An isotopic method to estimate conductive heat flux through Antarctic first-year sea ice

The deuterium concentration profile in a first-year Antarctic sea-ice cover is used to deduce a growth-rate curve. Time variations of the conductive heat flux throughout the growth period are then estimated from this growth-rate curve. Results indicate that the isotopic determination of sea ice grow...

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Bibliographic Details
Main Authors: Souchez, Roland, Tison, Jean-Louis, Jouzel, Jean
Format: Article in Journal/Newspaper
Language:English
Published: 1989
Subjects:
Online Access:http://hdl.handle.net/2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/29492
Description
Summary:The deuterium concentration profile in a first-year Antarctic sea-ice cover is used to deduce a growth-rate curve. Time variations of the conductive heat flux throughout the growth period are then estimated from this growth-rate curve. Results indicate that the isotopic determination of sea ice growth rate can be considered as an alternate method for determining the conductive heat flux through a young sea-ice cover. However, there is need for a further test of the method by measuring in situ temperatures and growth rates during the formation of first-year sea ice. -from Authors SCOPUS: NotDefined.j info:eu-repo/semantics/published