Typhoon Omar( in 1992)

in typhoon •  7 years ago 

Typhoon Omar of 1992, known in the Philippines as Typhoon Lusing, was the strongest and costliest typhoon to strike Guam since Typhoon Pamela in 1976. The cyclone formed on August 23 from the monsoon trough across the western Pacific Ocean. Moving westward, Omar slowly intensified into a tropical storm, although another tropical cyclone nearby initially impeded further strengthening. After the two storms became more distant, Omar quickly strengthened into a powerful typhoon. On August 28, it made landfall on Guam with winds of 195 km/h (120 mph). The typhoon reached its peak intensity the next day, with estimated 1‑minute winds of 240 km/h (150 mph), making it a "super typhoon" according to the Joint Typhoon Warning Center (JTWC). Omar weakened significantly before striking eastern Taiwan on September 4, proceeding into eastern China the next day and dissipating on September 9.
On Guam, Omar caused one death and $457 million (1992 USD) in damage. Strong gusts up to 248 km/h (154 mph) left nearly the entire island without power for several days. The outages disrupted the water system and prevented the island-based JTWC from issuing advisories for 11 days. Omar damaged or destroyed 2,158 houses, leaving 3,000 people homeless. In response to the destruction, the island's building codes were updated to withstand winds of 250 km/h (155 mph), and insurance companies discontinued new policies for structures not made of concrete. While passing well north of the Philippines, the typhoon killed 11 people and wrought ₱903 million ($35.4 million) worth of damage to 538 houses. Omar then brushed the southern islands of Japan with strong gusts and light rainfall, causing ¥476 million JPY ($3.8 million USD) in crop losses. In Taiwan, scattered flooding caused three deaths and $65 million in damage, mostly to agriculture.
Metrological history:
Typhoon Omar originated from a tropical disturbance that was first noted on August 20 over the open Pacific Ocean, which exhibited persistent convection, or thunderstorms. During this early phase, two tropical cyclones dissipated and another became extratropical across the western Pacific basin; this caused the monsoon trough, which spawned most of the storms in the basin, to realign in a more climatologically appropriate manner. According to the Japan Meteorological Agency (JMA), Omar developed into a tropical depression at 1800 UTC on August 23. The Joint Typhoon Warning Center (JTWC) assessed a slower pace of strengthening, issuing a tropical cyclone formation alert at 2100 UTC before initiating advisories on Tropical Depression 15W on August 24.

As the depression traveled generally westward, the JTWC upgraded it to Tropical Storm Omar on August 25, and the JMA followed suit on the next day. Omar began to slow as it tracked westward. Outflow from nearby Tropical Storm Polly to the west produced a stream of strong wind shear over Omar, slowing intensification. The JTWC noted that the shear could decouple Omar's wind circulation from its convection, possibly weakening the storm. However, as Omar and Polly moved farther apart, a high-pressure ridge developed between the storms. This caused Omar to drift northward and then west-northwestward into a region with decreased shear, which allowed it to resume strengthening. Early on August 27, the JTWC upgraded the system to a typhoon, and an eye began to appear around 23:00 UTC that day. Omar entered a phase of rapid intensification on August 28, at which point the JMA also classified it as a typhoon. The typhoon made landfall on Guam soon after, with 1‑minute sustained winds of about 195 km/h (120 mph). The eye, 37 km (23 mi) in diameter, slowly crossed the northern portion of the small island over a period of 2.5 hours.

At 1800 UTC on August 29, Omar reached its peak intensity with 10‑minute sustained winds of 185 km/h (115 mph) and a minimum barometric pressure of 920 mbar (hPa; 27.17 inHg) as estimated by the JMA; this intensity was maintained for 24 hours before a steady weakening trend began. The JTWC estimated higher 1‑minute winds of around 240 km/h (150 mph), making Omar a super typhoon. Two days later, the typhoon came close enough to the Philippines to warrant monitoring from PAGASA, who named the storm Lusing. By 1500 UTC on September 3, the JMA downgraded Omar to a tropical storm, although the JTWC maintained its typhoon intensity through the next day. Heading generally westward, the storm made landfall on the east coast of Taiwan near Hualien City on September 4. After traversing the island in seven hours, Omar exited the coast of Yunlin County and emerged into the Taiwan Strait. The storm crossed the body of water and moved ashore in eastern China near Xiamen, Fujian, on September 5. Inland, Omar quickly degenerated into a tropical depression before turning west-southwest. It proceeded across southern China while heavily weakening, and completely dissipated over northern Vietnam on September 9.
Preparations and impact:
Guam
Ahead of the storm on August 25, the United States Department of Defense set the Condition of Readiness (COR) at stage 3 on Guam, indicating destructive winds were possible within 48 hours. A day later, the COR was raised to stage 2; all but two United States Navy ships were sortied from the harbor to prevent damage, and the remainder rode out the storm southwest of Guam. On August 28, COR 1 was declared, the highest level. In response, all fixed-wing aircraft and helicopters on the island were moved into hangars or transported to Japan or the Philippines. All schools were closed for the duration of Omar's passage over Guam. Flight operations were suspended for at least two days, stranding 5,000 passengers on the island. About 3,100 people rode out the storm in emergency shelters.

Omar was the strongest and most damaging typhoon to hit Guam since Typhoon Pamela in 1976. The typhoon was felt on all parts of Guam; tropical-storm-force winds affected the island for 16 hours, and wind gusts were estimated to have reached 248 km/h (154 mph) in areas beneath the western eyewall. However, the high winds caused the anemometer at Hagåtña to fail during the eye's passage, and the radar at Andersen Air Force Base was lost, preventing accurate wind speed assessments. The lowest barometric pressure was 940 mbar (27.76 inHg) at Apra Harbor. Omar's slow movement resulted in prolonged heavy rainfall, peaking at 519 mm (20.44 in) at the Guam National Weather Service Office in Tiyan and reaching 417 mm (16.41 in) at Andersen AFB.

Damage on Guam was heaviest from the central region to the northern coast, in particular to tourist areas and military bases. The Naval Computer and Telecommunications Area Master Station was shut down due to power outages and water damage to the generators. Two US Navy ships, the USS Niagara Falls (AFS-3) and the USS White Plains (AFS-4)—both naval supply ships—went aground due to rough seas and strong winds, and the dry dock at Apra Harbor was washed ashore. Omar destroyed dozens of businesses on the island. High winds knocked a crane into an apartment building and downed 400 wooden and 20 concrete power poles across Tumon, leaving 70% of the island without power. Throughout Guam, Omar disrupted transportation and communication systems, and led to the failure of water pumping systems. Landslides covered roads, and low-lying areas were flooded. About 2,000 homes were destroyed and another 2,200 were damaged to varying degrees, displacing nearly 3,000 people. Destruction was heaviest to wooden structures; buildings made of concrete fared relatively well during the storm. Island-wide, damage totaled $457 million, split nearly evenly between the military bases and civilian damage. One person died on Guam, and more than 200 people required emergency treatment—including about 80 injured by flying debris.title.gif

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