the day, the JTWC noted that the storm "[appeared] to be rapidly intensifying", which is a term referring to a quick drop in barometric pressure that usually coincides with a sharp increase in winds. By late on May 18, an eye feature became evident on satellite imagery, [7] and at 0000 UTC on May 19, the JTWC assessed Laila as producing peak winds of 75 mph (120 km/h), the equivalent of a minimal hurricane. [8] A few hours later, the IMD upgraded Laila to a severe cyclonic storm. [9]
After reaching peak intensity, Laila briefly decelerated as it moved around tan increasing, and the cyclone began weakening as it remained just off the coast. [10] Between 1100 and 1200 UTC on May 20, Laila made landfall near Bapatla, Andhra Pradesh. [11]
Death toll | ||
---|---|---|
Region | Total deaths | Source(s) |
Sri Lanka | 20 | [12] |
Andhra Pradesh | 36 | [13] |
Tamil Nadu | 9 | [14] |
Totals: | 65 |
Cyclone Laila displaced nearly 280,000 people, triggering floods, delaying flights and submerging many areas of capital Colombo. The indirect impact of the cyclone was compounded as heavy pre-monsoonal showers set in over parts of the country as the storm developed over the Bay of Bengal. The Sri Lanka air force helicopters and navy vessels were pressed into service to ferry stranded passengers from Colombo to the international airport after parts of the connecting roads were washed away. All international and domestic flights were either delayed or cancelled because of heavy rain. Colombo experienced 350 mm of rain over the last five days ending May 20. [15]
Thousands of passengers were also stranded after railway tracks were flooded across the country. Several train stations had to suspend operations. The Lankan Parliament, located in a Colombo suburb, was adjourned after an adjoining lake threatened to overflow and flood the premises. The weather conditions experienced were caused after Sri Lanka was hit by 'feeder bands' (clouds on the outer spirals of a cyclone but connected to its centre) of the cyclone as it moved up the Indian east coast. [16]
Early in the duration of the cyclone, the IMD noted the potential for heavy rainfall and gusty winds along the coast of Andhra Pradesh. The agency advised fishermen to avoid being in open seas. Additionally, the agency contacted state governments in the region to warn of the storm's threat. [4] The weather office has stated that the cyclone will not have an effect on the monsoon season. [17]
Cyclone Laila battered Ongole town; it received heavy rain of 320 mm on May 20 and 142 mm on May 21, and has made rivulets like Gundlakamma, Addavagu and Pothurajukalva swollen. Addanki received the highest rainfall of 522 mm, followed by Maddipadu with 510 mm and Kothapatnam 258 mm in 24 hours on May 21. [18]
The cyclone caused heavy destruction in Prakasam, Krishna and Guntur districts and preliminary reports prepared by the State government put the loss at over Rs 500 crore. [19] According to a BBC report, Cyclone Laila was the worst storm to hit Andhra Pradesh in 14 years. [20]
Nine people were killed in rain related incidents in Tamil Nadu, as the cyclonic storm "Laila" battered the Coastal areas in Northern parts of Tamil Nadu, Chennai city and its suburbs. [14]
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 2008 North Indian cyclone season was one of the most disastrous tropical cyclone seasons in modern history, causing more than 140,000 fatalities and over US$15 billion in damage. At the time, it was the costliest season in the North Indian Ocean, until it was surpassed by 2020. The season has no official bounds but cyclones tend to form between April and December. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean. There are two main seas in the North Indian Ocean—the Bay of Bengal, which is east of India, and the Arabian Sea, which is west of India. The official Regional Specialized Meteorological Centre in this basin is the India Meteorological Department (IMD), however the Joint Typhoon Warning Center releases unofficial advisories for military interests. An average of four to six storms form in the North Indian Ocean every season. Cyclones occurring between the meridians 45°E and 100°E are included in the season by the IMD.
The 2003 North Indian Ocean cyclone season was the last season that tropical cyclones were not publicly labeled by India Meteorological Department (IMD). Also was mostly focused in the Bay of Bengal, where six of the seven depressions developed. The remaining system was a tropical cyclone that developed in the Arabian Sea in November, which was also the only system that did not affect land. There were three cyclonic storms, which was below the average of 4–6. Only one storm formed before the start of the monsoon season in June, although it was also the most notable. On May 10, a depression formed in the central Bay of Bengal, and within a few days became a very severe cyclonic storm. After it stalled, it drew moisture from the southwest to produce severe flooding across Sri Lanka, killing 254 people and becoming the worst floods there since 1947. Damage on the island totaled $135 million (2003 USD). The storm eventually made landfall in Myanmar on May 19. It is possible that the storm contributed to a deadly heat wave in India due to shifting air currents.
The 2002 North Indian Ocean cyclone season was a below average season in terms of tropical cyclone formation. The season had no official bounds, but most storms formed in either May or after October. No depressions or storms formed during the monsoon season from July to September, the first such instance on record. 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 Joint Typhoon Warning Center (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 2000 North Indian Ocean cyclone season was fairly quiet compared to the year before, 1999 North Indian Ocean cyclone season, 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 1990 North Indian Ocean cyclone season featured a below average total of twelve cyclonic disturbances and one of the most intense tropical cyclones in the basin on record. During the season the systems were primarily monitored by the India Meteorological Department, while other warning centres such as the United States Joint Typhoon Warning Center also monitored the area. During the season, there were at least 1,577 deaths, while the systems caused over US$693 million in damages. The most significant system was the 1990 Andhra Pradesh cyclone, which was the most intense, damaging, and the deadliest system of the season.
The 2008 North Indian Ocean cyclone season officially ran throughout the year during 2008, with the first depression forming on April 27. The timeline includes information that was not operationally released, meaning that information from post-storm reviews by the Joint Typhoon Warning Center (JTWC), and the India Meteorological Department (IMD), such as information on a storm that was not operationally warned on. This timeline documents all the storm formations, strengthening, weakening, landfalls, extratropical transitions, as well as dissipation's during the 2008 North Indian Ocean cyclone season.
The 1991 North Indian Ocean Cyclone season was an extremely deadly and destructive season causing the deaths of more than 138,000 people and over $1.5 billion in damages. It was the period in which tropical cyclones formed to the north of the equator in the Indian Ocean. During the season tropical cyclones were monitored by the India Meteorological Department (IMD) and the Joint Typhoon Warning Center. The IMD assigned all depressions that it monitored with BOB followed by a number in numerical order. The JTWC also assigned a number and either the letter A or B depending on where the depression was when the first advisory was issued.
The 2009 North Indian Ocean cyclone season was an event in the annual cycle of tropical cyclone formation. The North Indian Ocean cyclone season has no official 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.
The 2010 North Indian Ocean cyclone season was one of the most active tropical cyclone season in the North Indian Ocean since 1998. The season saw 8 depressions and 5 named storms forming in the region.
Cyclonic Storm Phyan developed as a tropical disturbance to the southwest of Colombo in Sri Lanka on November 4, 2009. Over the next couple of days, the disturbance gradually developed before weakening as it made landfall on Southern India on November 7. After the disturbance emerged into the Arabian Sea, it rapidly became more of a concern to the India Meteorological Department (IMD) reporting early on November 9 that the disturbance had intensified into a Depression, and designated it as Depression ARB 03 whilst the Joint Typhoon Warning Center (JTWC) issued a Tropical Cyclone Formation Alert. Later that day, the JTWC designated the system as Cyclone 04A. During the next day, the Depression turned towards the northeast the IMD reported that it had intensified into a Cyclonic Storm and named it as Phyan.
Severe Cyclonic Storm Jal was the fifth named cyclonic storm and the fourth Severe Cyclonic Storm of the 2010 North Indian Ocean cyclone season. Jal developed from a low-pressure area in the South China Sea that organized into a Tropical Depression on October 28. Jal is a Sanskrit word, meaning water. At least 54 people are known to have been killed in India. As a tropical depression, Jal produced torrential rains over parts of Thailand and Malaysia, triggering severe flooding which killed 59 and four people in the two countries respectively. In Sri Lanka, heavy rainfall with strong winds have caused flooding affecting around 80,000 people. In Thailand, Jal was responsible for 78 deaths, being the 4th deadliest tropical cyclone in the country.
The 2012 North Indian Ocean cyclone season was a very inactive season. The season had a very late start, with the first system forming in October. During the season, only five systems formed, of which only two became cyclonic storms. Both the storms made landfall, and they, along with the deep depressions, were responsible for 128 deaths and economic losses worth at least $56.7 million.
The 2013 North Indian Ocean cyclone season was an event in the annual cycle of tropical cyclone formation, in which tropical cyclones formed in the North Indian Ocean and Arabian Sea. The season had no official bounds, but cyclones typically formed between May and December, with the peak from October to November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean.
The 2016 North Indian Ocean cyclone season was an event in the annual cycle of tropical cyclone formation. It was the deadliest season since 2010, killing more than 400 people. The season was an average one, seeing four named storms, with one further intensifying into a very severe cyclonic storm. The first named storm, Roanu, developed on 19 May while the season's last named storm, Vardah, dissipated on 18 December. 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.
Cyclonic Storm Roanu was a relatively weak tropical cyclone that caused severe flooding in Sri Lanka and Bangladesh during May 2016. It is the first tropical cyclone of the annual cyclone season. Roanu originated from a low-pressure area that formed south of Sri Lanka, which gradually drifted north and intensified into a cyclonic storm on 19 May. However, wind shear and land interaction caused it to weaken slightly, before reintensifying as it accelerated towards the coast of Bangladesh.
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.
The 2022 North Indian Ocean cyclone season was an event in the annual cycle of tropical cyclone formation. It was an above-average season in terms of depressions and average in terms of deep depressions, but slightly below average in terms of cyclonic storms. It was also the least deadly North Indian Ocean cyclone season since 1988, according to official data. The season's strongest tropical cyclone was Cyclone Asani, with maximum wind speeds of 100 km/h and a minimum barometric pressure of 982 hPa. The North Indian Ocean cyclone season has no official bounds, but cyclones tend to form between April and December, with the peak from May to November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northern Indian Ocean.
Severe Cyclonic Storm Phethai was a tropical cyclone which affected some portions of Sri Lanka and India during December 2018. The fourteenth depression, ninth deep depression, seventh cyclonic storm, and fifth severe cyclonic storm of the 2018 North Indian Ocean cyclone season, Phethai developed from an area of low pressure that formed over the Bay of Bengal on December 13. Having forecasted not to develop significantly, the depression then strengthened to a deep depression later that day before becoming a cyclonic storm on December 15. Phethai further intensified and peaked to a severe cyclonic storm, the following day. The system then steadily weakened due to land interaction and increasing wind shear, before making landfall as a disorganized system over Andhra Pradesh on December 17. It degenerated to an area of low-pressure inland later that day.