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Volume 12, issue 1
Ocean Sci., 12, 71–86, 2016
https://doi.org/10.5194/os-12-71-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue: Oceanographic processes on the continental shelf: observations...

Ocean Sci., 12, 71–86, 2016
https://doi.org/10.5194/os-12-71-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 15 Jan 2016

Research article | 15 Jan 2016

Modeling the ocean and atmosphere during an extreme bora event in northern Adriatic using one-way and two-way atmosphere–ocean coupling

M. Ličer et al.

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Cited articles

Artegiani, A., Bregant, D., Paschini, E., Pinardi, N., Raicich, F., and Russo, A.: The Adriatic Sea General Circulation I: Air-Sea Interactions and Water Mass Structure, J. Phys. Oceanogr., 27, 1492–1514, https://doi.org/10.1175/1520-0485(1997)027<1492:TASGCP>2.0.CO;2, 1997.
Benetazzo, A., Bergamasco, A., Bonaldo, D., Falcieria, F. M., Sclavo, M., Langone, L., and Carniel, S.: Response of the Adriatic Sea to an intense cold air outbreak: dense water dynamics and wave-induced transport, Prog. Oceanogr., 128, 115–138, https://doi.org/10.1016/j.pocean.2014.08.015, 2014.
Blumberg, A. F. and Mellor, G. L.: A description of a three-dimensional coastal ocean circulation model, in: Three-Dimensional Coastal Ocean Models, edited by: Heaps, N., American Geophysical Union, Washington, DC, USA, 1–16, 1987.
Cosoli, S., Ličer, M., Vodopivec, M., and Malačič, V.: Surface circulation in the Gulf of Trieste (northern Adriatic Sea) from radar, model, and ADCP comparisons, J. Geophys. Res.-Oceans, 118, 6183–6200, https://doi.org/10.1002/2013JC009261, 2013.
Cushman-Roisin, B., Gačić, M., Poulain, P.-M., and Artegiani, A.: Physical Oceanography of the Adriatic Sea. Past, Present and Future, Springer, London, UK, 47–48, 2001.
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We compare the northern Adriatic response to an extreme bora event, as simulated by one-way and two-way (i.e. with ocean feedback to the atmosphere) atmosphere-ocean coupling. We show that two-way coupling yields significantly better estimates of heat fluxes, most notably sensible heat flux, across the air-sea interface. When compared to observations in the northern Adriatic, two-way coupled system consequently leads to a better representation of ocean temperatures throughout the event.
We compare the northern Adriatic response to an extreme bora event, as simulated by one-way and...
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