1997 Pacific typhoon season

1997 Pacific typhoon season

Infobox hurricane season
Track=1997 Pacific typhoon season summary.jpg
Basin=WPac
Year=1997
First storm formed=January 19, 1997
Last storm dissipated=December 22, 1997
Strongest storm name=Ivan, Joan, Keith
Strongest storm pressure=872
Strongest storm winds=160
Total storms=29
Total hurricanes=24
Total intense=11
Fatalities=515
five seasons=1995, 1996, 1997, 1998, 1999

The 1997 Pacific typhoon season has no official bounds; it ran year-round in 1997, but most tropical cyclones tend to form in the northwestern Pacific Ocean between May and November. [Gary Padgett. [http://www.typhoon2000.ph/garyp_mgtcs/may03sum.txt May 2003 Tropical Cyclone Summary.] Retrieved on 2006-08-26.] These dates conventionally delimit the period of each year when most tropical cyclones form in the northwestern Pacific Ocean.

The scope of this article is limited to the Pacific Ocean, north of the equator and west of the International Date Line. Storms that form east of the Date Line and north of the equator are called hurricanes; see 1997 Pacific hurricane season. Tropical Storms formed in the entire west Pacific basin were assigned a name by the Joint Typhoon Warning Center. Tropical depressions in this basin have the "W" suffix added to their number. 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.

torms

The season was unusual in the number of super typhoons that occurred in the basin, with eleven typhoons reaching winds of at least 135 knots. They were Isa, Nestor, Rosie, Winnie, Bing, Oliwa (from Central Pacific), Ginger, Ivan, Joan, Keith, and Paka (from Central Pacific). This was due to the strong El Niño of 1997-1998, which contributed to the record amounts of not only super typhoons but also tropical storms in the Western and Eastern Pacific. Fortunately, most of the stronger systems remained at sea.

Tropical Storm Hannah (Atring)

Infobox Hurricane Small
Basin=WPac


Track=Hannah 1997 track.pngFormed=January 19
Dissipated=January 27
1-min winds=50
Pressure=987
In early January, an area of convection developed along a near-equatorial trough just west of the International Date Line. It tracked steadily westward, and remained disorganized for about week. On January 18, deep convection increased as a low-level circulation began to form, and at 0000 UTC on January 19 it developed into Tropical Depression 01W while located to the southwest of Guam. Based on satellite imagery estimates, the Joint Typhoon Warning Center upgraded it to Tropical Storm Hannah six hours after first forming. The deep convection quickly organized into well-defined cyclonic bands, and early on January 20 Hannah attained its peak intensity of 60 mph near the island of Yap. Increased southeasterly wind shear weakened the storm, leaving its dwindling convection situated along the northern portion of the circulation. Interaction with a large and powerful extratropical cyclone left the storm moving erratically, and on January 22 Hannah weakened to tropical depression status. Its motion turned to a steady southwestward motion, and on January 27 Hannah dissipated a short distance east of the Philippine island of Mindanao.cite web|author=Joint Typhoon Warning Center|year=1999|title=Tropical Storm Hannah (01W) ATCR|accessdate=2007-04-19|url=https://metocph.nmci.navy.mil/jtwc/atcr/1997atcr/ch3/01ww.htm]

Near the end of its duration, the Philippine Atmospheric, Geophysical and Astronomical Services Administration began issuing warnings on Hannah when was a tropical depression; the institution named the storm Tropical Depression Atring.cite web|author=The United Nations Task Force on El Niño, et. al|year=1999|title=The 1997-1998 El Niño Event: A Scientific and Technical Retrospect|publisher=World Meteorological Organization|accessdate=2007-04-19|url=http://web.archive.org/web/20060311135947/http://www.wmo.ch/nino/WMO905-e.pdf] The storm was never tracked by the Japan Meteorological Agency. There were no reports of significant damage or injuries.

uper Typhoon Isa

Infobox Hurricane Small
Basin=WPac


Track=Isa 1997 track.pngFormed=April 9
Dissipated=April 24
1-min winds=145
Pressure=892
Isa developed from a disturbance in the monsoon trough near the Caroline Islands on April 12. It moved erratically at first, though after attaining tropical storm status it curved westward due to the subtropical ridge to its north. Isa very gradually intensified, and on April 20 the typhoon reached peak 1-min winds of 270 km/h (165 mph), as reported by the Joint Typhoon Warning Center; Japan Meteorological Agency reported maximum 10-min winds of 155 km/h (100 mph). After turning northward, it accelerated to the northeast, and merged with a larger extratropical cyclone on April 24.cite web|author=Joint Typhoon Warning Center|year=1999|title=Typhoon Isa (02W) ATCR|accessdate=2007-04-26|url=https://metocph.nmci.navy.mil/jtwc/atcr/1997atcr/ch3/02ww.htm]

Early in its duration, Isa caused light rainfall and moderate winds on Pohnpei. Later, a stationary rainband from the typhoon dropped heavy precipitation on Guam during its dry season. Damage in the Guam National Weather Service area of responsibility totaled $1 million (1997 USD, $1.3 million 2006 USD), the majority of it from crop damage. No deaths were reported.cite web|author=National Climatic Data Center|year=1997|title=Event Report for Typhoon Isa|accessdate=2007-04-26|url=http://www4.ncdc.noaa.gov/cgi-win/wwcgi.dll?wwevent~ShowEvent~315211]

Tropical Storm Jimmy

Infobox Hurricane Small
Basin=WPac


Track=Jimmy 1997 track.pngFormed=April 22
Dissipated=April 26
1-min winds=55
Pressure=984
A low-level equatorial westerly wind system developed an area of convection on April 18, the same system that previously developed Typhoon Isa. It drifted west-northwestward, and on April 21 separated from the westerly wind system. At 0400 UTC on April 22, the Joint Typhoon Warning Center (JTWC) issued a Tropical Cyclone Formation Alert on the system, and two hours later the JTWC issued the first warning on Tropical Storm Jimmy about 1360 km (845 mi) southeast of Guam.cite web|author=Joint Typhoon Warning Center|year=1999|title=Tropical Storm Jimmy (03W) ATCR|accessdate=2007-04-20|url=https://metocph.nmci.navy.mil/jtwc/atcr/1997atcr/ch3/03ww.htm] Coinciding with its first warning, the Japan Meteorological Agency (JMA) classified it as a tropical depression.cite web|author=Japan Meteorological Agency|year=1997|title=1997 Western Pacific Best Track|accessdate=2007-04-20|url=http://www.jma.go.jp/jma/jma-eng/jma-center/rsmc-hp-pub-eg/Besttracks/bst1997.txt]

Jimmy continued northwestward through a break in the subtropical ridge caused by Isa, and it steadily intensified as it tracked through an area of light vertical wind shear. It recurved to the northeast, and shortly after reaching its westernmost point Jimmy attained its peak intensity of 55 mph on April 24. Conversely, JMA assessed Jimmy as remaining a minimal tropical storm throughout its duration. After maintaining peak winds for about 18 hours, to increased southwesterly winds aloft quickly weakened the storm, and late on April 25 JTWC issued its final advisory on Jimmy after its low-level circulation center became completely exposed from the deep convection. On April 26, Jimmy was absorbed by an approaching frontal trough over the open Pacific Ocean. The storm had little effects on land.

Tropical Storm Kelly

Infobox Hurricane Small
Basin=WPac
Track=Kelly 1997 track.pngFormed=May 4
Dissipated=May 11
1-min winds=45
Pressure=991
A low-level equatorial trough developed an area of convection on May 4. The low strengthened as it became more organized over the next two days. Late on May 6, the JTWC issued a TCFA and the system was declared Tropical Depression 04W shortly after. The depression slowly intensified and was upgraded to a Tropical Storm early on May 8 and was named Kelly. Kelly was able to intensify slightly before strong vertical wind shear displaced the center, weakening Kelly. Kelly was downgraded to a Tropical Depression on May 10 and the remnant circulation dissipated the next day. [http://metocph.nmci.navy.mil/jtwc/atcr/1997atcr/pdf/wnp/04w.pdf]

Tropical Storm Levi (Bining)

Infobox Hurricane Small
Basin=WPac


Track=Levi 1997 track.pngFormed=May 25
Dissipated=June 4
1-min winds=45
Pressure=991
Tropical Depression 5W drifted eastward through the Philippines in late May. The heavy rain it brought caused mudslides that killed 33 people. The depression continued northeastward, becoming a tropical storm, and transitioning to an extratropical storm on May 30. [Joint Typhoon Warning Center. [https://metocph.nmci.navy.mil/jtwc/atcr/1997atcr/ch3/05ww.htm Tropical Storm Levi.] Retrieved on 2007-01-07.]

From May 26-29, Philippine Atmospheric, Geophysical and Astronomical Services Administration tracked the storm, and named it Bining.

Typhoon Marie

Infobox Hurricane Small
Basin=WPac


Track=Marie 1997 track.pngFormed=May 25
Dissipated=June 2
1-min winds=90
Pressure=954

uper Typhoon Nestor

Infobox Hurricane Small
Basin=WPac



Track=Nestor 1997 track.pngFormed=June 1
Dissipated=June 15
1-min winds=140
Pressure=898

Typhoon Opal (Kuring)

Infobox Hurricane Small
Basin=WPac



Track=Opal 1997 track.pngFormed=June 13
Dissipated=June 21
1-min winds=90
Pressure=954
From June 15-18, Philippine Atmospheric, Geophysical and Astronomical Services Administration tracked the storm, and named it Kuring.

Typhoon Peter (Daling)

Infobox Hurricane Small
Basin=WPac



Track=Peter 1997 track.pngFormed=June 23
Dissipated=June 30
1-min winds=70
Pressure=972
From June 22-26, Philippine Atmospheric, Geophysical and Astronomical Services Administration tracked the storm, and named it Daling.

uper Typhoon Rosie (Elang)

Infobox Hurricane Small
Basin=WPac



Track=Rosie 1997 track.pngFormed=July 18
Dissipated=July 29
1-min winds=140
Pressure=898
On July 18, Tropical Depression 10W formed near Caroline Islands. 10W was upgraded to Tropical Storm Rosie and became a Category 5 Super Typhoon on July 22. Rosie moved northward and began to weaken. Rosie made a landfall as a Category 1 typhoon at Shikoku, Japan on July 26. Two people were killed because of Rosie. [Joint Typhoon Warning Center. [https://metocph.nmci.navy.mil/jtwc/atcr/1997atcr/ch3/10ww.htm Super Typhoon Rosie (10W).] Retrieved on 2007-01-07.]

From July 22-26, Philippine Atmospheric, Geophysical and Astronomical Services Administration tracked the storm, and named it Elang.

Tropical Storm Scott

Infobox Hurricane Small
Basin=WPac


Track=Scott 1997 track.pngFormed=July 20
Dissipated=August 3
1-min winds=55
Pressure=984
In the middle of July, a mid-level circulation formed within the Tropical Upper Tropospheric Trough. The circulation built toward the surface, and by July 20 the system developed a low-level circulation with scattered associated convection.cite web|author=Joint Typhoon Warning Center|year=1999|title=Tropical Storm Scott (11W) ATCR|accessdate=2007-04-25|url=https://metocph.nmci.navy.mil/jtwc/atcr/1997atcr/ch3/11ww.htm] Based on its organization, the Japan Meteorological Agency (JMA) classified the system as a weak tropical depression early on July 20 while located about 820 km (510 mi) northeast of Farallon de Pajaros, the northernmost island in the Northern Mariana Islands. Early development was impeded by the outflow from Typhoon Rosie; after drifting northwestward for 2 days the system turned to the northeast, and by July 24 the influence from Rosie greatly diminished. Accordingly, the organization of the depression quickly increased, and on July 24 the Joint Typhoon Warning Center (JTWC) classified it as Tropical Depression 11W.

A building anticyclone to its northwest forced the depression southeastward. It became steadily less organized, and on July 26 JTWC issued a final warning on the system, believing it to be dissipating. Shortly thereafter, however, the system began re-organizing, and on July 27 the system developed into Tropical Storm Scott. The storm tracked northwestward, then westward, and finally turned to the northeast. Scott gradually strengthened to attain peak winds of 105 km/h (65 mph) on July 29. JMA had upgraded the depression to tropical storm status on July 28, and assessed its peak intensity at 75 km/h (45 mph). Scott maintained its peak intensity for about 12 hours before slowly weakening as it accelerated northeastward. On August 2, the storm merged with an approaching frontal trough, and the following day JMA considered Scott dissipated while located near the Alaskan island of Gareloi. Tropical Storm Scott never affected land. The storm was the only tropical cyclone during the season to not form from the monsoon trough.cite web|author=Joint Typhoon Warning Center|year=1999|title=Summary of Western North Pacific and North Indian Ocean Tropical Cyclones|accessdate=2007-04-25|url=https://metocph.nmci.navy.mil/jtwc/atcr/1997atcr/ch3/chap3.htm]

Typhoon Tina (Huling)

Infobox Hurricane Small
Basin=WPac



Track=Tina 1997 track.pngFormed=July 31
Dissipated=August 9
1-min winds=90
Pressure=954
From July 31-August 6, Philippine Atmospheric, Geophysical and Astronomical Services Administration tracked the storm, and named it Bining.

Typhoon Victor (Goring)

Infobox Hurricane Small
Basin=WPac



Formed=July 28
Dissipated=August 4
1-min winds=65
Pressure=976
Track=Victor 1997 track.pngFrom July 30-31, Philippine Atmospheric, Geophysical and Astronomical Services Administration tracked the storm, and named it Goring.

uper Typhoon Winnie (Ibiang)

Infobox Hurricane Small
Basin=WPac



Track=Winnie 1997 track.pngFormed=August 5
Dissipated=August 23
1-min winds=140
Pressure=898
On August 5, a tropical depression formed near the Marshall Islands. It headed northwestward, slowly strengthening to a tropical storm on the 9th. Intensification became more rapid as conditions became more favorable, and Winnie reached typhoon strength on the 10th. 2 days later, it became the 4th Super Typhoon of the season with peak winds of 160 mph. Soon after, the eye became ragged and large, with an outer eyewall reaching 200 miles in diameter. On the 18th, a minimal Typhoon Winnie passed north of Taiwan and hit eastern China, where it winded down until dissipating on the 19th. The remnant continued northeastward, bringing heavy rain and damage across China until the 23rd. Winnie caused 64 deaths, 39 of which were in Taiwan from the heavy rain. [Joint Typhoon Warning Center. [https://metocph.nmci.navy.mil/jtwc/atcr/1997atcr/ch3/14ww.htm Super Typhoon Winnie (14W).] Retrieved on 2007-01-07.]

Typhoon Yule

Infobox Hurricane Small
Basin=WPac


Track=Yule 1997 track.pngFormed=August 16
Dissipated=August 23
1-min winds=65
Pressure=976
Typhoon Yule merged with Tropical Depression 16W early in its life. It briefly held typhoon strength

Typhoon Zita (Luming)

Infobox Hurricane Small
Basin=WPac



Track=Zita 1997 track.pngFormed=August 19
Dissipated=August 23
1-min winds=75
Pressure=967
The Philippine Atmospheric, Geophysical and Astronomical Services Administration tracked the storm early in its duration, and named it Luming.

Typhoon Amber (Miling)

Infobox Hurricane Small
Basin=WPac



Track=Amber 1997 track.pngFormed=August 19
Dissipated=August 30
1-min winds=110
Pressure=933
Typhoon Amber was the eighteenth tropical cyclone of the season. The tropical depression initially tracked slowly west-northwest between the subtropical ridge and Typhoon Zita and developed at a faster than normal pace. By August 26, Tropical Storm Cass formed to the west-southwest, which accelerated Amber's forward motion to the northwest due to a fujiwara interaction. It underwent eyewall replacement cycles from August 25 through August 27, and tracked across Taiwan/Taipei with maximum sustained winds of 95 knots, then through the Formosa Strait into China as a minimal typhoon. [Joint Typhoon Warning Center. [https://metocph.nmci.navy.mil/jtwc/atcr/1997atcr/pdf/wnp/18w.pdf Typhoon Amber.] Retrieved on 2007-01-07.]

Throughout much of its duration, Philippine Atmospheric, Geophysical and Astronomical Services Administration tracked the storm, and named it Miling.

uper Typhoon Bing

Infobox Hurricane Small
Basin=WPac


Track=Bing 1997 track.pngFormed=August 19
Dissipated=August 30
1-min winds=135
Pressure=904

Tropical Storm Cass

Infobox Hurricane Small
Basin=WPac


Track=Cass 1997 track.pngFormed=August 28
Dissipated=August 30
1-min winds=45
Pressure=991

uper Typhoon Oliwa

Infobox Hurricane Small
Basin=WPac


Track=Oliwa 1997 track.pngFormed=August 28
Dissipated=September 17
1-min winds=140
Pressure=898
On August 28, the monsoon formed into Tropical Depression 2C in the Central Pacific. It headed slowly westward, becoming a tropical storm on September 3. It crossed the International Date Line, and continued to slowly strengthen to become a typhoon on September 8. Oliwa rapidly strengthened on September 9 to reach a peak of 160 mph winds; the sixth Super Typhoon of the year. Oliwa slowly weakened as it moved westward, and hit Japan on September 15 and September 16. It turned to the northeast, and dissipated on September 17 after causing 7 deaths and widespread damage from flooding. [Joint Typhoon Warning Center. [https://metocph.nmci.navy.mil/jtwc/atcr/1997atcr/pdf/wnp/02cw.pdf Super Typhoon Oliwa (02C).] Retrieved on 2007-01-07.]

Typhoon David

Infobox Hurricane Small
Basin=WPac


Track=David 1997 track.pngFormed=September 11
Dissipated=September 20
1-min winds=95
Pressure=949

Tropical Storm Ella

Infobox Hurricane Small
Basin=WPac



Track=Ella 1997 track.pngFormed=September 21
Dissipated=September 23
1-min winds=40
Pressure=994

Typhoon Fritz

Infobox Hurricane Small
Basin=WPac


Track=Fritz 1997 track.pngFormed=September 23
Dissipated=September 26
1-min winds=75
Pressure=967

uper Typhoon Ginger

Infobox Hurricane Small
Basin=WPac


Track=Ginger 1997 track.pngFormed=September 21
Dissipated=October 1
1-min winds=145
Pressure=892

Tropical Storm Hank

Infobox Hurricane Small
Basin=WPac



Track=Hank 1997 track.pngFormed=October 3
Dissipated=October 5
1-min winds=35
Pressure=997

uper Typhoon Ivan (Narsing)

Infobox Hurricane Small
Basin=WPac


Track=Ivan 1997 track.pngFormed=October 9
Dissipated=October 26
1-min winds=160
Pressure=872
Two near-equatorial troughs of low pressure, having formed from westerly low-level winds, developed into Tropical Depressions 27W and 28W on October 9 and October 11, respectively. Both poorly organized, they headed generally westward without much convection. On the 13th, 27W became Tropical Storm Ivan and on the 14th, 28W became Tropical Storm Joan. The two were within convert|500|nmi|km|abbr=off|lk=on of each other, but they were separate enough to strengthen on their own. On the 15th, while crossing the Northern Mariana Islands, they both reached typhoon intensity. Rapid intensification came soon after, and Ivan and Joan became the 8th and 9th Super Typhoons of the year on the 17th. The two underwent the Fujiwhara effect, bringing Ivan more westerly and Joan more northerly. After reaching peaks of convert|300|km/h|mph|abbr=on|lk=off winds within 12 hours of each other, they slowly weakened to Category 4's. Ivan struck the northern Philippines at this intensity causing 1 death, while Joan restrengthened to a Category 5. They both turned to the northeast, and slowly dissipated.

How they reached their extreme intensities at such a close distance to each other is unknown. Normally, when two tropical cyclones are relatively close to each other, one typically shears the other. In this case, they both maintained Category 5 intensity for at least a day within a relatively close distance of each other. The monsoon trough, which typically helps intensify Western Pacific typhoons, was absent from these storms. Pressures were higher than normal, and the initial disturbances were very poorly organized. Regardless, they are among the strongest Super Typhoons of the world with convert|300|km/h|mph|abbr=on|lk=off winds each. [Joint Typhoon Warning Center. [https://metocph.nmci.navy.mil/jtwc/atcr/1997atcr/ch3/27-28ww.htm Super Typhoons Ivan (27W) and Joan (28W).] Retrieved on 2007-01-07.]

uper Typhoon Joan

Infobox Hurricane Small
Basin=WPac



Track=Joan 1997 track.pngFormed=October 11
Dissipated=October 25
1-min winds=160
Pressure=872

uper Typhoon Keith

Infobox Hurricane Small
Basin=WPac



Track=Keith 1997 track.pngFormed=October 22
Dissipated=November 10
1-min winds=155
Pressure=872
The tenth of eleven tropical cyclones to attain super typhoon intensity in the western North Pacific during 1997, Keith formed at low latitudes in the Marshall Islands. It was one of ten TCs which formed east of 160° E and south of 20° N — within the "El Niño". Keith was a recurving TC which passed between the Islands of Rota and Tinian (only convert|50|nmi|km|abbr=on|lk=off|disp=s apart) on the west-bound leg of its recurving track. NEXRAD imagery from Guam indicated the eye wall cloud of Keith never touched land as it threaded the narrow channel between these two islands. As such, the Mariana Islands were spared the full force of Keith. Keith's compact wind and cloud structure were revealed by Guam's NEXRAD Equatorial westerly winds bounded by twin near-equatorial troughs preceded the formation of Keith and a Southern Hemisphere twin. [Joint Typhoon Warning Center. [https://metocph.nmci.navy.mil/jtwc/atcr/1997atcr/ch3/29w.htm Super Typhoon Keith (29W).] Retrieved on 2007-01-07.]

Typhoon Linda (Openg)

Infobox Hurricane Small
Basin=WPac



Track=Linda Pacific 1997 track.pngFormed=October 25
Dissipated=November 9
1-min winds=65
Pressure=976
Typhoon Linda, after moving through the Philippines and the South China Sea, hit the Malay Peninsula on November 3. It restrengthened in the Bay of Bengal, but vertical shear caused Linda to dissipate on the 9th.

On the 2nd of November, Linda hit the southern tip of Vietnam, the Ca Mau province, causing unprecedented havoc with over 435 people were reported killed and 3,660 fishermen gone missing [http://vietnamnet.vn/xahoi/2007/11/756065/] . Nearly 80,000 houses are reported as destroyed and almost 140,000 as badly damaged. Infrastructure (roads, schools and hospitals) also suffered heavily and huge swathes of rice paddy were swamped. The hardest hit provinces were Kien Giang, Ca Mau, Bac Lieu, Soc Trang, Tra Vinh, Ben Tre and Vung Tau. It was the worst typhoon to strike the area in 100 years. [http://www.reliefweb.int/rw/rwb.nsf/db900sid/OCHA-64CQJT?OpenDocument]

Elsewhere in Thailand and the Philippines , Linda caused further deaths from flooding and heavy damage.Joint Typhoon Warning Center. [https://metocph.nmci.navy.mil/jtwc/atcr/1997atcr/ch3/30w.htm Typhoon Linda (30W).] Retrieved on 2007-01-07.]

Typhoon Mort (Pining)

Infobox Hurricane Small
Basin=WPac



Formed=November 7
Dissipated=November 16
1-min winds=65
Pressure=976
Track=Mort 1997 track.pngFrom November 12-16, Philippine Atmospheric, Geophysical and Astronomical Services Administration tracked the storm, and named it Pining.

uper Typhoon Paka (Rubing)

Infobox Hurricane Small
Basin=WPac



Track=Paka 1997 track.pngFormed=November 28
Dissipated=December 22
1-min winds=160
Pressure=901
The final super typhoon of the year developed in the Central Pacific on November 28. It moved westward, strengthening into a tropical storm before crossing the International Date Line on December 7. Conditions were marginally favorable for development, and Paka remained a tropical storm until December 10, when it was able to become a typhoon. Five days later, Paka reached Super Typhoon strength, the eleventh of the year. The next day it crossed over Guam, and on December 18, Paka reached a peak of 185 mph winds. After causing major damage across the smaller Western Pacific island groups, Paka rapidly weakened and dissipated on December 22. [Joint Typhoon Warning Center. [https://metocph.nmci.navy.mil/jtwc/atcr/1997atcr/ch3/05cw.htm Super Typhoon Paka (05C).] Retrieved on 2007-01-07.]

Accumulated Cyclone Energy (ACE) Ranking

References

ee also

*1997 Pacific hurricane season
*1997 Atlantic hurricane season
*1997-98 South-West Indian Ocean cyclone season
*1997-98 Australian region cyclone season
*1997-98 South Pacific cyclone season
*1997 North Indian Ocean cyclone season

External links

* [http://www.typhoon2000.ph Typhoon2000 Philippine typhoon website] .
* [http://www.typhoon2000.ph/plotting/PhilippineTyphoonChart.gifPhilippine Area of Responsibility] .
* [https://metocph.nmci.navy.mil/jtwc.html Joint Typhoon Warning Center] .
* [http://www.weather.gov.hk/informtc/sound/tc_pronunciatione.htm Meaning of Tokyo Typhoon Centre names] .


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