Sediment transport and bathymetric change at Hornafjörður tidal inlet : Field data analysis and mathematical modeling

Commercial fishing makes the coastal inlet in Hornafjörður to an important navigational link for the port of Höfn in southeast Iceland. Low water depth caused through sediment accumulation along the ebb shoal generates navigational problems and the phenomenon of glacial rebound seems to intensify th...

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Main Author: Klante, Clemens
Format: Text
Language:English
Published: Lund University 2018
Subjects:
Online Access:https://lup.lub.lu.se/record/5904bc2d-f7d0-4ec4-95f7-e6f13377417c
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spelling ftulundlup:oai:lup.lub.lu.se:5904bc2d-f7d0-4ec4-95f7-e6f13377417c 2023-05-15T16:50:59+02:00 Sediment transport and bathymetric change at Hornafjörður tidal inlet : Field data analysis and mathematical modeling Klante, Clemens 2018 https://lup.lub.lu.se/record/5904bc2d-f7d0-4ec4-95f7-e6f13377417c eng eng Lund University https://lup.lub.lu.se/record/5904bc2d-f7d0-4ec4-95f7-e6f13377417c TVVR; 18(5002) (2018) Water Engineering thesis/master info:eu-repo/semantics/other text 2018 ftulundlup 2023-02-01T23:36:30Z Commercial fishing makes the coastal inlet in Hornafjörður to an important navigational link for the port of Höfn in southeast Iceland. Low water depth caused through sediment accumulation along the ebb shoal generates navigational problems and the phenomenon of glacial rebound seems to intensify this problem. Economic losses caused by the inability of fishing boats to navigate through the coastal inlet due to insufficient water depth along the ebb shoal are estimated with 4.5 million ISK (ca. $ 50.000) per year and effect the local society. This thesis aims to gain a better understanding of the complex morphology caused by large longshore sediment transports and local gradients with the help of mathematical modeling. With this knowledge measures such as structures and different activities to ensure sufficient navigational depth can be implement. A intense investigation of local transport patterns with the help of bathymetry measurements has been carried to intensify the knowledge about local particularities. This knowledge has been used to set up a sufficient mathematical model with the help of the open TELEMAC-MASCARET system. Results show that the morphologic pattern for high energy events are governed by the tidal flow and wave currents to almost same parts and sediment movements along the ebb shoal could be minimized with the implementation of a structure along the south barrier. Text Iceland Lund University Publications (LUP) Höfn ENVELOPE(-22.500,-22.500,65.433,65.433) Hornafjörður ENVELOPE(-15.292,-15.292,64.261,64.261) South Barrier ENVELOPE(73.583,73.583,-53.150,-53.150)
institution Open Polar
collection Lund University Publications (LUP)
op_collection_id ftulundlup
language English
topic Water Engineering
spellingShingle Water Engineering
Klante, Clemens
Sediment transport and bathymetric change at Hornafjörður tidal inlet : Field data analysis and mathematical modeling
topic_facet Water Engineering
description Commercial fishing makes the coastal inlet in Hornafjörður to an important navigational link for the port of Höfn in southeast Iceland. Low water depth caused through sediment accumulation along the ebb shoal generates navigational problems and the phenomenon of glacial rebound seems to intensify this problem. Economic losses caused by the inability of fishing boats to navigate through the coastal inlet due to insufficient water depth along the ebb shoal are estimated with 4.5 million ISK (ca. $ 50.000) per year and effect the local society. This thesis aims to gain a better understanding of the complex morphology caused by large longshore sediment transports and local gradients with the help of mathematical modeling. With this knowledge measures such as structures and different activities to ensure sufficient navigational depth can be implement. A intense investigation of local transport patterns with the help of bathymetry measurements has been carried to intensify the knowledge about local particularities. This knowledge has been used to set up a sufficient mathematical model with the help of the open TELEMAC-MASCARET system. Results show that the morphologic pattern for high energy events are governed by the tidal flow and wave currents to almost same parts and sediment movements along the ebb shoal could be minimized with the implementation of a structure along the south barrier.
format Text
author Klante, Clemens
author_facet Klante, Clemens
author_sort Klante, Clemens
title Sediment transport and bathymetric change at Hornafjörður tidal inlet : Field data analysis and mathematical modeling
title_short Sediment transport and bathymetric change at Hornafjörður tidal inlet : Field data analysis and mathematical modeling
title_full Sediment transport and bathymetric change at Hornafjörður tidal inlet : Field data analysis and mathematical modeling
title_fullStr Sediment transport and bathymetric change at Hornafjörður tidal inlet : Field data analysis and mathematical modeling
title_full_unstemmed Sediment transport and bathymetric change at Hornafjörður tidal inlet : Field data analysis and mathematical modeling
title_sort sediment transport and bathymetric change at hornafjörður tidal inlet : field data analysis and mathematical modeling
publisher Lund University
publishDate 2018
url https://lup.lub.lu.se/record/5904bc2d-f7d0-4ec4-95f7-e6f13377417c
long_lat ENVELOPE(-22.500,-22.500,65.433,65.433)
ENVELOPE(-15.292,-15.292,64.261,64.261)
ENVELOPE(73.583,73.583,-53.150,-53.150)
geographic Höfn
Hornafjörður
South Barrier
geographic_facet Höfn
Hornafjörður
South Barrier
genre Iceland
genre_facet Iceland
op_source TVVR; 18(5002) (2018)
op_relation https://lup.lub.lu.se/record/5904bc2d-f7d0-4ec4-95f7-e6f13377417c
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