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dc.contributor.authorJózef P. Girjatowicz
dc.date.accessioned2017-05-08T21:41:14Z
dc.date.available2017-05-08T21:41:14Z
dc.date.copyrightMarch 2011
dc.date.issued2011
dc.identifier.other%28asce%29cr%2E1943-5495%2E0000029.pdf
dc.identifier.urihttp://yetl.yabesh.ir/yetl/handle/yetl/59365
dc.description.abstractThe paper describes basic ice parameters: date of first ice appearance, date of last ice disappearance, duration of ice season, number of days with ice, and maximum ice thickness in winter on the southern Baltic Sea coast. These parameters are used to develop descriptions of the ice regime along the coast, including frequency. The archive data originates from Germany, Poland, and Russia. The missing data were completed by the correlation and regression analysis method. The data concerning the areas of Arkona, Sassnitz, Koserow, Karnin, Kamminke, Ueckermünde, Krasnoflotskoje, Baltijsk, and Ušakovo cover the period from 1950–1951 through 1989–1990, whereas the data concerning the areas of Szczecin, Trzebież, Świnoujście, Kołobrzeg, Darłowo, Ustka, Łeba, Rozewie, Hel, Puck, Gdynia, Świbno, Tolkmicko, and Krynica Morska cover the period from 1946–1947 through 1999–2000. In sheltered basins (internal), the ice phenomena appear earliest (on average, in December) and disappear latest (on average, in March). The intensity increases eastward in accordance with the severity of ice conditions. On the other hand, in unsheltered basins (open sea water) the ice appears later—on average, in January—and it disappears in late February to early March. The intensity increases westward, primarily influenced by bathymetric factors.
dc.publisherAmerican Society of Civil Engineers
dc.titleIce Conditions on the Southern Baltic Sea Coast
dc.typeJournal Paper
dc.journal.volume25
dc.journal.issue1
dc.journal.titleJournal of Cold Regions Engineering
dc.identifier.doi10.1061/(ASCE)CR.1943-5495.0000020
dc.treeJournal of Cold Regions Engineering:;2011:;Volume ( 025 ):;issue: 001
dc.contenttypeFulltext


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