Meteorological history | |
---|---|
Formed | 1 November 1989 |
Dissipated | 10 November 1989 |
Super cyclonic storm | |
3-minute sustained (IMD) | |
Highest winds | 230 km/h (145 mph) |
Lowest pressure | 930 hPa (mbar);27.46 inHg |
Very strong typhoon | |
10-minute sustained (JMA) | |
Highest winds | 165 km/h (105 mph) |
Lowest pressure | 960 hPa (mbar);28.35 inHg |
Category 5-equivalent tropical cyclone | |
1-minute sustained (SSHWS/JTWC) | |
Highest winds | 260 km/h (160 mph) |
Overall effects | |
Fatalities | 1,036 total |
Damage | $521 million (1989 USD) |
Areas affected | Thailand,Myanmar,India |
IBTrACS | |
Part of the 1989 Pacific typhoon and North Indian Ocean cyclone seasons |
Typhoon Gay,also known as the Kavali Cyclone of 1989, [1] was a small but powerful tropical cyclone which caused more than 800 fatalities in and around the Gulf of Thailand in November 1989. The worst typhoon to affect the Malay Peninsula in thirty-five years,Gay originated from a monsoon trough over the Gulf of Thailand in early November. Owing to favorable atmospheric conditions,the storm rapidly intensified,attaining winds over 120 km/h (75 mph) by 3 November. [nb 1] Later that day,Gay became the first typhoon since 1891 to make landfall in Thailand,striking Chumphon Province with winds of 185 km/h (115 mph). The small storm emerged into the Bay of Bengal and gradually reorganized over the following days as it approached southeastern India. On 8 November,Gay attained its peak intensity as a Category 5-equivalent cyclone with winds of 260 km/h (160 mph). The cyclone then moved ashore near Kavali,Andhra Pradesh. Rapid weakening ensued inland,and Gay dissipated over Maharashtra early on 10 November.
The typhoon's rapid development took hundreds of vessels by surprise,leading to 275 offshore fatalities. Of these,91 occurred after an oil drilling ship,the Seacrest ,capsized amid 6–11 m (20–36 ft) swells. Across the Malay Peninsula,588 people died from various storm-related incidents. Several towns in coastal Chumphon were destroyed. Losses throughout Thailand totaled ฿ 11 billion (US $497 million). [nb 2] Striking India as a powerful cyclone,Gay damaged or destroyed about 20,000 homes in Andhra Pradesh,leaving 100,000 people homeless. In that country,69 deaths and ₹410 million (US $25.3 million) in damage were attributed to Gay.
In early November, a monsoon trough over the Gulf of Thailand showed signs of tropical cyclogenesis. A small, concentrated area of convection quickly developed over a low-pressure area within the trough, and on 2 November the system became sufficiently organized for the Joint Typhoon Warning Center (JTWC) to issue a Tropical Cyclone Formation Alert. [nb 3] Owing to its small size, the system began strengthening within the narrow gulf by taking advantage of warm waters and good outflow. Moving generally northwestward, it became a tropical depression later that day and underwent rapid intensification. As the newly named Tropical Storm Gay strengthened, it "presented a paradox to forecasters", according to Lieutenant Dianne K. Crittenden; synoptic data from Malaysia and Thailand indicated decreasing wind speeds and increasing barometric pressures around the storm, but these observations were later interpreted as increased subsidence. [3]
Strengthening faster than anticipated, Gay attained typhoon status early on 3 November. Later that day, the storm developed an eye before passing over the Seacrest, an oil drilling ship. [3] On 4 November, Gay's winds increased to 185 km/h (115 mph), equivalent to a Category 3 hurricane on the Saffir–Simpson hurricane scale, before making landfall in Chumphon Province, Thailand, at 0600 UTC. [4] The Japan Meteorological Agency assessed that the storm had ten-minute sustained winds of 140 km/h (85 mph) and a pressure of 960 mbar (hPa; 28.35 inHg). [5] [nb 4] Crossing the Kra Isthmus, Gay weakened to minimal typhoon status as it entered the Bay of Bengal. [3] [4] According to the India Meteorological Department (IMD), [nb 5] Gay was the first typhoon since 1891 to form in the Gulf of Thailand and enter the Bay of Bengal. [8] Responding to a ridge to its north, Gay maintained a west-northwestward to northwestward track for the next four days. The storm gradually restrengthened as it moved through an area of low wind shear and warm waters; however, this was limited by restrictions to the cyclone's outflow. [3] Early on 6 November, Gay passed near the Andaman Islands as a Category 2-equivalent cyclone. [4]
After changing little in intensity for much of 6 November, Gay strengthened as the ridge to its north intensified and the previous restrictions to its outflow diminished. The storm moved due west through a small fetch of warmer waters, fueling the process of intensification over the next 42 hours. Based on estimates provided through the use of the Dvorak technique, the JTWC assessed Gay to have attained its peak intensity as a Category 5-equivalent cyclone with winds of 260 km/h (160 mph) early on 8 November. [3] [4] Around this time, the IMD estimated that the storm had three-minute sustained winds of 230 km/h (145 mph), classifying Gay as a modern-day super cyclonic storm. [1] [9] Additionally, the agency estimated the cyclone's central pressure to have decreased to 930 mbar (hPa; 27.46 inHg). [10] Around 1800 UTC, Gay made landfall over a sparsely populated area near Kavali, India, in Andhra Pradesh. Upon coming ashore, the storm's eye was about 20 km (12 mi) wide, with gale-force winds within 95 km (60 mi) of the center. [3] [11] Now over land, Gay no longer had access to warm waters, causing it to weaken to a tropical storm less than twelve hours after this landfall. [3] The storm continued to deteriorate while moving across India, before it completely dissipated over Maharashtra on 10 November. [4]
The most powerful storm to affect the Gulf of Thailand in more than thirty-five years, Gay produced 6–11 m (20–36 ft) swells which caught many ships in the region off-guard. [12] At least 16 vessels were reported missing by 5 November, including the 106 m (348 ft) Unocal Corporation oil drilling ship Seacrest . [13] According to survivors, the vessel received no warning of the developing typhoon. [14] Just when all crew members were about to abandon ship, the eye passed over. Winds fluctuated violently and changed direction, preventing the ship from remaining stabilized despite being within safe operating limits. The vessel abruptly capsized with all 97 crew members on board during the overnight hours of 3 November, before any life boats could be deployed. [13] [14] Initial rescue attempts on 4 November were hampered by rough seas. [15] Two days after the sinking, four rescue ships and two helicopters in the region were searching for survivors; [13] four people were rescued from the wreckage on 6 November. Divers from the Thai Navy were sent to search the capsized vessel for anyone trapped inside. [16] Of the crew, only six survived; 25 bodies were recovered, and the remaining 66 members were presumed dead. [14] [17] Losses from the sinking of the Seacrest totaled $40 million. [18] Another 20 cargo and fishing ships sank during the storm, resulting in 140 fatalities. [19]
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Striking Thailand with unprecedented strength, Typhoon Gay caused catastrophic damage across many of its provinces. [12] Areas between Chumphon and Rayong provinces were severely affected by heavy rains, high winds and large swells. [21] Rainfall amounts peaked at Chumphon, where 7.64 inches (194 mm) fell during the cyclone's passage. [22] Widespread disruption of communication and electricity occurred in most areas south of Bangkok; many households remained without power for weeks. [23] Damaging winds uprooted numerous trees and power poles and toppled wooden houses built on stilts. [24] Exacerbated by deforestation, [20] flash flooding triggered by the storm damaged or destroyed thousands of homes and caused at least 365 fatalities. [25] Several towns and villages across Chumphon province were devastated, and one of the destroyed villages "looked like it had been bombed" according to the Bangkok Post . [26] Entire districts were reportedly "flattened" in Chumphon and Prachuap Khiri Khan provinces. [24] The typhoon destroyed many schools across Chumphon and Surat Thani provinces, many of which were constructed of wood. All structures close to the storm's path had their windows and doors blown out, and some multi-story buildings lost their upper floors. A few schools constructed from reinforced concrete sustained little damage. [27] More than a thousand roads and 194 bridges were damaged or washed away. [20] At the height of the floods, over 250,000 hectares (620,000 acres) of land was under water. [28] Onshore, 558 fatalities were attributed to the storm, and another 44 died just offshore. [20] Throughout Thailand, approximately 47,000 homes were damaged or destroyed, and more than 200,000 people were affected, of which about 153,000 were left homeless. [20] [28] Monetary losses reached 11 billion baht (US$456.5 million), ranking Gay as one of the costliest disasters in the country's history. [29]
Within a week of the storm's passage, the Government of Thailand began distributing relief goods to residents throughout the affected provinces. [23] Despite the effort by the government, 2,500 people from Pa Thiew and Tha Sae demonstrated for additional and more intensive aid on 9 November. These protests were soon dispersed. [30] Following considerable criticism for downplaying the impact of the typhoon, Prime Minister Chatichai Choonhavan delayed his visit to the United States to oversee relief efforts. [25] By 15 November the United States pledged to donate US$25,000 for recovery operations. Telephone connection was restored from Bangkok to Prachuap Khiri Khan by this time; however, areas further south remained disconnected. Generators were brought in to keep hospitals and government offices running since much of Chumphon Province remained without electricity for more than two weeks. As the scale of damage became more apparent, a request for international aid was made by 17 November to the United Nations Disaster Relief Organization. Upon the announcement of the request, six countries pledged to provide nearly US$510,000 in funds collectively. [20] [23] Agriculture across Surat Thani Province was severely affected by the typhoon in the long-term as well. In the four years following Typhoon Gay, land use for orchards, rubber, and oil palm plantations decreased from 33.32 percent to 30.53 percent. Additionally, rice paddy coverage decreased from 22.96 percent to 13.03 percent. [31]
Following post-storm surveys, it was determined that most of the severely damaged schools had been built improperly –building codes in Thailand mandate that structures withstand up to 120 kgf/m2 of pressure from winds. In the years following the typhoon, studies determined how best to rebuild: reinforced concrete structures which can last fifty years. [27]
After crossing the Malay Peninsula, Gay moved through the Andaman Islands on 6 November. As a precautionary measure, all air and sea traffic were suspended to the region. Winds in excess of 120 km/h (75 mph) battered North Andaman Island, causing two structures to collapse. [8] A few days before the cyclone made landfall, officials in Andhra Pradesh began evacuating roughly 50,000 residents along the coast and stockpiled relief goods. Some people were forced to leave vulnerable locations in the Visakhapatnam and Srikakulam districts. [32] [33] Local meteorologists warned that the storm was comparable to a cyclone in 1977 that killed more than ten thousand. [34] Striking the southern coast of Andhra Pradesh, Gay produced wind gusts estimated at 230 km/h (145 mph). [35] Along the coast, a storm surge of 3.5 m (11 ft) inundated areas up to 3 km (1.9 mi) inland, washing away numerous structures. [10] [36] About 20 km (12 mi) outside of Kavali, a 91 m (299 ft) tall, steel lattice microwave tower collapsed after experiencing winds estimated at 142 km/h (88 mph). [37] Transportation and communication across the region was disrupted and 20,000 homes were damaged or destroyed, leaving at least 100,000 people homeless. [38] Nearly every structure in Annagaripalem were severely damaged or destroyed. [39] Offshore, 25 fishermen drowned near Machilipatnam after ignoring warnings to return to port. [40] Throughout Andhra Pradesh, 69 fatalities and ₹410 million (US$25.3 million) worth of damage was attributed to Gay. [10] [41] In the months after the storm, concrete shelters were built to house displaced persons. [39]
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 1989 Pacific typhoon season was the first of six consecutive years of above-average activity in the Western Pacific. It was an extremely active season spawning 32 tropical storms, 20 typhoons and five super typhoons. It has no official bounds; it ran year-round in 1989, but most tropical cyclones tend to form in the northwestern Pacific Ocean between May and November. These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean. The first storm, Winona, formed on January 15, while the final storm, Jack, dissipated on December 27. This season was also quite a deadly season that were caused by a few notable storms such as Tropical Storm Cecil, which was the worst storm to impact Vietnam in over 50 years, and Typhoon Gay, which directly impacted the Malay Peninsula as the worst typhoon in 35 years. Both of these storms make up around half of the total fatalities of the entire season alone.
Typhoon Ike, known in the Philippines as Typhoon Nitang, was the second deadliest tropical cyclone in the 20th century in the Philippines. Ike originated from an area of disturbed weather southeast of Guam on August 21, 1984, and five days later, developed into a tropical depression. Following an increase in organization, the depression attained tropical storm intensity on August 27. Initially tracking west-southwest, the storm gradually gained strength as wind shear resulted relaxed and Ike became a typhoon on August 30. Continuing to rapidly intensity, Ike turned west and attained peak intensity on September 1, with the Japan Meteorological Agency estimating winds of 170 km/h (105 mph). At around 14:00 UTC that day, Ike made landfall on the northeastern tip of Mindanao. The cyclone emerged into the South China Sea on September 3 as a tropical storm before re-intensifying into a typhoon and moving onshore Hainan. Ike then struck the Chinese mainland as a tropical storm in Guangxi and dissipated on September 6.
Typhoon Nina, known in the Philippines as Typhoon Sisang, was the most intense typhoon to strike the Philippines since Typhoon Irma in 1981. Typhoon Nina originated from an area of convection near the Marshall Islands in mid-November 1987. It gradually became better organized, and on November 19, was first classified as a tropical cyclone. Moving west-northwest, Nina attained tropical storm intensity that evening. Late on November 20, Nina passed through the Chuuk Lagoon in the Federated States of Micronesia. After a brief pause in intensification, Nina intensified into a typhoon on November 22. Two days later, the typhoon intensified suddenly, before attaining its peak 10 minute intensity of 165 km/h. During the afternoon of November 25, Nina moved ashore in Southern Luzon at the same intensity. It gradually weakened over land, before entering the South China Sea and turning to the north. By November 30, Nina dissipated.
Tropical Storm Kim, known in the Philippines as Tropical Depression Rosing, was the only storm in 1983 to move from the Western Pacific basin into the North Indian Ocean basin. Kim originated as a weak tropical disturbance that formed to the northeast of Truk during the second week of October. It drifted westward over the subsequent days, and on October 15, while located over the South China Sea, the disturbance was classified as a tropical depression. Late the following day, the system was briefly upgraded into a tropical storm, but the storm dissipated quickly after making landfall in Vietnam early on October 17. After trekking across Indochina, the remnants of Kim moved into the Andaman Sea and re-developed into a tropical cyclone on October 19. However, Kim dissipated for good the next day while located inland over Burma.
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.
The 1989 North Indian Ocean cyclone season was a below-average season in annual cycle of tropical cyclone formation. Despite this, the season had the second highest Accumulated Cyclone Energy in the basin on record behind only 2019 and 2023. 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 (JTWC) releases unofficial advisories. An average of five tropical cyclones 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.
Cyclonic Storm Keila was the first named storm of the 2011 North Indian Ocean cyclone season. A weak system for much of its duration, Keila developed in the western Arabian Sea in late October 2011, amid an area of marginally favorable conditions. On November 2, it briefly organized enough to be classified as a cyclonic storm, which has maximum sustained winds of at least 65 km/h (40 mph). Given the name Keila by the India Meteorological Department (IMD), the storm quickly moved ashore southern Oman near Salalah, and weakened while meandering over the country. The remnants soon after moved offshore, dissipating on November 4.
Typhoon Alex, known in the Philippines as Typhoon Etang, affected the Taiwan, China, and South Korea during July 1987. Typhoon Alex developed from the monsoon trough that spawned a tropical disturbance late on July 21 southwest of Guam which organized into a tropical depression shortly thereafter. The system steadily became better organized, and the next day, a tropical depression had developed. Satellite intensity estimates gradually increased, and on July 23, the depression intensified into Tropical Storm Alex. After initially tracking west-northwest, Tropical Storm Alex started tracking northwest. An eye developed on July 24, and on the next day, Alex was classified as a typhoon, when Alex attained its peak intensity of 120 km/h (75 mph) and a minimum barometric pressure of 970 mbar (29 inHg). Alex weakened while tracking more northward, though interaction with Taiwan resulted in a more westward track starting on July 27. The storm struck near Shanghai as a tropical storm, and weakened over land, although it remained identifiable through August 2.
Typhoon Nepartak, known in the Philippines as Typhoon Weng, was a modest tropical cyclone that struck the central Philippines and the southern China island of Hainan in November 2003. Forming as a tropical depression on November 11 between Yap and Guam, the system moved westward and slowly intensified. It received the name Nepartak midday on November 12 from the Japan Meteorological Agency, becoming the 20th named storm of the 2003 Pacific typhoon season. On November 13, Napartak struck Samar in the Philippines and bisected the island chain. Up to four million people lost power, and transportation ground to a halt; over 5,000 individuals became stranded on ships forced to stay in port during the tropical storm. It was reported that 13 individuals died in the storm in the Philippines.
Severe Tropical Storm Cecil in May of 1989 caused devastating floods in central Vietnam, killing 751 people. The storm developed as a tropical depression over the South China Sea on May 22. Tracking north-northwestward, the system steadily intensified, attaining peak winds of 110 km/h (68 mph). The Joint Typhoon Warning Center (JTWC) assessed Cecil to have been slightly stronger with one-minute sustained winds of 140 km/h (87 mph). The storm made landfall near Hoi An, Vietnam early on May 25 and quickly weakened. The system later dissipated over Laos on May 26.
Typhoon Cimaron, known in the Philippines as Super Typhoon Paeng, was the most intense tropical cyclone to strike the Philippine island of Luzon since Typhoon Zeb in 1998. Originating from a tropical depression on October 25, Cimaron developed within an environment strongly favoring tropical cyclogenesis east of the Philippines. On October 28, the system underwent rapid intensification, culminating in attaining its peak strength with winds of 185 km/h (115 mph). Estimates from the Joint Typhoon Warning Center ranked the system as a Category 5-equivalent super typhoon with one-minute sustained winds of 260 km/h (160 mph), though this is argued to have underrepresented the typhoon's strength. The system moved ashore near Casiguran, Aurora in northern Luzon at peak strength. Crossing the island, Cimaron emerged over the South China Sea where conditions allowed for temporary reorganization. After becoming nearly stationary on November 1, the typhoon executed a tight anti-cyclonic loop and rapidly weakened. The storm degenerated into a tropical depression on November 4, before dissipating three days later off the coast of Vietnam.
Extremely Severe Cyclonic Storm Forrest, also referred to as Tropical Storm Forrest while in the western Pacific basin before its Thai crossover, was a powerful tropical cyclone that prompted the evacuation of 600,000 people in Bangladesh in late November 1992. Originating from an area of disturbed weather near the Caroline Islands on November 9, Forrest was classified as a tropical depression three days later over the South China Sea. Tracking generally west, the system steadily organized into a tropical storm, passing Vietnam to the south, before striking Thailand along the Malay Peninsula on November 15. Once over the Bay of Bengal, Forrest turned northward on November 17 and significantly intensified. It reached its peak intensity on November 20 as a Category 4-equivalent cyclone on the Saffir–Simpson hurricane scale with winds of 230 km/h (140 mph). Hostile environmental conditions soon affected the cyclone as it turned abruptly east-northeastward. Forrest made landfall in northwestern Myanmar as a weakening system on November 21 before dissipating early the next day.
Severe Tropical Storm Tess known in the Philippines as Tropical Storm Welpring was the second of three tropical cyclones to directly impact the Philippines in a two-week time frame in 1988. An area of disturbed weather near the Philippines was first observed on November 1. Following an increase in organization, the disturbance was designated as a tropical cyclone on November 4. Moving west, Tess steadily strengthened due to favorable conditions aloft. During the evening of November 5, Tess was estimated to have achieved its highest intensity, with winds of 115 km/h (70 mph). Rapid weakening then ensured as Tess neared Vietnam, and after making landfall in the country on November 6, Tess dissipated the next day.
The 1996 Andhra Pradesh cyclone was a small but powerful storm that left heavy damage in the Indian state of Andhra Pradesh. It formed on 4 November in the eastern Bay of Bengal. Moving westward, it quickly organized and developed a well-defined eye. On 6 November, the cyclone struck about 50 km (31 mi) south of Kakinada, Andhra Pradesh at peak intensity. The India Meteorological Department estimated peak winds of 145 km/h (90 mph), while the American-based Joint Typhoon Warning Center (JTWC) assessed peak winds of 215 km/h (135 mph). Soon after landfall, the cyclone weakened and dissipated by 7 November.
The October 1996 India cyclone had an unusual and protracted path that spanned much of the northern Indian Ocean. It originated in a weather disturbance that formed on October 14 in the southern Bay of Bengal, off India's east coast. Moving westward, it struck Andhra Pradesh on October 17 as a well-defined low-pressure area. It crossed southern India and reorganized in the Arabian Sea off the western coast of India. The system developed into a depression on October 22 and quickly intensified while moving northward. By October 24, the cyclone approached hurricane intensity as it developed an eye, reaching peak winds of at least 110 km/h (70 mph). On October 25, the storm abruptly stalled and weakened off Gujarat, and progressed southwestward as a minimal storm. It was no longer classifiable as a tropical cyclone by October 28, although its remnants persisted until November 2 when they dissipated east of Somalia.
Typhoon Cary, known as Typhoon Ising in the Philippines, was the second of two tropical cyclones to affect Vietnam in a week. An area of disturbed weather developed southwest of Pohnpei on August 6, 1987. The system initially remained disorganized, but by August 14, Cary had attained tropical storm intensity. After initially moving north-northwest, Cary turned west-northwest, although intensification was slow to occur. On August 15, Cary was upgraded into a typhoon, and on August 17, the typhoon peaked in intensity. Typhoon Cary then made landfall in northern Luzon while at peak intensity. Across the Philippines, 954 houses were damaged and an additional 89 were destroyed, which left 55,567 people, or 13,247 families that were either homeless or otherwise sought shelter. Five people died in the country while damage totaled $5.58 million (1987 USD), including $1.45 million from agriculture and $4.13 million from infrastructure. The storm weakened over land, but re-intensified into a typhoon over the South China Sea. On August 21, Typhoon Cary passed just south of Hainan, where hundreds of homes were damaged but no fatalities occurred, and subsequently entered the Gulf of Tonkin. The storm weakened as it approached Vietnam, and on August 23, the storm dissipated inland over Laos. Across Vietnam, almost 40,000 ha of land were flooded or destroyed. Twenty people were killed and many others were injured.
Typhoon Betty, known in the Philippines as Typhoon Aring, was the strongest typhoon to strike the Philippines in ten years. An area of disturbed weather developed on October 27, 1980, near Truk Atoll. After turning east from south, the disturbance was classified as a tropical storm on October 29 as it passed near Guam, causing only minor damage. Following a turn to the west-northwest, Betty attained typhoon intensity the next day. On November 4, Betty peaked in intensity. Later that day, Betty moved ashore over Luzon, introducing a rapid weakening trend. Over land, Betty then began to turn north due to a weakening subtropical ridge to its north and a trough offshore Taiwan. By November 8, Betty, after moving offshore, had completed its transition into an extratropical cyclone, and dissipated that same day.
Typhoon Warren, known in the Philippines as Typhoon Huaning, struck the Philippines and China during July 1988. An area of disturbed weather developed within the vicinity of the Caroline Islands during the second week of July. A tropical depression developed southeast of Guam on July 12, and on the next day, intensified into a tropical storm. Tracking generally west-northwest, Warren deepened into a typhoon on July 14. The storm subsequently entered a period of rapid intensification, commencing with Warren reaching its highest intensity on July 16. The following evening, the typhoon brushed Luzon, resulting in a weakening trend, although Warren was still a typhoon when it made landfall near Shantou. Warren rapidly dissipated inland.
The 1994 Bangladesh cyclone was a powerful tropical cyclone in the Bay of Bengal. The cyclone closely followed the path, strength, and time of year of a deadly cyclone in 1991 that killed more than 138,000 people. The 1994 cyclone formed on April 29 as a depression, which organized and intensified significantly over the subsequent few days. On May 2, the cyclone attained winds of 215 km/h (135 mph), according to the India Meteorological Department (IMD). That day, the storm made landfall in southeastern Bangladesh, and rapidly weakened over land, before dissipating on May 3.