Modeling the volcanic signal in the atmospheric CO2 record

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Global dimming and brightening: A review (2009, background): “This ‘fertilization effect’ has for example become evident after the volcanic eruption of Mount Pinatubo, where a substantial slowdown of the increase in atmospheric CO2 concentration occurred [Jones and Cox, 2001].”
Strong carbon cycle feedbacks in a climate model with interactive CO2 and sulphate aerosols (2003, methodology): “The reason for this is mostly associated with the climatic effects of the Pinatubo volcanic eruption which enhanced terrestrial uptake by cooling the northern and tropical lands [Jones and Cox, 2001b; Lucht et al., 2002].”
Dynamic global vegetation modelling: quantifying terrestrial ecosystem responses to large-scale environmental change (2007, methodology): “Jones and Cox (2001) used GCM simulations incorporating the TRIFFID DGVM to suggest that post-Pinatubo climatic anomalies overall produced enhanced NPP in the tropics, while respiration globally was reduced.”
Climate and carbon-cycle variability over the last millennium (2010, background): “They conclude that the CO2 decrease in the atmosphere is explained mainly by reduced heterotrophic respiration on land in response to surface cooling corroborating findings by Jones and Cox (2001).”