typhoon kai-tak: a perfect ocean’s storm

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Typhoon Kai-Tak: A perfect ocean’s storm Tzu-Ling Chiang 1 , C.-R. Wu 1 , and L.-Y. Oey 2 1 Department of Earth Sciences, National Taiwan Normal University, Taiwan 2 Program in Atmospheric and Oceanic Sciences, Princeton University, USA 2nd IWMO, Norfolk May 25, 2010

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Page 1: Typhoon Kai-Tak: A perfect ocean’s storm

Typhoon Kai-Tak:A perfect ocean’s storm

Tzu-Ling Chiang1, C.-R. Wu1, and L.-Y. Oey2

1Department of Earth Sciences, National Taiwan Normal University, Taiwan2Program in Atmospheric and Oceanic Sciences, Princeton University, USA

2nd IWMO, NorfolkMay 25, 2010

Page 2: Typhoon Kai-Tak: A perfect ocean’s storm

2000_Kai-Tak• July/3 - July/11, 2000

• Max. wind speed: 38.6 m/s

• Saffir-Simpson hurricane scale: Category-1

• Propagation speed: 0.65~1.96 m/s (during July 6~8, 2000)

• Lin et al. (2003) reported that Kai-Tak triggered a 30-foldincrease in surface chlorophyll-a concentration.

Page 3: Typhoon Kai-Tak: A perfect ocean’s storm

The South China Sea model (POM)(Wu and Chiang, 2007; Chiang et al., 2008)

• Domain:99°E~124°E, 2°N~27°N

• Resolution:horizontal: 1/16° (~6.25 km)vertical: 26 sigma levels

• Forcing:6-hourly 0.5°× 0.5°QSCAT/NCEP blend wind product (Milliff et al., 1999)

• SST:weekly 1° AVHRR SST

• IC & BC:daily output of EAMS model (Wu and Hsin et al., 2005; Hsin et al., 2008)

Page 4: Typhoon Kai-Tak: A perfect ocean’s storm

The South China Sea model

IC & BC:daily output of EAMS model (Wu and Hsin et al., 2005; Hsin et al., 2008)

Page 5: Typhoon Kai-Tak: A perfect ocean’s storm

Obs.

Model

Velocity

Page 6: Typhoon Kai-Tak: A perfect ocean’s storm

Obs.

Model

Temperature

Page 7: Typhoon Kai-Tak: A perfect ocean’s storm

Cf. drag coefficient formula

(Trenberth, 1989)

?

Page 8: Typhoon Kai-Tak: A perfect ocean’s storm

Cf. drag coefficient formula⎪⎩

⎪⎨

>+≤≤

<+×= −

(m/s)10W0.065W,0.49(m/s)10W31.14,

(m/s)3W1.56/W),(0.6210C 3

d

⎪⎩

⎪⎨

<≤−+≤<+

≤×= −

(m/s)100W19,0.0023158W0.0234W1.364(m/s)19W110.065W,0.49

(m/s)11W1.2,10C

2

3d

Page 9: Typhoon Kai-Tak: A perfect ocean’s storm

PnCn TRMMUV&SST TMI/SST

Page 10: Typhoon Kai-Tak: A perfect ocean’s storm

PoCo PnCo PnCn PnwCn

<= WSmax (K-T)

Page 11: Typhoon Kai-Tak: A perfect ocean’s storm

SCScase study

Case Study WS KCWoKo standard run C+L Y

WoKc1 blocked LS C+L N

WoKc2 blocked EBC C+L N

WcKo climate WS C Y

WlKo local WS L Y

Page 12: Typhoon Kai-Tak: A perfect ocean’s storm
Page 13: Typhoon Kai-Tak: A perfect ocean’s storm

2000WS+2000TS 2000WS+WOA01‐JulyTS                                          2000WS+2001TS8.7 4.1                                                     5.1

Page 14: Typhoon Kai-Tak: A perfect ocean’s storm

Kai-Tak (2000) Utor (2001) 0.65~1.85 m/s ~7.5m/s C1; 10.8℃ C1; 3.8℃

Best track from JTWC(http://weather.unisys.com/hurricane/)

SST from TRMM/TMI

•Utor belongs to a medium moving storm during July 5~6, 2001, and the maximum SST drop was about 3.8℃.

Page 15: Typhoon Kai-Tak: A perfect ocean’s storm

cf. obs. & modelcold SST pool

(degree C)min SST

(20000708-9)pre-typhoon condition

(20000702-03)delta SST

TRMMTMI/SST

118.5-120E, 19-20.5N21-24

118.9E, 19.9N ~21.8

~30.7 ~9

SCSMSST

118.2-120.2E, 19-20.7N19-24

119.3E, 19.7N~19.9

~30.2 ~10

Page 16: Typhoon Kai-Tak: A perfect ocean’s storm

PnCn TRMMSST TMI/SST

GHRSST

Page 17: Typhoon Kai-Tak: A perfect ocean’s storm

AVISO PnCn PnCnSSHA SSHA SSH

Page 18: Typhoon Kai-Tak: A perfect ocean’s storm

WOA01-June WOA01-July

1999-June 2000-June

2001-June 2002-June 2003-June

43.86 54.50

42.94 29.14

42.44 43.51 47.49

Page 19: Typhoon Kai-Tak: A perfect ocean’s storm

WOA01-June WOA01-July

1999-June 2000-June

2001-June 2002-June 2003-June

30.00 50.00

38.00 24.33

30.00 38.00 46.67