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TCAR - Typhoon Committee

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

CHAPTER 5 - RESEARCH FELLOWSHIP TECHNICAL REPORT<br />

KETSANA formed as TD at 00 UTC 25/09/2009<br />

and moved mainly westward for the whole of<br />

its existence. It strengthened into TS intensity at<br />

00 UTC 26/09/2009 and crossed Luzon Island<br />

to the South China Sea. Maintaining westward<br />

motion in the South China Sea it was upgraded<br />

into TY at 06 UTC 28/09/2009 , reaching its<br />

maximum intensity with Vmax of 70 kts and<br />

central minimum of 960 hPa. Turning to SW<br />

direction KETSANA hit Central Vietnam almost<br />

with its maximum intensity on 29/09/2009 then<br />

weakened rapidly into a TD at 06 30/09/2009.<br />

As can be seen from Fig. 14 and Tab.9 the CMA’s<br />

track forecasts also had NW bias and forecasts<br />

from 2009092800 toward the landfall had large<br />

errors when TY KETSANA suddenly turned to<br />

SW then made landfall.<br />

Fig. 14. Track of TY KETSANA (0916) and<br />

forecasts of CMA’s typhoon track prediction<br />

model. Other explanations are similar to those in<br />

Fig.6.<br />

Table 9. Verification for track forecasts of TY<br />

KETSANA (0916) ( position errors, km)<br />

4.10. TY 0917 PARMA<br />

PARMA formed as TD south of Guam at 06<br />

UTC 27/09/2009. At 06 UTC 29/09/2009 it<br />

gained intensity of TS. It move WNW and further<br />

intensified into TY and reached its maximum<br />

intensity with Vmax of 100 kts and central<br />

pressure of 930 hPa in 18 hours later. It moved<br />

NW and hit Northern Luzon Island on 03/10/2009<br />

and remained in this area moving slowly back and<br />

forth for 6 days and weakened into TD. However,<br />

PARMA intensified again into a TS when moving<br />

westward into the South China Sea at 00 UTC<br />

10/10/2009. Moving WNW and crossing Hainan<br />

Island it suddenly gained rapid intensification with<br />

Vmax of 70 kts in the Gulf of Tonkin then it moved<br />

SW and weakened into a TD in sea water. This<br />

TS had very complicated track, intensification<br />

change and lasted for long time (about 2 weeks).<br />

Model track forecasts in Fig. 15 indicated<br />

obvious north bias for almost whole life time of<br />

TY PARMA, especially for the period before and<br />

after hitting Philippines Island. Two first forecasts<br />

starting from 2009092900 and 2009092906<br />

had large errors for +12h and +24h forecasts<br />

2009<br />

Date and time 00 +12h +24h +36h +48h +60h +72h<br />

2009092518 24.7 162.6 210.9 171.3 156.0 111.2 125.8<br />

2009092600 11.1 194.6 108.2 46.3 61.7 67.9 132.3<br />

2009092606 92.2 162.2 147.3 167.1 111.7 92.6 88.8<br />

2009092612 35.0 86.4 78.1 86.2 181.6 320.7 431.9<br />

2009092618 15.4 54.8 39.6 39.0 72.2 193.8 305.8<br />

2009092700 15.4 11.1 46.3 86.9 242.2 325.3 414.8<br />

2009092706 15.4 63.0 44.5 35.0 143.4 175.1 -<br />

2009092712 22.2 64.2 30.8 154.1 196.4 274.4 -<br />

2009092718 10.7 54.6 92.5 162.5 178.2 - -<br />

2009092800 22.2 39.6 123.4 169.8 303.2 - -<br />

2009092806 0.0 81.9 207.1 310.6 - - -<br />

2009092812 15.4 135.3 208.0 310.6 - - -<br />

2009092818 11.1 100.6 239.4 - - - -<br />

2009092900 24.7 172.9 301.6 - - - -<br />

2009092906 0.0 284.0 - - - - -<br />

2009092912 53.6 259.7 - - - - -<br />

2009092918 39.1 - - - - - -<br />

2009093000 99.1 - - - - - -<br />

FCST TIMES 18 16 14 12 10 8 6<br />

Average (km) 29.1 120.5 134.1 145.0 164.7 195.1 249.9<br />

Min (km) 0.0 11.1 30.8 35.0 72.2 67.9 88.8<br />

Max (km) 99.1 284.0 301.6 310.6 303.2 325.3 431.9<br />

293

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