TCAR - Typhoon Committee
TCAR - Typhoon Committee
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