Wave energy fluxes and multi-decadal shoreline changes

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Standard

Wave energy fluxes and multi-decadal shoreline changes. / Kabuth, Alina Kristin; Kroon, Aart.

I: Ocean Dynamics, Bind 64, Nr. 5, 2014, s. 741-754.

Publikation: Bidrag til tidsskrift › Tidsskriftartikel › Forskning › fagfællebedømt

Harvard

Kabuth, AK & Kroon, A 2014, 'Wave energy fluxes and multi-decadal shoreline changes', Ocean Dynamics, bind 64, nr. 5, s. 741-754. https://doi.org/10.1007/s10236-014-0709-6

APA

Kabuth, A. K., & Kroon, A. (2014). Wave energy fluxes and multi-decadal shoreline changes. Ocean Dynamics, 64(5), 741-754. https://doi.org/10.1007/s10236-014-0709-6

Vancouver

Kabuth AK, Kroon A. Wave energy fluxes and multi-decadal shoreline changes. Ocean Dynamics. 2014;64(5):741-754. https://doi.org/10.1007/s10236-014-0709-6

Author

Kabuth, Alina Kristin ; Kroon, Aart. / Wave energy fluxes and multi-decadal shoreline changes. I: Ocean Dynamics. 2014 ; Bind 64, Nr. 5. s. 741-754.

Bibtex

@article{c82a860966074bc487b3fadb8fbae5f5,
title = "Wave energy fluxes and multi-decadal shoreline changes",
abstract = "Spatial patterns of multidecadal shoreline changes in two microtidal, low-energetic embayments of southern Zealand, Denmark, were investigated by using the directional distribution of wave energy fluxes. The sites include a barrier island system attached to moraine bluffs, and a recurved spit adjacent to a cliff coast. The barrier island system is characterized by cross-shore translation and by an alignment of the barrier alongshore alternating directions of barrier-spit progradation in a bidirectional wave field. The recurved spit adjacent to the cliff coast experienced shoreline rotation through proximal erosion and distal lateral accretion in a unidirectional wave climate. The multidecadal shoreline changes were coupled to a slope-based morphological coastal classification. All erosive shores occurred within a narrow range of onshore and offshore coastal slopes. The alongshore variability of directional distributions of wave energy fluxes furthermore outlined potential sediment sources and sinks for the evolution of the barrier island system and for the evolution of the recurved spit.",
author = "Kabuth, {Alina Kristin} and Aart Kroon",
year = "2014",
doi = "10.1007/s10236-014-0709-6",
language = "English",
volume = "64",
pages = "741--754",
journal = "Ocean Dynamics",
issn = "1616-7341",
publisher = "Springer",
number = "5",

}

RIS

TY - JOUR

T1 - Wave energy fluxes and multi-decadal shoreline changes

AU - Kabuth, Alina Kristin

AU - Kroon, Aart

PY - 2014

Y1 - 2014

N2 - Spatial patterns of multidecadal shoreline changes in two microtidal, low-energetic embayments of southern Zealand, Denmark, were investigated by using the directional distribution of wave energy fluxes. The sites include a barrier island system attached to moraine bluffs, and a recurved spit adjacent to a cliff coast. The barrier island system is characterized by cross-shore translation and by an alignment of the barrier alongshore alternating directions of barrier-spit progradation in a bidirectional wave field. The recurved spit adjacent to the cliff coast experienced shoreline rotation through proximal erosion and distal lateral accretion in a unidirectional wave climate. The multidecadal shoreline changes were coupled to a slope-based morphological coastal classification. All erosive shores occurred within a narrow range of onshore and offshore coastal slopes. The alongshore variability of directional distributions of wave energy fluxes furthermore outlined potential sediment sources and sinks for the evolution of the barrier island system and for the evolution of the recurved spit.

AB - Spatial patterns of multidecadal shoreline changes in two microtidal, low-energetic embayments of southern Zealand, Denmark, were investigated by using the directional distribution of wave energy fluxes. The sites include a barrier island system attached to moraine bluffs, and a recurved spit adjacent to a cliff coast. The barrier island system is characterized by cross-shore translation and by an alignment of the barrier alongshore alternating directions of barrier-spit progradation in a bidirectional wave field. The recurved spit adjacent to the cliff coast experienced shoreline rotation through proximal erosion and distal lateral accretion in a unidirectional wave climate. The multidecadal shoreline changes were coupled to a slope-based morphological coastal classification. All erosive shores occurred within a narrow range of onshore and offshore coastal slopes. The alongshore variability of directional distributions of wave energy fluxes furthermore outlined potential sediment sources and sinks for the evolution of the barrier island system and for the evolution of the recurved spit.

U2 - 10.1007/s10236-014-0709-6

DO - 10.1007/s10236-014-0709-6

M3 - Journal article

VL - 64

SP - 741

EP - 754

JO - Ocean Dynamics

JF - Ocean Dynamics

SN - 1616-7341

IS - 5

ER -

ID: 130923494