Mechanisms behind the temporary shutdown of deep convection in the labrador sea: Lessons from the great salinity anomaly years 1968-71

Journal of Climate

Volumn 25, Issue 19, 2012, Pages 6743-6755

  Gelderloos, Renske ^a   Straneo, Fiammetta ^b   Katsman, Caroline A ^a  

^a ROYAL NETHERLANDS METEOROLOGICAL INSTITUTE KNMI   (Netherlands)

^b WOODS HOLE OCEANOGRAPHIC INSTITUTION   (United States)

Author keywords

Atmosphere ocean interaction; Intermediate waters; Oceanic variability

Indexed keywords

ARCTIC OCEAN; ATMOSPHERE-OCEAN INTERACTIONS; ATMOSPHERIC DATA; ATMOSPHERIC FORCING; DEEP CONVECTION; DENSE WATERS; FRESHWATER FLUXES; GREENLAND ICE SHEET; LABRADOR SEA; MIXED-LAYER MODELS; OCEANIC VARIABILITY; SEA SURFACE TEMPERATURE (SST); SUBSURFACE WATERS; SURFACE FRESHENING; THERMAL EXPANSION COEFFICIENTS; TIGHT COUPLING;

HEAT FLUX; OCEANOGRAPHY;

WATER;

ADVECTION; ATMOSPHERE-HYDROSPHERE INTERACTION; HEAT FLUX; INTERMEDIATE WATER; OCEANIC CONVECTION; SALINITY; SEA SURFACE TEMPERATURE; TEMPERATURE GRADIENT;

ARCTIC; ARCTIC OCEAN; ATLANTIC OCEAN; ATLANTIC OCEAN (NORTH); GREENLAND; GREENLAND ICE SHEET; LABRADOR SEA;

EID: 84867686854     PISSN: 08948755     EISSN: None     Source Type: Journal    
DOI: 10.1175/JCLI-D-11-00549.1     Document Type: Article

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