Seawater Icicles of the Adriatic SeaSource: Bulletin of the American Meteorological Society:;2019:;volume 100:;issue 006::page 987DOI: 10.1175/BAMS-D-18-0118.1Publisher: 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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| contributor author | Malačič, Vlado | |
| contributor author | Žagar, Nedjeljka | |
| date accessioned | 2019-10-05T06:53:17Z | |
| date available | 2019-10-05T06:53:17Z | |
| date copyright | 1/24/2019 12:00:00 AM | |
| date issued | 2019 | |
| identifier other | BAMS-D-18-0118.1.pdf | |
| identifier uri | http://yetl.yabesh.ir/yetl1/handle/yetl/4263739 | |
| description 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. | |
| publisher | American Meteorological Society | |
| title | Seawater Icicles of the Adriatic Sea | |
| type | Journal Paper | |
| journal volume | 100 | |
| journal issue | 6 | |
| journal title | Bulletin of the American Meteorological Society | |
| identifier doi | 10.1175/BAMS-D-18-0118.1 | |
| journal fristpage | 987 | |
| journal lastpage | 994 | |
| tree | Bulletin of the American Meteorological Society:;2019:;volume 100:;issue 006 | |
| contenttype | Fulltext |