Morphodynamic evolution of two deltas in arctic environments, east coast of Greenland

Publikation: Bidrag til bog/antologi/rapport › Konferencebidrag i proceedings › Forskning › fagfællebedømt

Standard

Morphodynamic evolution of two deltas in arctic environments, east coast of Greenland. / Kroon, Aart; Pedersen, Jørn Bjarke Torp; Sigsgaard, Charlotte.

The Proceedings of the Coastal Sediments 2011 . Bind 3 Singapore : World Scientific, 2011. s. 2299-2310.

Publikation: Bidrag til bog/antologi/rapport › Konferencebidrag i proceedings › Forskning › fagfællebedømt

Harvard

Kroon, A, Pedersen, JBT & Sigsgaard, C 2011, Morphodynamic evolution of two deltas in arctic environments, east coast of Greenland. i The Proceedings of the Coastal Sediments 2011 . bind 3, World Scientific, Singapore, s. 2299-2310, Proceedings of the Coastal Sediments 2011, Miami, USA, 02/05/2011. https://doi.org/10.1142/9789814355537_0172

APA

Kroon, A., Pedersen, J. B. T., & Sigsgaard, C. (2011). Morphodynamic evolution of two deltas in arctic environments, east coast of Greenland. I The Proceedings of the Coastal Sediments 2011 (Bind 3, s. 2299-2310). World Scientific. https://doi.org/10.1142/9789814355537_0172

Vancouver

Kroon A, Pedersen JBT, Sigsgaard C. Morphodynamic evolution of two deltas in arctic environments, east coast of Greenland. I The Proceedings of the Coastal Sediments 2011 . Bind 3. Singapore: World Scientific. 2011. s. 2299-2310 https://doi.org/10.1142/9789814355537_0172

Author

Kroon, Aart ; Pedersen, Jørn Bjarke Torp ; Sigsgaard, Charlotte. / Morphodynamic evolution of two deltas in arctic environments, east coast of Greenland. The Proceedings of the Coastal Sediments 2011 . Bind 3 Singapore : World Scientific, 2011. s. 2299-2310

Bibtex

@inproceedings{de10c94722154319ba53b008193af372,
title = "Morphodynamic evolution of two deltas in arctic environments, east coast of Greenland",
abstract = "Changes in fluvial channel patterns on deltas have a significant impact on the coastal morphology along its fringes. Lateral channel migration can locally cause cliff erosion and introduce an extra sediment source in the local budget of an active delta plain. Stabilization of channels or even channel lobe switching reduce the fluvial impact on the delta and introduce the formation of beach ridges and spits along the (former) delta edge. These accumulative features are formed in the ice-free summer periods and fed by alongshore sediment input from adjacent shores due to wave-driven alongshore currents, and by the reworking of the sediments on the delta plain by wave-driven cross-shore processes. ",
author = "Aart Kroon and Pedersen, {J{\o}rn Bjarke Torp} and Charlotte Sigsgaard",
year = "2011",
doi = "10.1142/9789814355537_0172",
language = "English",
isbn = "981-4355-789",
volume = "3",
pages = "2299--2310",
booktitle = "The Proceedings of the Coastal Sediments 2011",
publisher = "World Scientific",
address = "United States",
note = "Proceedings of the Coastal Sediments 2011 ; Conference date: 02-05-2011 Through 06-05-2011",

}

RIS

TY - GEN

T1 - Morphodynamic evolution of two deltas in arctic environments, east coast of Greenland

AU - Kroon, Aart

AU - Pedersen, Jørn Bjarke Torp

AU - Sigsgaard, Charlotte

PY - 2011

Y1 - 2011

N2 - Changes in fluvial channel patterns on deltas have a significant impact on the coastal morphology along its fringes. Lateral channel migration can locally cause cliff erosion and introduce an extra sediment source in the local budget of an active delta plain. Stabilization of channels or even channel lobe switching reduce the fluvial impact on the delta and introduce the formation of beach ridges and spits along the (former) delta edge. These accumulative features are formed in the ice-free summer periods and fed by alongshore sediment input from adjacent shores due to wave-driven alongshore currents, and by the reworking of the sediments on the delta plain by wave-driven cross-shore processes.

AB - Changes in fluvial channel patterns on deltas have a significant impact on the coastal morphology along its fringes. Lateral channel migration can locally cause cliff erosion and introduce an extra sediment source in the local budget of an active delta plain. Stabilization of channels or even channel lobe switching reduce the fluvial impact on the delta and introduce the formation of beach ridges and spits along the (former) delta edge. These accumulative features are formed in the ice-free summer periods and fed by alongshore sediment input from adjacent shores due to wave-driven alongshore currents, and by the reworking of the sediments on the delta plain by wave-driven cross-shore processes.

U2 - 10.1142/9789814355537_0172

DO - 10.1142/9789814355537_0172

M3 - Article in proceedings

SN - 981-4355-789

VL - 3

SP - 2299

EP - 2310

BT - The Proceedings of the Coastal Sediments 2011

PB - World Scientific

CY - Singapore

T2 - Proceedings of the Coastal Sediments 2011

Y2 - 2 May 2011 through 6 May 2011

ER -

ID: 33437516