Deep-ocean heat uptake and equilibrium climate response

By Chao Li, Jin-Song von Storch, Jochem Marotzke. Climate Dynamics, 2013

178 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/254364e1a3c90f5f50cf3e91bc8a8d3f31edc490

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Citations in the corpus

The Dependence of Global Cloud and Lapse Rate Feedbacks on the Spatial Structure of Tropical Pacific Warming (2018, background): “…the spatial structure of surface temperature change is complicated by different time-scale responses in the climate system (e.g., Held et al. 2010; Li et al. 2013), unforced variability on annual to multidecadal time scales (e.g., Kosaka and Xie 2013; Dai et al. 2015), and temporal and spatial…”
Contribution of Antarctica to past and future sea-level rise (2016, unknown): “This assumption is based on the thermal inertia of the deep ocean (thousands of years) 47 , its longwave radiative feedback on atmospheric temperatures 77 , and its relative isolation from surface variations.”
Atmospheric component of the MPI‐M Earth System Model: ECHAM6 (2013, background): “Very long integrations with ECHAM5 coupled to the MPIOM show that as the deep ocean comes into equilibrium the asymmetry between the poles is somewhat reduced [Li et al., 2012].”
Forcing, feedbacks and climate sensitivity in CMIP5 coupled atmosphere‐ocean climate models (2012, background): “time scales if changes in the state of the deep ocean influence the pattern of surface warming and atmospheric feedbacks, especially in the Southern Ocean [Held et al., 2010; Li et al., 2012; Senior and Mitchell, 2000].”
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 (2013, background): “Indeed, the strength of the feedbacks can saturate, which would impact the equilibrium temperature response (Li et al. 2013). b. Thermal inertia parameters and temperature: Comparison with the EBM-1 The thermal inertia physical parameters and the relaxation times are given in Table 2 and…”
Developments in the MPI‐M Earth System Model version 1.2 (MPI‐ESM1.2) and Its Response to Increasing CO2 (2019, background): “For cases where a high throughput is essential, for example, for conducting multimillenial simulations (Li et al., 2013; Mikolajewicz et al., 2018; Ziemen et al., 2014), teaching, or development and testing purposes, we have created the MPI-ESM1.”
Robust increase in equilibrium climate sensitivity under global warming (2013, methodology): “Furthermore, it remains unclear whether the regression method is representative of the long-term equilibrium response [Li et al., 2013].”
Loss of cultural world heritage and currently inhabited places to sea-level rise (2014, background): “As a consequence, the SLR that is to be expected if temperatures are sustained over a millennial time scale is much larger than that projected for the year 2100 (Goelzer et al 2012, Fettweis et al 2013, Li et al 2013, Levermann et al 2013).”