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dc.contributor.authorMohammed Khaled;Islam A. K. M. Saiful;Islam G. M. Tarekul;Alfieri Lorenzo;Khan Md. Jamal Uddin;Bala Sujit Kumar;Das Mohan Kumar
dc.date.accessioned2019-02-26T07:50:15Z
dc.date.available2019-02-26T07:50:15Z
dc.date.issued2018
dc.identifier.other%28ASCE%29HE.1943-5584.0001705.pdf
dc.identifier.urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4249738
dc.description.abstractThis is the first study to assess the possible changes in floods in the Bangladesh part of the densely populated Ganges–Brahmaputra–Meghna (GBM) delta at 1.5°C, 2°C, and 4°C global warming levels. This study was undertaken with the aim of joining the efforts of the global scientific community to assist in the preparation of the upcoming Special Report on 1.5 Degrees by the Intergovernmental Panel on Climate Change. The future changes in the possibilities of peak synchronization of nearby large rivers were assessed for the first time. Peak synchronization is critical for flood assessment in low-lying delta regions like Bangladesh. Results indicate that the flood peaks of the GBM rivers are more likely to synchronize in the future. Results also indicate that the flood magnitudes may become more severe in the future. At global warming levels of 1.5°C, 2°C, and 4°C, flood flows with a 1-year return period are projected to increase by about 27%, 29%, and 54% for the Ganges; 8%, 24%, and 63% for the Brahmaputra; and 15%, 38%, and 81% for the Meghna, respectively, compared with a baseline of 1986–25.
dc.publisherAmerican Society of Civil Engineers
dc.titleFuture Floods in Bangladesh under 1.5°C, 2°C, and 4°C Global Warming Scenarios
dc.typeJournal Paper
dc.journal.volume23
dc.journal.issue12
dc.journal.titleJournal of Hydrologic Engineering
dc.identifier.doi10.1061/(ASCE)HE.1943-5584.0001705
dc.page4018050
dc.treeJournal of Hydrologic Engineering:;2018:;Volume ( 023 ):;issue: 012
dc.contenttypeFulltext


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