Meteorological history | |
---|---|
Formed | May 12,2007 |
Dissipated | May 15,2007 |
Cyclonic storm | |
3-minute sustained (IMD) | |
Highest winds | 85 km/h (50 mph) |
Lowest pressure | 988 hPa (mbar);29.18 inHg |
Category 1-equivalent tropical cyclone | |
1-minute sustained (SSHWS/JTWC) | |
Highest winds | 120 km/h (75 mph) |
Lowest pressure | 976 hPa (mbar);28.82 inHg |
Overall effects | |
Fatalities | 14 direct |
Damage | $982 million (2007 USD) |
Areas affected | Andaman Islands,Nicobar Islands,Bangladesh,Burma |
IBTrACS | |
Part of the 2007 North Indian Ocean cyclone season |
Cyclonic Storm Akash (JTWC designation:01B) was the first named tropical cyclone of the 2007 North Indian Ocean cyclone season. Warned by both India Meteorological Department (IMD) and Joint Typhoon Warning Center (JTWC),it formed from an area of disturbed weather on the Bay of Bengal on May 12,and gradually organized as it drifted northward. An eye began to develop as it approached land,and after reaching peak 3-min sustained winds of 85 km/h (55 mph) it struck about 115 km (71 mi) south of Chittagong in Bangladesh. Akash rapidly weakened over land,and advisories were discontinued on May 15.
The storm initially brought heavy rainfall to the Andaman and Nicobar Islands. Upon striking Bangladesh,Cyclonic Storm Akash produced a moderate storm tide,along with strong winds and heavy rains. The storm left dozens of boats missing,with three fisherman confirmed killed and another 50 missing. Near the coast,thousands of houses were damaged from the flooding caused by the storm. In Burma,its storm tide caused some coastal flooding. In all,14 people were killed and damages amounted to US$982 million.
During the second week of May, low pressures persisted across the Bay of Bengal. An area of convection developed on May 11, and the next day the India Meteorological Department (IMD) classified it as a depression. [1] The system drifted northward, [2] and initially moderate wind shear kept the deep convection on the periphery of the consolidating low-level circulation center. [3] Gradually, banding features developed along the eastern semicircle, and with decreasing amounts of wind shear the system organized further. [4] By May 13, the pressure had dropped to 1000 mbar as wind shear levels dropped significantly. An anticyclone developed over the system, while a mid-latitude trough over northeastern India provided favorable outflow. Convection continued to consolidate around the low-level circulation, [5] and with well-defined banding features and a central dense overcast over the center of circulation, the Joint Typhoon Warning Center (JTWC) upgraded it to Tropical Cyclone 01B at 1121 UTC on May 13 while located about 545 km (339 mi) west-northwest of Yangon, Burma. [6]
Upon first being upgraded, the storm tracked steadily northward due to a break in a mid-level ridge. [6] Early on May 14, IMD upgraded the system to deep depression status, [7] and six hours later classified it as Cyclonic Storm Akash after attaining 3-min sustained winds of 40 mph (65 km/h). [8] Akash continued to organize, with deep convection wrapping fully around the low-level circulation. [9] An eye began to form as the storm approached land, and at 1800 UTC on May 14 JTWC estimated 1-min sustained winds of 120 km/h (75 mph). [10] Officially, Akash attained peak 3-min sustained winds of 85 km/h (55 mph) and a minimum central pressure of 988 hPa. [11] Additionally, meteorologists in Burma estimated Akash peaked with winds of 160 km/h (100 mph). [12] As it interacted with the mid-latitude westerlies, it began to become extratropical. [10] Shortly after reaching peak winds, Akash made landfall about 115 km (71 mi) south of Chittagong. The storm weakened rapidly as it continued inland, [13] and early on May 15 IMD issued its final advisory on the system; [14] shortly thereafter, JTWC discontinued advisories. [13] The name was contributed by India, Akash means Sky in Hindi language.
In its daily tropical weather outlook, the India Meteorological Department warned fishermen on the Andaman and Nicobar Islands to not go into the ocean due to the anticipated rough seas. [2] Upon approaching the coast of Bangladesh, officials canceled all flights to and from the Shah Amanat International Airport. Additionally, authorities at the port of Chittagong worked to protect cargo ships from the storm, [15] and it was ultimately closed for a period of 19 hours. [16] [17] In preparation for Akash, officials advised coastal residents to evacuate further inland; [15] about 80,000 total residents left for emergency shelters. [16] About 40,000 Red Cross volunteers were prepared to aid those potentially affected. [15]
Precipitation | Storm | Location | Ref. | ||
---|---|---|---|---|---|
Rank | mm | in | |||
1 | 1,051.2 | 41.39 | Komen 2015 | Chittagong | [18] |
2 | ~300 | ~12.00 | Rashmi 2008 | [19] | |
3 | 280 | 11.02 | Monsoon Depression — Sep. 2004 | Barisal | [20] |
4 | 253 | 10.00 | Viyaru 2013 | Patuakhali | [21] |
5 | 227.2 | 8.94 | Trop. Depression — Oct. 2004 | Rangpur | [22] |
6 | 220.0 | 8.66 | Bhola 1970 | Maya Bandar | [23] |
7 | 200 | 7.87 | Sidr 2007 | [24] | |
8 | 130 | 5.11 | Aila 2009 | Chittagong | [25] |
9 | 129 | 5.07 | Bijli 2009 | [26] | |
10 | 53 | 2.13 | Akash 2007 | [27] |
The India Meteorological Department estimated winds of 45–55 km/h (28–34 mph) affected the Andaman and Nicobar Islands, though no land reports were received. [2] In Sittwe in Burma, the storm produced a storm tide of 3 m (9.8 ft), which flooded coastal areas. [12]
In Chittagong, about 115 km (71 mi) north of where Akash moved ashore, surface stations reported peak winds of 37 km/h (23 mph) and a pressure of 996.8 hPa. [13] Near its landfall location, Akash produced high tides that flooded coastal areas with up to 1.5 m (4.9 ft) of water, [16] destroying at least 30 businesses. [12] The cyclone destroyed 205 houses and left an additional 845 damaged. [27] Akash caused moderate crop damage near the coast, [12] including 2 hectares (4.9 acres) of destroyed lands of shrimp farms. [17] Heavy precipitation was reported, with one station reporting a total of 53 mm (2.1 in); [27] the rainfall caused flooding in inland areas. [16] The heavy rains, caused by outer bands of the cyclone before it made landfall, limited play in Chittagong in the third One Day International cricket match between India and Bangladesh, before the match was abandoned. [28] Strong winds caused power outages throughout Cox's Bazar District, [16] and downed about 200 trees on St. Martin's Island. The cyclone left a total of 10 boats unaccounted for, with about 50 fishermen missing. In total, three fisherman were confirmed killed, all on St. Martin's Island, [17] with two people left hospitalized. [29] The passage of Cyclone Akash left many people homeless. Initially there was no response from the government. [29] In all, 14 people were killed by Akash and damages amounted to US$982 million. [30]
The 1991 Bangladesh cyclone was among the deadliest tropical cyclones on record. Forming out of a large area of convection over the Bay of Bengal on April 24, the tropical cyclone initially developed gradually while meandering over the southern Bay of Bengal. On April 28, the storm began to accelerate northeastwards under the influence of the southwesterlies, and rapidly intensified to super cyclonic storm strength near the coast of Bangladesh on April 29. After making landfall in the Chittagong district of southeastern Bangladesh with winds of around 250 km/h (155 mph), the cyclone rapidly weakened as it moved through northeastern India, degenerating into a remnant low over the Yunnan province in western China.
Severe Cyclonic Storm Agni was a tropical cyclone of the 2004 North Indian Ocean cyclone season notable for its record proximity to the equator. It was the second North Indian Ocean cyclone to receive a name, after Onil earlier in the year. Agni formed on November 28 well to the southwest of India in the Arabian Sea, and steadily intensified as it tracked northwestward. The Joint Typhoon Warning Center (JTWC) estimated peak 1 minute sustained winds of 120 km/h (75 mph), while the India Meteorological Department (IMD) estimated peak 3 minute sustained winds of 100 km/h (60 mph); the IMD is the official warning center for the north Indian Ocean. After peaking, it weakened due to wind shear, dry air, and cooler waters, and the JTWC issued its final advisory on December 3 as it approached the coast of Somalia. The remnants of Agni moved along the Somalian coastline until dissipating on December 5.
The 2007 North Indian Ocean cyclone season was one of the most active North Indian Ocean cyclone seasons on record. 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.
Below is a timeline of the 2007 North Indian Ocean cyclone season, documenting major events with regards to tropical cyclone formation, strengthening, weakening, landfall, extratropical transition, as well as dissipation. The 2007 North Indian Ocean cyclone season was an ongoing event in the annual cycle of tropical cyclone formation.
The 1997 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.
The 1998 North Indian Ocean cyclone season was an active season in annual cycle of tropical cyclone formation. 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 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 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 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 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.
Cyclonic Storm Rashmi was the seventh tropical cyclone of the 2008 North Indian Ocean cyclone season and second cyclonic storm, as well as the fifth tropical cyclone in the Bay of Bengal that year. A fairly weak tropical cyclone, it caused some notable damage in Bangladesh and India.
Cyclonic Storm Bijli, was the first tropical cyclone to form during the 2009 North Indian Ocean cyclone season. Bijli formed from an area of Low Pressure on April 14. Later that evening, RSMC New Delhi upgraded the low-pressure area to a Depression and designated it as BOB 01. The Joint Typhoon Warning Center (JTWC) then issued a Tropical Cyclone Formation Alert for the system and soon after designated it as Tropical Depression 01B. On the evening of April 15, both RSMC New Delhi and the JTWC reported that the system had intensified into a tropical storm, with the former naming it Bilji. Soon after, Bilji reached its peak intensity as it approached the coast of Bangladesh. However, on the morning of April 17, Bijli weakened to a deep depression due to land interaction, before making landfall just south of Chittagong. The remnants of Bilji continued to weaken as they tracked across northern Myanmar, before RSMC New Delhi issued their last advisory on April 18. The word Bijli refers to lightning in Hindi.
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 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.
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.
Cyclonic Storm Viyaru, operationally known as Cyclonic Storm Mahasen, was a relatively weak tropical cyclone that caused loss of life across six countries in Southern and Southeastern Asia. Originating from an area of low pressure over the southern Bay of Bengal in early May 2013, Viyaru slowly consolidated into a depression on May 10. The depression gained forward momentum and attained gale-force winds on May 11 and was designated as Cyclonic Storm Viyaru, the first named storm of the season. Owing to adverse atmospheric conditions, the depression struggled to maintain organized convection as it moved closer to eastern India. On May 14, the exposed circulation of Viyaru turned northeastward. The following day, conditions again allowed for the storm to intensify. Early on May 16, the cyclone attained its peak intensity with winds of 85 km/h (55 mph) and a barometric pressure of 990 mbar. Shortly thereafter Viyaru made landfall near Chittagong, Bangladesh. On May 17, it moved over the eastern Indian state of Nagaland.
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.
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.
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.
The 2023 North Indian Ocean cyclone season was an above-average and deadly season, becoming the deadliest season since 2017, mainly due to Cyclone Mocha. With nine depressions and six cyclonic storms forming, it became the most active season, featuring the second-highest accumulated cyclone energy (ACE) on record only behind 2019. It also had the most extremely severe cyclonic storms on record, tieing with 1999 and 2019. 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. However, a cyclone can form at any time during the year shown by an unnamed depression that affected Sri Lanka in January-February.
The 2024 North Indian Ocean cyclone season is an ongoing event in the annual cycle of tropical cyclone formation. The 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.