An examination of climate sensitivity for idealised climate change experiments in an intermediate general circulation model
By Piers M. Forster, M. Blackburn, R. Glover, K. Shine. 2000
141 citations recorded by the source corpus.
Subfields: Economics and Econometrics, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/4d04063f5ba0ff72889a8f95cfa021db9769c923
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Citations in the corpus
- Transport impacts on atmosphere and climate: Aviation (2009, unknown): “Forster et al.”
- Efficacy of climate forcings (2005, background): “…pollution as a climate forcing [Hansen, 2002] because it was realized that the climate effect of pollutants such as soot and ozone was complex, depending especially on their spatial distribution [RFCR; Forster et al., 1997, 2000; Shine and Forster, 1999; Ramaswamy et al., 2001; Joshi et al., 2003].”
- Stratospheric Communication of El Niño Teleconnections to European Winter (2009, background): “…Circulation Model (IGCM) is a fast general circulation model of intermediate complexity, based on the spectral dynamical core of Hoskins and Simmons (1975) with a range of moist physical processes, such as surface, boundary layer, convective, and radiative schemes (e.g., see Forster et al. 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, unknown): “By assuming additivity of the temperature response patterns (Forster et al. 2000; Boer and Yu 2003a), the surface air temperature response is the sum of the three balance responses, T5Teq 1TU 1TD .”
- “Sunshade World”: A fully coupled GCM evaluation of the climatic impacts of geoengineering (2008, background): “It is greatest at the equator and less at high latitudes, but the latitudinal gradient is less steep than for the solar forcing, and not symmetric across the equator, with a minimum over Antarctica [Forster et al., 2000].”
- Climate response to regional radiative forcing during the twentieth century (2009, background): “1 a), with ∼45p enhancement for extratropical relative to tropical CO 2 forcing (comparable to other studie”
- A comparison of climate response to different radiative forcings in three general circulation models: towards an improved metric of climate change (2003, methodology): “However, besides all these uncertainties there is a growing consensus that, given the same global mean radiative forcing, perturbations restricted to high latitudes are more effective in terms of global mean temperature response than low-latitude forcings (Hansen et al. 1997; Forster et al. 2000 ).”