Typhoon Oliwa

Typhoon Oliwa
Typhoon (JMA scale)
Category 5 (Saffir–Simpson scale)

Typhoon Oliwa in the western Pacific
Formed September 2, 1997
Dissipated September 20, 1997
(Extratropical after September 17, 1997)
Highest winds 10-minute sustained: 185 km/h (115 mph)
1-minute sustained: 260 km/h (160 mph)
Lowest pressure 915 hPa (mbar); 27.02 inHg
Fatalities 12 total
Damage $50.1 million (1997 USD)
Areas affected Northern Mariana Islands and Japan
Part of the 1997 Pacific hurricane season, 1997 Pacific typhoon season

Typhoon Oliwa was one of a record eleven super typhoons in the 1997 Pacific typhoon season. It formed in the central Pacific Ocean on September 2 to the southwest of Hawaii, but it became a typhoon in the western Pacific. Oliwa explosively deepened on September 8, increasing its winds from 85 mph to 160 mph in a 24‑hour period. Afterward, it slowly weakened, and after passing east of Okinawa, Oliwa turned northeast and struck Japan with winds of 85 mph (140 km/h). There, it affected 30,000 people and killed 13; thousands of houses were flooded, and some were destroyed.[1] Offshore South Korea, the winds and waves wrecked 28 boats, while one boat went missing with a crew of 10 people. Typhoon Oliwa dissipated on September 19 in northern Pacific Ocean near the International Date Line.

Meteorological history

Map plotting the track and intensity of the storm according to the Saffir–Simpson hurricane wind scale

The origins of Typhoon Oliwa were from an unusually eastward extension of the monsoon trough in late August 1997.[2] The tropical disturbance organized southwest of Hawaii, and slowly organized. On September 2, the Central Pacific Hurricane Center (CPHC) initiated advisories on Tropical Depression Two-C about 590 miles (950 km) southwest of Johnston Island, slightly east of the International Date Line. The depression quickly attained tropical storm status, and the CPHC gave it the name "Oliwa", meaning "Oliver" in the Hawaiian language.[3]

A moderately powerful ridge persisted north of Tropical Storm Oliwa, which caused a slow west to west-northwest track. Water temperatures were slightly warmer than usual, and there was a favorable upper-level environment for strengthening. Initially, however, Oliwa was somewhat disorganized on satellite imagery, and on September 4, as it crossed the International Date Line, there may have been multiple circulations. Upon entering the western Pacific Ocean, the Joint Typhoon Warning Center (JTWC) and the Japan Meteorological Agency (JMA) began issuing advisories on the system (9719).[3][4] Despite the favorable conditions, further intensification was slow, and it reached typhoon status - winds of at least 75 mph (120 km/h) - on September 8. Prior to that time, Oliwa co-existed with a weak tropical cyclone that formed in a similar location in the south Pacific.[5]

About twelve hours after reaching typhoon status, Oliwa began to undergo unexpected explosive deepening. In a 24‑hour period, the JTWC assessed the typhoon as nearly doubling in intensity, from 85 to 160 mph (140 to 260 km/h 1-min winds), while the pressure dropped 69 mbar to a minimum of 898 mbar; based on the estimated intensity, the JTWC classified Oliwa as a super typhoon.[5] The JMA, which is the official agency of the western Pacific, assessed Oliwa as reaching a peak of 115 mph (185 km/h 10-min winds), with a pressure of 915 mbar.[4] Around that time, satellite imagery indicated a possible eyewall mesovorticy, which is a small scale rotational feature found in the eyewall of an intense tropical cyclone. Additionally, concentric eyewalls developed in the center of Oliwa, which typically occur in strong typhoons.[5]

After maintaining peak intensity for 36 hours, Oliwa gradually weakened as it continued to the west-northwest, during which it passed through the Northern Marianas Islands. On September 14, the typhoon slowed to the north of Okinawa, and it turned to the northeast toward Japan.[5] As a weakened typhoon, Oliwa moved ashore on Makurazaki, Kagoshima, Kyushu with winds of 85 mph (140 km/h) late on September 15. It weakened to tropical storm strength while crossing Japan, and deteriorated further to tropical depression status on September 16.[4] On September 17, the JTWC issued the final advisory on Oliwa while it was in the eastern portion of the Sea of Japan.[5] The JMA maintained advisories as the storm crossed northern Japan, and it accelerated over the open Pacific Ocean. On September 19, Oliwa dissipated near the International Date Line to the south of the Aleutian Islands.[4]

Impact and records

While weakening after peaking in intensity, Oliwa passed about 60 miles (95 km) north of Agrihan in the Northern Marianas Islands. Sustained winds on the island reached 75 mph (120 km/h), with gusts to 85 mph (135 km/h). The winds downed two coconut trees onto a radio antenna, which left the island temporarily without contact to the outside world.[6] On the Japanese island of Kyushu, where Oliwa made landfall as a weakened typhoon, thousands of homes were flooded, and dozens were destroyed.[5] Its slow movement caused heavy rainfall that created a mudslide in Tashiro, Kagoshima, killing three people. Across Kagoshima Prefecture, officials issued evacuations due to flooding, although many did not heed the warnings. In the prefecture, the typhoon destroyed 131 buildings and damaged about 1,700 more. Damage there was estimated at 14 million yen (1997 JPY, $150,000 in 1997 USD).[7] Across Japan, Typhoon Oliwa caused 12 fatalities and displaced a total of 30,000 people. Total damage amounted to 4.36 billion yen ($50.1 million USD).[8][9] Offshore the South Korea coast, the winds and strong waves wrecked 28 vessels, and 10 people were reported missing from one ship.[5]

Typhoon Oliwa was one of eleven super typhoons in the western Pacific, which is tied to the previous record of eleven; a typical typhoon season has four super typhoons. The period of heightened activity was the result of one of the most powerful El Niño events on record. The track Oliwa was unusual, due to its origin as a cyclone from the central Pacific Ocean and its path over the Northern Marianas Islands and Japan.[5] The typhoon was one of only two during the season to undergo explosive deepening, which is a decrease in barometric pressure of ≥2.5 mbar per hour for a period of at least 12 hours. In 24 hours, the pressure dropped 69 mbar, which averages 2.9 mbar per hour; such values are usually estimated in the western Pacific using the Dvorak technique.[2]

The name was not retired, although due to the low activity in the central Pacific Ocean, the name will not be used for several years.

See also

References

  1. ↑ Benjamin C. Hablutzel, ,"National Weather Service",04/12/2012
  2. 1 2 Mark A. Lander and Charles P. Guard, Joint Typhoon Warning Center (2001). "Western North Pacific, North Indian Ocean, and Southern Hemisphere Tropical Cyclones of 1997". American Meteorological Society. Retrieved 2010-03-13.
  3. 1 2 Central Pacific Hurricane Center (2007). "The 1997 Central Pacific Tropical Cyclone Season". Retrieved 2010-03-13.
  4. 1 2 3 4 Japan Meteorological Agency (1997). "Best Track of the 1997 Pacific Typhoon Season". Retrieved 2007-04-29.
  5. 1 2 3 4 5 6 7 8 Joint Typhoon Warning Center (2001). "1997 Annual Tropical Cyclone Report" (PDF). Retrieved 2010-03-13.
  6. ↑ National Climatic Data Center (1997). "Event Report". Retrieved 2010-03-13.
  7. ↑ Shimashita Kagoshima University Faculty of Science (1997-10-06). "Disaster by Typhoon No. 9719". Retrieved 2010-04-12.
  8. ↑ "Typhoon 199719 災害情報" (in Japanese). National Institute of Informatics. 1998. Retrieved July 21, 2010.
  9. ↑ Dartmouth Flood Observatory (2008). "1997 Flood Archive". Retrieved 2010-03-13.
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