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  • Radiative fluxes x
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Steven J. Phipps, Helen V. McGregor, Joëlle Gergis, Ailie J. E. Gallant, Raphael Neukom, Samantha Stevenson, Duncan Ackerley, Josephine R. Brown, Matt J. Fischer, and Tas D. van Ommen

models and 2.8° longitude by 1.6° latitude for the ocean model. There are 18 vertical levels in the atmosphere and 21 in the ocean. Mk3L produces a realistic simulation of the modern climate ( Phipps et al. 2011 ) and has utility for studying the response of the climate system to both natural and anthropogenic forcings ( Phipps and Brown 2010 ; Phipps et al. 2012 ). Flux adjustments with a fixed annual cycle are used to minimize drift and to improve the realism of the simulated climate. The spatial

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