Assessment of Twentieth-Century Regional Surface Temperature Trends using the GFDL CM2 Coupled Models

By T. Knutson, T. Delworth, K. Dixon, I. Held, Jian Lu, V. Ramaswamy, M. Schwarzkopf, Georgiy L. Stenchikov, R. Stouffer. 2006

248 citations recorded by the source corpus.

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Citations in the corpus

SPEAR: The Next Generation GFDL Modeling System for Seasonal to Multidecadal Prediction and Projection (2020, unknown): “…are part of a seamless seasonal to centennial climate prediction and projection effort at GFDL, as the same models that are used for seasonal and decadal prediction have also been used for century‐scale climate change projections (Held et al., 2010, 2019; Knutson et al., 2006; Merlis et al., 2014).”
Reconciling Non-Gaussian Climate Statistics with Linear Dynamics (2009, background): “1 2009 American Meteorological Society Unauthenticated | Downloaded 05/27/22 09:14 PM UTC radiative forcings (e.g., Knutson et al. 2006 and references therein), the approximate linearity of the global atmospheric response to tropical SST changes (e.g., Barsugli and Sardeshmukh 2002; Schneider et…”
The dynamical core, physical parameterizations, and basic simulation characteristics of the atmospheric component AM3 of the GFDL global coupled model CM3 (2011, unknown): “1 ensemble (Knutson et al. 2006) are 0.56 8 , 0.52 8 , and 0.66 8 C, respectively.”
Arctic Oscillation response to volcanic eruptions in the IPCC AR4 climate models (2006, background): “IPCC AR4 runs [Miller et al., 2005; Knutson et al., 2005] do not reproduce the observed trends over recent decades in the AO component of the circulation, and thus do not capture the”
GFDL's CM2 Global Coupled Climate Models. Part I: Formulation and Simulation Characteristics (2006, methodology): “Both models have been used to run a suite of climate change experiments for the 2007 Intergovernmental Panel on Climate Change (IPCC) Assessment Report 4 (AR4) and are able to simulate the main features of the observed warming of the twentieth century (Knutson et al. 2006).”
Decadal prediction skill in a multi-model ensemble (2012, background): “This trend definition merely describes a large part of the temperature behaviour over most of the globe (cf. Knutson et al 2006).”
How reliable are climate models? (2007, methodology): “However, evaluation of the CPDN ensemble against observations of present-day climate suggests that climate sensitivity is less likely to be extremely high than Tellus 59A (2007), 1 would be inferred directly from this ensemble (Piani et al., 2005; Knutti et al., 2006; see Section 6.3).”
Equilibrium Response of an Atmosphere–Mixed Layer Ocean Model to Different Radiative Forcing Agents: Global and Zonal Mean Response (2008, background): “…adjustments not resulting from surface temperature change, such as cloud changes caused by aerosol changes, are evaluated as feedbacks (Shine et al. 2003; Lambert and Faull 2007); and 4) anomalous radiative fluxes at the tropopause do not necessarily scale to the surface air temperature changes.”