Abstract
The Aegean Sea is an intriguing sub-basin of the Mediterranean, due to (a) its capability to produce large amounts of very dense water, temporarily becoming the major producer of Eastern Mediterranean Bottom Water (recorded during the EMT period) and (b) due to its direct connection with the Black Sea that supplies the Aegean Sea with light, low-salinity waters which contribute buoyancy to the surface layers, and potentially control local convection processes. Thus, a similarity with the North Atlantic rises, in the sense of gradually increased stratification due to the addition of low-salinity surface waters, in an area capable to produce very dense waters, and thus possibly turning the North Aegean to a natural laboratory for studying such intriguing processes. The buoyancy exchanges with the atmosphere over the Aegean basin are partially controlled by the buoyancy gain and the subsequent formation of a shallow surface layer of the modified Black Sea waters. In this chapter, we examine the characteristics and variability of the heat and freshwater and the overall buoyancy fluxes with the exchanges with the atmosphere, focusing on the potential role of the interaction with the Black Sea.
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References
Zodiatis G (1994) Advection of Black Sea water in the North Aegean Sea. Glob Atmos Ocean Syst 2:41–60
Zervakis V, Georgopoulos D (2002) Hydrology and circulation in the North Aegean (eastern Mediterranean) throughout 1997 and 1998. https://doi.org/10.12681/mms.254
Beşiktepe ŞT (2003) Density currents in the two-layer flow: an example of Dardanelles outflow. Oceanol Acta 26:243–253. https://doi.org/10.1016/S0399-1784(03)00015-X
Olson DB, Kourafalou VH, Johns WE et al (2007) Aegean surface circulation from a satellite-tracked drifter array. J Phys Oceanogr 37:1898–1917. https://doi.org/10.1175/JPO3028.1
Skliris N, Mantziafou A, Sofianos S, Gkanasos A (2010) Satellite-derived variability of the Aegean Sea ecohydrodynamics. Cont Shelf Res 30:403–418. https://doi.org/10.1016/j.csr.2009.12.012
Androulidakis YS, Krestenitis YN, Psarra S (2017) Coastal upwelling over the North Aegean Sea: observations and simulations. Cont Shelf Res 149:32–51. https://doi.org/10.1016/j.csr.2016.12.002
Mamoutos I, Zervakis V, Tragou E et al (2017) The role of wind-forced coastal upwelling on the thermohaline functioning of the North Aegean Sea. Cont Shelf Res 149:52–68. https://doi.org/10.1016/j.csr.2017.05.009
Poulos SE, Drakopoulos PG, Collins MB (1997) Seasonal variability in sea surface oceanographic conditions in the Aegean Sea (eastern Mediterranean): an overview. J Mar Syst 13:225–244
Bakun A, Agostini VN (2001) Seasonal patterns of wind-induced upwelling/downwelling in the Mediterranean Sea. Sci Mar 65. https://doi.org/10.3989/scimar.2001.65n3243
Papadopoulos A, Varlas G (2020) Weather systems affecting the meteorological conditions over the Aegean Sea. Springer, Berlin, pp 1–25
Anagnostopoulou C, Zanis P, Katragkou E et al (2014) Recent past and future patterns of the Etesian winds based on regional scale climate model simulations. Clim Dyn 42:1819–1836. https://doi.org/10.1007/s00382-013-1936-0
Nielsen JN (1912) Hydrography of the Mediterranean and adjacent waters. In: Schmidt J (ed) Report of the Danish oceanographic expedition, 1908–1910 to the Mediterranean and adjacent waters, vol vol 1. Andr. Fred Høst & Søn, Copenhagen, pp 72–191
Theocharis A, Georgopoulos D, Lascaratos A, Nittis K (1993) Water masses and circulation in the central region of the Eastern Mediterranean: Eastern Ionian, South Aegean and Northwest Levantine, 1986-1987. Deep Res Part II 40:1121–1142. https://doi.org/10.1016/0967-0645(93)90064-T
Malanotte-Rizzoli P, Manca BB, D’Alcalà MR et al (1997) A synthesis of the Ionian Sea hydrography, circulation and water mass pathways during POEM-phase I. Prog Oceanogr 39:153–204. https://doi.org/10.1016/S0079-6611(97)00013-X
Roether W, Klein B, Manca BB et al (2007) Transient eastern Mediterranean deep waters in response to the massive dense-water output of the Aegean Sea in the 1990s. Prog Oceanogr 74:540–571. https://doi.org/10.1016/j.pocean.2007.03.001
Bunker AF, Charnock H, Goldsmith RA (1982) A note on the heat balance of the Mediterranean and Red Seas. J Mar Res 40:73–84
May RW (1983) Climatological flux estimated in the Mediterranean Sea, vol 2: air-sea fluxes. NORDA Rep. 58, Nav. Ocen. Res. Dev. Activ., NSTL Station, Mississipi
Garrett C, Outerbridge R, Thompson K (1993) Interannual variability in Mediterranean heat and buoyancy fluxes. J Clim 6:900–910
Slutz RJ, Lubker SJ, Hiscox JD et al (1985) Comprehensive ocean-atmosphere data set; release 1
Vervatis VD, Sofianos SS, Skliris N et al (2013) Mechanisms controlling the thermohaline circulation pattern variability in the Aegean-Levantine region. A hindcast simulation (1960-2000) with an eddy resolving model. Deep Res Part I Oceanogr Res Pap 74:82–97. https://doi.org/10.1016/j.dsr.2012.12.011
Petalas S, Mamoutos I, Tragou E, Zervakis V (2019) A 30-year hindcast of the interconnected eastern Mediterranean – Black Sea system: a first step towards climate projections for the Aegean Sea. Geophys Res Abstr 21:EGU2019-13821
Haidvogel DB, Arango HG, Hedstrom K et al (2000) Model evaluation experiments in the North Atlantic Basin: simulations in nonlinear terrain-following coordinates. Dyn Atmos Ocean 32:239–281. https://doi.org/10.1016/S0377-0265(00)00049-X
Shchepetkin AF, Mcwilliams JC (1998) Quasi-monotone advection schemes based on explicit locally adaptive dissipation. Mon Weather Rev 126:1541–1580. https://doi.org/10.1175/1520-0493(1998)126<1541:QMASBO>2.0.CO;2
Shchepetkin AF, McWilliams JC (2005) The regional oceanic modeling system (ROMS): a split-explicit, free-surface, topography-following-coordinate oceanic model. Ocean Model 9:347–404. https://doi.org/10.1016/J.OCEMOD.2004.08.002
Pinardi N, Allen I, Demirov E et al (2003) The Mediterranean ocean forecasting system: first phase of implementation (1998–2001). Ann Geophys 21:3–20. https://doi.org/10.5194/angeo-21-3-2003
European Centre for Medium-Range Weather Forecast – ECMWF (2009) ERA-Interim project. In: Res. Data Arch. Natl. Cent. Atmos. Res. Comput. In-formation Syst. Lab. Boulder, Color. https://doi.org/10.5065/D6CR5RD9. Accessed 19 Jan 2018
Donnelly C, Andersson JCM, Arheimer B (2016) Using flow signatures and catchment similarities to evaluate the E-HYPE multi-basin model across Europe. Hydrol Sci J 61:255–273. https://doi.org/10.1080/02626667.2015.1027710
Sevault F, Somot S, Alias A et al (2014) A fully coupled Mediterranean regional climate system model: design and evaluation of the ocean component for the 1980–2012 period. Tellus A Dyn Meteorol Oceanogr 66:23967. https://doi.org/10.3402/tellusa.v66.23967
Acknowledgements
The authors wish to thank Vassilis Zervakis for his valuable comments on the manuscript. The numerical simulations were performed with computational time granted from the Greek Research & Technology Network (GRNET) in the National HPC facility – ARIS – under project ID petalas-EMBS2.
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Tragou, E., Petalas, S., Mamoutos, I. (2022). Air–Sea Interaction: Heat and Fresh-Water Fluxes in the Aegean Sea. In: Anagnostou, C.L., Kostianoy, A.G., Mariolakos, I.D., Panayotidis, P., Soilemezidou, M., Tsaltas, G. (eds) The Aegean Sea Environment. The Handbook of Environmental Chemistry, vol 127. Springer, Cham. https://doi.org/10.1007/698_2021_841
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DOI: https://doi.org/10.1007/698_2021_841
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