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TCAR - Typhoon Committee

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2.1 REPORT ON INDIVIDUAL<br />

TROPICAL CYCLONES WHICH<br />

AFFECTEDMEMBERS OF THE<br />

TYPHOON COMMITTEE<br />

2.1 Overview<br />

This is a summary of the tropical cyclones that<br />

developed over the western North Pacific and the<br />

adjacent seas bounded by the Equator, 45 o N, 100 o E<br />

and 180 o E. In 2009, a total number of 22 tropical<br />

cyclones (TCs) with tropical storm (TS) intensity or<br />

higher formed in the western North Pacific and the<br />

South China Sea, of which 13 reached typhoon (TY)<br />

intensity, 3 at severe tropical storm (STS) intensity<br />

and 6 at tropical storm (TS) intensity. The total number<br />

of tropical cyclones with tropical storm intensity or<br />

higher is less than the 30 year average (1971 – 2000)<br />

of 26.7.<br />

There were no tropical cyclones developed over the<br />

western North Pacific and South China Sea from<br />

January to April. The first tropical cyclone for the year<br />

2009 occurred in May with the formation of Kujira.<br />

The most intense cyclone was Nida (0922) which had<br />

an estimated wind of 213 km/h and a minimum sealevel<br />

pressure of about 905 hPa when it was located<br />

over the western North Pacific about 370 km west of<br />

Guam. <strong>Typhoon</strong> Lupit (0920) was the tropical cyclone<br />

with the longest life span in 2009 which lasted for<br />

16.5 days.<br />

In 2009, nine tropical cyclones made landfall over<br />

coastal area of China, two crossed Taiwan, five<br />

affected Japan, twelve affected the Philippines and<br />

five made landfall over Vietnam.<br />

KUJIRA (0901) formed as a tropical depression<br />

off the south-eastern coast of Luzon on 1 May and<br />

moved generally northeastwards. It intensified into a<br />

tropical storm and then further intensified into a sever<br />

tropical storm on 3 May. Keeping its northeastwards<br />

track, it was upgraded into a typhoon the next day. It<br />

weakened into a severe tropical storm on 7 May and<br />

then a tropical storm on that afternoon. Kujira became<br />

an extra-tropical cyclone to the east of Japan later.<br />

CHAN-HOM (0902) formed as a tropical depression<br />

over the central part of South China Sea on 2 May<br />

and moved slowly northeastwards and intensified<br />

<strong>TCAR</strong><br />

CHAPTER 2 - TROPICAL CYCLONES 2008<br />

TROPICAL CYCLONES IN 2009<br />

into a tropical storm on 3 May. Moving slowly<br />

northwards, Chan-hom further intensified into a<br />

severe tropical storm the next day. It turned to move<br />

east-northeastwards on 6 May and was upgraded<br />

into a typhoon. Chan-hom crossed Luzon Island soon<br />

after being downgraded into a sever tropical storm.<br />

It weakened into a tropical storm and further into a<br />

tropical depression over the sea east of the Philippines<br />

on 9 May, then turned to move to the north. Keeping<br />

its northerly track, it dissipated south of Okinawa on<br />

13 May.<br />

LINFA (0903) formed as a tropical depression over<br />

the northern part of South China Sea on 17 June and<br />

moved slowly. It intensified into a tropical storm the<br />

next day. Moving northwards, Linfa intensified into<br />

a severe tropical storm over the same waters on 19<br />

June. While moving northeastwards along the coast<br />

of southern China, it was weakening into a tropical<br />

depression on 22 June. It further weakened into an<br />

extra-tropical cyclone over the East China Sea on 23<br />

June.<br />

NANGKA(0904) formed as a tropical depression over<br />

the sea east of the Philippines on 22 June. Moving<br />

west-northwestwards, it intensified into a tropical<br />

storm the next day. Nangka crossed the central<br />

Philippines and entered the South China on 24 June.<br />

Continuing its north-northwesterly trajectory, Nangka<br />

made landfall over the coastal area east of Hong Kong<br />

and weakened into a tropical depression on 26 June<br />

and then dissipated later over southern China.<br />

SOUDELOR (0905) formed as a tropical depression<br />

off the northern coast of Luzon on 9 July and moved<br />

west-northwestwards across the northern part of<br />

South China Sea. It intensified into a tropical storm<br />

on 11 July. Continuing to move west-northwestwards,<br />

Soudelor crossed the northern tip of Leizhou<br />

Peninsula and weakened into a tropical depression on<br />

12 July. It made landfall over the coast of northern<br />

Viet Nam and then dissipated the next day.<br />

MOLAVE (0906) formed as a tropical depression<br />

over the sea east of the Philippines on 15 July and<br />

moved generally northwestwards. It intensified into<br />

a tropical storm the next day. While crossing the<br />

Luzon Strait on 17 July, it further intensified into a<br />

severe tropical storm and then a typhoon. Keeping<br />

its west-northwestwards track, it made landfall<br />

over Shenzhen in the late hour on 18 July. Molave<br />

2009<br />

157

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