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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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