2015
DOI: 10.1080/01490419.2015.1053640
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Modeling Storm Surge and its Associated Inland Inundation Extent Due to Very Severe Cyclonic Storm Phailin

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Cited by 31 publications
(7 citation statements)
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“…The most important of these ingredients is an accurate bathymetry and topography (Krien et al, 2016(Krien et al, , 2017Murty et al, 1986). Second, it is required to have a large-scale modelling domain comprising the whole Ganges-Brahmaputra-Meghna (GBM) estuarine network (Johns and Ali, 1980;Oliveira et al, 2020) at a high-enough model resolution (Krien et al, 2017;Kuroda et al, 2010). The modelling framework is required to simulate tide and surge together to account for the tide-surge interactions (As-Salek and Yasuda, 2001;Johns and Ali, 1980;Kuroda et al, 2010;Murty et al, 1986).…”
mentioning
confidence: 99%
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“…The most important of these ingredients is an accurate bathymetry and topography (Krien et al, 2016(Krien et al, , 2017Murty et al, 1986). Second, it is required to have a large-scale modelling domain comprising the whole Ganges-Brahmaputra-Meghna (GBM) estuarine network (Johns and Ali, 1980;Oliveira et al, 2020) at a high-enough model resolution (Krien et al, 2017;Kuroda et al, 2010). The modelling framework is required to simulate tide and surge together to account for the tide-surge interactions (As-Salek and Yasuda, 2001;Johns and Ali, 1980;Kuroda et al, 2010;Murty et al, 1986).…”
mentioning
confidence: 99%
“…Second, it is required to have a large-scale modelling domain comprising the whole Ganges-Brahmaputra-Meghna (GBM) estuarine network (Johns and Ali, 1980;Oliveira et al, 2020) at a high-enough model resolution (Krien et al, 2017;Kuroda et al, 2010). The modelling framework is required to simulate tide and surge together to account for the tide-surge interactions (As-Salek and Yasuda, 2001;Johns and Ali, 1980;Kuroda et al, 2010;Murty et al, 1986). Furthermore, an online coupling of the hydrodynamics and the short waves is also necessary to account for the wave set-up (Deb and Ferreira, 2016;Krien et al, 2017).…”
mentioning
confidence: 99%
“…() and Srinivasa Kumar et al . (). These study attempts to generate various possible scenarios of storm surge and inundation data using the state‐of‐the‐art ADCIRC (advanced circulation) model with various combinations of cyclone parameters on the synthetic tracks.…”
Section: Introductionmentioning
confidence: 97%
“…The Figure 3 c illustrates the enlarged view on the extent of maximum horizontal inundation with the Phailin cyclone. Sreenivasa Kumar et al 20 reported that the maximum inundation extent of about 430 m occurred neared Ganjam for Phailin cyclone (Figure 3 c). Their study showed that the modelled inundation extent varied between 50 and 430 m, and increased over regions where the topographical slope was less than 1 : 100, and post-storm survey data at 29 coastal stations were used to validate the model-simulated inundation extent 20 .…”
Section: Progress In Inundation Modelling For the Indian Subcontinentmentioning
confidence: 99%
“…14 for more details. The recent studies on storm surge modelling and coastal flooding for the east coast of India include a coupled hydrodynamic modelling system for very severe cyclones such as Phailin 19,20 , Thane 21,22 , Aila 23 . Compared to storm-surge events, the extent of flooding and destruction is extremely higher for tsunami events.…”
mentioning
confidence: 99%