Typhoon Gene

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Map key
Saffir–Simpson scale
  Tropical depression (≤38 mph, ≤62 km/h)
  Tropical storm (39–73 mph, 63–118 km/h)
  Category 1 (74–95 mph, 119–153 km/h)
  Category 2 (96–110 mph, 154–177 km/h)
  Category 3 (111–129 mph, 178–208 km/h)
  Category 4 (130–156 mph, 209–251 km/h)
  Category 5 (≥157 mph, ≥252 km/h)
  Unknown
Storm type
Disc Plain black.svg Tropical cyclone
Solid black.svg Subtropical cyclone
ArrowUp.svg Extratropical cyclone, remnant low, tropical disturbance, or monsoon depression

The origins of Typhoon Gene, the fifth tropical cyclone of September 1990, can be traced back to an area of disturbed weather with a surface pressure of 1008 mbar (29.8 inHg) first noted by the Joint Typhoon Warning Center (JTWC) at 06:00 UTC early on September 18. Little development occurred over the next five days, [1] although the Japan Meteorological Agency (JMA) classified the disturbance as a tropical depression on the morning of September 22. [2] [nb 1] A Tropical Cyclone Formation Alert (TCFA) was issued at 06:00 UTC on September 23, followed by an increase in the disturbance's organization. [1] Around that time, the system was located roughly 1,170 km (725 mi) south-southeast of Okinawa. [4] Further development was aided by a tropical upper tropospheric trough to its west and the warm ocean waters of the Kuroshio Current. Initially, the disturbance tracked generally westward, south of a subtropical ridge. Shower activity steadily increased and a Dvorak estimate of T2.0/55 km/h (35 mph) prompted the JTWC to designate it a tropical depression midday on September 23. [1] Twelve hours later, the JMA reported that the depression had strengthened into a tropical storm, [5] [nb 2] and after the system improved in organization and its outflow expanded, [1] the JTWC followed suit. [7] At this time, Tropical Storm Gene was situated 980 km (610 mi) south-southeast of Okinawa. [4]

Tropical Storm Gene intensified at the climatological rate of one T number per day as it tracked westward on a course initially resembling a straight runner. [1] At 00:00 UTC on September 25, the JMA classified Gene as a severe tropical storm. [2] The storm then turned northwest as it approached a break in the subtropical ridge. Although restricted upper-level outflow prevented rapid intensification, a Dvorak intensity estimate of T4.0/120 km/h (75 mph) [1] lead to both agencies to declare Gene a typhoon on the evening of September 25. [5] Around the time of the upgrade, Gene was located 380 km (235 mi) south-southwest of Okinawa. [4] At 00:00 UTC on September 26, the JMA raised its intensity to 130 km/h (80 mph) for its maximum sustained winds, while the agency also estimated a minimum pressure of 965 mbar (28.5 inHg). [2] However, the JTWC suggested that Gene was still slowly strengthening, and did not attain its maximum intensity of 90 mph (145 km/h) until 18:00 UTC that day. [7]

Gene recurved to the northeast on September 27 in response to a shortwave trough [1] while passing through the Ryukyu Islands. [4] According to the JTWC, Gene maintained its peak intensity until 06:00 UTC on September 29, [1] although the JMA estimated that a weakening trend had begun six hours earlier. [2] The typhoon continued to recurve and skirted Kyushu and Shikoku on September 29 before tracking just south of Honshu the following day. [4] Based on surface observations, the JTWC downgraded Gene into a tropical storm at 06:00 UTC that day, [1] with the JMA doing the same at around the same time. The JMA classified Gene as an extratropical cyclone at noon, [2] even though the JTWC did not follow suit until six hours later. [1] Finally, the JMA stopped tracking the extratropical remnants of Gene on October 1. [5]

Impact

The typhoon dropped heavy rainfall across much of the Japanese archipelago. [8] A peak rainfall total occurred of 619 mm (24.4 in) in the city of Miyazaki, 563 mm (22.2 in) of which fell in a 24-hour time span. [9] A peak hourly rainfall total of 91 mm (3.6 in) was observed at Shimizu. [10] Moreover, a maximum wind gust of 159 km/h (99 mph) was recorded on Muroto. [11] In Tokushima Prefecture, a minimum central pressure of 970 mbar (28.6 inHg) was observed. [12]

In Okinawa Prefecture, one person was hurt and damage accumulated to ¥77.2 million yen. [13] On Shikoku Island, little damage was reported. [12] A total of 214 homes were damaged in Kōchi Prefecture and ten others were leveled. There were also eleven landslides. Damage in the prefecture totaled ¥1.2 billion yen. [14] Two people were killed in Miyazaki Prefecture because of landslides and another drowned into a river, [15] and an additional ten were wounded. Throughout the prefecture, 4,688 houses suffered damage, while an additional ninety-two dwellings were destroyed, which led to 18,449 homeless. Furthermore, 2,700 households lost power in the city Miyazaki while 8,339 households lost power in Nichinan. Prefecture-wide, damage totaled ¥10.8 billion yen, primarily from the western portion of the prefecture. [16] In Kagoshima Prefecture, five people suffered injuries, including two in a landslide. A total of 229 houses were damaged and seventy more were destroyed; consequently, 194 people lost their homes. In the town of Takayama, located in Kagoshima Prefecture, over 100,000 fish died. According to authorities, nearly 30,000 residencies were left without power. Across the prefecture, damage amounted to ¥15.3 billion yen. [17] Throughout the entire island of Kyushu, 150 national flights were cancelled. [18]

In Wakayama Prefecture, sixty-seven homes were damaged and damage was estimated at ¥187 million yen. Four buildings were destroyed in Shingu City, resulting in twenty homeless. [19] Three flights were cancelled and three others were delayed at the Okayama Airport. [20] Elsewhere, in Kanagawa Prefecture, heavy rains triggered fifty-nine landslides. A total of 1,713 homes were damaged and 915 others were destroyed, which resulted in 2,956 homeless individuals. [21] Ninety bullet trains were cancelled between Tokyo and Osaka. [15] In nearby Oshima Subprefecture, heavy rains forced the closure of nine roads. Throughout Tokyo, eight structures were damaged and twelve flights were delayed. [22] A 49-year-old man was killed in a landslide in Shizuoka. [15] Across Shizuoka prefecture, heavy rains caused 143 landslides. There, 1,697 homes were damaged, with 144 others destroyed. Roads were damaged in 162 locations. Nearly 900 ha (2,225 acres) of arable land was inundated. [23] In Mie Prefecture, two people were presumed dead after they drowned in a river and three others were hurt. A total of 1,079 homes were damaged and thirty-nine others were demolished, which resulted in 130 people homeless. Damage there was assessed at ¥2.62 billion yen. [24] At the Narita International Airport, sixty-eight flights were delayed. In Chiba Prefecture, there was one minor injury. A total of 213 houses were destroyed and eighteen others were damaged. Embankments were damaged at eighty-five sites across the prefecture. [25] Seventy-five individuals lost their homes in Yamanashi Prefecture, where damage totaled to ¥716 million yen. [26] Elsewhere, 304 dwellings were damaged and twenty-eight were demolished along coastal areas of Saitama Prefecture. [27] Damage in Gunma prefecture totaled ¥53.8 million yen. [28]

The typhoon hit the Japanese archipelago ten days after Typhoon Flo, [29] which claimed forty lives and caused over $4 billion in damage. [30] The storm also forced the cancellation of the final round of the Top Cup Tokai Classic. [31] Much of the southwestern portion of the country suffered the worst damage from the typhoon. [29] Nationwide, six fatalities were reported and twenty others sustained injuries. A total 210 houses were destroyed while 13,318 others were flooded. [8] Landslides triggered by heavy rain were reported at 340 places and roads were damaged at 182 locations. [4] All Nippon Airways cancelled ninety domestic flights and Japan Airlines cancelled ten flights. [15] More than 200,000 people were affected by cancellation of flights and train services. [4] Thirty-one ships and 10,560 acres (4,273 ha) of farmland were damaged. Monetary damage totaled ¥22.9 billion yen or US$158 million. [8] [nb 3] [nb 4]

See also

Notes

  1. ↑ The Japan Meteorological Agency is the official Regional Specialized Meteorological Center for the western Pacific Ocean. [3]
  2. ↑ Wind estimates from the JMA and most other basins throughout the world are sustained over 10 minutes, while estimates from the United States-based Joint Typhoon Warning Center are sustained over 1 minute. 10-minute winds are about 1.14 times the amount of 1-minute winds. [6]
  3. ↑ All currencies are converted from Japanese yen to United States Dollars using this with an exchange rate of the year 1990.
  4. ↑ All damage totals are in 1990 values of their respective currencies.

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References

  1. 1 2 3 4 5 6 7 8 9 10 Joint Typhoon Warning Center; Naval Pacific Meteorology and Oceanography Center (1992). Annual Tropical Cyclone Report: 1990 (PDF) (Report). United States Navy, United States Air Force. pp. 152, 153. Archived from the original (PDF) on October 19, 2016. Retrieved July 13, 2017.
  2. 1 2 3 4 5 Japan Meteorological Agency (October 10, 1992). RSMC Best Track Data – 1990–1999 (Report). Archived from the original (.TXT) on January 22, 2013. Retrieved July 13, 2017.
  3. ↑ "Annual Report on Activities of the RSMC Tokyo – Typhoon Center 2000" (PDF). Japan Meteorological Agency. February 2001. p. 3. Retrieved July 13, 2017.
  4. 1 2 3 4 5 6 7 Hong Kong Observatory (1991). "Part III – Tropical Cyclone Summaries". Meteorological Results: 1990 (PDF). Meteorological Results (Report). Hong Kong Observatory. p. 15. Retrieved July 13, 2017.
  5. 1 2 3 Kenneth R. Knapp; Michael C. Kruk; David H. Levinson; Howard J. Diamond; Charles J. Neumann (2010). 1990 GENE (1990261N12141). The International Best Track Archive for Climate Stewardship (IBTrACS): Unifying tropical cyclone best track data (Report). Bulletin of the American Meteorological Society. Retrieved July 13, 2017.
  6. ↑ Christopher W Landsea; Hurricane Research Division (April 26, 2004). "Subject: D4) What does "maximum sustained wind" mean? How does it relate to gusts in tropical cyclones?". Frequently Asked Questions. National Oceanic and Atmospheric Administration's Atlantic Oceanographic and Meteorological Laboratory. Retrieved July 13, 2017.
  7. 1 2 Typhoon 21W Best Track (TXT) (Report). Joint Typhoon Warning Center. December 17, 2002. Retrieved July 13, 2017.
  8. 1 2 3 Asanobu, Kitamoto. Typhoon 199020 (Gene). Digital Typhoon (Report). National Institute of Informatics. Retrieved July 14, 2017.
  9. ↑ Asanobu, Kitamoto. AMeDAS MIYAZAKI (87376) @ Typhoon 199020. Digital Typhoon (Report). National Institute of Informatics. Retrieved July 22, 2017.
  10. ↑ Asanobu, Kitamoto. AMeDAS SHIMIZU (74516) @ Typhoon 199020. Digital Typhoon (Report). National Institute of Informatics. Retrieved July 22, 2017.
  11. ↑ Asanobu, Kitamoto. AMeDAS MUROTOMISAKI (74371) @ Typhoon 199020. Digital Typhoon (Report). National Institute of Informatics. Retrieved June 30, 2017.
  12. 1 2 Asanobu, Kitamoto. Typhoon 1990-895-12. Digital Typhoon (Report). National Institute of Informatics. Retrieved July 14, 2017.
  13. ↑ Asanobu, Kitamoto. Typhoon 1990-927-03. Digital Typhoon (Report). National Institute of Informatics. Retrieved July 14, 2017.
  14. ↑ Asanobu, Kitamoto. Typhoon 1990-893-10. Digital Typhoon (Report). National Institute of Informatics. Retrieved July 14, 2017.
  15. 1 2 3 4 "Four Dead, 13 Injured In Storm". Associated Press. September 30, 1990.
  16. ↑ Asanobu, Kitamoto. Typhoon 1990-830-07. Digital Typhoon (Report). National Institute of Informatics. Retrieved July 14, 2017.
  17. ↑ Asanobu, Kitamoto. Typhoon 1990-827-15. Digital Typhoon (Report). National Institute of Informatics. Retrieved July 14, 2017.
  18. ↑ "Japanese typhoon leaves 1 missing". Toronto Star. Reuters. September 30, 1990.
  19. ↑ Asanobu, Kitamoto. Typhoon 1990-777-06. Digital Typhoon (Report). National Institute of Informatics. Retrieved July 14, 2017.
  20. ↑ Asanobu, Kitamoto. Typhoon 1990-768-14. Digital Typhoon (Report). National Institute of Informatics. Retrieved July 14, 2017.
  21. ↑ Asanobu, Kitamoto. Typhoon 1990-670-11. Digital Typhoon (Report). National Institute of Informatics. Retrieved July 14, 2017.
  22. ↑ Asanobu, Kitamoto. Typhoon 1990-662-11. Digital Typhoon (Report). National Institute of Informatics. Retrieved July 14, 2017.
  23. ↑ Asanobu, Kitamoto. Typhoon 1990-656-18. Digital Typhoon (Report). National Institute of Informatics. Retrieved July 14, 2017.
  24. ↑ Asanobu, Kitamoto. Typhoon 1990-651-11. Digital Typhoon (Report). National Institute of Informatics. Retrieved July 14, 2017.
  25. ↑ Asanobu, Kitamoto. Typhoon 1990-648-16. Digital Typhoon (Report). National Institute of Informatics . Retrieved July 14, 2017.
  26. ↑ Asanobu, Kitamoto. Typhoon 1990-638-10. Digital Typhoon (Report). National Institute of Informatics. Retrieved July 14, 2017.
  27. ↑ Asanobu, Kitamoto. Typhoon 1990-626-14. Digital Typhoon (Report). National Institute of Informatics. Retrieved July 14, 2017.
  28. ↑ Asanobu, Kitamoto. Typhoon 1990-624-13. Digital Typhoon (Report). National Institute of Informatics. Retrieved July 14, 2017.
  29. 1 2 "Tokyo hit by weakened Typhoon Gene". United Press International. September 30, 1990.
  30. ↑ Asanobu, Kitamoto. Typhoon 199019 (Flo). Digital Typhoon (Report). National Institute of Informatics. Retrieved July 14, 2017.
  31. ↑ "Typhoon helps Marsh". The Advertiser. October 1, 1990.
Typhoon Gene (Oyang)
Gene sept 29 1990 0518Z.jpg
Typhoon Gene on September 29 1990
Tropical cyclones of the 1990 Pacific typhoon season
1990 Pacific typhoon season summary.jpg
STS
Koryn
TS
Lewis
TY
Marian
TD
TD
TD
TD
TD
TD
TD
04W
STS
Nathan
TY
Ofelia
TY
Percy
TD
TD
TS
Robyn
TD
TD
TD
TD
STS
Tasha
TY
Steve
TY
Vernon
STS
Winona
TY
Yancy
TS
Aka
TY
Zola
TY
Abe
TY
Becky
TD
Cecil
TY
Dot
TY
Ed
TY
Flo
TY
Gene
TY
Hattie
TS
Ira
TD
Jeana
TY
Kyle
TS
Lola
TY
Mike
STS
Nell
TD
Susang
TY
Owen
TY
Page
TY
Russ
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