ICT in Agriculture and Disaster Management - Bangladesh ...
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Table 5. Extent of soil sal<strong>in</strong>ity dur<strong>in</strong>g about last four decades (1973-2009) <strong>in</strong> coastal areas<br />
Year<br />
Total Salt<br />
Sal<strong>in</strong>ity Class<br />
affected area S1<br />
S2<br />
S3<br />
S4<br />
('000' ha) 2.0-4.0 dS/m 4.1-8.0 dS/m 8.1-16.0 dS/m >16.0 dS/m<br />
1973 833.45 287.37 426.43 79.75 39.90<br />
2000 1020.75 289.76 307.20 336.58 87.14<br />
2009 1056.19 328.39 274.21 351.68 101.14<br />
Per cent <strong>in</strong>crease + 35.44 + 38.63 - 32.99 + 15.1 + 14.0<br />
(+) or decrease (-)<br />
dur<strong>in</strong>g<br />
2000-2009<br />
Source: Ahsan 2010.<br />
Cyclones <strong>and</strong> storm surges<br />
Figure 8. Cyclone prone zone of <strong>Bangladesh</strong><br />
Tropical cyclones are important features of the<br />
weather <strong>and</strong> climate of south Asia. The major<br />
cyclogenesis of this region exists <strong>in</strong> the<br />
northern Indian Ocean, which particularly<br />
affects <strong>Bangladesh</strong> <strong>and</strong> parts of India. Because<br />
of the funnel shape <strong>and</strong> geographic location of<br />
<strong>Bangladesh</strong>, severe cyclone <strong>and</strong> tidal surges<br />
are common along the 710 km coastal belt<br />
caus<strong>in</strong>g severe damage to life <strong>and</strong> property.<br />
Figure 8 depicts the cyclone prone zone of<br />
<strong>Bangladesh</strong>. Records of last 200 years show<br />
that at least 70 major cyclones hit the coastal<br />
belt of <strong>Bangladesh</strong>. Dur<strong>in</strong>g last 35 years,<br />
nearly 900,000 people died due to catastrophic<br />
cyclones. The Noakhali- Chittagong coast<br />
received 40 percent of the cyclones, which is<br />
the most vulnerable area for the l<strong>and</strong>fall of<br />
cyclones.<br />
The Chittagong-Cox's Bazaar coast received around 27 percent, while Khulna /<br />
Sundarban <strong>and</strong> Barisal-Noakhali coasts are relatively less vulnerable (Rahman, 2001).<br />
Some examples of severe tropical cyclones are the Barisal cyclone of 1584, the<br />
Bakerganj cyclone of 1876, the 12 November 1970 cyclone, the May 1985 Urir Char<br />
cyclone, <strong>and</strong> the April 1991 cyclone. High <strong>in</strong>tensity storm surges jeopardize the<br />
expansion of energy-recovery activities <strong>in</strong> the coastal areas <strong>and</strong> support<strong>in</strong>g <strong>in</strong>dustries,<br />
especially <strong>in</strong> the offshore areas (Islam & Ahmad, 2004).<br />
Low-flow conditions<br />
Low-flow conditions <strong>in</strong> the rivers are often observed <strong>in</strong> the w<strong>in</strong>ter months (lean<br />
period) when surface water irrigation becomes severely constra<strong>in</strong>ed. Under such<br />
conditions, the farmers have to take necessary actions to ensure irrigation by<br />
exploit<strong>in</strong>g groundwater resources. Low-flow conditions do not cause direct<br />
vulnerability to crop production, but cause economic hardship to the farmers of<br />
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