Decreasing intensity of open-ocean convection in the Greenland and Iceland seas-Reference-Cited by-同舟云学术

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Decreasing intensity of open-ocean convection in the Greenland and Iceland seas

Published:2015-06-29 Issue:9 Volume:5 Page:877-882
ISSN:1758-678X
Container-title:Nature Climate Change
language:en
Short-container-title:Nature Clim Change

Author:

Moore G. W. K.,Våge K.,Pickart R. S.,Renfrew I. A.

Publisher

Springer Science and Business Media LLC

Subject

Social Sciences (miscellaneous),Environmental Science (miscellaneous)

Link

http://www.nature.com/articles/nclimate2688.pdf

Reference30 articles.

1. Curry, J. A. et al. Seaflux. Bull. Am. Meteorol. Soc. 85, 409–424 (2004).

2. Mauritzen, C. Production of dense overflow waters feeding the North Atlantic across the Greenland-Scotland Ridge.1. Evidence for a revised circulation scheme. Deep-Sea Res. I 43, 769–806 (1996).

3. Dickson, B. From the Labrador Sea to global change. Nature 386, 649–650 (1997).

4. Hurrell, J. W. Decadal trends in the North-Atlantic Oscillation—regional temperatures and precipitation. Science 269, 676–679 (1995).

5. Jahnke-Bornemann, A. & Bruemmer, B. The Iceland-Lofotes pressure difference: Different states of the North Atlantic low-pressure zone. Tellus A 61, 466–475 (2009).

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