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Distribution and Circulation of Labrador Sea Water
Labrador Sea Water Distribution Circulation
2009/2/8
Labrador Sea Water is the final product of the cyclonic circulation of Subpolar Mode Water in the open northern North Atlantic (McCartney and Talley, 1982). The temperature and salinity of the convect...
The Formation of Labrador Sea Water. Part II. Mesoscale and Smaller-Scale Processes
Labrador Sea Water Mesoscale Smaller-Scale Processes
2009/2/6
In a previous paper, Clarke and Gascard argued that the formation of Labrador Sea Water was taking place in a cyclonic gyre set up each winter in the western Labrador Sea.
Within the gyre and at it...
The Formation of Labrador Sea Water. Part I：Large-Scale Processes
Labrador Sea Water Large-Scale Processes
2009/2/6
Data obtained in the western Labrador Sea during March 1976 by Hudson are analysed to show that new Labrador Sea Water was being formed at this time. On the basis of hydrographic and moored current-me...
The Formation of Labrador Sea Water. Part III：The Evolution of Oxygen and Nutrient Concentration
Labrador Sea Water Oxygen Concentration Nutrient Concentration
2009/1/5
Oxygen, nutrient, and tritium concentrations observed in the western Labrador Sea in March 1976 during deep convective renewal of Labrador Sea water are analyzed to show how a newly formed water mass ...
Labrador Sea Water in the Eastern North Atlantic. Part II：Mixing Dynamics and the Advective–Diffusive Balance
Labrador Sea Water Mixing Dynamics Advective–Diffusive Balance
2008/12/11
Deep wintertime convection in the Labrador Basin produces Labrador Sea Water (LSW), which spreads throughout the North Atlantic. The LSW is not formed with constant characteristics but varies on decad...
Labrador Sea Water in the Eastern North Atlantic. Part I：A Synoptic Circulation Inferred from a Minimum in Potential Vorticity
Labrador Sea Water Potential Vorticity Synoptic Circulation
2008/12/11
A synoptic distribution of Labrador Sea Water (LSW) in the eastern North Atlantic is determined from a regularly sampled, but sparse (3° resolution), survey covering 39° to 54°N, 11° to 34°W during sp...
How Does Labrador Sea Water Enter the Deep Western Boundary Current
Labrador Sea Water Enter Western Boundary Current
2008/6/9
Labrador Sea Water (LSW), a dense water mass formed by convection in the subpolar North Atlantic, is an important constituent of the meridional overturning circulation. Understanding how the water mas...
Labrador Sea Water: Pathways, CFC Inventory, and Formation Rates
Labrador Sea Pathways CFC Inventory Formation Rates
2008/6/4
In 1997, a unique hydrographic and chlorofluorocarbon (CFC: component CFC-11) dataset was obtained in the subpolar North Atlantic. To estimate the synopticity of the 1997 data, the recent temporal evo...
Labrador Sea Water Tracked by Profiling Floats—From the Boundary Current into the Open North Atlantic
Labrador Sea Water Tracked Profiling Floats Boundary Current
2008/6/4
Fifteen profiling floats were injected into the deep boundary current off Labrador. They were ballasted to drift in the core depth of Labrador Sea Water (LSW) at 1500-m depth and were deployed in two ...