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Turbulent behaviour within a coastal boundary layer, observations and modelling at the Isola del Giglio

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Abstract

The hydrodynamics of coastal areas is characterized by the interaction among phenomena occurring at different spatial and temporal scales, such as the interaction of a large-scale ocean current with the local bathymetry and coastline, and local forcing conditions. In order to take into account all relevant phenomena, the study of the hydrodynamics of coastal zones requires a high-spatial and temporal resolution for both observations and simulation of local currents. This resolution can be obtained by using X-band radar, which allows simultaneous measurement of waves and currents in a range of 1–3 miles from the coastline, as well as high-resolution numerical models implemented in the area and configured through multiple nesting techniques in order to reach resolutions comparable to such coastal observations. Such an integrated monitoring system was implemented at the Isola del Giglio in 2012, after the accident of the Costa Concordia ship. Results can be used as a cross-validation of data produced independently by radar observations and numerical models. In addition, results give some important insights on the dynamics of the coastal boundary layer, both for what concerns the attenuation in the profile of the depth-averaged velocities which typically occur in turbulent boundary layers, as well as for the production, detachment and evolution of vorticity produced by the interaction of large-scale ocean currents with the coastline and the subsequent time evolution of such boundary layer. This transition between large-scale regional currents and the coastal boundary layer is often neglected in regional forecasting systems, but it has an important role in the ocean turbulence processes.

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References

  • Artale V, Astraldi M, Buffoni G, Gasparini GP (1994) Seasonal variability of gyre scale circulation in the northern Tyrrhenian Sea. J Geophys Res Oceans 99(C7):14127–14137

    Article  Google Scholar 

  • Bassin CJ, Washburn L, Brzezinski M, McPhee- Shaw E (2005) Sub- mesoscale coastal eddies observed by high frequency radar: a new mechanism for delivering nutrients to kelp forests in the Southern California Bight. Geophys Res Lett 32(12):L12604

  • Baey JM, Renouard D, D'hieres GC (1995) Preliminary results about the stability of an intermediate water current. Deep Sea Research Part I: Oceanographic Research Papers 42(11–12):2063–2073

  • Bolaños R, Sørensen JVT, Benetazzo A, Carniel S, Sclavo M (2014) Modelling ocean currents in the northern Adriatic Sea. Cont Shelf Res 87:54–72

  • Capet X, McWilliams JC, Molemaker MJ, Shchepetkin AF (2008) Mesoscale to submesoscale transition in the California Current system. Part I: flow structure, eddy flux, and observational tests. J Phys Oceanogr 38(1):29–43

  • Carniel S, Warner JC, Chiggiato J, Sclavo M (2009) Investigating the impact of surface wave breaking on modeling the trajectories of drifters in the northern Adriatic Sea during a wind-storm event. Ocean Modelling 30(2–3):225–239

  • Chiggiato J, Jarosz E, Book JW, Dykes J, Torrisi L, Poulain P-M, Gerin R, Horstmann J, Beşiktepe S (2012) Dynamics of the circulation in the Sea of Marmara: numerical modeling experiments and observations from the Turkish straits system experiment. Ocean Dynamics 62(1):139–159

  • Chiggiato J, Oddo P (2008) Operational Ocean Models in the Adriatic Sea: a skill assessment. Ocean Science 4(1):61–71

  • Csanady GT (1972a) The coastal boundary layer in Lake Ontario. Part I: the spring regime. J Phys Oceanogr 2(1):41–53

    Article  Google Scholar 

  • Csanady GT (1972b) The coastal boundary layer in Lake Ontario: part II. The summer-fall regime. J Phys Oceanogr 2:168–176

    Article  Google Scholar 

  • Cutroneo L, Ferretti G, Scafidi D, Ardizzone GD, Vagge G, Capello M (2017) Current observations from a looking down vertical V-ADCP: interaction with winds and tide? The case of Giglio Island (Tyrrhenian Sea, Italy). Oceanologia 59(2):139–152

    Article  Google Scholar 

  • Dong C, McWilliams JC (2007a) A numerical study of island wakes in the Southern California Bight. Cont Shelf Res 27(9):1233–1248

    Article  Google Scholar 

  • Dong C, McWilliams JC, Shchepetkin AF (2007b) Island wakes in deep water. J Phys Oceanogr 37(4):962–981

    Article  Google Scholar 

  • Doglioli AM, Griffa A, Magaldi MG (2004) Numerical study of a coastal current on a steep slope in presence of a cape: the case of the Promontorio di Portofino. J Geophys Res Oceans 109(C12):C12033

  • Hayward TL, Mantyla AW (1990) Physical, chemical and biological structure of a coastal eddy near Cape Mendocino. J Mar Res 48(4):825–850

    Article  Google Scholar 

  • Hessner K, Reichert K, Borge JCN, Stevens CL, Smith MJ (2014) High-resolution X-band radar measurements of currents, bathymetry and sea state in highly inhomogeneous coastal areas. Ocean Dynamics 64(7):989–998

  • Huang W, Gill E (2012) Surface current measurement under low sea state using dual polarized X-band nautical radar. IEEE J. Select. Topics Appl. Earth Observat. Remote Sens. 5(6):1868–1873

  • Jones OP, Simons RR, Jones EJW, Harris JM (2006) Influence of seabed slope and Coriolis effects on the development of sandbanks near headlands. J Geophys Res Oceans 111(C3):C03020

  • Katsman CA, Spall MA, Pickart RS (2004) Boundary current eddies and their role in the restratification of the Labrador Sea. J Phys Oceanogr 34(9):1967–1983

    Article  Google Scholar 

  • Ludeno G, Brandini C, Lugni C, Arturi D, Natale A, Soldovieri F, Gozzini B, Serafino F (2014a) Remocean System for the detection of the reflected waves from the Costa Concordia ship wreck. IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing 7(7):3011–3018

  • Ludeno G, Flampouris S, Lugni C, Soldovieri F, Serafino F (2014b) A novel approach based on marine radar data analysis for high resolution bathymetry map generation. IEEE Geosci Remote Sens Lett 11(1):234–238

    Article  Google Scholar 

  • Ludeno G, Reale F, Dentale F, Pugliese Carratelli E, Natale A, Serafino F (2015) Estimating nearshore bathymetry from X-band radar data. Coastal ocean observing systems: advances and syntheses 15:265–280

  • Ludeno G, Nasello C, Raffa F, Ciraolo G, Soldovieri F, Serafino F (2016) A comparison between drifter and X-band wave radar for sea surface current estimation. Remote Sens 8(9):695

    Article  Google Scholar 

  • Magaldi MG, Ozgokmen TM, Griffa A, Chassignet EP, Iskandarani M, Peters H (2008) Turbulent flow regimes behind a coastal cape in a stratified and rotating environment. Ocean Modelling 25(1–2):65–82

  • Nickols KJ, Gaylord B, Largier JL (2012) The coastal boundary layer: predictable current structure decreases alongshore transport and alters scales of dispersal. Mar Ecol Prog Ser 464:17–35

    Article  Google Scholar 

  • Nieto Borge JC, RodrÍguez GR, Hessner K, González PI (2004) Inversion of marine radar images for surface wave analysis. J Atmos Ocean Technol 21(8):1291–1300

    Article  Google Scholar 

  • Papadakis MP, Chassignet EP, Hallberg RW (2003) Numerical simulations of the Mediterranean Sea outflow: impact of the entrainment parameterization in an isopycnic coordinate ocean model. Ocean Model 5(4):325–356

  • Pineda J, Hare JA, Sponaugle S (2007) Larval dispersal and transport in the coastal ocean and consequences for population connectivity. Oceanography 20:22–39

    Article  Google Scholar 

  • Polli S (1955) Variazioni delle costanti armoniche delle maree col livello del mare. Ann Geofis 8(2):202–207

    Google Scholar 

  • Schlichting H (1979) Boundary-layer theory 1–419

  • Senet CM, Seemann J, Ziemer F (2001) The near-surface current velocity determined from image sequences of the sea surface. IEEE Trans Geosci Remote Sens 39:492–505

    Article  Google Scholar 

  • Serafino F, Lugni C, Soldovieri F (2010) A novel strategy for the surface current determination from marine Xband radar data. IEEE Geosci Remote Sens Lett 7:231–235

  • Serafino F, Lugni C, Ludeno G, Arturi D, Uttieri M, Buonocore B, Zambianchi, E, Budillon G, Soldovieri F (2012) REMOCEAN: a flexible X-band radar system for sea-state monitoring and surface current estimation. Geosci Remote Sens Let 9(5):822–826

  • Shchepetkin AF, McWilliams JC (1998) Quasi-monotone advection schemes based on explicit locally adaptive dissipation. Mon Weather Rev 126:1541–1580

    Article  Google Scholar 

  • Shchepetkin AF, McWilliams JC (2005) The Regional Ocean Modeling System: a split-explicit, free-surface, topography following coordinates ocean model. Ocean Model 9:347–404

    Article  Google Scholar 

  • Signell RP, Geyer WR (1991) Transient eddy formation around headlands. J. Geophys. Res. Oceans 96(2):2561–2575

  • Stern ME, Chassignet EP (2000) Mechanism of eddy separation from coastal currents. J Mar Res 58(2):269–295

    Article  Google Scholar 

  • Stern ME, Whitehead JA (1990) Separation of a boundary jet in a rotating fluid. J Fluid Mech 217:41–69

    Article  Google Scholar 

  • St John MA, Pond S (1992) Tidal plume generation around a promontory: effects on nutrient concentrations and primary productivity. Cont Shelf Res 12(2–3):339–354

  • Young IR, Rosenthal W, Ziemer F (1985) A three-dimensional analysis of marine radar images for the determination of ocean wave directionality and surface currents. J Geophys Res 90(1):1049–1059

  • Wolanski E, Imberger J, Heron ML (1984) Island wakes in shallow coastal waters. J Geophys Res 89(6):10553–10569

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Acknowledgements

This study was partly supported by the EU projects MOMAR and SICOMAR (Transnational Maritime Program Italy-France, 2007–2013). The authors thank their friend Matthew Vannini for his help in proofreading of this paper.

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Correspondence to Carlo Brandini.

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Responsible Editor: Ulf Gräwe

This article is part of the Topical Collection on the 18th Joint Numerical Sea Modelling Group Conference, Oslo, Norway, 10–12 May 2016

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Brandini, C., Taddei, S., Doronzo, B. et al. Turbulent behaviour within a coastal boundary layer, observations and modelling at the Isola del Giglio. Ocean Dynamics 67, 1163–1178 (2017). https://doi.org/10.1007/s10236-017-1080-1

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  • DOI: https://doi.org/10.1007/s10236-017-1080-1

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