Abstract
Periodic intensifications of Antarctic Intermediate Water flow occurred as part of the millennial-scale climate oscillations in the glacial period.
Cite
CITATION STYLE
APA
Jung, S. J., Kroon, D., Ganssen, G., Peeters, F., & Ganeshram, R. (2010). Southern Hemisphere intermediate water formation and the bi-polar seesaw. PAGES News, 18(1), 36–38. https://doi.org/10.22498/pages.18.1.36
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