Interhemispheric gradient of atmospheric radiocarbon reveals natural variability of Southern Ocean winds

Tree ring Δ14C data (Reimer et al., 2004; McCormac et al., 2004) indicate that atmospheric Δ14C varied on multi-decadal to centennial timescales, in both hemispheres, over the period between AD 950 and 1830. The Northern and Southern Hemispheric Δ14C records display similar variability, but from the...

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Bibliographic Details
Published in:Climate of the Past
Main Authors: Rodgers, K. B., Mikaloff-Fletcher, S. E., Bianchi, D., Beaulieu, C., Galbraith, E. D., Gnanadesikan, A., Hogg, A. G., Iudicone, D., Lintner, B. R., Naegler, T., Reimer, P. J., Sarmiento, J. L., Slater, R. D.
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2011
Subjects:
Online Access:https://doi.org/10.5194/cp-7-1123-2011
https://noa.gwlb.de/receive/cop_mods_00026634
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https://cp.copernicus.org/articles/7/1123/2011/cp-7-1123-2011.pdf