Posted at 03:45h
in
미분류
by 이오스인테리어
Kinematics of the Pacific equatorial undercurrent: an Eulerian and Lagrangian approach from GCM results
Arakawa, A. & Lamb, V. R. Computational design of the basic dynamical processes of the UCLA general circulation model. Gen. Circ. Model. Atmos. 17, 173–265 (1977).
Marshall, B. J. et al. Morphometric and stable isotopic differentiation of Orbulina universa morphotypes from the Cariaco Basin, Venezuela. ).
Raitzsch, M. et al. Boron isotope-based seasonal paleo-pH reconstruction for the Southeast Atlantic – a multispecies approach using habitat preference of planktonic foraminifera. Earth Planet. Sci. Lett. 487, 138–150 (2018).
Guillermic, M. et al. Seawater pH reconstruction using boron isotopes in multiple planktonic foraminifera species with different depth habitats and their potential to constrain pH and pCO2 gradients. Biogeosciences 17, 3487–3510 (2020).
Bartoli, G., Honisch, B. & Zeebe, R. E. Atmospheric CO2 decline during the Pliocene intensification of Northern Hemisphere glaciations. Paleoceanography 26, PA4213 (2011).
Honisch, B., Hemming, N. G., Archer, D., Siddall, M. & McManus, J. F. Atmospheric carbon dioxide concentration across the mid-Pleistocene transition. Science 324, 1551–1554 (2009).
Sosdian, S. M. et al. Constraining the evolution of Neogene ocean carbonate chemistry using the boron isotope pH proxy. Earth Planet. Sci. Lett. 498, 362–376 (2018).
de la Vega, E., Chalk, T. B., Wilson, P. A., Bysani, R. P. & Foster, G. L. Atmospheric CO2 during the mid-Piacenzian warm period and the M2 glaciation. Sci. Rep. 10, 11002 (2020).
Liu, Z. & Herbert, T. D. High-latitude influence on the eastern equatorial Pacific climate sopra the early Pleistocene epoch. Nature 427, 720–723 (2004).
Regenberg, M. et al. Global dissolution effects on planktonic foraminiferal Mg/Ca ratios controlled by the calcite?saturation state of bottom waters.