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Útgáfa síðunnar 19. mars 2012 kl. 01:31

North Iceland Jet

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The North Icelandic Jet is a deep-reaching current that flows along the continental slope of Iceland. North Icelandic Jet advects overflow water into the Denmark Strait and constitutes a pathway that is distinct from the East Greenland Current. It is a cold current that runs west across the top of Iceland, then southwest between Greenland and Iceland at a depth of about 600 meters (almost 2,000 feet). The North Icelandic Jet is deep and narrow (about 12 mile wide) and can carry more than a million cubic meters of water per second. It was not discovered until 2004.

References

• Kjetil Våge,Robert S. Pickart, Michael A. Spall,Héðinn Valdimarsson, Steingrímur Jónsson, Daniel J. Torres, Svein Østerhus & Tor Eldevik, Significant role of the North Icelandic Jet in the formation of Denmark Strait overflow water, Nature Geoscience 4, 723–727 (2011) doi:10.1038/ngeo1234

• Steingrimur Jonsson and Hedinn Valdimarsson, A new path for the Denmark Strait overflow water from the Iceland, GEOPHYSICAL RESEARCH LETTERS, VOL. 31, L03305, doi:10.1029/2003GL019214

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