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Typhoon Parma

Pacific typhoon in 2009

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Through Rain, Flood and China

Typhoon Parma was named by PAGASA as Pepeng when it entered the Philippine Area of Responsibility days after Typhoon Ketsana wreaked havoc on the country; Parma spared the capital and instead lashed the northern part of Luzon island. Parma added to the damage brought about by the earlier Typhoon Ketsana, affecting thousands of families on the north, especially in the province of Pangasinan where the San Roque Dam inadvertently released water to prevent its breach. However, in the first week of October, Parma interacted with the incoming Typhoon Melor on the Pacific (via a Fujiwhara interaction), rendering it stationary as it made landfall on Southern Taiwan. Days later, the greatly weakened Parma retreated back to Luzon, making further landfalls on Ilocos Norte and Cagayan. The now Severe Tropical Storm Parma then began to wane its strength, as it crossed Luzon island for the second time. It then emerged on the South China Sea as a tropical depression, before restrengthening into a tropical storm and striking Hainan and Vietnam before finally dissipating in October 14.

Parma's bizarre, long-lived, and erratic track over northern Luzon led to near-record levels of rainfall, causing devastating flooding that led to Parma becoming one of the deadliest typhoons to hit the Philippines in a decade. Due to the high death toll and damages, both the JMA and PAGASA retired Parma and Pepeng from their respective naming lists.

Meteorological history

During September 26, the Joint Typhoon Warning Center (JTWC) started to monitor an area of convection that was located about 445 km (275 mi), to the southeast of Guam. The system had an elongated low-level circulation center with convection developing around the center. Upper level analysis showed that the system was located in an area of low vertical wind shear and had a good poleward outflow into a tropical upper tropospheric trough (TUTT). During the next day, convection started to consolidate before both the Japan Meteorological Agency (JMA) and the JTWC initiated advisories on the system, with the JTWC designating it as Tropical Depression 19W. After being classified, the depression remained weak and poorly organized, as it lay close to Tropical Storm 18W. During September 28, as the depression moved away from 18W, the JTWC reported that the depression had intensified into a tropical storm despite it remaining poorly organized, and acquired the name Parma.

Parma started to intensify to a typhoon as it moved closer to the Philippines, and soon underwent rapid intensification as it developed a pinhole eye. On October 1, Parma reached its peak intensity with winds of 250 km/h (155 mph). Afterwards, Parma started a weakening trend as it moved closer to the Philippines, and on October 3 made landfall on northern Luzon, Philippines. During its landfall in the Philippines, Parma began to travel northwest towards China. It slowed down and weakened (due to interactions with Typhoon Melor), then turned back south towards the Philippines. Parma made a second landfall on October 6 with sustained winds of 105 kilometres per hour (65 mph). It weakened to a tropical depression before emerging off the east coast of Luzon on October 7, remaining stationary for a day. On October 8 it made a third landfall the eastern coast of Cagayan, then moved slowly across Luzon, eventually emerging in the South China Sea. After regaining some strength, it travelled westward and hit the island of Hainan, China, with winds of 39 miles per hour (63 km/h). It then made a final landfall in Vietnam on October 13, and dissipated over the country on October 14.

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