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Storm Zoltan brought heavy rainfall, accompanied by thunderstorms and winds ranging between 90 and 115\n \n \n $$\\mathrm {km\\,h^{-1}}$$<\/jats:tex-math>\n \n \n km<\/mml:mi>\n \n \n h<\/mml:mi>\n \n -<\/mml:mo>\n 1<\/mml:mn>\n <\/mml:mrow>\n <\/mml:msup>\n <\/mml:mrow>\n <\/mml:math>\n <\/jats:alternatives>\n <\/jats:inline-formula>\n , with gusts reaching up to 140\n \n \n $$\\mathrm {km\\,h^{-1}}$$<\/jats:tex-math>\n \n \n km<\/mml:mi>\n \n \n h<\/mml:mi>\n \n -<\/mml:mo>\n 1<\/mml:mn>\n <\/mml:mrow>\n <\/mml:msup>\n <\/mml:mrow>\n <\/mml:math>\n <\/jats:alternatives>\n <\/jats:inline-formula>\n along the coast which caused severe damage, particularly in northern Germany. Characteristics of the inflowing water at the Fehmarn Belt buoy (FEB), Darss Sill station (DAR) and the Arkona Basin buoy\u00a0(ARK), including salinity, temperature, dissolved oxygen and ocean currents properties, were analysed to understand the impact of storm Zoltan in the western Baltic Sea. In addition to the damage along its path, following the onset of strong westerly winds associated with storm Zoltan, a large volume of water, containing saline (17\u201322 psu), cold (5\u20136\u00a0\u00b0C), and oxygen-rich 7\u20138 (\n \n \n $$\\,\\mathrm { ml\\,l^{-1}}$$<\/jats:tex-math>\n \n \n \n \n ml<\/mml:mi>\n \n \n l<\/mml:mi>\n \n -<\/mml:mo>\n 1<\/mml:mn>\n <\/mml:mrow>\n <\/mml:msup>\n <\/mml:mrow>\n <\/mml:mrow>\n <\/mml:math>\n <\/jats:alternatives>\n <\/jats:inline-formula>\n ) water from the Kattegat and the North Sea reached into the western Baltic Sea. The sea level at Landsort Norra increased by +57 cm over a period of 14 days, from 15 December to 29 December 2023. This resulted in a total volume change of 198\n \n \n $$\\mathrm {km^3}$$<\/jats:tex-math>\n \n \n km<\/mml:mi>\n 3<\/mml:mn>\n <\/mml:msup>\n <\/mml:math>\n <\/jats:alternatives>\n <\/jats:inline-formula>\n in the entire Baltic Sea, with 169\n \n \n $$\\mathrm {km^3}$$<\/jats:tex-math>\n \n \n km<\/mml:mi>\n 3<\/mml:mn>\n <\/mml:msup>\n <\/mml:math>\n <\/jats:alternatives>\n <\/jats:inline-formula>\n and 29\n \n \n $$\\mathrm {km^3}$$<\/jats:tex-math>\n \n \n km<\/mml:mi>\n 3<\/mml:mn>\n <\/mml:msup>\n <\/mml:math>\n <\/jats:alternatives>\n <\/jats:inline-formula>\n provided via the Belt Sea and the Sound Sea, respectively. Observations at the DAR indicated a significant inflow between 19 December 2023 and 1 January 2024 with salinity above 13 psu, temperature below 5.5\u00a0\u00b0C and dissolved oxygen of about 7.5\u20138\n \n \n $$\\mathrm { ml\\,l^{-1}}$$<\/jats:tex-math>\n \n \n ml<\/mml:mi>\n \n \n l<\/mml:mi>\n \n -<\/mml:mo>\n 1<\/mml:mn>\n <\/mml:mrow>\n <\/mml:msup>\n <\/mml:mrow>\n <\/mml:math>\n <\/jats:alternatives>\n <\/jats:inline-formula>\n . While the maximum salinity of the bottom layer at\u00a0the DAR\u00a0was about 17 psu, the ARK\u00a0exhibited significantly higher salinities, reaching up to 22 psu at the bottom layer. During the main inflow period, 75\n \n \n $$\\mathrm {km^3}$$<\/jats:tex-math>\n \n \n km<\/mml:mi>\n 3<\/mml:mn>\n <\/mml:msup>\n <\/mml:math>\n <\/jats:alternatives>\n <\/jats:inline-formula>\n of highly saline water entered the western Baltic Sea. This corresponds to an average salt transport of 1.75 Gt into the western Baltic Sea (1.39 Gt from the Belt Sea and 0.36 Gt from the Sound Sea), representing more than 20% of the total annual salt import into the Baltic Sea), which places the event in the moderate range of major Baltic inflows. This event brought an amount of about 0.8\n \n \n $$\\mathrm {10^6}$$<\/jats:tex-math>\n \n \n 10<\/mml:mn>\n 6<\/mml:mn>\n <\/mml:msup>\n <\/mml:math>\n <\/jats:alternatives>\n <\/jats:inline-formula>\n t oxygen into the Baltic Sea. This was the strongest inflow into the Baltic Sea since 2016.\n <\/jats:p>","DOI":"10.1038\/s41598-024-67328-8","type":"journal-article","created":{"date-parts":[[2024,7,17]],"date-time":"2024-07-17T16:26:02Z","timestamp":1721233562000},"update-policy":"https:\/\/doi.org\/10.1007\/springer_crossmark_policy","source":"Crossref","is-referenced-by-count":10,"title":["Observation of a moderate major Baltic Sea inflow in December 2023"],"prefix":"10.1038","volume":"14","author":[{"given":"Kaveh","family":"Purkiani","sequence":"first","affiliation":[],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"Kerstin","family":"Jochumsen","sequence":"additional","affiliation":[],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"Jens-Georg","family":"Fischer","sequence":"additional","affiliation":[],"role":[{"vocabulary":"crossref","role":"author"}]}],"member":"297","published-online":{"date-parts":[[2024,7,17]]},"reference":[{"issue":"371\u2013400","key":"67328_CR1","doi-asserted-by":"publisher","first-page":"1954","DOI":"10.1098\/rsta.1954.0002","volume":"246","author":"JA Rossiter","year":"1953","unstructured":"Rossiter, J. 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