Typhoon Bilis (2000)

Last updated

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 predecessor to Typhoon Bilis began as a developing area of disturbed weather well south-southeast of Guam on August 15. Satellite analysis revealed a broad low-pressure area associated with the developing convection. Within an area supportive of tropical cyclogenesis, the disturbance gradually organized and intensified. [1] At 0600  UTC on August 17, the Joint Typhoon Warning Center  (JTWC) began classifying the system as a tropical depression. [2] The Japan Meteorological Agency  (JMA) followed suit the following day at 1200 UTC. [3] Tracking northwestward, the favorable conditions allowed the depression to quickly strengthen and attain tightly wrapped rainbands, [1] prompting the JMA to upgrade the system to tropical storm status at 0600 UTC on August 19, [3] thus designating the storm with the name Bilis. [4]

This period of rapid strengthening continued throughout the day's course, with the system reaching severe tropical storm intensity twelve hours after naming and then typhoon intensity at 1200 UTC on August 20. [3] Water vapor satellite imagery at the time indicated that Bilis maintained a well-organized outflow pattern. As a result of its rapid intensification, Bilis grew in size, exhibiting a behavior typical of tropical cyclones originating from the northwest Pacific monsoon trough. In addition, the typhoon developed an eye early on August 20, though in its initial stages the eye was irregular in shape. [1] At 1200 UTC on August 21, the JTWC determined Bilis to have reached super typhoon intensity. [nb 1] . [1] Six hours later, the JMA indicated that the typhoon had reached its peak intensity with maximum sustained winds of 205 km/h (127 mph) and a minimum barometric pressure of 920  mbar (hPa; 27.17  inHg). [3] By this point Bilis' eye had become cloud-free and well defined. The typhoon maintained this intensity with little fluctuation for roughly the ensuing eighteen hours as it tracked northwest. [3] Early on August 22, microwave imagery indicated concentric eyewalls, a sign of a possible eyewall replacement cycle. [1]

Still at peak intensity, [3] Bilis made landfall on the coast of southern Taiwan at 1400 UTC on August 22. [4] Concurrently, the storm's internal structure began to show signs of disruption, and its eye began to shrink. The typhoon accelerated over the island, and as such emerged into the Taiwan Strait no longer than five or six hours after landfall. [1] Despite the short stint over land, Bilis had greatly weakened, and was only a minimal typhoon upon its reentry over water. [3] However, there was a large discrepancy between JMA and JTWC intensity estimates, with the latter suggesting that Bilis had only weakened slightly. [1] Nonetheless, the typhoon made its final landfall Jinjiang, Fujian at 0300 UTC on August 24. This greatly weakened Bilis, and three hours later the JMA downgraded it as a tropical storm. [3] Shortly after landfall, the weakening tropical cyclone became quasi-stationary just inland of Mainland China. By this point convection was intermittent and short-lived, [1] and at 1200 UTC the JMA classified the system as a tropical depression. [3] Though the JTWC discontinued its monitoring activities, [2] the depression began to assume a northerly course on August 24. At 1200 UTC the next day, the depression was determined to have diffused into a remnant low while still inland. Bilis' remnants continued to track northeast, across the Yellow Sea, and dissipated on August 27 shortly after entering the Korean Peninsula. [3]

Preparations and impact

Typhoon Bilis (Isang)
Bilis 2000-08-21 0235Z.jpg
Bilis near peak intensity on August 21
IBTrACS OOjs UI icon edit-ltr-progressive.svg
Deaths and damage by region
RegionTotal
deaths		Damage
(USD)		Source
China 57 [4]
Taiwan 14 [4]
Totals:71

Taiwan

In preparation for Bilis, offices were closed across the island. In addition to the closure of businesses, flights to and from the island were rescheduled, and a typhoon relief center was established. [5] Due to the threat of landslides, a landslide warning was issued for Taiwan. [6] Though the storm had not yet made landfall, one person was killed in Taipei on August 22 after they were buried by a landslide triggered by the impending typhoon; this accounted for the first fatality caused by Bilis. [5] Along with flight rescheduling, numerous airports were closed, and the Taiwan Stock Exchange was set to close on August 23. Meanwhile, hospitals extended service times in anticipation for patient admittance. Taiwanese coast guard members regulated fishing activity due to the threat of deadly wave action. [7] The Port of Kaohsiung was closed throughout the duration of the storm. [8] Due to the heightened demand for vegetables in the lead-up to the storm, the cost of such foods increased by 20 to 30 percent. [9]

Bilis was a highly destructive tropical cyclone for Taiwan. Damage to the island's agricultural, fishing, and forestry industries amounted to US$133.5 million. The typhoon caused 14 fatalities and injured an additional 80 people. Power outages adversely impacted approximately 600,000 households, and 400 homes across Taiwan were destroyed. [4] Several hundred thousand families experienced water shortage following the storm. [10] In Cheng-Kung, a weather station recorded a 281 km/h (175 mph) wind gust, which broke the station's anemometer. [1] A single landslide in the town of Jenai buried nine farmers. Tens of thousands of people were displaced during the storm, and moved into evacuation shelters set up by the government. [8] Eight people shooting a film on the outskirts of Kaohsiung became stranded and thus improvised a shelter to ride out the storm. [11] In eastern Hualien County, 250 houses succumbed to strong winds. [1] The winds also felled trees and blew light vehicles around, blocking roads. [12] Heavy rainfall associated with Bilis flooded roughly 40,000  ha (100,000  ac) of orchards and rice paddies. Following Bilis' passage of Taiwan, a magnitude 5.7 earthquake struck the island, exacerbating the already worsened conditions. [1]

Mainland China

Typhoon Bilis upon making landfall in East China late on August 22 Bilis 22 Aug 2000 2331Z.jpg
Typhoon Bilis upon making landfall in East China late on August 22

Preparations for Typhoon Bilis on the Chinese mainland began on August 22, when the Xiamen Meteorological Observatory issued a warning for Fujian Province. [13] The typhoon was anticipated to be the worst storm to affect Xiamen so far in 2000. [14] As was the case in Taiwan, all three airports in the province were closed, and ferry service was suspended in preparation for the storm. [15] Likewise, Xiamen Airlines cancelled all scheduled flights. [14]

Despite becoming a weaker storm upon its landfall in China as opposed to its landfall on Taiwan, [1] Bilis caused more fatalities and accrued a greater damage cost in China. Economic losses in China totaled US$534 million, with most of the losses occurring in Fujian Province. A total of 57 people were killed, though an additional 1,077 people were either wounded or went missing. [4] Due to felled trees, a railway line from Fuzhou to Mawei blocked rail service. [15] Bilis spawned several tornadoes in the area of Yueqing, ravaging four villages and destroying 20 buildings. [4]

Elsewhere

As a developing disturbance, the precursor to Bilis dropped heavy rain on Guam on August 18. Peaking at 52 mm (2.0 in), the rain was the result of the storm's surface wind flow. [16] After becoming a tropical cyclone, Bilis' outer rainbands dropped heavy rainfall on Okinawa Prefecture in the Ryukyu Islands. Total rainfall amounts peaked at 136 mm (5.4 in) in Iriomote-jima. Two other stations recorded rainfall totals in excess of 100 mm (3.9 in). The typhoon also produced some gusty winds across the islands, with sustained winds peaking at 65 km/h (40 mph) on Yonaguni. [17] While a weakening remnant system, Bilis caused torrential precipitation across South Korea. At Kunsan Air Base, 468 mm (18.4 in) of rain was recorded over a 48-hour period; this two-day total was over three times the August average for the location. [1]

See also

Notes

  1. ↑ A super typhoon is an informal classification used by the JTWC to denote Pacific typhoons with 1-minute sustained winds greater than 150 mph (240 km/h).

Related Research Articles

<span class="mw-page-title-main">2005 Pacific typhoon season</span>

The 2005 Pacific typhoon season was the least active typhoon season since 2000, producing 23 named storms, of which 13 became typhoons. It was an event in the annual cycle of tropical cyclone formation, in which tropical cyclones form in the western Pacific Ocean. The season ran throughout 2005, though most tropical cyclones typically develop between May and October. The season's first named storm, Kulap, developed on January 13, while the season's last named storm, Bolaven, dissipated on November 20. The season's first typhoon, Haitang, reached typhoon status on July 13, and became the first super typhoon of the year three days later.

<span class="mw-page-title-main">2006 Pacific typhoon season</span>

The 2006 Pacific typhoon season was a destructive and deadly season, although it was near-average in terms of activity with a total of 23 named storms, 15 typhoons, and six super typhoons. Compared to the previous season, more typhoons inflicted damage across several countries, particularly China and the Philippines, some of which made landfall at higher intensities. The ratio of intense typhoons to all typhoons is at 0.73, the highest since 1970.

<span class="mw-page-title-main">2003 Pacific typhoon season</span>

The 2003 Pacific typhoon season was a slightly below average yearlong period of tropical cyclogenesis exhibiting the development of 45 tropical depressions, of which 21 became named storms; of those, 14 became typhoons. Though every month with the exception of February and March featured tropical activity, most storms developed from May through October. During the season, tropical cyclones affected the Philippines, Japan, China, the Korean Peninsula, Indochina, and various islands in the western Pacific.

<span class="mw-page-title-main">2001 Pacific typhoon season</span>

The 2001 Pacific typhoon season was an average season with twenty-six named storms, sixteen typhoons and three super typhoons, with a near normal Accumulated Cyclone Energy (ACE) of 307.3 units. It ran year-round in 2001, with most tropical cyclones in the northwestern Pacific Ocean tending between May and November.

<span class="mw-page-title-main">1988 Pacific typhoon season</span>

The 1988 Pacific typhoon season was a very active season in terms of named storms, though it only featured 11 typhoons and 1 super typhoon. It had no official bounds; it ran year-round in 1988, but most tropical cyclones formed between May and November. Tropical storms that formed in the entire west Pacific basin were assigned a name by the Joint Typhoon Warning Center. Tropical depressions that enter or form in the Philippine area of responsibility are assigned a name by the Philippine Atmospheric, Geophysical and Astronomical Services Administration or PAGASA. This can often result in the same storm having two names.

<span class="mw-page-title-main">Typhoon Krosa (2007)</span> Pacific typhoon in 2007

Typhoon Krosa, also known in the Philippines as Super Typhoon Ineng, was a powerful typhoon that impacted both China and Taiwan. The 18th tropical cyclone, the 15th named storm, and the 11th typhoon of the 2007 Pacific typhoon season, Krosa formed from a tropical system east of the Philippines in late September. The system became a depression on October 1, and on the following day, the depression quickly developed into a severe tropical storm. In the following days, Krosa rapidly intensified into a Category 4 super typhoon and reached peak intensity of 105 knots (194 km/h). Krosa would slowly weaken before making landfall on Taiwan. After making landfall on Taiwan, Krosa quickly weakened into a minimal typhoon, and rapidly weakened into a tropical depression between Zhejiang and Fujian provinces. Krosa transitioned into an extratropical cyclone on October 8. Extratropical remnants of Krosa dissipated on October 12.

<span class="mw-page-title-main">Timeline of the 2008 Pacific typhoon season</span>

This timeline documents all the storm formations, strengthening, weakening, landfalls, extratropical transitions, as well as dissipation during the 2008 Pacific typhoon season. The 2008 Pacific typhoon season officially started on January 1, 2008 and ended on January 1, 2009.

<span class="mw-page-title-main">Timeline of the 2009 Pacific typhoon season</span>

This timeline documents all of the events of the 2009 Pacific typhoon season which was the period that tropical cyclones formed in the Western Pacific Ocean during 2009, with most of the tropical cyclones forming between May and November. The scope of this article is limited to the Pacific Ocean, north of the equator between 100°E and the International Date Line. Tropical storms that form in the entire Western Pacific basin are assigned a name by the Japan Meteorological Agency. Tropical depressions that form in this basin are given a number with a "W" suffix by the United States' Joint Typhoon Warning Center. In addition, the Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) assigns names to tropical cyclones that enter or form in the Philippine area of responsibility. These names, however, are not in common use outside of the Philippines.

<span class="mw-page-title-main">Timeline of the 2010 Pacific typhoon season</span>

This timeline documents all of the events of the 2010 Pacific typhoon season. Most of the tropical cyclones forming between May and November. The scope of this article is limited to the Pacific Ocean, north of the equator between 100°E and the International Date Line. Tropical storms that form in the entire Western Pacific basin are assigned a name by the Japan Meteorological Agency. Tropical depressions that form in this basin are given a number with a "W" suffix by the United States' Joint Typhoon Warning Center. In addition, the Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) assigns names to tropical cyclones that enter or form in the Philippine area of responsibility. These names, however, are not in common use outside of the Philippines.

<span class="mw-page-title-main">Typhoon Kujira (2003)</span> Pacific typhoon in 2003

Typhoon Kujira, known in the Philippines as Typhoon Amang, was a long-lived tropical cyclone that lasted for 16 days and affected the island nations of Micronesia, Taiwan, and Japan in April 2003, as well as the earliest typhoon in a calendar year to ever make landfall on the latter. Forming from a broad area of disturbed weather as a tropical depression on April 9 well removed from any landmasses, Kujira quickly intensified in its early stages, and was upgraded to a tropical storm just two days after cyclogenesis. Strengthening slowed afterwards, though the storm attained typhoon intensity on April 14. Intensification continued and late on April 15, Kujira reached its peak intensity with winds of 165 km/h (103 mph) and a minimum barometric pressure of 930 mbar. Following peak intensity, Kujira began to track northwest and oscillate in strength, cresting an additional two times in intensity. On April 21, the typhoon was downgraded to tropical storm intensity and began to track erratically for several days east of Taiwan. However, on April 24, Kujira resumed a northward track and begin to weaken, and on April 24 was downgraded to tropical depression strength as it made landfall on Kyushu. Following landfall Kujira transitioned into an extratropical cyclone and continued to persist before these extratropical remnants crossed the International Dateline towards the end of April 2003.

<span class="mw-page-title-main">Typhoon Wayne (1983)</span> Pacific typhoon in 1983

Typhoon Wayne, known in the Philippines as Typhoon Katring, was an intense tropical cyclone that brought significant flooding to the Philippines in July 1983. The typhoon originated from an area of disturbed weather that formed far from land towards the end of July. Late on July 22, Wayne developed gale-force winds while moving west. The next day, it was estimated to have become a typhoon, and Wayne subsequently entered a period of rapid deepening. During the morning hours of July 24, the typhoon was estimated to have reached its peak intensity of 205 km/h (125 mph), but soon began to weaken due to interaction with land. By the time it moved ashore in southern China on July 25, Wayne had weakened considerably. After moving inland, Wayne weakened rapidly. The following day, Wayne was no longer a tropical cyclone.

<span class="mw-page-title-main">Timeline of the 2013 Pacific typhoon season</span>

Most of the tropical cyclones of the 2013 Pacific typhoon season formed between May and November of that year. The scope of this article is the Pacific Ocean north of the equator, between 100°E and the International Date Line. Tropical storms which form in the Western Pacific basin are assigned a name by the Japan Meteorological Agency (JMA). Tropical depressions forming in this basin are given a number with a "W" suffix by the United States' Joint Typhoon Warning Center (JTWC). The Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) assigns names to tropical cyclones that enter or form in the Philippine area of responsibility, but these names are not in common use outside the Philippines.

<span class="mw-page-title-main">Timeline of the 2011 Pacific typhoon season</span>

This timeline documents all of the events of the 2011 Pacific typhoon season, the period that tropical cyclones formed in the Western Pacific Ocean in 2011. Most of the tropical cyclones formed between May and November 2011. The scope of this article is limited to the Pacific Ocean, north of the equator between 100°E and the International Date Line. Tropical storms that form in the entire Western Pacific basin are assigned a name by the Japan Meteorological Agency (JMA). Tropical depressions that form in this basin are given a number with a "W" suffix by the United States' Joint Typhoon Warning Center (JTWC). In addition, the Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) assigns names to tropical cyclones that enter or form in the Philippine area of responsibility. These names, however, are not in common use outside of the Philippines.

<span class="mw-page-title-main">Tropical Storm Morakot (2003)</span> Pacific tropical storm in 2003

Tropical Storm Morakot, known in the Philippines as Tropical Storm Juaning, brought significant rainfall to Taiwan before alleviating drought conditions in mainland China in August 2003. The tenth named storm in the western Pacific that year, Morakot spawned from an area of disturbed weather in the Philippine Sea on July 31. Tracking northwest, favorable conditions allowed for the intensification of the system to tropical storm strength on August 2. Morakot reached peak intensity later that day with winds of 85 km/h (50 mph) and a minimum barometric pressure of 992 mbar. This intensity was held for several hours until less conducive atmospheric conditions slightly weakened the system; this was followed by Morakot making landfall on southern Taiwan on August 3. Subsequently, the storm weakened and moved into the Taiwan Strait before making its final landfall near Quanzhou, China the next day. The storm quickly weakened over the Chinese mainland, and dissipated entirely several hours after landfall.

<span class="mw-page-title-main">Typhoon Krovanh (2003)</span> Pacific typhoon in 2003

Typhoon Krovanh, known in the Philippines as Typhoon Niña, was a moderate tropical cyclone that caused a swath of damage stretching from the Philippines to Vietnam in August 2003. The fifteenth named storm and sixth typhoon in the western Pacific that year, Krovanh originated from a tropical disturbance within the monsoon trough on August 13. Despite rather favorable conditions, the initial tropical depression did not intensify significantly and degenerated into a remnant low on August 18. However, these remnants were able to reorganize and the system was reclassified as a tropical cyclone a day later. Intensification was rather rapid upon the storm's reformation – the depression reached tropical storm status on August 20 and then typhoon intensity two days later. Shortly after, Krovanh made landfall on Luzon at peak intensity with winds of 120 km/h (75 mph). The typhoon emerged into the South China Sea as a much weaker tropical storm, though it was able to restrengthen over warm waters. Once again at typhoon intensity, Krovanh clipped Haiyan before moving over the Leizhou Peninsula on its way to a final landfall near Cẩm Phả, Vietnam on August 25. Quick weakening due to land interaction occurred as Krovanh moved across northern Vietnam, where the storm met its demise the following day.

<span class="mw-page-title-main">Timeline of the 2014 Pacific typhoon season</span>

This timeline documents all of the events of the 2014 Pacific typhoon season. Most of the tropical cyclones forming between May and November. The scope of this article is limited to the Pacific Ocean, north of the equator between 100°E and the International Date Line. Tropical storms that form in the entire Western Pacific basin are assigned a name by the Japan Meteorological Agency. Tropical depressions that form in this basin are given a number with a "W" suffix by the United States' Joint Typhoon Warning Center. In addition, the Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA) assigns names to tropical cyclones that enter or form in the Philippine area of responsibility. These names, however, are not in common use outside of the Philippines.

<span class="mw-page-title-main">Timeline of the 2012 Pacific typhoon season</span>

This timeline documents all of the events of the 2012 Pacific typhoon season. The scope of this article is limited to the Pacific Ocean, north of the equator between 100°E and the International Date Line. During the season, 34 systems were designated as tropical depressions by either the Japan Meteorological Agency (JMA), the Philippine Atmospheric, Geophysical and Astronomical Services Administration (PAGASA), the Joint Typhoon Warning Center (JTWC), or other National Meteorological and Hydrological Services such as the China Meteorological Administration and the Hong Kong Observatory. Since the JMA runs the Regional Specialized Meteorological Centre (RSMC) for the Western Pacific, they assigned names to tropical depressions which developed into tropical storms in the basin. PAGASA also assigned local names to systems which are active in their area of responsibility; however, these names are not in common use outside of the Philippines.

<span class="mw-page-title-main">Typhoon Joan (1959)</span> Pacific typhoon in 1959

Typhoon Joan was an intense typhoon that caused minor damages in relative to the strength of the typhoon. Joan was the strongest typhoon of 1959 Pacific typhoon season, and one of the most intense Pacific typhoons on record. Joan formed from a surface center to the northeast of Guam on August 23, in which Japan Meteorological Agency began to track and classify the system as a tropical depression on the next day. A reconnaissance aircraft was sent to investigate the surface center and in 03:25 UTC on August 25 the surface center was classified as a tropical storm by Joint Typhoon Warning Center. The storm rapidly intensified into a typhoon in the same day it was formed. By the next three days as Joan tracks towards Taiwan, Joan explosively intensified to attain peak intensity with the pressure of 885 millibars (26.1 inHg), which is tied with Nina as the most intense Pacific typhoon on the record at the time. Shortly afterwards, Joan attained peak strength as a Category 5 equivalent super typhoon on the Saffir–Simpson hurricane scale with winds of 165 knots (190 mph) before making landfall in Taiwan as a 160 knots (180 mph) typhoon, which was according to JTWC is the strongest landfall in the recorded history at the time. After making landfall, Joan weakened into a 110 knots (130 mph) typhoon before making landfall on Fujian, China as a Category 2 equivalent typhoon on the Saffir–Simpson hurricane scale with winds of 95 knots (109 mph). Once onshore, Joan did not degenerate quickly as Joan remained as a tropical cyclone for about one day before transitioning into a extratropical cyclone in 18:00 UTC of August 31. Extratropical remnants of Joan quickly traversed through South Korea and Japan before being last noted on 18:00 UTC, September 2.

<span class="mw-page-title-main">Typhoon Mary (1960)</span> Pacific typhoon in 1960

Typhoon Mary, also nicknamed "Bloody Mary" by the Joint Typhoon Warning Center (JTWC), was an extremely damaging storm that was part of the 1960 Pacific typhoon season. It began as a circulation in a trough in the South China Sea. A tropical depression formed on June 2, as it was traveling clockwise. It became a tropical storm on the next day, and received the name Mary. It slowly moved across the sea, strengthening to a typhoon. Mary made landfall in Hong Kong on June 8, and moved through Guangdong and Fujian. It reemerged back to the Pacific Ocean, and restrengthened into a typhoon temporarily. It then traveled east, weakening and becoming extratropical on June 12.

<span class="mw-page-title-main">Typhoon Gerald</span> Pacific typhoon in 1987

Typhoon Gerald, known in the Philippines as Typhoon Neneng, affected the Philippines, Taiwan, and China during September 1987. A tropical depression developed on September 4, and within 24 hours, intensified into a tropical storm. After initially moving erratically within the Philippine Sea, Gerald moved west-northwest and then northwest while steadily deepening. Gerald obtained typhoon intensity on September 8, and the following day, attained maximum intensity. Shortly thereafter, the typhoon skirted southwestern Taiwan, which resulted in a steady weakening trend. On September 10, Gerald moved ashore north of Hong Kong near Amoy. Gerald dissipated the next day.

References

  1. 1 2 3 4 5 6 7 8 9 10 11 12 13 Padgett, Gary (August 2000). "Monthly Global Tropical Cyclone Summary August 2000". Australiansevereweather.com. Retrieved January 3, 2014.
  2. 1 2 National Climatic Data Center. "2000 BILIS (2000230N08139)". International Best Track Archive for Climate Stewardship. Asheville, North Carolina: University of North Carolina at Asheville. Retrieved January 3, 2014.
  3. 1 2 3 4 5 6 7 8 9 10 "Annual Report on the Activities of the RSMC Tokyo – Typhoon Center 2000" (PDF). Tokyo, Japan: Japan Meteorological Agency. Retrieved January 3, 2014.
  4. 1 2 3 4 5 6 7 Joint Typhoon Warning Center (2001). "Annual Tropical Cyclone Report 2000" (PDF). Pearl Harbor, Hawaii: United States Naval Oceanography Portal. Retrieved January 3, 2014.
  5. 1 2 "Taiwan prepares for 146mph killer typhoon". The Evening Standard. London, United Kingdom. August 22, 2000. p. 17.
  6. ↑ "AP News Digest (0600 GMT, August 22)". Taipei, Taiwan. Associated Press. August 22, 2000.
  7. ↑ "Strong typhoon heads toward Taiwan after killing man". Taipei, Taiwan. Associated Press. August 22, 2000.
  8. 1 2 Medina, Marcos Calo (August 22, 2000). "Typhoon Bilis slams into Taiwan with immense force". Taipei, Taiwan. Associated Press.
  9. ↑ Noi, Goh Sui (August 23, 2003). "Taiwanese take cover as typhoon sweeps in". The Straits Times. Taipei, Taiwan.
  10. ↑ "Tropical Cyclones in 2000" (PDF). Kowloon, Hong Kong: Hong Kong Observatory. April 2001. Retrieved January 3, 2014.
  11. ↑ Medina, Marcos Calo (August 22, 2000). "Strong typhoon batters southern Taiwan". Taipei, Taiwan. Associated Press.
  12. ↑ "Powerful Typhoon Batters Taiwan". The Toronto Star. Toronto, Canada. Associated Press and Reuters. August 23, 2000.
  13. ↑ "Xiamen on Alert Against Typhoon Bilis". Xiamen, China. Xinhua. August 22, 2000.
  14. 1 2 "Typhoon Bilis to Hit East China Province At Noon". Xiamen, China. Xinhua. August 23, 2000.
  15. 1 2 "Typhoon Bilis Hits Fujian Province". Fuzhou, China. Xinhua. August 23, 2000.
  16. ↑ "Storm Data – August 2000" (PDF). Storm Data and Unusual Weather Phenomena. 42 (8). Asheville, North Carolina: National Climatic Data Center: 202. August 2000. Retrieved January 3, 2014.
  17. ↑ KITAMOTO Asanobu. "Digital Typhoon: Typhoon 200010 (BILIS) - Disaster Information". Digital Typhoon Disaster Database. National Institute of Informatics. Retrieved January 3, 2014.
This page is based on this Wikipedia article
Text is available under the CC BY-SA 4.0 license; additional terms may apply.
Images, videos and audio are available under their respective licenses.