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A model-data comparison of the Holocene global sea surface temperature evolution ArchiMer
Lohmann, G.; Pfeiffer, M.; Laepple, T.; Leduc, G.; Kim, J-h..
We compare the ocean temperature evolution of the Holocene as simulated by climate models and reconstructed from marine temperature proxies. We use transient simulations from a coupled atmosphere-ocean general circulation model, as well as an ensemble of time slice simulations from the Paleoclimate Modelling Intercomparison Project. The general pattern of sea surface temperature (SST) in the models shows a high-latitude cooling and a low-latitude warming. The proxy dataset comprises a global compilation of marine alkenone- and Mg/Ca-derived SST estimates. Independently of the choice of the climate model, we observe significant mismatches between modelled and estimated SST amplitudes in the trends for the last 6000 yr. Alkenone-based SST records show a...
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Ano: 2013 URL: https://archimer.ifremer.fr/doc/00496/60739/65189.pdf
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High-latitude obliquity as a dominant forcing in the Agulhas current system ArchiMer
Caley, T.; Kim, J-h; Malaize, B.; Giraudeau, J.; Laepple, T.; Caillon, N.; Charlier, K.; Rebaubier, H.; Rossignol, L.; Castaneda, I. S.; Schouten, S.; Damste, J. S. Sinninghe.
The Agulhas Current transport of heat and salt from the Indian Ocean into the South Atlantic around South Africa (Agulhas leakage), can affect the Atlantic meridional overturning circulation (AMOC) and, thus, influence global climate. However, efforts to elucidate forcing mechanisms connecting the Agulhas leakage with the upstream dynamics of the current have been hampered by a lack of climate records extracted from the area where the Agulhas current originates. We determine 800-kyr sea surface temperature (SST) and salinity (SSS) records from the "precursor" region of the Agulhas current and show that these records contain strong 100-kyr and 41-kyr cycles. This latter obliquity-driven cycle is nearly in phase with changes in the annual mean insolation and...
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Ano: 2011 URL: https://archimer.ifremer.fr/doc/00228/33904/32363.pdf
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