Sediment transfer from beach to shoreface: The sediment budget of an accreting beach on the Danish North Sea coast

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Standard

Sediment transfer from beach to shoreface: The sediment budget of an accreting beach on the Danish North Sea coast. / Aagaard, Troels.

I: Geomorphology, Bind 135, Nr. 1-2, 01.12.2011, s. 143-157.

Publikation: Bidrag til tidsskrift › Tidsskriftartikel › Forskning › fagfællebedømt

Harvard

Aagaard, T 2011, 'Sediment transfer from beach to shoreface: The sediment budget of an accreting beach on the Danish North Sea coast', Geomorphology, bind 135, nr. 1-2, s. 143-157. https://doi.org/10.1016/j.geomorph.2011.08.012

APA

Aagaard, T. (2011). Sediment transfer from beach to shoreface: The sediment budget of an accreting beach on the Danish North Sea coast. Geomorphology, 135(1-2), 143-157. https://doi.org/10.1016/j.geomorph.2011.08.012

Vancouver

Aagaard T. Sediment transfer from beach to shoreface: The sediment budget of an accreting beach on the Danish North Sea coast. Geomorphology. 2011 dec. 1;135(1-2):143-157. https://doi.org/10.1016/j.geomorph.2011.08.012

Author

Aagaard, Troels. / Sediment transfer from beach to shoreface: The sediment budget of an accreting beach on the Danish North Sea coast. I: Geomorphology. 2011 ; Bind 135, Nr. 1-2. s. 143-157.

Bibtex

@article{cd5c397ae7fd4c8ba32da82f5bf48238,
title = "Sediment transfer from beach to shoreface: The sediment budget of an accreting beach on the Danish North Sea coast",
abstract = "The sediment budget along the southern part of the exposed Danish North Sea coast was assessed through a combination of cross-shore profile analysis, numerical modeling and field measurements of cross-shore and longshore sediment transport at the boundary between the upper and the lower shorefaces. The beaches along this coast are accreting but observed sediment storage is far smaller than sediment supplied by southerly directed wave-driven currents. The excess sediment volumes are transferred seaward across the shoreface by systematically offshore-migrating nearshore bars that deliver sediment to the lower shoreface from where it is eventually removed by northward-directed wind-generated currents. In the geological past, sediment storage rates were much larger than at present and it is likely that the rate of storage along this coastline decreased as shoreface geometry adjusted towards equilibrium associated with shoreface steepening.",
author = "Troels Aagaard",
year = "2011",
month = dec,
day = "1",
doi = "10.1016/j.geomorph.2011.08.012",
language = "English",
volume = "135",
pages = "143--157",
journal = "Geomorphology",
issn = "0169-555X",
publisher = "Elsevier",
number = "1-2",

}

RIS

TY - JOUR

T1 - Sediment transfer from beach to shoreface: The sediment budget of an accreting beach on the Danish North Sea coast

AU - Aagaard, Troels

PY - 2011/12/1

Y1 - 2011/12/1

N2 - The sediment budget along the southern part of the exposed Danish North Sea coast was assessed through a combination of cross-shore profile analysis, numerical modeling and field measurements of cross-shore and longshore sediment transport at the boundary between the upper and the lower shorefaces. The beaches along this coast are accreting but observed sediment storage is far smaller than sediment supplied by southerly directed wave-driven currents. The excess sediment volumes are transferred seaward across the shoreface by systematically offshore-migrating nearshore bars that deliver sediment to the lower shoreface from where it is eventually removed by northward-directed wind-generated currents. In the geological past, sediment storage rates were much larger than at present and it is likely that the rate of storage along this coastline decreased as shoreface geometry adjusted towards equilibrium associated with shoreface steepening.

AB - The sediment budget along the southern part of the exposed Danish North Sea coast was assessed through a combination of cross-shore profile analysis, numerical modeling and field measurements of cross-shore and longshore sediment transport at the boundary between the upper and the lower shorefaces. The beaches along this coast are accreting but observed sediment storage is far smaller than sediment supplied by southerly directed wave-driven currents. The excess sediment volumes are transferred seaward across the shoreface by systematically offshore-migrating nearshore bars that deliver sediment to the lower shoreface from where it is eventually removed by northward-directed wind-generated currents. In the geological past, sediment storage rates were much larger than at present and it is likely that the rate of storage along this coastline decreased as shoreface geometry adjusted towards equilibrium associated with shoreface steepening.

U2 - 10.1016/j.geomorph.2011.08.012

DO - 10.1016/j.geomorph.2011.08.012

M3 - Journal article

VL - 135

SP - 143

EP - 157

JO - Geomorphology

JF - Geomorphology

SN - 0169-555X

IS - 1-2

ER -

ID: 34361078