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: Other/Unknown Material
Language:English
Published: Lunds universitet/Avdelningen för Teknisk vattenresurslära 2018
Subjects:
Online Access:http://lup.lub.lu.se/student-papers/record/8955078
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spelling ftulundlupsp:oai:lup-student-papers.lub.lu.se:8955078 2023-07-30T04:04:24+02:00 Sediment transport and bathymetric change at Hornafjörður tidal inlet - Field data analysis and mathematical modeling Klante, Clemens 2018 application/pdf http://lup.lub.lu.se/student-papers/record/8955078 eng eng Lunds universitet/Avdelningen för Teknisk vattenresurslära http://lup.lub.lu.se/student-papers/record/8955078 ISSN: 1101-9824 Coastal Inlet Hornafjörður Morphology TELEMAC ebb shoal mathematical modeling Technology and Engineering H2 2018 ftulundlupsp 2023-07-11T20:08:33Z 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. Island states like Iceland need reliable connections to their harbors to ensure the import and export of goods as well as the wealth of industries like fishing. This connection is determined by a sufficient water depth. In coastal areas, especially along the shore and at coastal inlets the sea bed changes constantly and sedimentation can interrupt the nautical connection to the open sea. Due to that, knowledge about how the sea bed behaves is important to help decision makers and engineers to implement strategies and different coastal structures to retain a sufficient water depth for the navigation of water vessels. Forces ... Other/Unknown Material Iceland Lund University Publications Student Papers (LUP-SP) Barrier Island ENVELOPE(78.396,78.396,-68.431,-68.431) 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 Student Papers (LUP-SP)
op_collection_id ftulundlupsp
language English
topic Coastal Inlet
Hornafjörður
Morphology
TELEMAC
ebb shoal
mathematical modeling
Technology and Engineering
spellingShingle Coastal Inlet
Hornafjörður
Morphology
TELEMAC
ebb shoal
mathematical modeling
Technology and Engineering
Klante, Clemens
Sediment transport and bathymetric change at Hornafjörður tidal inlet - Field data analysis and mathematical modeling
topic_facet Coastal Inlet
Hornafjörður
Morphology
TELEMAC
ebb shoal
mathematical modeling
Technology and 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. Island states like Iceland need reliable connections to their harbors to ensure the import and export of goods as well as the wealth of industries like fishing. This connection is determined by a sufficient water depth. In coastal areas, especially along the shore and at coastal inlets the sea bed changes constantly and sedimentation can interrupt the nautical connection to the open sea. Due to that, knowledge about how the sea bed behaves is important to help decision makers and engineers to implement strategies and different coastal structures to retain a sufficient water depth for the navigation of water vessels. Forces ...
format Other/Unknown Material
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 Lunds universitet/Avdelningen för Teknisk vattenresurslära
publishDate 2018
url http://lup.lub.lu.se/student-papers/record/8955078
long_lat ENVELOPE(78.396,78.396,-68.431,-68.431)
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 Barrier Island
Höfn
Hornafjörður
South Barrier
geographic_facet Barrier Island
Höfn
Hornafjörður
South Barrier
genre Iceland
genre_facet Iceland
op_relation http://lup.lub.lu.se/student-papers/record/8955078
ISSN: 1101-9824
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