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MORFODINAMIKA ŠLJUNČANOG ŽALA PLOČE U UVJETIMA JAKOG JUGA

Research output: Contribution to Journal/MagazineJournal articlepeer-review

Published

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MORFODINAMIKA ŠLJUNČANOG ŽALA PLOČE U UVJETIMA JAKOG JUGA. / Lončar, Goran; Carević, Dalibor; Ilić, Suzana et al.
In: Hrvatske Vode, Vol. 28, No. 113, 30.09.2020, p. 205-216.

Research output: Contribution to Journal/MagazineJournal articlepeer-review

Harvard

Lončar, G, Carević, D, Ilić, S, Krvavica, N & Kalinić, F 2020, 'MORFODINAMIKA ŠLJUNČANOG ŽALA PLOČE U UVJETIMA JAKOG JUGA', Hrvatske Vode, vol. 28, no. 113, pp. 205-216. <https://www.voda.hr/hr/casopis-hrvatske-vode/broj-113>

APA

Lončar, G., Carević, D., Ilić, S., Krvavica, N., & Kalinić, F. (2020). MORFODINAMIKA ŠLJUNČANOG ŽALA PLOČE U UVJETIMA JAKOG JUGA. Hrvatske Vode, 28(113), 205-216. https://www.voda.hr/hr/casopis-hrvatske-vode/broj-113

Vancouver

Lončar G, Carević D, Ilić S, Krvavica N, Kalinić F. MORFODINAMIKA ŠLJUNČANOG ŽALA PLOČE U UVJETIMA JAKOG JUGA. Hrvatske Vode. 2020 Sept 30;28(113):205-216.

Author

Lončar, Goran ; Carević, Dalibor ; Ilić, Suzana et al. / MORFODINAMIKA ŠLJUNČANOG ŽALA PLOČE U UVJETIMA JAKOG JUGA. In: Hrvatske Vode. 2020 ; Vol. 28, No. 113. pp. 205-216.

Bibtex

@article{131dae77eb734ca18216c876556f4da2,
title = "MORFODINAMIKA {\v S}LJUN{\v C}ANOG {\v Z}ALA PLO{\v C}E U UVJETIMA JAKOG JUGA",
abstract = "An analysis of the morphodynamics of the artificially filled gravel beach Plo{\v c}e in Rijeka was conducted. The numerical simulations of wave deformations and gravel sediment transport were initially performed for hypothetical wave events with event directions SSE (157.50), S (1800), SSW (202.50) and SW (225°), a variation of significant wave heights (HS = 1.0 m, 1.5 m and 2.0 m) and corresponding peak wave periods. The parameterization of the numerical model is based on the results of the empirical pattern of the along-the-coast component of gravel sediment transport and the results of a laboratory investigation of the transverse component of gravel sediment transport. This was followed by a numerical simulation of the morphodynamics for one intense sirocco event (March 6, 2020), using the actual wave conditions recorded at the wave station located in immediate proximity of the beach Plo{\v c}e and the sea level dynamics recorded at the mareographic station Bakar. The verification of the model simulation results for the actual environmental conditions was performed by comparing the positions and quantities of eroded/accumulated material along the shore with the terrain image processing in the form of point clouds. The total volumes of the eroded and accumulated gravel sediment based on image processing are in agreement with the model values.",
keywords = "gravel beach, morphodynamics, numerical model",
author = "Goran Lon{\v c}ar and Dalibor Carevi{\'c} and Suzana Ili{\'c} and Nino Krvavica and Filip Kalini{\'c}",
year = "2020",
month = sep,
day = "30",
language = "Croatian",
volume = "28",
pages = "205--216",
journal = "Hrvatske Vode",
issn = "1330-1144",
publisher = "Hrvatske Vode",
number = "113",

}

RIS

TY - JOUR

T1 - MORFODINAMIKA ŠLJUNČANOG ŽALA PLOČE U UVJETIMA JAKOG JUGA

AU - Lončar, Goran

AU - Carević, Dalibor

AU - Ilić, Suzana

AU - Krvavica, Nino

AU - Kalinić, Filip

PY - 2020/9/30

Y1 - 2020/9/30

N2 - An analysis of the morphodynamics of the artificially filled gravel beach Ploče in Rijeka was conducted. The numerical simulations of wave deformations and gravel sediment transport were initially performed for hypothetical wave events with event directions SSE (157.50), S (1800), SSW (202.50) and SW (225°), a variation of significant wave heights (HS = 1.0 m, 1.5 m and 2.0 m) and corresponding peak wave periods. The parameterization of the numerical model is based on the results of the empirical pattern of the along-the-coast component of gravel sediment transport and the results of a laboratory investigation of the transverse component of gravel sediment transport. This was followed by a numerical simulation of the morphodynamics for one intense sirocco event (March 6, 2020), using the actual wave conditions recorded at the wave station located in immediate proximity of the beach Ploče and the sea level dynamics recorded at the mareographic station Bakar. The verification of the model simulation results for the actual environmental conditions was performed by comparing the positions and quantities of eroded/accumulated material along the shore with the terrain image processing in the form of point clouds. The total volumes of the eroded and accumulated gravel sediment based on image processing are in agreement with the model values.

AB - An analysis of the morphodynamics of the artificially filled gravel beach Ploče in Rijeka was conducted. The numerical simulations of wave deformations and gravel sediment transport were initially performed for hypothetical wave events with event directions SSE (157.50), S (1800), SSW (202.50) and SW (225°), a variation of significant wave heights (HS = 1.0 m, 1.5 m and 2.0 m) and corresponding peak wave periods. The parameterization of the numerical model is based on the results of the empirical pattern of the along-the-coast component of gravel sediment transport and the results of a laboratory investigation of the transverse component of gravel sediment transport. This was followed by a numerical simulation of the morphodynamics for one intense sirocco event (March 6, 2020), using the actual wave conditions recorded at the wave station located in immediate proximity of the beach Ploče and the sea level dynamics recorded at the mareographic station Bakar. The verification of the model simulation results for the actual environmental conditions was performed by comparing the positions and quantities of eroded/accumulated material along the shore with the terrain image processing in the form of point clouds. The total volumes of the eroded and accumulated gravel sediment based on image processing are in agreement with the model values.

KW - gravel beach

KW - morphodynamics

KW - numerical model

M3 - Journal article

AN - SCOPUS:85126463886

VL - 28

SP - 205

EP - 216

JO - Hrvatske Vode

JF - Hrvatske Vode

SN - 1330-1144

IS - 113

ER -