World ocean thermohaline circulation

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World ocean thermohaline circulation. The global conveyor belt thermohaline circulation is driven primarily by the formation and sinking of deep water (from around 1500m to the Antarctic bottom water overlying the bottom of the ocean) in the Norwegian Sea. When the strength of the haline forcing increases due to excess precipitation, runoff, or ice melt the conveyor belt will weaken or even shut down. The variability in the strength of the conveyor belt will lead to climate change in Europe and it could also influence in other areas of the global ocean.

Sources

Climate change 1995, Impacts, adaptations and mitigation of climate change: scientific-technical analyses, contribution of working group 2 to the second assessment report of the intergovernmental panel on climate change, UNEP and WMO, Cambridge press univeristy, 1996

Link to web-site

http://www.grida.no/publications/vg/climate/page/3085.aspx

Cartographer/
Designer

Philippe Rekacewicz, UNEP/GRID-Arendal

Appears in

Vital Climate Graphics

Published

2000

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