Articles | Volume 14, issue 1
https://doi.org/10.5194/os-14-41-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/os-14-41-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Note on the directional properties of meter-scale gravity waves
Charles Peureux
CORRESPONDING AUTHOR
Laboratoire d'Océanographie Physique et Spatiale, Univ. Brest, CNRS, Ifremer, IRD, 29200 Plouzané, France
Alvise Benetazzo
Institute of Marine Sciences, Italian National Research Council, Venice, Italy
Fabrice Ardhuin
Laboratoire d'Océanographie Physique et Spatiale, Univ. Brest, CNRS, Ifremer, IRD, 29200 Plouzané, France
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Ocean Sci., 20, 639–660, https://doi.org/10.5194/os-20-639-2024, https://doi.org/10.5194/os-20-639-2024, 2024
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We investigated the behaviour of air bubble plumes in the upper ocean in various stormy conditions. We conducted a field experiment in the North Adriatic Sea using high-resolution sonar. We found that bubble penetration depths respond rapidly to wind and wave forcings and can be triggered by the cooling of the water masses. We also found a strong connection between bubble depths and theoretical CO2 gas transfer. Our findings have implications for air–sea interaction studies.
Stefania A. Ciliberti, Enrique Alvarez Fanjul, Jay Pearlman, Kirsten Wilmer-Becker, Pierre Bahurel, Fabrice Ardhuin, Alain Arnaud, Mike Bell, Segolene Berthou, Laurent Bertino, Arthur Capet, Eric Chassignet, Stefano Ciavatta, Mauro Cirano, Emanuela Clementi, Gianpiero Cossarini, Gianpaolo Coro, Stuart Corney, Fraser Davidson, Marie Drevillon, Yann Drillet, Renaud Dussurget, Ghada El Serafy, Katja Fennel, Marcos Garcia Sotillo, Patrick Heimbach, Fabrice Hernandez, Patrick Hogan, Ibrahim Hoteit, Sudheer Joseph, Simon Josey, Pierre-Yves Le Traon, Simone Libralato, Marco Mancini, Pascal Matte, Angelique Melet, Yasumasa Miyazawa, Andrew M. Moore, Antonio Novellino, Andrew Porter, Heather Regan, Laia Romero, Andreas Schiller, John Siddorn, Joanna Staneva, Cecile Thomas-Courcoux, Marina Tonani, Jose Maria Garcia-Valdecasas, Jennifer Veitch, Karina von Schuckmann, Liying Wan, John Wilkin, and Romane Zufic
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Ocean Sci., 18, 1665–1689, https://doi.org/10.5194/os-18-1665-2022, https://doi.org/10.5194/os-18-1665-2022, 2022
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Louis Marié, Fabrice Collard, Frédéric Nouguier, Lucia Pineau-Guillou, Danièle Hauser, François Boy, Stéphane Méric, Peter Sutherland, Charles Peureux, Goulven Monnier, Bertrand Chapron, Adrien Martin, Pierre Dubois, Craig Donlon, Tania Casal, and Fabrice Ardhuin
Ocean Sci., 16, 1399–1429, https://doi.org/10.5194/os-16-1399-2020, https://doi.org/10.5194/os-16-1399-2020, 2020
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Xavier Couvelard, Florian Lemarié, Guillaume Samson, Jean-Luc Redelsperger, Fabrice Ardhuin, Rachid Benshila, and Gurvan Madec
Geosci. Model Dev., 13, 3067–3090, https://doi.org/10.5194/gmd-13-3067-2020, https://doi.org/10.5194/gmd-13-3067-2020, 2020
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Guillaume Boutin, Camille Lique, Fabrice Ardhuin, Clément Rousset, Claude Talandier, Mickael Accensi, and Fanny Girard-Ardhuin
The Cryosphere, 14, 709–735, https://doi.org/10.5194/tc-14-709-2020, https://doi.org/10.5194/tc-14-709-2020, 2020
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We investigate the interactions of surface ocean waves with sea ice taking place at the interface between the compact sea ice cover and the open ocean. We use a newly developed coupling framework between a wave and an ocean–sea ice numerical model. Our results show how the push on sea ice exerted by waves changes the amount and the location of sea ice melting, with a strong impact on the ocean surface properties close to the ice edge.
Thomas Holding, Ian G. Ashton, Jamie D. Shutler, Peter E. Land, Philip D. Nightingale, Andrew P. Rees, Ian Brown, Jean-Francois Piolle, Annette Kock, Hermann W. Bange, David K. Woolf, Lonneke Goddijn-Murphy, Ryan Pereira, Frederic Paul, Fanny Girard-Ardhuin, Bertrand Chapron, Gregor Rehder, Fabrice Ardhuin, and Craig J. Donlon
Ocean Sci., 15, 1707–1728, https://doi.org/10.5194/os-15-1707-2019, https://doi.org/10.5194/os-15-1707-2019, 2019
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FluxEngine is an open-source software toolbox designed to allow for the easy and accurate calculation of air–sea gas fluxes. This article describes new functionality and capabilities, which include the ability to calculate fluxes for nitrous oxide and methane, optimisation for running FluxEngine on a stand-alone desktop computer, and extensive new features to support the in situ measurement community. Four research case studies are used to demonstrate these new features.
Alvise Benetazzo, Luigi Cavaleri, Hongyu Ma, Shumin Jiang, Filippo Bergamasco, Wenzheng Jiang, Sheng Chen, and Fangli Qiao
Ocean Sci., 15, 725–743, https://doi.org/10.5194/os-15-725-2019, https://doi.org/10.5194/os-15-725-2019, 2019
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Pedro Veras Guimarães, Fabrice Ardhuin, Peter Sutherland, Mickael Accensi, Michel Hamon, Yves Pérignon, Jim Thomson, Alvise Benetazzo, and Pierre Ferrant
Ocean Sci., 14, 1449–1460, https://doi.org/10.5194/os-14-1449-2018, https://doi.org/10.5194/os-14-1449-2018, 2018
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Fabrice Ardhuin, Yevgueny Aksenov, Alvise Benetazzo, Laurent Bertino, Peter Brandt, Eric Caubet, Bertrand Chapron, Fabrice Collard, Sophie Cravatte, Jean-Marc Delouis, Frederic Dias, Gérald Dibarboure, Lucile Gaultier, Johnny Johannessen, Anton Korosov, Georgy Manucharyan, Dimitris Menemenlis, Melisa Menendez, Goulven Monnier, Alexis Mouche, Frédéric Nouguier, George Nurser, Pierre Rampal, Ad Reniers, Ernesto Rodriguez, Justin Stopa, Céline Tison, Clément Ubelmann, Erik van Sebille, and Jiping Xie
Ocean Sci., 14, 337–354, https://doi.org/10.5194/os-14-337-2018, https://doi.org/10.5194/os-14-337-2018, 2018
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Aurore Voldoire, Bertrand Decharme, Joris Pianezze, Cindy Lebeaupin Brossier, Florence Sevault, Léo Seyfried, Valérie Garnier, Soline Bielli, Sophie Valcke, Antoinette Alias, Mickael Accensi, Fabrice Ardhuin, Marie-Noëlle Bouin, Véronique Ducrocq, Stéphanie Faroux, Hervé Giordani, Fabien Léger, Patrick Marsaleix, Romain Rainaud, Jean-Luc Redelsperger, Evelyne Richard, and Sébastien Riette
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Francesco Marcello Falcieri, Lakshmi Kantha, Alvise Benetazzo, Andrea Bergamasco, Davide Bonaldo, Francesco Barbariol, Vlado Malačič, Mauro Sclavo, and Sandro Carniel
Ocean Sci., 12, 433–449, https://doi.org/10.5194/os-12-433-2016, https://doi.org/10.5194/os-12-433-2016, 2016
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Between January 30th and February 4th we collected the first turbulence observations in the Gulf of Trieste under different wind forcing and water column structure. The vertical profiles of the turbulence kinetic energy dissipation rates showed that the presence near the sea floor of different water masses, inflowing from the open sea, can prevent the complete mixing of the water column. This dumping effect is enhanced when these masses present higher suspended sediment concentrations.
Francesco Barbariol, Francesco Marcello Falcieri, Carlotta Scotton, Alvise Benetazzo, Sandro Carniel, and Mauro Sclavo
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The analysis presented in the paper aims at extending the classification capabilities of Self-Organizing Maps (SOM) within the context of ocean waves. Indeed, the intrinsic SOM difficulty in representing extremes of the wave climate is discussed and alternative strategies are proposed in order to represent the whole wave climate at a given location. Among them, a two-step SOM together with a double-side map provides the best results.
V. E. Brando, F. Braga, L. Zaggia, C. Giardino, M. Bresciani, E. Matta, D. Bellafiore, C. Ferrarin, F. Maicu, A. Benetazzo, D. Bonaldo, F. M. Falcieri, A. Coluccelli, A. Russo, and S. Carniel
Ocean Sci., 11, 909–920, https://doi.org/10.5194/os-11-909-2015, https://doi.org/10.5194/os-11-909-2015, 2015
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Sea surface temperature and turbidity, derived from satellite imagery, were used to characterize river plumes in the northern Adriatic Sea during a significant flood event in November 2014. Circulation patterns and sea surface salinity, from an operational coupled ocean-wave model, supported the interpretation of the plumes' interaction with the receiving waters and among them.
Cited articles
Alves, J. H. G. and Banner, M. L.: Performance of a saturation-based
dissipation rate source term in modeling the fetch-limited evolution of wind
waves, J. Phys. Oceanogr., 33,
1274–1298,
https://doi.org/10.1175/1520-0485(2003)033<1274:poasds>2.0.co;2,
2003. a
Ardhuin, F., Marié, L., Rascle, N., Forget, P., and Roland, A.:
Observation
and estimation of Lagrangian, Stokes and Eulerian currents induced by wind
and waves at the sea surface, J. Phys. Oceanogr., 39,
2820–2838,
https://doi.org/10.1175/2009jpo4169.1,
2009. a, b
Aubourg, Q. and Mordant, N.: Nonlocal resonances in weak turbulence of
gravity-capillary waves, Phys. Rev. Lett., 114,
https://doi.org/10.1103/PhysRevLett.114.144501, 2015. a
Banner, M. L. and Young, I. R.: Modeling spectral dissipation in the
evolution
of wind waves. Part I: assessment of existing model performance, J. Phys. Oceanogr., 24, 1550–1570,
https://doi.org/10.1175/1520-0485(1994)024<1550:msdite>2.0.co;2,
1994. a
Benetazzo, A., Barbariol, F., Bergamasco, F., Torsello, A., Carniel, S., and
Sclavo, M.: Observation of extreme sea waves in a space-time ensemble,
J. Phys. Oceanogr., 45, 2261–2275,
https://doi.org/10.1175/JPO-D-15-0017.1, 2015. a, b, c
Breivik, Ø., Janssen, P. A. E. M., and Bidlot, J.-R.: Approximate Stokes
Drift Profiles in Deep Water, J. Phys. Oceanogr., 44, 2433–2445,
https://doi.org/10.1175/jpo-d-14-0020.1,
2014. a, b
Bréon, F. M. and Henriot, N.: Spaceborne observations of ocean glint
reflectance and modeling of wave slope distributions, J. Geophys. Res.,
111, C06005,
https://doi.org/10.1029/2005jc003343,
2006. a
Duennebier, F. K., Lukas, R., Nosal, E.-M., Aucan, J., and Weller, R. A.:
Wind,
Waves, and Acoustic Background Levels at Station ALOHA, J. Geophys. Res., 117, C03017, https://doi.org/10.1029/2011JC007267, 2012. a, b
Dysthe, K. B., Trulsen, K., Krogstad, H. E., and Socquet-Juglard, H.:
Evolution of a narrow-band spectrum of random surface gravity waves, J. Fluid
Mech., 478, 1–10, https://doi.org/10.1017/s0022112002002616, 2003. a
Ewans, K. C.: Observations of the Directional Spectrum of Fetch-Limited
Waves,
J. Phys. Oceanogr., 28, 495–512,
https://doi.org/10.1175/1520-0485(1998)028<0495:ootdso>2.0.co;2
1998. a, b
Farrell, W. E. and Munk, W.: Booms and busts in the deep, J. Phys.
Oceanogr., 40, 2159–2169, 2010. a
Gagnaire-Renou, E., Benoit, M., and Forget, P.: Ocean wave spectrum
properties
as derived from quasi-exact computations of nonlinear wave-wave interactions,
J. Geophys. Res., 115, C12058,
https://doi.org/10.1029/2009JC005665,
2010. a
Graber, H. C., Terray, E. A., Donelan, M. A., Drennan, W. M., Leer, J. C. V.
and Peters, D. B. : ASIS–A New Air-Sea Interaction Spar Buoy: Design and
Performance at Sea,
J. Atmos. Ocean. Tech., 17, 708–720,
https://doi.org/10.1175/1520-0426(2000)017<0708:AANASI>2.0.CO;2,
2000. a
Hasselmann, K.: On the non-linear energy transfer in a gravity wave spectrum,
part 1: general theory, J. Fluid Mech., 12, 481–501,
https://doi.org/10.1017/s0022112062000373,
1962. a
Hasselmann, K.: Feynman diagrams and interaction rules of wave-wave
scattering
processes, Rev. Geophys., 4, 1–32,
https://doi.org/10.1029/rg004i001p00001,
1966.
Hwang, P. H., Wang, D. W., Walsh, E. J., Krabill, W. B., and Swift, R. N.:
Airborne measurement of the wavenumber spectra of ocean surface waves. Part
II: directional distribution, J. Phys. Oceanogr., 30,
2768–2787,
https://doi.org/10.1175/1520-0485(2001)031<2768:AMOTWS>2.0.CO;2,
2000. a
Janssen, P. A. E. M.: On some consequences of the canonical transformation in
the Hamiltonian theory of water waves, J. Fluid Mech., 637,
1–44,
https://doi.org/10.1017/s0022112009008131,
2009. a
Kenyon, K. E.: Stokes drift for random gravity waves, J. Geophys.
Res., 74, 6991–6994,
https://doi.org/10.1029/jc074i028p06991,
1969. a
Krogstad, H. E. and Trulsen, K.: Interpretations and observations of ocean
wave
spectra, Ocean Dynam., 62, 973–991,
https://doi.org/10.1007/s10236-010-0293-3,
2010. a
Long, C. E. and Resio, D. T.: Wind wave spectral observations in Currituck
Sound, North Carolina, J. Geophys. Res., 112, C05001,
https://doi.org/10.1029/2006JC003835, 2007. a
Longuet-Higgins, M. S.: A theory of the origin of microseisms, Phil. Trans.
Roy. Soc. London A, 243, 1–35,
https://doi.org/10.1098/rsta.1950.0012,
1950. a
Munk, W.: An Inconvenient Sea Truth: Spread, Steepness, and Skewness of
Surface Slopes, Annu. Rev. Mar. Sci., 1, 377–415,
https://doi.org/10.1146/annurev.marine.010908.163940, 2009. a, b
Newville, M., Stensitzki, T., Allen, D. B., and Ingargiola, A.: LMFIT:
Non-Linear Least-Square Minimization and Curve-Fitting for
Python, https://doi.org/10.5281/zenodo.11813, 2014. a
Plant, W. J.: A relationship between wind stress and wave slope, J.
Geophys. Res., 87, 1961–1967,https://doi.org/10.1029/jc087ic03p01961, 1982. a
Romero, L. and Melville, K. W.: Airborne Observations of Fetch-Limited Waves
in
the Gulf of Tehuantepec, J. Phys. Oceanogr., 40, 441–465,
https://doi.org/10.1175/2009jpo4127.1,
2010. a
Senet, C. M., Seemann, J., and Zeimer, F.: The near-surface current velocity
determined from image sequences of the sea surface, IEEE T.
Geosci. Remote, 39, 492–505,
https://doi.org/10.1109/36.911108,
2001. a, b
Stewart, R. H. and Joy, J. W.: HF radio measurements of surface currents,
Deep-Sea Res., 21, 1039–1049,
https://doi.org/10.1016/0011-7471(74)90066-7,
1974. a
Toffoli, A., Onorato, M., Bitner-Gregersen, E. M., and Monbaliu, J.:
Development of a bimodal structure in ocean wave spectra, J. Geophys. Res.,
115, C03006,
https://doi.org/10.1029/2009JC005495,
2010. a
Wang, D. W. and Hwang, P. A.: Evolution of the Bimodal Directional
Distribution
of Ocean Waves, J. Phys. Oceanogr., 31, 1200–1221,
https://doi.org/10.1175/1520-0485(2001)031<1200:eotbdd>2.0.co;2,
2001. a, b, c
Welch, P. D.: The use of fast Fourier transform for the estimation of power
spectra: a method based on time averaging over short, modified periodograms,
IEEE T. Acoust. Speech, 15, 70–73,
https://doi.org/10.1109/TAU.1967.1161901,
1967.
a
Wilson, D. K., Frisk, G. V., Lindstrom, T. E., and Sellers, C. J.:
Measurement
and prediction of ultralow frequency ocean ambient noise off the eastern
U.S. coast, J. Acoust. Soc. Am., 113, 3117–3133,
https://doi.org/10.1121/1.1568941,
2003. a
Wyatt, L. R.: Shortwave Direction and Spreading Measured with HF Radar, J.
Atmos. Ocean. Tech., 29, 286–299, https://doi.org/10.1175/jtech-d-11-00096.1,
2012. a
Young, I. R., Verhagen, L. A., and Banner, M. L.: A note on the bimodal
directional spreading of fetch-limited wind waves, J. Geophys.
Res., 100, 773–778,
https://doi.org/10.1029/94jc02218,
1995. a
Yueh, S. H., Tang, W., Fore, A. G., Neumann, G., Hayashi, A., Freedman, A.,
Chaubell, J., and Lagerloef, G. S. E.: L-Band Passive and Active Microwave
Geophysical Model Functions of Ocean Surface Winds and Applications to
Aquarius Retrieval, IEEE T. Geosci. Remote, 51,
4619–4632,
https://doi.org/10.1109/tgrs.2013.2266915,
2013. a
Short summary
Little is known on the short ocean wave (1 to 20 m wave length typically) directional distribution. It has been measured from a platform in the Adriatic Sea using a three-dimensional reconstruction technique, used for the first time for this purpose. In this record, while longer waves propagate along the wind direction, shorter waves have been found to propagate mainly along two oblique directions, more and more separated towards smaller scales.
Little is known on the short ocean wave (1 to 20 m wave length typically) directional...