Cyclone and Storm Surge - Iczmpwb.org
Cyclone and Storm Surge - Iczmpwb.org Cyclone and Storm Surge - Iczmpwb.org
2.42 All the islands are situated within the middle reaches of the Hooghly estuary. Some of these are: nayachara, Ghoramara, Lohachara, Bedford, Sagar, Sikarpur, Kankramari, Mahisani, Jambu, and Chuksar. Lohachara and Khasimara islands are already eroded in the estuarine environment. Ghoramara and Bedford islands are gradually being reduced in their size. Parts of Sagar Island (Bisalakshipur, Beguakhali, and Sikarpur) are also eroded by faster tidal currents (Paul 2002). The 11.5km long stretches of the sea front of the Sagar Island on its southwestern side, parts of the Jambu Island, and the seaward side of the Chuksar Island are dominated by shoreline features and backshore dune fields. Waves and currents deposit sand in the shore zone of open sea-facing islands of the Hooghly estuary. Strong onshore winds, particularly in the pre-monsoon season, transport sand from the sea beach to the back-shore areas where dense vegetation cover attracts sand particles to accumulate into sand dunes. Dunes are less frequent weher abundant sand supply is absent (Paul 1994). The most extensive landforms found in the Hooghly estuary channels are the tidal flats, which are mostly restricted to intertidal zone. Tidal flats occur in the sloping sides of estuary channel and minor tidal channel, and also on the island and bar surface. According to Paul (2002), there are two types of tidal flats in the Hooghly estuary – the sheltered flat and the open-sea tidal flat. Variation of wave heights and tidal ranges controls the geomorphic positions and morphologies of the tidal flats. Islands, bars, and deltaic flats of the inland estuarine section are usually sheltered from the effects of wind-driven waves. The sheltered section of the estuary with large tidal range enhances the deposition of fine-grained silts and clays to form mud flats and marshes in the islands and deltaic flats. Nayachara Island, Bedford Island, Sikarpur Island and Kankramari Char are good examples of such extensive growth of tidal flats. The shorelines of Sagar Island, Jambu Island, Chuksar Island, Frasergunj, and Bak-khali are exposed to wave attacks at the lower reaches of the Hooghly estuary. Here, the accumulation of sediment deposited by waves and currents has produced beaches in the shore zone. The human habitation within the islands is guarded by circuit embankments, which act more like polders. Some of the embankments (like those in Sagar Island) are looked after by the Kolkata Port Trust (KoPT), and the rest by the Irrigation and Waterways Department (I&WD) of the Government of West Bengal. However, the retired embankments (the embankment that is situated some distance away from the riverbank) are less prone to damages which can be severe due to the cyclinic strom surges. KoPT has prepared a scheme for river training works in the interior of the estuary on the basis of recommendations of various expert committees and on the basis of the results of Hydraulic
2.43 model studies carried out Kolkata, Pune and Hamburg (Germany). This is, of course, has been done with the intention of maintaining the navigable channels at Kolkata and Haldia ports. The protection measures for the Nayachara Island have been completed by the KPT under this scheme. The rest of the embankments under the I&WD need extensive repair and protection, if the interests of the population residing within these circuit embankments need to be protected. This is all the more important as most of the islands face the wrath of not only the storm surge waves, but also the strong gales associated with the cyclones. 2.7. Threat of damage from tropical cyclones The vulnerability of the eastern coastal region of the State of West Bengal due to cyclones is due to the two reasons: (a) Erosion of the river and creek banks of network of channels the due to strong river currents, and (b) The damage to the embankments by the impact of the wave dashes that generate due to cyclonic storms. These waves could be the direct waves from the oceans hitting the embankments facing the sea. Or, these could be the waves diffused in the tidal creeks that hit the embankments in the hinterland. The other threat from cyclonic storms is due to the damage of infrastructure due to the excessively strong winds. In the coastal regions of the state, the general socio-economic condition of the local populace is rather low. Consequently, the housing types mostly belong to those made of mud, bamboo and other locally available raw materials. The roofs of most of these kutcha houses are made of thatch, though baked tiles are also common. However, all these are quite vulnerable to strong gusts of wind. The cyclonic depressions also generate a lot of precipitation. The inhabited areas of Sundarbans are mostly enclosed by circuit embankments and hence a lot of rain results in waterlogged conditions at the time of cyclones. According to Kanjilal (2006), proper field drainage is required to bring excess water from the farm plots and the village area to the main drainage canals and to keep the ground water level sufficiently low. The slope required for the transport of this excess water needs to be in line with the available head determined by the difference in level of the farm plots and the water surface in the main canal to which the excess water needs to be evacuated. The system of canals and ponds which is supposed to: • Collect and to store the water to be used later for agricultural or domestic purposes,
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2.42<br />
All the isl<strong>and</strong>s are situated within the middle reaches of the Hooghly estuary. Some of these are:<br />
nayachara, Ghoramara, Lohachara, Bedford, Sagar, Sikarpur, Kankramari, Mahisani, Jambu, <strong>and</strong><br />
Chuksar. Lohachara <strong>and</strong> Khasimara isl<strong>and</strong>s are already eroded in the estuarine environment.<br />
Ghoramara <strong>and</strong> Bedford isl<strong>and</strong>s are gradually being reduced in their size. Parts of Sagar Isl<strong>and</strong><br />
(Bisalakshipur, Beguakhali, <strong>and</strong> Sikarpur) are also eroded by faster tidal currents (Paul 2002).<br />
The 11.5km long stretches of the sea front of the Sagar Isl<strong>and</strong> on its southwestern side, parts of the<br />
Jambu Isl<strong>and</strong>, <strong>and</strong> the seaward side of the Chuksar Isl<strong>and</strong> are dominated by shoreline features <strong>and</strong><br />
backshore dune fields. Waves <strong>and</strong> currents deposit s<strong>and</strong> in the shore zone of open sea-facing<br />
isl<strong>and</strong>s of the Hooghly estuary. Strong onshore winds, particularly in the pre-monsoon season,<br />
transport s<strong>and</strong> from the sea beach to the back-shore areas where dense vegetation cover attracts<br />
s<strong>and</strong> particles to accumulate into s<strong>and</strong> dunes. Dunes are less frequent weher abundant s<strong>and</strong> supply<br />
is absent (Paul 1994).<br />
The most extensive l<strong>and</strong>forms found in the Hooghly estuary channels are the tidal flats, which are<br />
mostly restricted to intertidal zone. Tidal flats occur in the sloping sides of estuary channel <strong>and</strong> minor<br />
tidal channel, <strong>and</strong> also on the isl<strong>and</strong> <strong>and</strong> bar surface. According to Paul (2002), there are two types<br />
of tidal flats in the Hooghly estuary – the sheltered flat <strong>and</strong> the open-sea tidal flat. Variation of wave<br />
heights <strong>and</strong> tidal ranges controls the geomorphic positions <strong>and</strong> morphologies of the tidal flats.<br />
Isl<strong>and</strong>s, bars, <strong>and</strong> deltaic flats of the inl<strong>and</strong> estuarine section are usually sheltered from the effects of<br />
wind-driven waves. The sheltered section of the estuary with large tidal range enhances the<br />
deposition of fine-grained silts <strong>and</strong> clays to form mud flats <strong>and</strong> marshes in the isl<strong>and</strong>s <strong>and</strong> deltaic<br />
flats. Nayachara Isl<strong>and</strong>, Bedford Isl<strong>and</strong>, Sikarpur Isl<strong>and</strong> <strong>and</strong> Kankramari Char are good examples of<br />
such extensive growth of tidal flats.<br />
The shorelines of Sagar Isl<strong>and</strong>, Jambu Isl<strong>and</strong>, Chuksar Isl<strong>and</strong>, Frasergunj, <strong>and</strong> Bak-khali are<br />
exposed to wave attacks at the lower reaches of the Hooghly estuary. Here, the accumulation of<br />
sediment deposited by waves <strong>and</strong> currents has produced beaches in the shore zone.<br />
The human habitation within the isl<strong>and</strong>s is guarded by circuit embankments, which act more like<br />
polders. Some of the embankments (like those in Sagar Isl<strong>and</strong>) are looked after by the Kolkata Port<br />
Trust (KoPT), <strong>and</strong> the rest by the Irrigation <strong>and</strong> Waterways Department (I&WD) of the Government of<br />
West Bengal. However, the retired embankments (the embankment that is situated some distance<br />
away from the riverbank) are less prone to damages which can be severe due to the cyclinic strom<br />
surges. KoPT has prepared a scheme for river training works in the interior of the estuary on the<br />
basis of recommendations of various expert committees <strong>and</strong> on the basis of the results of Hydraulic