yer fluid; 
terface is 
layer is 
t deal of 
e. Along 
yproaches 
, with the 
be drawn 
ı Gulf of 
low, the 
Vertical 
ry of the 
is clearly 
es during 
ng, which 
ong wind 
aves with 
of India is 
ie cyclone 
near coast 
more cold 
Navalgund 
ragement. 
; Director 
WR&OG) 
's TRMM 
A's Earth 
; greatly 
sea surface 
cations for 
ference on 
pril 24-28, 
3-604. 
Trends and 
ian Ocean. 
S. 2000. 
: the North 
ics.75:.11- 
1. Has the 
n the north 
IAPRS & SIS, Vol.34, Part 7, “Resource and Environmental Monitoring”, Hyderabad, India, 2002 
Stramma, L., P. Cornillon (1986) Satellite observation of Sea 
Surface Cooling by Hurricanes, J. Geophys. Res., 91, 5031- 
5035. 
Suetsugu, M. Kawamura, H. and Nishihama, S (2000) Sea 
Surface cooling caused by typhoons in the Western North 
Pacific Ocean. PORSEC Proceedings, Goa, India, 1, 258-262. 
m 
Oct. 28, 99. 18 GMT 
I ET 13 
ER WE XO ul 
SCAN 
An 
ICE 
| 
TRACK OF GRISSA SUPER ide DURING OCTOBER 1999 
Figure 1. Track of Orissa super cyclone during October, 1999. 
80 85 90 95 
  
E »310*C 
EN 3015*.309"C 
M 29.1°-30.0°C 
{#7 28.05°-28.95°C 
BE 27.18°-279°C 
ES 
Em 
un 
   
   
  
  
   
  
      
9$ 261*-270*'C | 20 
25.06° - 25.98° C 
24.15*- 24.9* C 
«240* C 
15 
2 
0 
  
  
  
80 85 90 95 
Figure 2. Weekly average Sea Surface Temperature image prior 
to cyclone (3-9 October, 1999). 
401 
  
80 85 90 
uw 
5 
  
M >310°C 
EH 30315*.309:C 
EN 291*-300*C 
28.05* .28.95* C 
Bl 27.15°-279°C 
20 SW 261*-270"C |20 
B 2505:.25895'c 
BE 24.15°- 249°C 
BH <240°C 
     
10 
  
  
  
80 85 90 95 
Figure 3. Weekly average Sea Surface Temperature image 
during cyclone (24-30 October, 1999). 
80 85 90 95 100 
EM <-1.5°C 
BEE -15°t -1.0°C 
Aa BENE -10*to -0.5*C 
  
; -D.5? to 0°C 
E Oto O5^C 
0.5? to 1.0°C 
E 1.0°t 15°C 
>1.6°C 
20 
- 
  
  
  
Figure 4. Difference between the Sea Surface Temperatures of 
cyclone and prior to cyclone from TMI (fig. 3 minus fig. 2).