Cyclone and Storm Surge - Iczmpwb.org
Cyclone and Storm Surge - Iczmpwb.org
Cyclone and Storm Surge - Iczmpwb.org
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4.25<br />
⎛ 2Rr<br />
⎞<br />
V = Vm<br />
⎜<br />
2 2<br />
⎟<br />
⎝ R + r ⎠<br />
(Jelesnianski, 1972) (36)<br />
With the surface winds estimated one can proceed to the computation of the stress at the sea surface.<br />
The surface stress is expressed by conventional quadratic law as:<br />
2<br />
F S ρ c u ( u + v<br />
2<br />
=<br />
a D a a a<br />
)<br />
1<br />
2<br />
1<br />
2<br />
= ) 2<br />
a D a a a<br />
2<br />
G S ρ c v ( u + v<br />
where, ua <strong>and</strong> va are the x <strong>and</strong> y components of surface wind, cD is the drag coefficient. Observational<br />
studies suggest that the drag coefficient may be related to the wind speed by:<br />
(37)<br />
cD = (1.00 + 0.07 v10 ) x 10-3 (38)<br />
in which v10 is the wind speed at 10m from the mean sea level. This expression is generally valid for<br />
wind speed less than 14 m sec-1. At wind speeds between 10 <strong>and</strong> 30 m sec-1 , cD varies from 2 x 10-<br />
3 to 3 x10-3 with no significant dependence on wind speed. Most of the workers use a uniform value of<br />
drag coefficient (Cd=2.8 x 10-3).<br />
4.9. Case Studies of <strong>Storm</strong> <strong>Surge</strong>s in coastal belt of West Bengal<br />
<strong>Storm</strong> surges associated with tropical cyclones having their l<strong>and</strong>fall in the coastal belt of West Bengal<br />
distributed in block-wise for the period 1891-2005, is depicted in Table-2. The block-wise frequency of<br />
these cyclones has been grouped based on their severity based upon the central pressure drop (∆P)<br />
while approaching the littoral belt of West Bengal state. As noticed from Table-2, the frequency of severe<br />
cyclones was highest in the Gosaba block with six severe extreme events in a total of 20 cases. Based<br />
on severe cyclones, the other blocks following Gosaba are Namkhana <strong>and</strong> Ramnagar which<br />
experienced two severe cyclones. Accordingly, four severe cyclones were selected viz; 1998 Gosaba<br />
cyclone, 1988 Gosaba cyclone, 1981 Namkhana cyclone <strong>and</strong> 202 Kultali cyclone. Among these four<br />
extreme events, the 1988 Gosaba cyclone was considered the most severe.<br />
Case -1: 1998 Gosaba <strong>Cyclone</strong><br />
The track <strong>and</strong> computed surge for the 1998 Gosaba cyclone is depicted in Figure-2(a). The simulation<br />
run was performed for 16 hours prior to the cyclone making its l<strong>and</strong>fall off Gosaba. The computed