Cyclone and Storm Surge - Iczmpwb.org
Cyclone and Storm Surge - Iczmpwb.org
Cyclone and Storm Surge - Iczmpwb.org
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2.47<br />
As such, since most of the embankments have been constructed by many years before by not so<br />
scientific methods, the failures of these is no surprise, especially if these do not have adequate<br />
gradient on the river side or on the l<strong>and</strong> side. Further, even if these are well constructed, the gradual<br />
undercutting of the riverbank may lead to weakening of the foundation of these embankments leading<br />
to a sudden collapse. If the embankments do not have adequate face pitching, there is a high chance<br />
of these getting eroded away by the impact of lashing waves generated in the ocean or the rivers due<br />
to cyclonic storms (Figure 2-12).<br />
Figure 2-12. Embankment failure due to wave dash<br />
It may also be possible that the embankment protection in the form of brick pitching may not be<br />
strong enough at places to bear the wave dash, leading to exposure of the river side bank <strong>and</strong><br />
consequent erosion.<br />
A study by Hazra (2006) comparing the earlier maps of the Sundarbans <strong>and</strong> present day satellite<br />
imageries has inferred important statistics about the vulnerability of the isl<strong>and</strong>s in the region due to<br />
cyclonic effects. The researcher <strong>and</strong> his team had calculated the length of the embankments from<br />
Survey of India Topographic sheets (No.79B/4, 79B/8, 79B11, 79B/12,79B/ 16, 79C/1, 79C/2, 79C/5,<br />
79C/6, 79C/9, 79C/10, 79C/13, 79C/14, of 1969). The embankments were then digitized <strong>and</strong> length<br />
calculated, which was found to be around 3110.33 Km. Comparing this with the recent IRS 1D LISS<br />
III <strong>and</strong> PAN data of 2001, it was found out that some parts of the embankments have already been<br />
washed out by cyclones <strong>and</strong> erosion. It has also been inferred that due to high rate of siltation on the