Seasonal variations in water structure under fast ice near Syowa Station, Antarctica, in 1976
Formation of homogeneous water was observed in the surface layer above a depth of 400m in the Ongul Strait in early September of 1976 when fast ice had the maximum thickness. This water was produced from stratified water as a result of haline convection induced by the exclusion of brine during the g...
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| Format: | Article in Journal/Newspaper |
| Language: | English Japanese |
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National Institute of Polar Research
1982
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| Online Access: | https://doi.org/10.15094/00008286 https://doaj.org/article/4aceab9db32d4205ab4ccd31303f78e7 |