Earth systems model of intermediate complexity information
Class of climate models
Earth systems models of intermediate complexity (EMICs) form an important class of climate models, primarily used to investigate the earth's systems on long timescales or at reduced computational cost. This is mostly achieved through operation at lower temporal and spatial resolution than more comprehensive general circulation models (GCMs). Due to the nonlinear[disambiguation needed] relationship between spatial resolution and model run-speed, modest reductions in resolution can lead to large improvements in model run-speed.[1] This has historically allowed the inclusion of previously unincorporated earth-systems such as ice sheets and carbon cycle feedbacks. These benefits are conventionally understood to come at the cost of some model accuracy. However, the degree to which higher resolution models improve accuracy rather than simply precision is contested.[2][3]
^Cite error: The named reference Flato2011 was invoked but never defined (see the help page).
^Jakob, C. (2014). Going back to basics. Nature Climate Change, 4:1042–1045.
^Lovejoy, S. (2015). A voyage through scales, a missing quadrillion and why the climate is not what you expect. Climate
Dynamics, 44(11):3187–3210.
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