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Ghosh and Prakasam



































                                                     Figure 1. The study area map

                Hills, (ii) the north-eastern and eastern sides are defined   elevation, distance from the river, distance from the road,
                by the Naga and Barail ranges, and (iii) the southern and   and  geology  –  were  used  for  the  analysis.  Secondary
                south-eastern sides are composed of Mizo hills.     data were utilized to prepare all the model input layers.
                  The  central,  eastern,  and  Bangladesh  parts  of  the   The  training  and  validation  flood  points  were  drawn
                basin are floodplains of the river, which are highly flood-  from  the  National  Remote  Sensing  Centre  generated
                prone. Flooding is a recurring event in the Barak River   flood inundation maps of 14th July 2022 flood. The area
                floodplain; each year during monsoon season, large areas   under the curve (AUC) method validated the generated
                get inundated by river floods, causing significant property   maps.  After  the  preparation  of  the  input  layers,  input
                and crop damage and disrupting the communication    parameter weights were calculated for both Shannon’s
                system. Major floods occurred in the study area in 1991,   entropy  and  FR  models.  In  the  second  stage,  after
                1994, 1996, 2004, and 2009.  Floods in the Barak River   delineating flood hazard-susceptible areas, the flood risk
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                basin are frequent and severely impact the Barak Valley   of the hazard-susceptible villages was studied. For risk
                of  Assam, which comprises three districts: Cachar,   assessment, village boundaries, and associated parameter
                Karimganj, and Halikandi, with a total geographical area   data were derived using the Census of India 2011. Weights
                of 6,922 km . Silchar, the second largest city of Assam,   were assigned to four indicators for exposure assessment:
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                is located in the Cachar district along the banks of the   village-level elevation, river length, normalized difference
                Barak River. Barak Valley is one of the most densely   vegetation  index  (NDVI),  and  normalized  difference
                populated regions of  Assam, with a population of   water index (NDWI) using the AHP method. Similarly,
                1,736,617. Cachar is the second-most populated district,   weightages were assigned to six indicators – population
                while  Karimganj  and  Hailakandi  have  populations  of   density, household density, child population (0 – 6 years),
                1,228,686 and 659,296, respectively. These populations   illiteracy rate, marginal workers, and agricultural workers
                are spread across 2,307 villages and town areas. 21,22  –  for  assessing  the  vulnerability  of  the  villages.  In  the
                                                                    final stage, the risk index of the villages was derived by
                3. Methodology                                      combining both the exposure and vulnerability indices.


                Figure  2  shows  the  methodological  flowchart. Eight   3.1. Shannon’s entropy model
                flood  conditioning  factors  –  drainage  density,  drainage   Entropy  measures  each  system’s  instability,
                frequency,  topographic wetness index (TWI), slope,   abnormality, and unbalanced behavior.  The  theory
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                Volume 22 Issue 2 (2025)                        66                           doi: 10.36922/AJWEP025040019
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