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    Seawater Icicles of the Adriatic Sea

    Source: Bulletin of the American Meteorological Society:;2019:;volume 100:;issue 006::page 987
    Author:
    Malačič, Vlado
    ,
    Žagar, Nedjeljka
    DOI: 10.1175/BAMS-D-18-0118.1
    Publisher: American Meteorological Society
    Abstract: AbstractThe marine icicles that form on coastal constructions (e.g., piers and railings) are very common in polar and subpolar areas. The occasional formation of icicles in the coastal zones of the Mediterranean Sea occurs in relation to cold-air outbreaks from the polar region, such as the one presented in this paper in February 2018. The air temperatures over the northern Adriatic Sea, the northernmost part of the Mediterranean, dropped below ?2.1°C, a necessary condition for seawater to freeze, with salinity between 38.0 and 38.5 PSU. The formation of icicles on the coastal structures was further enabled by the bora wind and related high seas along the coast. Measurements presented in this paper confirm that the icicles in the Bay of Piran in the Gulf of Trieste (45.55°N) were formed from the seawater. The measured salinity level of the melted icicles, around 9 PSU, is a typical value reported for marine icicles in polar regions.
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      Seawater Icicles of the Adriatic Sea

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4263739
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    contributor authorMalačič, Vlado
    contributor authorŽagar, Nedjeljka
    date accessioned2019-10-05T06:53:17Z
    date available2019-10-05T06:53:17Z
    date copyright1/24/2019 12:00:00 AM
    date issued2019
    identifier otherBAMS-D-18-0118.1.pdf
    identifier urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4263739
    description abstractAbstractThe marine icicles that form on coastal constructions (e.g., piers and railings) are very common in polar and subpolar areas. The occasional formation of icicles in the coastal zones of the Mediterranean Sea occurs in relation to cold-air outbreaks from the polar region, such as the one presented in this paper in February 2018. The air temperatures over the northern Adriatic Sea, the northernmost part of the Mediterranean, dropped below ?2.1°C, a necessary condition for seawater to freeze, with salinity between 38.0 and 38.5 PSU. The formation of icicles on the coastal structures was further enabled by the bora wind and related high seas along the coast. Measurements presented in this paper confirm that the icicles in the Bay of Piran in the Gulf of Trieste (45.55°N) were formed from the seawater. The measured salinity level of the melted icicles, around 9 PSU, is a typical value reported for marine icicles in polar regions.
    publisherAmerican Meteorological Society
    titleSeawater Icicles of the Adriatic Sea
    typeJournal Paper
    journal volume100
    journal issue6
    journal titleBulletin of the American Meteorological Society
    identifier doi10.1175/BAMS-D-18-0118.1
    journal fristpage987
    journal lastpage994
    treeBulletin of the American Meteorological Society:;2019:;volume 100:;issue 006
    contenttypeFulltext
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