Fig. 13From: PSTEP: project for solar–terrestrial environment predictionImpact of interactive ozone chemistry in climate change simulations between mid-Holocene and preindustrial control period. Latitudinal distributions of the annual mean zonal mean surface air temperature (K) for each contribution are plotted: ALL consists of the contributions of the variations of orbital elements and the interactive chemical processes, whereas no-CHEM consists of only the contribution of the former by using the same ozone distribution prescribed in both simulations for mid-Holocene and preindustrial control. Contribution of the chemical processes, CHEM, is defined by ALL minus no-CHEM under the assumption of linear superposition. See Noda et al. (2018) for more detailBack to article page