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dc.date.accessioned2013-03-12T09:02:15Z
dc.date.available2013-03-12T09:02:15Z
dc.date.issued2006en_US
dc.date.submitted2007-06-01en_US
dc.identifier.urihttp://hdl.handle.net/10852/12427
dc.description.abstractAn infrared heating lamp has been used as the driving force in laboratory experiments simulating the thermohaline circulation of the world ocean. The radiative energy from the lamp absorbed at different depths in the laboratory tank, as well as the possible temperature effects, have been calculated. The results demonstrate that in the laboratory more than 50 % of the infrared radiation is absorbed within the upper 0.01 mm, more than 90 % within the upper 0.1 mm, and more than 99 % within the upper 1 mm, and that evidently most of the heat energy in the surface layer is quickly transported away by other physical processes.nor
dc.language.isoengen_US
dc.titleVertical transfer of infrared radiation in wateren_US
dc.typeResearch reporten_US
dc.date.updated2008-10-21en_US
dc.creator.authorAas, Eyvinden_US
dc.subject.nsiVDP::450en_US
dc.identifier.urnURN:NBN:no-20095en_US
dc.type.documentForskningsrapporten_US
dc.identifier.duo61323en_US
dc.identifier.bibsys082586136en_US
dc.identifier.fulltextFulltext https://www.duo.uio.no/bitstream/handle/10852/12427/2/Aas_Rapp._129.corr.pdf


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