Cyclone and Storm Surge - Iczmpwb.org
Cyclone and Storm Surge - Iczmpwb.org Cyclone and Storm Surge - Iczmpwb.org
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Chapter Four Hazard Analysis: Cyclone and Storm Surge 4.1. Cyclone hazard in coastal zones Tropical cyclones are the deadliest of all natural disaster worldwide, accounting for about 64% of the total loss of lives. The 80-100 tropical cyclones that occur worldwide each year cause, on an average, death of 20,000 people and a total economic loss of $6-7 billion (Southern 1979). The Indian subcontinent is the worst affected part of the world as far as the death toll associated with tropical cyclone is concerned. Out of 9-recorded cases of heavy loss of human lives (40,000 or more) by cyclones during the past 300 years, 7 cases (77%) occurred in Indian subcontinent (Frank and Hussain, 1971; Smith, 1989; Hebert et al., 1996). The tropical cyclones affect this region in two seasons: Pre-monsoon (April-May) and Post-monsoon (October-December). The peak frequency is found to be in the months of May and November. CHAPTER 4 The Bay of Bengal is potentially energetic for the development of cyclonic storms and accounts for about 7% of the global annual total number of storms (Gray, 1968). These storms usually move towards the west, northwest and north. Some of them recurve towards northeast after initial northwestward movement. Though, considered to be much weaker in intensity and smaller in size as compared to the cyclones of other regions, the Bay of Bengal cyclones, in particular, the post monsoon cyclones that cross east coast of India or Bangladesh are highly devastating. This is mainly due to dense populated coastal region, shallow bathymetry; nearly funnel shape of the coastline and the long stretch of the low-lying delta region embedded with large number of river systems. The casualty figures associated with major Bay of Bengal cyclones in the recent past are 3, 00,000 and 1, 31,000 in Bangladesh in 1970 and 1991 respectively; 10,000 and 1000 in 1977 and 1990 respectively in Andhra Pradesh (India) (Smith, 1989; Holland, 1993; Gupta, 1999). The super cyclone that crossed Orissa (India) coast on 29th November 1999 affected 129.66 lakhs people (about 10,000 people killed) and caused huge damage to properties (Kalsi, 2003). After independence, the most severe cyclone that crossed West Bengal coast was the cyclone of November 1988. Around 28.3 lacs people in 3893 villages were affected by the cyclone, killing 532 people.
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Chapter Four<br />
Hazard Analysis: <strong>Cyclone</strong> <strong>and</strong> <strong>Storm</strong> <strong>Surge</strong><br />
4.1. <strong>Cyclone</strong> hazard in coastal zones<br />
Tropical cyclones are the deadliest of all natural disaster worldwide, accounting for about 64% of the<br />
total loss of lives. The 80-100 tropical cyclones that occur worldwide each year cause, on an<br />
average, death of 20,000 people <strong>and</strong> a total economic loss of $6-7 billion (Southern 1979). The<br />
Indian subcontinent is the worst affected part of the world as far as the death toll associated with<br />
tropical cyclone is concerned. Out of 9-recorded cases of heavy loss of human lives (40,000 or more)<br />
by cyclones during the past 300 years, 7 cases (77%) occurred in Indian subcontinent (Frank <strong>and</strong><br />
Hussain, 1971; Smith, 1989; Hebert et al., 1996). The tropical cyclones affect this region in two<br />
seasons: Pre-monsoon (April-May) <strong>and</strong> Post-monsoon (October-December). The peak frequency is<br />
found to be in the months of May <strong>and</strong> November.<br />
CHAPTER 4<br />
The Bay of Bengal is potentially energetic for the development of cyclonic storms <strong>and</strong> accounts for<br />
about 7% of the global annual total number of storms (Gray, 1968). These storms usually move<br />
towards the west, northwest <strong>and</strong> north. Some of them recurve towards northeast after initial<br />
northwestward movement. Though, considered to be much weaker in intensity <strong>and</strong> smaller in size as<br />
compared to the cyclones of other regions, the Bay of Bengal cyclones, in particular, the post<br />
monsoon cyclones that cross east coast of India or Bangladesh are highly devastating. This is mainly<br />
due to dense populated coastal region, shallow bathymetry; nearly funnel shape of the coastline <strong>and</strong><br />
the long stretch of the low-lying delta region embedded with large number of river systems. The<br />
casualty figures associated with major Bay of Bengal cyclones in the recent past are 3, 00,000 <strong>and</strong> 1,<br />
31,000 in Bangladesh in 1970 <strong>and</strong> 1991 respectively; 10,000 <strong>and</strong> 1000 in 1977 <strong>and</strong> 1990<br />
respectively in Andhra Pradesh (India) (Smith, 1989; Holl<strong>and</strong>, 1993; Gupta, 1999). The super cyclone<br />
that crossed Orissa (India) coast on 29th November 1999 affected 129.66 lakhs people (about<br />
10,000 people killed) <strong>and</strong> caused huge damage to properties (Kalsi, 2003). After independence, the<br />
most severe cyclone that crossed West Bengal coast was the cyclone of November 1988. Around<br />
28.3 lacs people in 3893 villages were affected by the cyclone, killing 532 people.