Global ocean heat content in the Last Interglacial

The Last Interglacial (129–116 thousand years ago (ka)) represents one of the warmest climate intervals of the past 800,000 years and the most recent time when sea level was metres higher than today. However, the timing and magnitude of the peak warmth varies between reconstructions, and the relativ...

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Veröffentlicht in:	Nature geoscience 2020-01, Vol.13 (1), p.77-81
Hauptverfasser:	Shackleton, S., Baggenstos, D., Menking, J. A., Dyonisius, M. N., Bereiter, B., Bauska, T. K., Rhodes, R. H., Brook, E. J., Petrenko, V. V., McConnell, J. R., Kellerhals, T., Häberli, M., Schmitt, J., Fischer, H., Severinghaus, J. P.
Format:	Artikel
Sprache:	eng
Schlagworte:	704/106/125 704/106/2738 704/106/413 Antarctic ice Atmospheric circulation Cores Deglaciation Earth and Environmental Science Earth Sciences Earth System Sciences Enthalpy Geochemistry Geology Geophysics/Geodesy Heat Heat content Ice cores Interglacial periods Isotopes Mean temperatures Meltwater Ocean temperature Oceans Rare gases Records Sea level Sea level changes Sea level rise Seawater Temperature Thermal expansion
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