Decreasing overflow from the Nordic seas into the Atlantic Ocean through the Faroe Bank channel since 1950

Nature

Volumn 411, Issue 6840, 2001, Pages 927-930

  Hansen, Bogi ^a   Turrell, William R ^b   Østerhus, Svein ^c  

^a Faroese Fisheries Laboratory   (Faroe Islands)

^b MARINE LABORATORY   (United Kingdom)

^c BJERKNES CENTRE FOR CLIMATE RESEARCH   (Norway)

Author keywords

[No Author keywords available]

Indexed keywords

BANKS (BODIES OF WATER); HYDROGRAPHIC SURVEYS; SALINE WATER;

VOLUME FLUX;

OCEANOGRAPHY;

CHANNEL FLOW; DEEP WATER; THERMOHALINE CIRCULATION;

ARTICLE; ATLANTIC OCEAN; PRIORITY JOURNAL; SALINITY; SEA; TEMPERATURE DEPENDENCE; WATER FLOW;

ATLANTIC OCEAN;

EID: 0035927645     PISSN: 00280836     EISSN: None     Source Type: Journal    
DOI: 10.1038/35082034     Document Type: Article

References (18)

1. North Atlantic - Nordic Seas exchanges
2. The production of North Atlantic Deep Water: Sources, rates and pathways
3. Decadal variability in the composition of Faroe Shetland Channel Bottom Water
4. Variations of the Faroe Bank Channel overflow
5. The overflow through the Faroe Bank Channel
6. On the deep-water flow through the Faroe Bank Channel
7. Cold outflow from the Faroe Bank Channel
8. Topographic control of oceanic flows in deep passages and straits
9. The flow of Norwegian Sea Water through the Faroe Bank Channel
10. The abyss of the Nordic Seas is warming
11. Decadal variability in the outflow from the Nordic Seas to the deep Atlantic Ocean
12. Possible predictability in overflow from the Denmark Strait
13. The formation of Greenland Sea deep water: Double diffusion or deep convection?
14. Shifting seas in the greenhouse?
15. Long-term global warming scenarios computed with an efficient coupled climate model
16. Upper layer cooling and freshening in the Norwegian Sea in relation to atmospheric forcing
17. Decadal trends in the North Atlantic Oscillation: Regional temperatures and precipitation