The Canadian Centre for Climate Modelling and Analysis global coupled model and its climate

By G. Flato, G. Boer, W. Lee, N. McFarlane, D. Ramsden, M. C. Reader, Andrew J. Weaver. 2000

657 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/21e21290c15d2be83e652ba4419cb794399057ab

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Citations in the corpus

Range expansion of Ambrosia artemisiifolia in Europe is promoted by climate change. (2013, methodology): “[25]), the CSIRO Atmospheric Research Climate Model [26] and the Hadley Centre Coupled Model HadCM3 [27, 28].”
Automated regression-based statistical downscaling tool (2008, background): “CGCM1 is the first Generation of the coupled Canadian Global Climate Model (e.g. Flato et al., 2000).”
Global warming will affect the genetic diversity and uniqueness of Lycaena helle populations (2011, methodology): “Climate change simulations for both scenarios based on the CCCma and HADcm3 models (Flato et al., 2000; Gordon et al., 2000) for the year 2080 with a spatial resolution of 2.5 arc minutes were obtained via the Worldclim homepage.”
Endemic plant communities on special soils: early victims or hardy survivors of climate change? (2012, methodology): “1 (Flato et al. 2000; McFarlane et al. 2005).”
Potential for Range Expansion of Mountain Pine Beetle into the Boreal Forest of North America (2010, methodology): “To obtain these, the daily output of a global circulation model, CGCM-1 (Flato et al. 2000), with an annual 1% increase in CO2 starting in 2000 (a moderate scenario) for the period 1961–2030, was used.”
Population differences in juvenile survival under increasing drought are mediated by seed size in cork oak (Quercus suber L.). (2009, methodology): “To help us consider how these populations might respond to climate change, we determined the expected future climate for the studied populations over the three time periods (2011–2040, 2041–2070 and 2071–2080) by extrapolation of numeric data calculated using the model CGMC2 developed by the Canadia”
Description and evaluation of the bergen climate model: ARPEGE coupled with MICOM (2003, background): “1997) or grids where each atmospheric cell is exactly divided into an integer number of ocean grid cells, and where both models use the same (coarse) coastline (Mantoura et al. 1991; Flato et al. 2000; Gordon et al. 2000).”
Warming asymmetry in climate change simulations (2001, methodology): “The first version, CGCM1, and its control climate are described in some detail by Flato et al. [2000]. The horizontal diffusivity in CGCM1 is 2 x 10am2/s and the vertical diffusivity is 3 x 10 -5 m 2 Is.”
Modeling Impacts of Climate Change on Giant Panda Habitat (2012, methodology): “The MPS overall drops dramatically from 505 km2 in the current distribution down to 67 km2(CGCM3) and 38 km2 (HadCM3) in 2080 (Table 3).”
The Canadian Earth System Model version 5 (CanESM5.0.3) (2019, methodology): “The pattern of excessive heat accumulation in the thermocline is very similar to the pattern of bias seen in CMIP5 models on average (Flato et al., 2013, their Fig. 9.13). Also similar to CMIP5 models, there is a cold bias in the ocean below the thermocline. This suggests that the processes controll”
CLIMATE CHHANGE SENSITIVITY ASSESSMENT ON UPPER MISSISSIPPI RIVER BASIN STREAMFLOWS USING SWAT 1 (2006, methodology): “The five AOGCM models are the Canadian Centre for Climate Modelling and Analysis CCC model (Flato et al., 2000), the Centre for Climate Study Research CCSR model (Emori et al., 1999), the Geophysical Fluid Dynamics Laboratory GFDL model (Delworth et al., 2002), the CSIRO-Mk2 model described by…”
Polar amplification of climate change in coupled models (2003, background): “Canadian Centre for Climate Modelling and Analysis (Canada) Flato et al. (2000) CCC Th, leads”