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dc.contributor.authorJohannessen, Ola M.eng
dc.contributor.authorLygre, Kjetileng
dc.contributor.authorEldevik, Toreng
dc.date.accessioned2005-09-14T08:46:05Z
dc.date.available2005-09-14T08:46:05Z
dc.date.issued2005eng
dc.identifier.issn0065-8448en_US
dc.identifier.urihttps://hdl.handle.net/1956/788
dc.description.abstractIn the Boreas Basin in the northern Greenland Sea, convection has been observed to be localized as narrow structures - chimneys - in which the water masses may be homogeneous from the surface through great depths. An experiment was carried out in the ares by R/V Håkon Mosby of the University of Bergen with an aim to detect and investigate chimneys, their structure, and the inherent convective plumes.en_US
dc.format.extent4244926 byteseng
dc.format.mimetypeapplication/pdfeng
dc.language.isoengeng
dc.publisherAmerican Geophysical Unionen_US
dc.relation.ispartofseriesGeophysical Monograph Series;30
dc.subjectOceanographyeng
dc.titleConvective chimneys and plumes in the Northern Greenland Seaen_US
dc.typeChapter
dc.identifier.doihttps://doi.org/10.1029/xxxgmxx


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