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    Ice Conditions on the Southern Baltic Sea Coast

    Source: Journal of Cold Regions Engineering:;2011:;Volume ( 025 ):;issue: 001
    Author:
    Józef P. Girjatowicz
    DOI: 10.1061/(ASCE)CR.1943-5495.0000020
    Publisher: American Society of Civil Engineers
    Abstract: The 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.
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      Ice Conditions on the Southern Baltic Sea Coast

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    contributor authorJózef P. Girjatowicz
    date accessioned2017-05-08T21:41:14Z
    date available2017-05-08T21:41:14Z
    date copyrightMarch 2011
    date issued2011
    identifier other%28asce%29cr%2E1943-5495%2E0000029.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/59365
    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.
    publisherAmerican Society of Civil Engineers
    titleIce Conditions on the Southern Baltic Sea Coast
    typeJournal Paper
    journal volume25
    journal issue1
    journal titleJournal of Cold Regions Engineering
    identifier doi10.1061/(ASCE)CR.1943-5495.0000020
    treeJournal of Cold Regions Engineering:;2011:;Volume ( 025 ):;issue: 001
    contenttypeFulltext
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