Tropical Storm Warren (1984)

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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 precursor of Tropical Storm Warren was first noted on October 17 as a poorly organized area of convection over 550 km (340 mi) northeast of Mindanao Island. Initially, synoptic data suggested that the storm's circulation was broad, ill-defined, and positioned over the monsoon trough. The disturbance began to encounter lower wind shear, prompting a small increase in organization. At 15:00 UTC on October 18, a Tropical Cyclone Formation Alert (TCFA) was issued. The alert was cancelled less than 24 hours later, however, in response to a decrease in the storm's convection, as well as, strong wind shear and its close proximity to land. Over the next few days, the system moved over the Philippines, disrupting its surface circulation. Moving west-southwest, the disturbance entered the South China Sea on October 22. Despite initially remaining poorly organized, conditions aloft became much more conducive for development that evening, and aided by the monsoonal flow, the system developed a well-defined surface circulation. [1] At 00:00 UTC on October 23, both the Joint Typhoon Warning Center (JTWC) and the Japan Meteorological Agency (JMA) started tracking the system. [2] [nb 1] [4] The aforementioned circulation was at first exposed from the deep convection, but by 03:00 UTC on October 23, the storm had rapidly become better organized. Following a further increase in the system's organization, a second TCFA was issued at 11:30 UTC. Based on a Dvorak estimate of T2.5, the JTWC upgrade the system into a tropical depression at 18:00 UTC, [1] although post-season analysis from the agency suggests that the cyclone was a tropical storm by this time. Early on October 24, the JMA followed suit and upgraded Warren into a tropical storm. [5] [nb 2] Also around this time, the Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) started tracking the storm and assigned it with the local name Reming. [7]

Initially, Tropical Storm Warren drifted north [1] and then north-northwest. [8] Later on October 24, the center once again became partially exposed from the deep convection. Thereafter, Warren began to move erratically. [1] Early on October 25, the JMA classified Warren as a severe tropical storm. [2] After performing a small cyclonic loop, Warren, still embedded in the monsoon trough, began to drift westward, while a mid-latitude cyclone was located to the cyclone's north. [1] Later that day, Warren existed PAGASA's area of responsibility. [9] At 06:00 UTC on October 26, the JTWC designated Warren a typhoon while increasing the intensity of Warren to 120 km/h (75 mph), its maximum intensity. Meanwhile, the JMA estimates that Warren peaked in intensity, with winds of 115 km/h (70 mph) and a minimum barometric pressure of 980 mbar (29 inHg), an intensity it would remain at for several days. [5] Starting midday on October 26, Warren stalled out for the next 12 hours, only to drift east-northeast in response to the inflow to Typhoon Vanessa and a trough to its north. On October 28, after re-entering PASAGA's warning responsibility, [9] Warren slowed and made a cyclonic turn back to the east-northeast as the trough moved to the east of Warren and a subtropical ridge became center to the north of the cyclone. [1]

By October 29, Warren began to expand in size in response to a monsoonal surge of moisture into the South China Sea. This also caused the storm to inherit cooler, drier air, which prompted weakening [1] while also recurving towards the northeast. [8] At 00:00 UTC on October 29, the JTWC downgraded Warren into a tropical storm, [4] though the JMA would not follow suit until 36 hours later. [2] On August 30, the storm exited PASAGA's warning zone. [9] Thunderstorm activity continued to decrease, and by October 31, the low-level center had become displaced to the convection and the upper-level center. At 06:00 UTC that day, the JTWC issued the final warning on the cyclone while it was still producing winds of 55 km/h (35 mph). Despite this, the storm's center remained well-defined for an additional 24 hours. The remnants of the storm later crossed the coast of Vietnam, with winds of 55 to 65 km/h (35 to 40 mph). Late on November 1, the circulation had become less defined and increasingly difficult to locate, and the JTWC estimated that Warren dissipated the next day. [1] During the afternoon of November 2, the JMA ceased tracking Warren. [2]

Impact

The precursor disturbance to Warren drenched the nations in heavy rains that led to the deaths of 17. [10] As a result of Warren's turn to the west on October 28, the storm posed a serious threat to the Philippines. All U.S. Navy and Air Force bases in the region were placed in "Condition of Readiness I" early that day. Although no major damage ultimately occurred on the naval bases, winds of 45 km/h (27 mph) and 222 mm (8.74 in) of rain were recorded at Clark Air Base. [1] In the province of Bataan, 30 houses were destroyed, which led to 200 people without a home. [11] A family of 13 died after their house was buried in a landslide in Aurora. [12] Elsewhere, twelve other people died due landslides. [13]

Offshore Marinduque Island, strong waves generated by the storm sunk a 745 t (745,000 kg) vessel, Venus, [11] within three minutes. [14] Officially, the ship consisted of 83 passengers and 42 crewmen when it left Laoang for Samar Island, even though the captain claimed that there were as many as 240 aboard. [15] Later reports indicates that vessel had 200 passengers and 42 crewman on board. [16] A total of 174 were rescued, [13] including 96 people that were rescued via a fishing boat [11] and many others that was rescued by fishermen. [16] Twenty-nine people, [17] including two children, drowned due to the incident. [11] Nearby, a cargo container ship, the Lorcon 8, sank, but all 19 crewmen were rescued. [10] Nationwide, 73 people perished, [17] with 18 others hurt. A total of 10,815 people or 1,914 families were directly affected by the typhoon. [18] Furthermore, 740 houses were destroyed, with an additional 891 damaged. Damage was estimated at $239,000, with $59,000 from crops and $180,000 from both public and private infrastructure. [9] [nb 3]

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 Philippine currencies are converted to United States Dollars using Philippines Measuring worth with an exchange rate of the year 1984.

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References

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  2. 1 2 3 4 Japan Meteorological Agency (October 10, 1992). RSMC Best Track Data – 1980–1989 (Report). Archived from the original (.TXT) on December 5, 2014. Retrieved May 25, 2017.
  3. ↑ "Annual Report on Activities of the RSMC Tokyo – Typhoon Center 2000" (PDF). Japan Meteorological Agency. February 2001. p. 3. Retrieved May 25, 2017.
  4. 1 2 Typhoon 26W Best Track (TXT) (Report). Joint Typhoon Warning Center. December 17, 2002. Retrieved May 25, 2017.
  5. 1 2 Kenneth R. Knapp; Michael C. Kruk; David H. Levinson; Howard J. Diamond; Charles J. Neumann (2010). 1984 Warren (1984291N13130). The International Best Track Archive for Climate Stewardship (IBTrACS): Unifying tropical cyclone best track data (Report). Bulletin of the American Meteorological Society. Retrieved May 25, 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 May 25, 2017.
  7. ↑ Padua, Michael V. (November 6, 2008). PAGASA Tropical Cyclone Names 1963–1988 (TXT) (Report). Typhoon 2000. Retrieved May 25, 2017.
  8. 1 2 Hong Kong Observatory (1985). "Part III – Tropical Cyclone Summaries". Meteorological Results: 1984 (PDF). Meteorological Results (Report). Hong Kong Observatory. pp. 26–29. Retrieved May 25, 2017.
  9. 1 2 3 4 Destructive Typhoons 1970–2003 (Report). National Disaster Coordinating Council. November 9, 2004. Archived from the original on November 26, 2004. Retrieved May 28, 2017.
  10. 1 2 "International News". Associated Press. October 29, 1984.
  11. 1 2 3 4 "International News". United Press International. October 29, 1984.
  12. ↑ "International News". Associated Press. October 30, 1984.
  13. 1 2 "Storm kills at least 56". United Press International. October 30, 1984.
  14. ↑ De Castro, Eric (October 30, 1984). "Death toll from Warren rises to 56". United Press International.
  15. ↑ "International News (2)". United Press International. October 29, 1984.
  16. 1 2 "Rescuers Retrieve 12 More Bodies". Associated Press. October 30, 1984.
  17. 1 2 "Rescuers Recover 11 More Bodies, Death Toll At 29". Associated Press. November 2, 1984.
  18. ↑ Destructive Typhoons 1970–2003 (Report). National Disaster Coordinating Council. November 9, 2004. Archived from the original on November 9, 2004. Retrieved May 28, 2017.
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Severe Tropical Storm Warren (Reming)
Warren Oct 27 1984 0841Z.png
Warren at peak intensity on October 27