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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2017-07-01
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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 |
work_keys_str_mv |
AT earmenio analysisofdatacharacterizingtideandcurrentfluxesincoastalbasins AT fdeserio analysisofdatacharacterizingtideandcurrentfluxesincoastalbasins AT mmossa analysisofdatacharacterizingtideandcurrentfluxesincoastalbasins |
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