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200 - Typhoon Committee

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ESCAP/WMO<br />

<strong>Typhoon</strong> <strong>Committee</strong> Annual Review <strong>200</strong>7<br />

2.2. NARRATIVE REPORTS OF INDIVIDUAL TROPICAL CYCLONES<br />

WHICH AFFECTED MEMBERS OF THE TYPHOON COMMITTEE<br />

2.2.1 KONG-REY (0701)<br />

30 Mar – 6 April<br />

Stage<br />

JAPAN<br />

Times from Available Post Analysis<br />

HONG KONG<br />

TD 12UTC 30/03 06UTC 31/03<br />

TS 00UTC 01/04 18UTC 31/03<br />

STS 18UTC 01/04 18UTC 01/04<br />

T 00UTC 03/04 00UTC 03/04<br />

STS 18UTC 04/04 06UTC 04/04<br />

TS 06UTC 05/04 06UTC 05/04<br />

LOW 00UTC 06/04 -<br />

DISSIPATION 00UTC 07/04 -<br />

KONG-REY (0701) formed as a tropical depression (TD)<br />

over the western North Pacific around the Marshall<br />

Islands at 12UTC on 30 March <strong>200</strong>7 and moved westnorthwestwards.<br />

Kong-rey intensified into a tropical<br />

storm on 1 April. Keeping the northwestward track, it<br />

intensified into a severe tropical storm at 18UTC on 2<br />

April and further into a typhoon at 00UTC on 3 April.<br />

Kong-rey attained the peak strength with maximum<br />

sustained wind of 148 km/h and central pressure of 960<br />

hPa at 12UTC on 3 April. After turning east-northeastward,<br />

it was downgraded to tropical storm intensity at 06UTC<br />

on 5 April and then transformed into an extra-tropical<br />

cyclone east of Minamitorishima Islands the next day.<br />

Moving to the east, it dissipated on 7 April.<br />

204

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