{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,6,26]],"date-time":"2026-06-26T12:04:09Z","timestamp":1782475449353,"version":"3.54.5"},"reference-count":63,"publisher":"Copernicus GmbH","issue":"5","license":[{"start":{"date-parts":[[2018,9,11]],"date-time":"2018-09-11T00:00:00Z","timestamp":1536624000000},"content-version":"vor","delay-in-days":0,"URL":"https:\/\/creativecommons.org\/licenses\/by\/4.0\/"}],"content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["Ocean Sci."],"abstract":"<jats:p>Abstract. A simulation of the Turkish Straits\nSystem (TSS) using a high-resolution, three-dimensional, unstructured mesh\nocean circulation model with realistic atmospheric forcing for the 2008\u20132013\nperiod is presented. The depth of the pycnocline between the upper and lower\nlayers remains stationary after 6\u00a0years of integration, indicating that\ndespite the limitations of the modelling system, the simulation maintains its\nrealism. The solutions capture important responses to high-frequency\natmospheric events such as the reversal of the upper layer flow in the\nBosphorus due to southerly severe storms, i.e. blocking events, to the extent\nthat such storms are present in the forcing dataset. The annual average\ncirculations show two distinct patterns in the Sea of Marmara. When the wind\nstress maximum is localised in the central basin, the Bosphorus jet flows to\nthe south and turns west after reaching the Bozburun Peninsula. In contrast,\nwhen the wind stress maximum increases and expands in the north\u2013south\ndirection, the jet deviates to the west before reaching the southern coast\nand forms a cyclonic gyre in the central basin. In certain years, the mean\nkinetic energy in the northern Sea of Marmara is found to be comparable to\nthat of the Bosphorus inflow.<\/jats:p>","DOI":"10.5194\/os-14-999-2018","type":"journal-article","created":{"date-parts":[[2018,9,11]],"date-time":"2018-09-11T09:03:17Z","timestamp":1536656597000},"page":"999-1019","source":"Crossref","is-referenced-by-count":32,"title":["Circulation of the Turkish Straits System under interannual atmospheric forcing"],"prefix":"10.5194","volume":"14","author":[{"ORCID":"https:\/\/orcid.org\/0000-0002-1557-7502","authenticated-orcid":false,"given":"Ali","family":"Aydo\u011fdu","sequence":"first","affiliation":[],"role":[{"vocabulary":"crossref","role":"author"}]},{"ORCID":"https:\/\/orcid.org\/0000-0003-4765-0775","authenticated-orcid":false,"given":"Nadia","family":"Pinardi","sequence":"additional","affiliation":[],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"Emin","family":"\u00d6zsoy","sequence":"additional","affiliation":[],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"Gokhan","family":"Danabasoglu","sequence":"additional","affiliation":[],"role":[{"vocabulary":"crossref","role":"author"}]},{"ORCID":"https:\/\/orcid.org\/0000-0002-0646-5760","authenticated-orcid":false,"given":"\u00d6zg\u00fcr","family":"G\u00fcrses","sequence":"additional","affiliation":[],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"Alicia","family":"Karspeck","sequence":"additional","affiliation":[],"role":[{"vocabulary":"crossref","role":"author"}]}],"member":"3145","published-online":{"date-parts":[[2018,9,11]]},"reference":[{"key":"ref1","doi-asserted-by":"crossref","unstructured":"Alpar, B., Do\u011fan, E., Y\u00fcce, H., and Alt\u0131ok, H.: Sea level changes\nalong the Turkish coasts of the Black Sea, the Aegean Sea and the Eastern\nMediterranean, Mediterr. Mar. Sci., 1, 141\u2013156, 2000.\u2002a","DOI":"10.12681\/mms.285"},{"key":"ref2","doi-asserted-by":"crossref","unstructured":"Alt\u0131ok, H., Sur, H.\u00a0\u0130., and Y\u00fcce, H.: Variation of the cold\nintermediate water in the Black Sea exit of the Strait of Istanbul\n(Bosphorus) and its transfer through the strait, Oceanologia, 54, 233\u2013254,\n2012.\u2002a, b","DOI":"10.5697\/oc.54-2.233"},{"key":"ref3","doi-asserted-by":"crossref","unstructured":"Aydogdu, A., Hoar, T. J., Vukicevic, T., Anderson, J. L., Pinardi, N.,\nKarspeck, A., Hendricks, J., Collins, N., Macchia, F., and \u00d6zsoy, E.:\nOSSE for a sustainable marine observing network in the Sea of Marmara,\nNonlin. 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