The renewal of Labrador sea water
作者： J.R.N. Lazier
DOI: 10.1016/0011-7471(73)90058-2
关键词: Current (stream) 、 Salinity 、 Convection 、 Atlantic water 、 Oceanography 、 Geology 、 Surface water 、 Isopycnal 、 Labrador Sea Water 、 North Atlantic Deep Water
摘要: Abstract Temperature, salinity and dissolved oxygen data are analysed to study the renewal of Labrador Sea Water. It is suggested that occurs in winter central when cooled surface water sinks intermediate depths along isopycnal surfaces which rise meet sea because cyclonic circulation sea. The eventually ends up with properties Water a mixture warm, saline Atlantic West Greenland Current cold, less polar Current. An apparent instance deep convective 1500 meters 1967 discussed briefly.
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Columbus O’Donnell Iselin, A study of the circulation of the western North Atlantic Massachusetts Institute of Technology and Woods Hole Oceanographic Institution. ,(1936) , 10.1575/1912/1087
Arthur Lee, David Ellett, On the contribution of overflow water from the Norwegian Sea to the hydrographic structure of the North Atlantic Ocean Deep Sea Research and Oceanographic Abstracts. ,vol. 12, pp. 129- 142 ,(1965) , 10.1016/0011-7471(65)90019-7
Arthur Lee, David Ellett, On the water masses of the Northwest Atlantic Ocean Deep Sea Research and Oceanographic Abstracts. ,vol. 14, pp. 183- 190 ,(1967) , 10.1016/0011-7471(67)90004-6
J.C. Swallow, L.V. Worthington, Deep currents in the Labrador Sea Deep Sea Research and Oceanographic Abstracts. ,vol. 16, pp. 77- 84 ,(1969) , 10.1016/0011-7471(69)90052-7
, Observation of Formation of Deep Water in the Mediterranean Sea, 1969 Nature. ,vol. 227, pp. 1037- 1040 ,(1970) , 10.1038/2271037A0
G. Dietrich, Oceanic Polar Front Survey in the North Atlantic Research in Geophysics, Volume 2: Solid Earth and Interface Phenomena. ,vol. 2, pp. 291- ,(1964)