Analysis of data characterizing tide and current fluxes in coastal basins

Many coastal monitoring programmes have been carried out to investigate in situ hydrodynamic patterns and correlated physical processes, such as sediment transport or spreading of pollutants. The key point is the necessity to transform this growing amount of data provided by marine sensors into...

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Main Authors: E. Armenio, F. De Serio, M. Mossa
Format: Article
Language:English
Published: Copernicus Publications 2017-07-01
Series:Hydrology and Earth System Sciences
Online Access:https://www.hydrol-earth-syst-sci.net/21/3441/2017/hess-21-3441-2017.pdf
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spelling doaj-dc9f65194e2149dd8efebb0c8eb964202020-11-24T23:30:21ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79382017-07-01213441345410.5194/hess-21-3441-2017Analysis of data characterizing tide and current fluxes in coastal basinsE. Armenio0F. De Serio1M. Mossa2Department of Civil, Environmental, Land, Building Engineering and Chemistry, Polytechnic University of Bari, Via Orabona 4, 70125 Bari, ItalyDepartment of Civil, Environmental, Land, Building Engineering and Chemistry, Polytechnic University of Bari, Via Orabona 4, 70125 Bari, ItalyDepartment of Civil, Environmental, Land, Building Engineering and Chemistry, Polytechnic University of Bari, Via Orabona 4, 70125 Bari, ItalyMany coastal monitoring programmes have been carried out to investigate in situ hydrodynamic patterns and correlated physical processes, such as sediment transport or spreading of pollutants. The key point is the necessity to transform this growing amount of data provided by marine sensors into information for users. The present paper aims to outline that it is possible to recognize the recurring and typical hydrodynamic processes of a coastal basin, by conveniently processing some selected marine field data. The illustrated framework is made up of two steps. Firstly, a sequence of analysis with classic methods characterized by low computational cost was executed in both time and frequency domains on detailed field measurements of waves, tides, and currents. After this, some indicators of the hydrodynamic state of the basin were identified and evaluated. Namely, the assessment of the net flow through a connecting channel, the time delay of current peaks between upper and bottom layers, the ratio of peak ebb and peak flood currents and the tidal asymmetry factor exemplify results on the vertical structure of the flow, on the correlation between currents and tide and flood/ebb dominance. To demonstrate how this simple and generic framework could be applied, a case study is presented, referring to Mar Piccolo, a shallow water basin located in the inner part of the Ionian Sea (southern Italy).https://www.hydrol-earth-syst-sci.net/21/3441/2017/hess-21-3441-2017.pdf
collection DOAJ
language English
format Article
sources DOAJ
author E. Armenio
F. De Serio
M. Mossa
spellingShingle E. Armenio
F. De Serio
M. Mossa
Analysis of data characterizing tide and current fluxes in coastal basins
Hydrology and Earth System Sciences
author_facet E. Armenio
F. De Serio
M. Mossa
author_sort E. Armenio
title Analysis of data characterizing tide and current fluxes in coastal basins
title_short Analysis of data characterizing tide and current fluxes in coastal basins
title_full Analysis of data characterizing tide and current fluxes in coastal basins
title_fullStr Analysis of data characterizing tide and current fluxes in coastal basins
title_full_unstemmed Analysis of data characterizing tide and current fluxes in coastal basins
title_sort analysis of data characterizing tide and current fluxes in coastal basins
publisher Copernicus Publications
series Hydrology and Earth System Sciences
issn 1027-5606
1607-7938
publishDate 2017-07-01
description Many coastal monitoring programmes have been carried out to investigate in situ hydrodynamic patterns and correlated physical processes, such as sediment transport or spreading of pollutants. The key point is the necessity to transform this growing amount of data provided by marine sensors into information for users. The present paper aims to outline that it is possible to recognize the recurring and typical hydrodynamic processes of a coastal basin, by conveniently processing some selected marine field data. The illustrated framework is made up of two steps. Firstly, a sequence of analysis with classic methods characterized by low computational cost was executed in both time and frequency domains on detailed field measurements of waves, tides, and currents. After this, some indicators of the hydrodynamic state of the basin were identified and evaluated. Namely, the assessment of the net flow through a connecting channel, the time delay of current peaks between upper and bottom layers, the ratio of peak ebb and peak flood currents and the tidal asymmetry factor exemplify results on the vertical structure of the flow, on the correlation between currents and tide and flood/ebb dominance. To demonstrate how this simple and generic framework could be applied, a case study is presented, referring to Mar Piccolo, a shallow water basin located in the inner part of the Ionian Sea (southern Italy).
url https://www.hydrol-earth-syst-sci.net/21/3441/2017/hess-21-3441-2017.pdf
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