The 100 000-Yr Cycle in Tropical SST, Greenhouse Forcing, and Climate Sensitivity

By D. Lea. 2004

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Deglaciation in the tropical Indian Ocean driven by interplay between the regional monsoon and global teleconnections (2013, background): “A similar tropical warming lead over atmospheric CO2 rise has also been inferred from the Timor Sea region (Sarnthein et al., 2011), as well as a recent global compilation of deglacial warming records (Shakun et al., 2012) (Fig. 4). The SST lead over atmospheric CO2 is concurrent with the average so”
Past and future polar amplification of climate change: climate model intercomparisons and ice-core constraints (2006, background): “In order to fully exploit the paleoclimatic constraints on climate sensitivity, future work will be needed to disentangle the local radiative perturbation in response to changes in greenhouse gases from the internal feedbacks involving in particular tropical sea surface temperatures (Lea 2004), sea–”
Efficacy of climate forcings (2005, methodology): “the inferred climate sensitivity is larger [Lea, 2004] and the shape of the efficacy curve versus forcing would also change.”
Probabilistic assessment of sea level during the last interglacial stage (2009, background): “While the global mean temperature anomaly is uncertain, seasurface temperatures in the equatorial Paci c (Lea, 2004) and Atlantic (Weldeab et al.”