Transient Climate Response in a Two-Layer Energy-Balance Model. Part II: Representation of the Efficacy of Deep-Ocean Heat Uptake and Validation for CMIP5 AOGCMs

By O. Geoffroy, A. Voldoire, D. Oliviè. 2013

200 citations recorded by the source corpus.

Subfields: Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/ff4b0761e9d4eb43b9689df8c1f9b833275b87b8

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In Oceanography

Citations in the corpus

The ocean’s role in the transient response of climate to abrupt greenhouse gas forcing (2015, methodology): “These curves can be rather readily fit by analytical Green’s functions obtained from a two-layer model (see, e.g., Geoffroy et al. 2013a, b; Kostov et al. 2014).”
Observations, inferences, and mechanisms of the Atlantic Meridional Overturning Circulation: A review (2016, background): “Moreover, analyses suggest that differences in ocean heat uptake may explain a significant portion of the large intermodel spread in simulated warming [Raper et al., 2002; Boé et al., 2009; Hansen et al., 2011; Kuhlbrodt and Gregory, 2012; Geoffroy et al., 2013a, 2013b].”
The Dependence of Global Cloud and Lapse Rate Feedbacks on the Spatial Structure of Tropical Pacific Warming (2018, methodology): “This implies that the effective climate sensitivity should increase after 20 yr in abrupt4xCO2 owing to the change in warming pattern, recovering the results of Andrews et al. (2015) and Geoffroy et al. (2013) (among others) but using a different methodology.”
The Dependence of Radiative Forcing and Feedback on Evolving Patterns of Surface Temperature Change in Climate Models (2015, background): “A strong dependence of climate feedbacks on the pattern of SST change therefore raises a question about the applicability of estimates of climate sensitivity derived from the historical record (e.g., Gregory and Forster 2008; Otto et al. 2013).”
Transient Climate Response in a Two-Layer Energy-Balance Model. Part I: Analytical Solution and Parameter Calibration Using CMIP5 AOGCM Experiments (2013, methodology): “In this formulation of the radiative imbalance N , the assumption of linear dependency in T suffers from some limitations (Gregory et al. 2004; Williams et al. 2008; Winton et al. 2010; Held et al. 2010) that are addressed in Part II of this study (Geoffroy et al. 2013, hereafter Part II).”
The Cloud Feedback Model Intercomparison Project (CFMIP) contribution to CMIP6. (2016, background): “, 2015b), (d) the inconstancy of cloud feedbacks and effective climate sensitivity (e.g. Senior and Mitchell, 2000; Williams et al., 2008; Andrews et al., 2012; Geoffroy et al., 2013; Armour et al., 2013; Gregory and Andrews, 2016) and (e) the extent to which models with stronger or weaker cloud fee”
Insights from a refined decomposition of cloud feedbacks (2016, background): “…an underestimate of the actual equilibrium temperature change following a doubling of CO2, owing to the robust tendency for the net feedback to weaken as equilibrium is approached [Gregory et al., 2004; Armour et al., 2013; Block and Mauritsen, 2013; Geoffroy et al., 2013; Andrews et al., 2015].”