作者: Tor Eldevik , Jan Even Ø. Nilsen , Doroteaciro Iovino , K. Anders Olsson , Anne Britt Sandø
DOI: 10.1038/NGEO518
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摘要: The overflows from the Nordic seas maintain deep branch of North Atlantic circulation that is an important part global climate system. An analysis observed ocean temperatures and salinities between 1950 2005 shows water circulating in main source for change overflow waters.