Numerical Modeling of storm surge for the coastal region of Bangladesh

This thesis is submitted in partial fulfilment of the requirements for the degree of Bachelor of Science in Mathematics 2022.

מידע ביבליוגרפי
מחבר ראשי: Chaudhury, Samara
מחברים אחרים: Naher, Dr. Hasibun
פורמט: Thesis
שפה:English
יצא לאור: Brac University 2023
נושאים:
גישה מקוונת:http://hdl.handle.net/10361/18104
id 10361-18104
record_format dspace
spelling 10361-181042023-04-06T21:01:55Z Numerical Modeling of storm surge for the coastal region of Bangladesh Chaudhury, Samara Naher, Dr. Hasibun Department of Mathematics and Natural Sciences, BRAC University Numerical Modeling Storm Surge Coastal Region of Bangladesh Coastal zone management. This thesis is submitted in partial fulfilment of the requirements for the degree of Bachelor of Science in Mathematics 2022. Catalogued from PDF version of thesis. Includes bibliographical references (page 93-103). This study investigates the estimated water levels during a cyclonic storm due to the interaction of tide and surge which also includes air bubble entrainment along the coastal areas of Bangladesh. Thus, a two-dimensional, vertically integrated hydrodynamic model in Cartesian coordinates has been developed. The model equations are solved using finite difference schemes implementing a staggered C-grid. Nested scheme methods are used to incorporate the complexity of the coast in order to not waste central processing unit time. Along the northeast corner of the innermost scheme or the very fine mesh scheme (VFMS), the Meghna river discharge is considered and the coastal and island boundaries are approximated via proper stair steps. A stable tidal condition over the area of interest is produced by making the sea level oscillate with the major tidal constituent M2 through the southern open boundary of the parent scheme or the coarse mesh scheme (CMS). The model is used to compute the water levels due to tide-surge interaction including the air bubble effect for the April 1991 cyclone. The model results are found to compare well with the observations from Bangladesh Inland Water Transport Authority. Therefore, the model is found to adequately simulate water levels which is in the presence of air bubbles. Additionally, it can also be observed that water levels are affected by factors such as river discharge and inverse barometer among others. Samara Chaudhury B. Mathematics 2023-04-06T09:01:13Z 2023-04-06T09:01:13Z 2022 2022 Thesis ID: 15305022 http://hdl.handle.net/10361/18104 en BRAC University theses are protected by copyright. They may be viewed from this source for any purpose, but reproduction or distribution in any format is prohibited without written permission. 103 pages application/pdf Brac University
institution Brac University
collection Institutional Repository
language English
topic Numerical Modeling
Storm Surge
Coastal Region of Bangladesh
Coastal zone management.
spellingShingle Numerical Modeling
Storm Surge
Coastal Region of Bangladesh
Coastal zone management.
Chaudhury, Samara
Numerical Modeling of storm surge for the coastal region of Bangladesh
description This thesis is submitted in partial fulfilment of the requirements for the degree of Bachelor of Science in Mathematics 2022.
author2 Naher, Dr. Hasibun
author_facet Naher, Dr. Hasibun
Chaudhury, Samara
format Thesis
author Chaudhury, Samara
author_sort Chaudhury, Samara
title Numerical Modeling of storm surge for the coastal region of Bangladesh
title_short Numerical Modeling of storm surge for the coastal region of Bangladesh
title_full Numerical Modeling of storm surge for the coastal region of Bangladesh
title_fullStr Numerical Modeling of storm surge for the coastal region of Bangladesh
title_full_unstemmed Numerical Modeling of storm surge for the coastal region of Bangladesh
title_sort numerical modeling of storm surge for the coastal region of bangladesh
publisher Brac University
publishDate 2023
url http://hdl.handle.net/10361/18104
work_keys_str_mv AT chaudhurysamara numericalmodelingofstormsurgeforthecoastalregionofbangladesh
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