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parts of the Asia during monsoon frequently suffer from
severe floods. Some part of1ndia and Bangladesh
experiences floods almost every year with considerable
damage. Flood statistics for Bangladesh are available
since 1954 and are summarized in Table- 2.5 as follows:
table 2.5
The floods of 1954, 1955, 1974,
1987, 1988 all caused enormous damages to properties and
considerable loss of life. The consecutive floods of
1987 and 1988 caused heavy damage. Again during 1998
Bangladesh experienced most devastating and prolonged
flood in the history and caused serious disruption on
the economy of the country. Areas of Bangladesh was
flooded in 1998 is shown in Figure-2.4.
According
to government sources, the 1998 flood inundated about
100,000 km2. The 1998 floods affected 68% of the country,
and seriously impacted the livelihoods of 30 million
people. Overall damage was estimated at two to three
billion U.S. dollars. Final estimates showed that 51
districts and 307 Upazilas were inundated, about 1400
people were killed, 1.77 million houses were damaged, and
23,45,8713 people became homeless. The 1998 floods lasted
for over 10 weeks (WB, 2000).
The origin and wide-ranging impacts
of the 1998 flood, which began in July and ended in
September, are summarized below.
- The magnitude and duration of
the 1998 flood can be explained in large part by the
simultaneous realization of the impacts from three
factors:
- Heavy rainfall/snowmelt in India
and Nepal (which increased the flow in the rivers
entering Bangladesh.)
- Increased July rainfall within
critical river basins in Bangladesh (Ganges, Brahmaputra,
Meghna, Southeastern Basin) .
- Tidal surges in the Bay of
Bengal.
The first and second factors help
explain the magnitude of the 1998 flood. In this respect,
it is worth noting the extent to which the 1998 July
rainfall totals within some of Bangladesh's critical river
basins exceeded the typical July average.
The third factor, tidal surge
levels in the Bay of Bengal, with back water effects,
reduced the Bay's capacity to receive the floodwaters.
This, in part, contributed to the duration of the
flooding.
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