Geomorfološke promjene minijaturnog žala na kršu

Lancaster Environment Centre

Keywords

coastal spring, karst, miniature beach, Rijeka Bay, SfM photogrammetry, torrent

Research output: Contribution to Journal/Magazine › Journal article › peer-review

Published

Standard

Geomorfološke promjene minijaturnog žala na kršu. / Ružić, Igor; Benac, Čedomir; Ilić, Suzana et al.
In: Hrvatske Vode, Vol. 26, No. 103, 2018, p. 27-34.

Research output: Contribution to Journal/Magazine › Journal article › peer-review

Harvard

Ružić, I, Benac, Č, Ilić, S, Krvavica, N & Rubinić, J 2018, 'Geomorfološke promjene minijaturnog žala na kršu', Hrvatske Vode, vol. 26, no. 103, pp. 27-34.

APA

Ružić, I., Benac, Č., Ilić, S., Krvavica, N., & Rubinić, J. (2018). Geomorfološke promjene minijaturnog žala na kršu. Hrvatske Vode, 26(103), 27-34.

Vancouver

Ružić I, Benac Č, Ilić S, Krvavica N, Rubinić J. Geomorfološke promjene minijaturnog žala na kršu. Hrvatske Vode. 2018;26(103):27-34.

Author

Ružić, Igor ; Benac, Čedomir ; Ilić, Suzana et al. / Geomorfološke promjene minijaturnog žala na kršu. In: Hrvatske Vode. 2018 ; Vol. 26, No. 103. pp. 27-34.

Bibtex

@article{6b1b3966a43942018405c9b233f706a7,

title = "Geomorfolo{\v s}ke promjene minijaturnog {\v z}ala na kr{\v s}u",

abstract = "A 70 m long beach is located in the Uboka cove on the western cost of the Rijeka bay. From 2 January to 12 April 2012, 11 measurements of the beach topography were performed by applying the-from-Motion (SfM) photogrammetry which generated 3-D point clouds of high precision and resolution. The applied methodology facilitated an inexpensive and fast survey of geomorphological changes. Significant changes in the beach body were recorded, caused by the interaction of wave action and surface water and groundwater discharges and leading to the beach erosion through a formation of channels within its body. After water discharges the beach quickly recovered and resumed its original form through the wind wave action. The cahnnel position was quickly replaced by the beach berm, followed by a stable, high berm. In the case of channelled torrential watercourses on the beach, a significant increase in the velocities occurs in comparison to the natural runoff, as described in this paper, and leading up to potential permanent beach erosion.",

keywords = "coastal spring, karst, miniature beach, Rijeka Bay, SfM photogrammetry, torrent",

author = "Igor Ru{\v z}i{\'c} and {\v C}edomir Benac and Suzana Ili{\'c} and Nino Krvavica and Josip Rubini{\'c}",

year = "2018",

language = "Croatian",

volume = "26",

pages = "27--34",

journal = "Hrvatske Vode",

issn = "1330-1144",

publisher = "Hrvatske Vode",

number = "103",

}

RIS

TY - JOUR

T1 - Geomorfološke promjene minijaturnog žala na kršu

AU - Ružić, Igor

AU - Benac, Čedomir

AU - Ilić, Suzana

AU - Krvavica, Nino

AU - Rubinić, Josip

PY - 2018

Y1 - 2018

N2 - A 70 m long beach is located in the Uboka cove on the western cost of the Rijeka bay. From 2 January to 12 April 2012, 11 measurements of the beach topography were performed by applying the-from-Motion (SfM) photogrammetry which generated 3-D point clouds of high precision and resolution. The applied methodology facilitated an inexpensive and fast survey of geomorphological changes. Significant changes in the beach body were recorded, caused by the interaction of wave action and surface water and groundwater discharges and leading to the beach erosion through a formation of channels within its body. After water discharges the beach quickly recovered and resumed its original form through the wind wave action. The cahnnel position was quickly replaced by the beach berm, followed by a stable, high berm. In the case of channelled torrential watercourses on the beach, a significant increase in the velocities occurs in comparison to the natural runoff, as described in this paper, and leading up to potential permanent beach erosion.

AB - A 70 m long beach is located in the Uboka cove on the western cost of the Rijeka bay. From 2 January to 12 April 2012, 11 measurements of the beach topography were performed by applying the-from-Motion (SfM) photogrammetry which generated 3-D point clouds of high precision and resolution. The applied methodology facilitated an inexpensive and fast survey of geomorphological changes. Significant changes in the beach body were recorded, caused by the interaction of wave action and surface water and groundwater discharges and leading to the beach erosion through a formation of channels within its body. After water discharges the beach quickly recovered and resumed its original form through the wind wave action. The cahnnel position was quickly replaced by the beach berm, followed by a stable, high berm. In the case of channelled torrential watercourses on the beach, a significant increase in the velocities occurs in comparison to the natural runoff, as described in this paper, and leading up to potential permanent beach erosion.

KW - coastal spring

KW - karst

KW - miniature beach

KW - Rijeka Bay

KW - SfM photogrammetry

KW - torrent

M3 - Journal article

AN - SCOPUS:85074680937

VL - 26

SP - 27

EP - 34

JO - Hrvatske Vode

JF - Hrvatske Vode

SN - 1330-1144

IS - 103

ER -

Research

Keywords