Time-Lapse Photography of the Edge-of-Water Line Displacements of a Sandbar as a Proxy of Riverine Morphodynamics

A simple methodology to track the displacements of a sandbar from a fixed video camera, extracting its morphological features and deriving the associated fluvial morphology is presented, using a small reach of the Po River in Italy as a case study. A camera fixed on a bridge pier acquired images eve...

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Main Authors: Michael Nones, Renata Archetti, Massimo Guerrero
Format: Article
Language:English
Published: MDPI AG 2018-05-01
Series:Water
Subjects:
Online Access:http://www.mdpi.com/2073-4441/10/5/617
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spelling doaj-8c9fe5805f574cb3bac88e10e0297e2b2020-11-24T23:07:18ZengMDPI AGWater2073-44412018-05-0110561710.3390/w10050617w10050617Time-Lapse Photography of the Edge-of-Water Line Displacements of a Sandbar as a Proxy of Riverine MorphodynamicsMichael Nones0Renata Archetti1Massimo Guerrero2Interdepartmental Centre for Industrial Research in Building and Construction, University of Bologna, 40126 Bologna, ItalyDepartment of Civil, Chemical, Environmental, and Materials Engineering, University of Bologna, 40126 Bologna, ItalyDepartment of Civil, Chemical, Environmental, and Materials Engineering, University of Bologna, 40126 Bologna, ItalyA simple methodology to track the displacements of a sandbar from a fixed video camera, extracting its morphological features and deriving the associated fluvial morphology is presented, using a small reach of the Po River in Italy as a case study. A camera fixed on a bridge pier acquired images every twelve hours while hourly water levels are derived from a radar hydrometer located upstream of the study area. The quantification of the fluvial bathymetry is achieved by mapping multiple edge-of-water lines of a sandbar before and after high flow conditions in December 2017. Both from video information and 2-D numerical simulations, it is evident that flooding waves can easily remove sediments that accumulated on bars during low flow conditions in this area, redistributing them across the river channel. This video-based methodology—which confirms to be economically attractive if compared to more traditional monitoring systems—proves to be a valuable system to monitor long-term fluvial processes providing detailed indications on how to better plan river management activities.http://www.mdpi.com/2073-4441/10/5/617edge-of-water linesandbarvideo cameraiRIC modelriver morphodynamicsPo Rivertime-lapse photogrammetry
collection DOAJ
language English
format Article
sources DOAJ
author Michael Nones
Renata Archetti
Massimo Guerrero
spellingShingle Michael Nones
Renata Archetti
Massimo Guerrero
Time-Lapse Photography of the Edge-of-Water Line Displacements of a Sandbar as a Proxy of Riverine Morphodynamics
Water
edge-of-water line
sandbar
video camera
iRIC model
river morphodynamics
Po River
time-lapse photogrammetry
author_facet Michael Nones
Renata Archetti
Massimo Guerrero
author_sort Michael Nones
title Time-Lapse Photography of the Edge-of-Water Line Displacements of a Sandbar as a Proxy of Riverine Morphodynamics
title_short Time-Lapse Photography of the Edge-of-Water Line Displacements of a Sandbar as a Proxy of Riverine Morphodynamics
title_full Time-Lapse Photography of the Edge-of-Water Line Displacements of a Sandbar as a Proxy of Riverine Morphodynamics
title_fullStr Time-Lapse Photography of the Edge-of-Water Line Displacements of a Sandbar as a Proxy of Riverine Morphodynamics
title_full_unstemmed Time-Lapse Photography of the Edge-of-Water Line Displacements of a Sandbar as a Proxy of Riverine Morphodynamics
title_sort time-lapse photography of the edge-of-water line displacements of a sandbar as a proxy of riverine morphodynamics
publisher MDPI AG
series Water
issn 2073-4441
publishDate 2018-05-01
description A simple methodology to track the displacements of a sandbar from a fixed video camera, extracting its morphological features and deriving the associated fluvial morphology is presented, using a small reach of the Po River in Italy as a case study. A camera fixed on a bridge pier acquired images every twelve hours while hourly water levels are derived from a radar hydrometer located upstream of the study area. The quantification of the fluvial bathymetry is achieved by mapping multiple edge-of-water lines of a sandbar before and after high flow conditions in December 2017. Both from video information and 2-D numerical simulations, it is evident that flooding waves can easily remove sediments that accumulated on bars during low flow conditions in this area, redistributing them across the river channel. This video-based methodology—which confirms to be economically attractive if compared to more traditional monitoring systems—proves to be a valuable system to monitor long-term fluvial processes providing detailed indications on how to better plan river management activities.
topic edge-of-water line
sandbar
video camera
iRIC model
river morphodynamics
Po River
time-lapse photogrammetry
url http://www.mdpi.com/2073-4441/10/5/617
work_keys_str_mv AT michaelnones timelapsephotographyoftheedgeofwaterlinedisplacementsofasandbarasaproxyofriverinemorphodynamics
AT renataarchetti timelapsephotographyoftheedgeofwaterlinedisplacementsofasandbarasaproxyofriverinemorphodynamics
AT massimoguerrero timelapsephotographyoftheedgeofwaterlinedisplacementsofasandbarasaproxyofriverinemorphodynamics
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