Meteorological history | |
---|---|
Formed | June 20,1990 |
Dissipated | June 30,1990 |
Typhoon | |
10-minute sustained (JMA) | |
Highest winds | 150 km/h (90 mph) |
Lowest pressure | 950 hPa (mbar);28.05 inHg |
Category 4-equivalent typhoon | |
1-minute sustained (SSHWS/JTWC) | |
Highest winds | 215 km/h (130 mph) |
Overall effects | |
Fatalities | 27 total |
Damage | $426 million (1990 USD) |
Areas affected | Caroline Islands,Philippines,Taiwan,south China |
Part of the 1990 Pacific typhoon season |
Typhoon Percy,known in the Philippines as Typhoon Klaring,was the third tropical cyclone to affect the country in 1990. The fourth and the last tropical cyclone to be formed in June of the 1990 Pacific typhoon season, [1] Typhoon Percy originated from an area of disturbed weather spawned by the Western Pacific monsoon trough on June 20. That same day,the disturbance was classified as a tropical depression as it slowly organized and on June 21,the depression obtained tropical storm intensity. After initially tracking westward,Percy turned towards the southwest while slowly deepening. During this time,Percy affected several of the Carolina Islands. Thirty homes were damaged and airline services were halted in and out of Yap. Farther south-southwest,seven homes were destroyed on the Ngulu Atoll. Furthermore,one boy was killed on Koror,where numerous homes lost their roofs and communication lines were downed. Percy then turned back to the west-northwest and became a typhoon on June 23. It then began to deepen at a faster rate,with Percy attaining its maximum intensity of 145 km/h (90 mph) on June 25. Two days later,on June 27,increased wind shear began to induce a weakening trend and the typhoon brushed Luzon,where eight people were killed and over 30,000 lost their homes. Despite that however,damages in the country was minor.
After tracking through the South China Sea,Percy made landfall southwest of Xiamen on June 29,and on the next day,dissipated inland. In the province of Quanzhou,four people were killed while 100,000 trees were damaged along with 1,000 power lines. One person was killed in Zhangzhou. In Dongshan,one individual died,four others suffered injuries,and a third of the trees were downed. Moreover,in the province of Shantou,95 structures were destroyed and 201 were damaged. A total of 16 people were killed throughout southeastern China and more than 100 others sustained injuries. Damage was estimated at US$28 million (¥190 million).
Typhoon Percy originated from the eastern end of the Western Pacific monsoon trough that spawned an area of disturbed weather that was first noted by the Joint Typhoon Warning Center (JTWC) on the morning of June 20. Satellite imagery showed signs of a well-defined low-level circulation and the disturbance was situated in a weakly divergent environment aloft along with persistent convection. [1] On the same day, the Japan Meteorological Agency (JMA) upgraded the system into a tropical depression. [2] [nb 1] The system gradually became more organized as its outflow expanded, and following a marked increase in convection, the JTWC issued a Tropical Cyclone Formation Alert on the system at 03:00 UTC on June 21. Following a ship report of 65 km/h (40 mph) winds, [1] both the JTWC and JMA upgraded the system into Tropical Storm Percy. [4] [nb 2] After initially tracking westward, Percy turned and tracked southwestward for 36 hours, a move predicted by tropical cyclone forecast models but not foreseen by the JTWC. Meanwhile, the storm slowly intensified, aided by the development of an anticyclone caused aloft. [1] As Percy continued to intensify, Percy began to track west-northwestward around another upper-level anticyclone that was formed in the southeast of Typhoon Ofelia which would later merge with a subtropical ridge to its north. [1] By June 22, Percy was upgraded into a severe tropical storm by the JMA. [4] Following the development of an outflow channel to its south, hints of an eye became visible on satellite imagery. Based on a Dvorak classification of T4.0/120 km/h (75 mph), the JTWC upgraded Percy into a typhoon on the evening of June 23, [1] with the JMA subsequently following suit in the morning of June 24. [2]
After moving away from the Caroline Islands, the typhoon began to intensify at a faster clip as an outflow channel to its north opened, [1] even though the eye was initially ragged. On the evening of June 24, the JTWC raised the intensity of the system to 200 km/h (125 mph). [4] Early on the next day, the JTWC estimated that Percy obtained its peak intensity based on the Dvorak estimate of T6.0/210 km/h (130 mph) and a clear eye. [1] Meanwhile, the JMA reported that Percy attained its maximum intensity of 145 km/h (90 mph) and a minimum barometric pressure of 960 mbar (28.3 inHg). [4] Increased vertical wind shear took toll on the storm, [1] and by June 27, the JTWC dropped the intensity of the storm to 175 km/h (110 mph) [4] as the storm passed over northeastern Luzon. [6] Overland, the storm weakened slightly, but remained a typhoon upon entering the South China Sea. [6] Both computer models and the JTWC expected Percy to begin recurvature; however, the subtropical ridge did not weaken as expected and Percy continued west-northwest instead. [1] At 00:00 UTC on June 29, the JMA downgraded Percy to a severe tropical storm, [2] although the JTWC suggested that Percy was still a typhoon at the time. [4] Shortly thereafter, Percy moved onshore around 130 km (80 mi) southwest of Xiamen. [6] At 06:00 UTC, the JTWC downgraded Percy into a tropical storm, noting that the storm had become less organized. [1] By June 30, both the JTWC and JMA had ceased tracking the system, which had dissipated inland. [1] [2]
During its formative stages, Percy affected several of the Caroline Islands. The storm first passed about 75 km (45 mi) south of Sorol. The island of Pegelmol was nearly cut in half by the system by storm surge. Taro patches, coconut trees, and other crops were almost completely wiped out. Percy came within 100 km (60 mi) of Yap to the south-southwest, where gusts of up to 105 km/h (65 mph) were felt. There, widespread flooding was reported due to storm surge, with most roads on the island requiring closure [1] and 30 homes being damaged. [7] Airline services in and out Yap were halted. [8] To the south-southwest of Yap, the island of Ngulu Atoll bore the brunt of the typhoon. Gusts of up to 130 km/h (80 mph) resulted in the destruction of all crops on the island. Furthermore, seven homes were demolished while many others only lost their roofs. However, there were no fatalities. The typhoon passed 230 km (145 mi) north of Koror, [1] where a boy perished when he was swept by rain into mangrove trees near his home. [9] Meanwhile, radio towers, power lines and television lines were downed as several houses lost their roofs. [1]
Typhoon Percy was the third typhoon of 1990, and second within a week, after Typhoon Ofelia, to threaten the Philippines. [10] In the province of La Union, landslides killed six people. In suburban Quezon City, police reported that a woman fell into a creek and drowned. The Philippine Red Cross indicated that a baby girl drowned and two other individuals were listed as missing in floods in the Ilocos Region. According to the social welfare department, 31,206 people in 6,143 families lost their homes. [11] Overall, damage in the country was light. [12]
The typhoon posed enough of a threat to Hong Kong to warrant a No 1. hurricane signal briefly, but it was dropped within 24 hours. Nevertheless, a pressure of 999.4 mbar (29.51 inHg) was measured at the Hong Kong Royal Observatory early on June 29. Waglan Island recorded a mean hourly wind of 31 km/h (19 mph), with a gust of 45 km/h (28 mph). High Island received 245 mm (9.6 in) of rain during the passage of the storm, the highest in the region, 193 mm (7.6 in) fell in a 24-hour period. These rains resulted in flooding, especially in the New Territories, where there was slight damage to crops. In Kwai Chung, floodwaters were 0.6 m (2.0 ft) deep, sweeping away a ten-year-old boy. Two other villages lost power and eleven people had to be evacuated. [6]
In the provinces of Fujian and Guangdong of China, power lines were downed. Farm production was reduced by 400 million catties in Fujian. In Nan'ao, gales persisted for about 10 hours and more than 410 mm (15 in) of rainfall was recorded, the heaviest in 300 years. Floodwaters there were up to 2 m (6.6 ft) deep. In Quanzhou, four people were killed, another was injured, and 100,000 ha (250,000 acres) of crops were damaged. There, 100,000 trees were damaged along with 1,000 power lines. One person was killed and tens of millions in damage was reported in Zhangzhou. In Dongshan, one individual died and four others suffered injuries. A total of 30,000 ha (74,000 acres) of asparagus were damaged. One vessel was sunk and seven more were damaged. One third of the trees there were downed. Damage in Dongshan was estimated at ¥27 million (US$5.7 million). [nb 3] Elsewhere, 270,000 ha (670,000 acres) of farmland was flooded, including 174,000 ha (430,000 acres) of rice in Shantou. Ninety-five structures were destroyed and two hundred and one were damaged. Roughly 20 km (12 mi) of a highway was destroyed. Damage totaled ¥49 million (US$10 million). Overall, greater than 6,650 homes were damaged and numerous fishing boats sunk. Sixteen people were killed throughout southeastern China [13] and more than 100 others sustained injuries. [6] Damage was estimated at US$28 million. [13]
The remnants of Percy would interact with a frontal low and stagnate along the Korea Strait, causing heavy rainfall in Japan on July 2. As a result of this, flooding was recorded in many parts of Saga Prefecture. This flooding event caused fifteen buildings to be partially destroyed, over 250 roads to be damaged in some way, seventeen levee collapses, four bridges to be washed away, five injuries, and two deaths in the prefecture. In total, in Saga Prefecture, Percy's remnants caused 57.976 billion yen (USD$397.65 million) in damage. [14] [15]
Typhoon Mike, known in the Philippines as Super Typhoon Ruping, of 1990 was the strongest typhoon to hit the Philippines since Typhoon Irma in 1981 and Typhoon Nina in 1987. Forming from an area of persistent convection over the Caroline Islands, Mike was first designated on November 6, 1990 and moved generally westward. Later that day, the depression strengthened to Tropical Storm Mike near Yap. Mike became a typhoon early on November 9, and subsequently entered a period of rapid deepening. Late on November 10, the typhoon reached its maximum intensity of 115 mph (185 km/h), as estimated by the Japanese Meteorological Agency. After weakening slightly, Mike made landfall in the central Philippines. The storm weakened considerably due to land interaction, only to briefly re-intensify on November 14. Typhoon Mike turned west-northwest and later north-northwest, avoiding land interaction with Vietnam. Vertical wind shear increased, and on November 15, Mike weakened below typhoon intensity. Early the next day, the storm passed over western Hainan Island, and degraded to a tropical depression that night. After briefly emerging into the Gulf of Tonkin, Mike passed over Northern Vietnam and southern China, where it dissipated on November 18.
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.
Typhoon Dot, known in the Philippines as Typhoon Saling, was the strongest storm of the 1985 season. Dot originated from a small area of thunderstorm activity in early to mid October. The system was first classified on October 11, and steadily intensified over the next few days. Dot attained typhoon strength on October 15, and subsequently entered a period of explosive deepening, which was not anticipated by forecasters. The next day the intensification rate slowed, but that evening, Dot attained its maximum intensify. A steady weakening trend began on October 17, though the system maintained typhoon intensity through the passage of the Philippines. After entering the South China Sea late on October 18, Dot briefly re-intensified, only to weaken as it approached Vietnam. On October 21, Dot struck Vietnam while still a typhoon, but dissipated the next day over the high terrain of the nation.
Typhoon Dan, known in the Philippines as Typhoon Saling, was the third of a series of tropical cyclones that impacted the Philippines and Vietnam in October 1989. The storm developed on October 6, and tracked generally westward throughout its course. After crossing Luzon, the typhoon emerged into the South China Sea and reached its peak intensity, with sustained 10-minute winds of 140 km/h (85 mph), 1-minute winds of 130 km/h (80 mph), and a minimum barometric pressure of 960 millibars. The storm moved ashore in central Vietnam and dissipated after moving inland. The storm caused extensive damage throughout its course. In the Philippines, Dan left hundreds of thousands homeless and killed 58 people. Power outages were extensive in the Manila region. In Vietnam, the storm's high winds and heavy rains caused extensive damage and loss of life. More than 500,000 structures were damaged or destroyed and at least 43 people were killed across the country.
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 Amy, known in the Philippines as Typhoon Gening, was the second typhoon to strike China in a week during mid-July 1991. An area of convection was first observed on July 13 within the vicinity of Yap. A tropical depression developed the next day. While initially tracking westward, the system slowly deepened, becoming Tropical Storm Amy on July 16. After briefly turning northwestward, Amy intensified into a typhoon on July 17. Continuing to intensify as it tracked through the Luzon Strait, Amy reached its peak intensity of 175 km/h (110 mph) on July 18. That evening, the typhoon began to show signs of weakening, although it was still believed to have been a typhoon when it made landfall in the province of Guangdong on July 19, becoming the strongest tropical cyclone to hit the province in 22 years. Once inland, the storm rapidly weakened, and by late on July 20, had dissipated completely.
Typhoon Clara, known in the Philippines as Typhoon Rubing, left flooding in the northern Philippines and southern China during September 1981. An area of disturbed weather was first detected on September 11 near Ponape. After moving westward, the system gradually became better organized and thunderstorm activity increased. On September 16, the system attained tropical storm status. Two days later, Clara attained typhoon intensity and subsequently began to deepen at a faster rate. On September 19, Clara reached maximum intensity, before making landfall along the northern tip of Luzon. Clara steadily weakened after interacting with land, but by late on September 20, Clara leveled off in intensity over the South China Sea. The next day, Clara moved ashore to the east-northeast of Hong Kong while still at typhoon intensity before rapidly dissipating over land.
Typhoon Rammasun, known in the Philippines as Typhoon Florita, was the first of four typhoons to contribute to heavy rainfall and deadly flooding in the Philippines in July 2002. The fifth tropical cyclone of the 2002 Pacific typhoon season, Rammasun developed around the same time as Typhoon Chataan, only further to the west. The storm tracked northwestward toward Taiwan, and on July 2 it attained its peak intensity with winds of 155 km/h (96 mph). Rammasun turned northward, passing east of Taiwan and China. In Taiwan, the outer rainbands dropped rainfall that alleviated drought conditions. In China, the rainfall occurred after previously wet conditions, resulting in additional flooding, although damage was less than expected; there was about $85 million in crop and fishery damage in one province.
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 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.
Typhoon Kim, known in the Philippines as Typhoon Osang, was the second typhoon in a week to directly affect the Philippines during July 1980. Like Typhoon Joe, Kim formed from the near equatorial monsoon trough in the northwestern Pacific Ocean on July 19. The disturbance tracked quickly westward-northwest underneath a subtropical ridge, reaching tropical storm strength on the July 21 and typhoon strength on July 23. After developing an eye, Kim began to rapidly intensify, and during the afternoon of July 24, peaked in intensity as a super typhoon. Several hours later, Kim made landfall over the Philippines, but the storm had weakened considerably by this time. Throughout the Philippines, 40 people were killed, 2 via drownings, and 19,000 others were directly affected. A total of 12,000 homes were destroyed and 5,000 villages were flooded. Less than a week earlier, the same areas were affected by Joe; however, Kim was considered the more damaging of the two typhoons. Land interaction took its toll on Kim, and upon entering the South China Sea, the storm was down below typhoon intensity. Kim continued northwestward but its disrupted circulation prevented re-intensification, and it remained a tropical storm until hitting southern China July 27 to the northeast of Hong Kong, where only slight damage was reported. Later that day, Kim dissipated.
Typhoon Dinah, known as Typhoon Luding in the Philippines, was the costliest tropical cyclone to form in the 1987 Pacific typhoon season. It also was the fourth typhoon to form during August 1987. An area of low pressure developed near Guam on August 19, and two days later, the low reached tropical storm intensity as it moved generally west. Intensification was initially gradual, with Dinah becoming a typhoon early on August 24, before it subsequently intensified at a faster pace. Dinah reached its highest strength on August 26 before turning northward on August 28 and into a less favorable conditions aloft, which prompted weakening. Dinah entered the Sea of Japan after passing near Okinawa on August 29, where Dinah leveled off in intensity. The system then began to recurve towards southwestern Japan, and after tracking through the area, Dinah transitioned into an extratropical cyclone on August 31, although the remnants could be traced for four more days as it approached the International Date Line.
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 Agnes, known in the Philippines as Typhoon Undang, was the fourth final tropical cyclone to affect the Philippines during the 1984 Pacific typhoon season. An area of disturbed weather developed near the equator and the Caroline Islands on October 28. Following an increase in organization, the cyclone was designated a tropical storm on October 31. After tracking northwest initially, Agnes turned west-northwest the next day, a course that the system would maintain for the rest of its lifetime. Agnes intensified into a typhoon on November 2, and on November 4, attained peak intensity. The storm then made landfall on Samar Island, part of the Philippines, at that intensity. The storm weakened over land, but re-intensified over the South China Sea; Agnes obtained a secondary peak intensity on November 6. The next day, Typhoon Agnes moved ashore Vietnam while still at typhoon intensity. The storm rapidly deteriorated over land and dissipated by November 8 over Thailand.
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 Faith, known in the Philippines as Typhoon Norming, struck both the Philippines and Vietnam during December 1998. A tropical disturbance developed within the vicinity of the western Caroline Islands during early December. At midday on December 8, the system developed into a tropical depression. Tracking northwest at a brisk pace, the depression gradually intensified, and was upgraded into a tropical storm at noon on December 9. Quickly intensifying, Faith turned to the west-northwest, and after tracking near Samar Island on the evening of December 10, Faith attained typhoon intensity. After clipping the northern tip of Palawan Island, the typhoon entered the South China Sea at peak intensity. Across the Philippines, 33 people were killed, with 30 others wounded and 36 others listed missing. A total of 6,423 homes were damaged and 3,234 houses were destroyed, leaving more than 20,000 homeless. Damage was estimated at $25.9 million, with $6.82 million from crops, $15.9 million from public infrastructure, and $3.37 million from private infrastructure.
Typhoon Robyn, known in the Philippines as Typhoon Openg, was a mid-season tropical cyclone that brushed Japan during August 1993. Typhoon Robyn originated from a near equatorial monsoon trough in the eastern Caroline Islands in late July. Tracking west-northwest, a tropical depression developed on August 1, and became a tropical storm the next day. Following an increase in organization, Robyn obtained typhoon intensity on August 5. The typhoon briefly tracked west before veering to the northwest while intensifying. On August 7, Robyn attained its peak intensity of 160 km/h (99 mph), with a barometric pressure of 940 mbar (28 inHg). After passing through the Ryukyu Islands, Robyn skirted past western Kyushu on August 9 while steadily weakening. Midday on August 10, Robyn lost typhoon intensity over the Sea of Japan. The next day, the system was declared an extratropical cyclone.
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.
Typhoon Ofelia, known as Typhoon Bising in the Philippines, was the first of two typhoons in 1990 to directly affect the Philippines within a week. Typhoon Ofelia originated from an area of disturbed weather embedded in the monsoon trough situated near the Caroline Islands. Slowly organizing, the disturbance tracked westward, and was designated a tropical depression on June 15. After an increase in convection, the depression was upgraded into a tropical storm on June 17. On June 19, Ofelia turned northwest and after development of a central dense overcast, Ofelia was upgraded into a typhoon late on June 20. After turning north, Ofelia obtained its maximum intensity following the development of an eye. The typhoon skirted past the northeastern tip of Luzon and near the east coast of Taiwan, commencing a rapid weakening trend. On the evening on June 23, Ofelia struck the southern portion of Zhejiang. The storm then began to track north, recurving towards the Korean Peninsula. The storm tracked through the province of Jiangsu, and at 00:00 UTC on June 24, transitioned into an extratropical cyclone, only to merge with a frontal zone on June 25.
Typhoon Eli, known in the Philippines as Typhoon Konsing, struck the Philippines and Hainan during mid-July 1992. A weak low pressure system developed in the Philippine Sea on July 7, which became a tropical depression on the next day. The depression tracked west-northwest and strengthened into a tropical storm on July 10. After turning more westward, Eli steadily intensified, and obtained typhoon intensity that evening. The storm attained its highest intensity of 130 km/h (80 mph) early on July 11 before striking northern Luzon. After entering the South China Sea, the storm maintained most of its intensity as it approached Hainan, although agencies disagree on how precisely strong it was. After passing through Hainan late on July 13, Eli passed through the Gulf of Tonkin on the next day before striking Vietnam, where Eli quickly dissipated.