Articles | Volume 6, issue 4
https://doi.org/10.5194/os-6-1013-2010
© Author(s) 2010. This work is distributed under the Creative Commons Attribution 3.0 License.
Research article
| 
13 Dec 2010
Research article |
| 13 Dec 2010
Stability and forcing of the Iceland-Faroe inflow of water, heat, and salt to the Arctic
Related subject area
Approach: In situ Observations | Depth range: Thermocline | Geographical range: Deep Seas: North Atlantic | Phenomena: Current Field
The flow field of the upper hypoxic eastern tropical North Atlantic oxygen minimum zone
Ocean Sci., 12, 153–167, 2016
Cited articles
Astthorsson, O. S., Gislason, A., and Jonsson, S.: Climate variability and the Icelandic marine ecosystem, Deep-Sea Res. Pt. II, 54, 2456–2477, 2007.
Biastoch, A., Käse, R. H., and Stammer, D. B.: The sensitivity of the Greenland-Scotland Ridge Overflow to Forcing Changes, J. Phys. Oceanogr., 33, 2307–2319, 2003.
Broecker, W. S., Peteet, D. M., and Rind, D.: Does the ocean-atmosphere system have more than one stable mode of operation?, Nature, 315, 21–26, 1985.
Emery, W. J. and Thomson, R. E.: Data Analysis Methods in Physical Oceanography, Second and Revised Edition, Elsevier Science B. V., Amsterdam, 638 pp., 2001.
Gill, A. E.: Atmosphere-Ocean Dynamics, Academic Press, London, 662 pp., 1982.
