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Cyclone hazard and unpredictability:
preparing coastal communities
Yugraj Singh Yadava, Director, Bay of Bengal Programme Inter-Governmental Organisation
T
he Bay of Bengal (BoB) forms the north-eastern part of
the Indian Ocean. Resembling a triangle in shape, the Bay
is bordered by Bangladesh, India, Indonesia, Malaysia,
Maldives, Myanmar, Sri Lanka and Thailand. It is also the
largest bay in the world by area.
A number of large rivers and their tributaries flow into the BoB,
which is situated in the monsoon belt and receives high rainfall. It
is a hot spot of biological diversity thanks to its coral reefs, estuar-
ies, coastal wetlands and mangroves. More than a quarter of the
world’s population resides in the countries around the bay, many
of them living below the international poverty line of US$1 per day
and dependent on coastal resources for food and livelihood security.
Cyclones in the Bay of Bengal
The BoB is also periodically in the news for the destructive cyclones
1
storms that occur from time to time. Of the 30 deadliest cyclones in
world history from 1584 to 2008, as many as 22 have occurred here.
Three recent cyclones, Sidr (2007), Nargis (2008) and Aila (2009),
have caused great loss of life and property in Bangladesh, Myanmar
and India respectively.
With a long coastline of over 8,000 kilometres, the Indian subcon-
tinent is exposed to nearly 10 per cent of the world’s tropical
cyclones. Most of these have their genesis over the BoB and strike
the east coast of India. On average, five to six tropical cyclones form
every year, of which two or three could be severe. About four times
as many cyclones occur in the BoB as in the Arabian Sea.
Bangladesh, due to its unique geographic location, frequently
suffers from devastating tropical cyclones. The funnel-shaped
northern portion of the BoB causes tidal bores when cyclones
make landfall, affecting thousands of people living in the coastal
areas. One of the most devastating natural disasters
in recorded history was the 1970 Bhola cyclone in
Bangladesh (then East Pakistan) that alone claimed
more than 500,000 lives. The maximum recorded wind
speed of this cyclone was about 222 kilometres per hour
and the maximum storm surge height was about 10.6
metres. The cyclone occurred during high tide, causing
enormous damage. Table 1 provides a summary of loss
of life and damage to property from cyclones in the BoB
during the period 1900–2010.
Cyclone warning systems in the region
Ocean Observation Systems (OOS) have become vital
for countries bordering the BoB. In 1996, the Indian
National Institute of Ocean Technology (NIOT) estab-
lished the National Data Buoy Programme with the
objective of operating, maintaining and developing
moored buoy observational networks and related tele-
communication facilities in the Indian seas. These data
buoys are offshore floating platforms, fitted with mete-
orological and oceanographic sensors and moored at
specific locations to observe met-ocean data at regular
intervals. The buoys are powered by lithium batter-
ies and are equipped with Global Positioning Systems
(GPS) to provide their locations. The observed data is
then transmitted through satellite along with the loca-
tion reference, in synoptic hours, to the state-of-the-art
shore station facility at NIOT, Chennai. The OOS team
at NIOT has also developed, tested and established a
Tsunami Buoy System, using bottom pressure recorders
in the Indian seas. The new venture has expanded the
2018
Country
Bangladesh
India
Maldives
2
Myanmar
Sri Lanka
Tropical cyclones (nos)
84
97
1
17
5
Killed
626 843
159 130
0
144 663
1 160
Total affected
73 556 523
87 392 126
23 849
3 935 844
2 060 000
Estimated damage (US$ Million)
4 765.98
8 600.90
30.00
4 079.39
137.30
Table 1: Summary of casualties in the countries around the BoB due to tropical cyclones, 1900 – 2010
Source: EM-DAT, OFDA/CRED International Disaster Database. Université Catholique de Louvain, Brussels, Belgium




