Articles | Volume 6, issue 6
https://doi.org/10.5194/cp-6-827-2010
https://doi.org/10.5194/cp-6-827-2010
21 Dec 2010
 | 21 Dec 2010

A multi-variable box model approach to the soft tissue carbon pump

A. M. de Boer, A. J. Watson, N. R. Edwards, and K. I. C. Oliver

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Subject: Carbon Cycle | Archive: Modelling only | Timescale: Pleistocene
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Cited articles

Adkins, J. F., McIntyre, K., and Schrag, D. P.: The salinity, temperature, and δ18O of the glacial deep ocean, Science, 298, 1769–1773, 2002a.
Adkins, J. F., McIntyre, K., and Schrag, D. P.: The temperature, salinity and δ18O of the lgm deep ocean, Geochim. Cosmochim. Acta, 66, A7–a7, 2002b.
Anderson, R. F., Ali, S., Bradtmiller, L. I., Nielsen, S. H. H., Fleisher, M. Q., Anderson, B. E., and Burckle, L. H.: Wind-driven upwelling in the southern ocean and the deglacial rise in atmospheric CO2, Science, 323, 1443–1448, 2009.
Bradtmiller, L. I., Anderson, R. F., Fleisher, M. Q., and Burckle, L. H.: Diatom productivity in the equatorial pacific ocean from the last glacial period to the present: A test of the silicic acid leakage hypothesis, Paleoceanography, 21, PA4201, https://doi.org/10.1029/2006PA001282, 2006.
Brovkin, V., Ganopolski, A., Archer, D., and Rahmstorf, S.: Lowering of glacial atmospheric CO2 in response to changes in oceanic circulation and marine biogeochemistry, Paleoceanography, 22, PA4202, https://doi.org/10.1029/2006PA001380, 2007.
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