Volcanic signals in oceans

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Observations, inferences, and mechanisms of the Atlantic Meridional Overturning Circulation: A review (2016, background): “In addition to the effects of greenhouse gases, the AMOC may be influenced by anthropogenic aerosols [Delworth and Dixon, 2006; Stenchikov et al., 2009; Gregory, 2010; Cowan and Cai, 2013; Ding et al., 2014].”
Anthropogenic and Natural Radiative Forcing (2014, background): “, 2007), there is new work indicating extended volcanic impacts via long-term memory in the ocean heat content and sea level (Stenchikov et al., 2009; Gregory, 2010; Otterä et al., 2010).”
External forcing as a metronome for Atlantic multidecadal variability (2010, background): “Volcanic eruptions tend to strengthen the AMOC through their direct radiative coolin”
What is the current state of scientific knowledge with regard to seasonal and decadal forecasting? (2012, background): “In particular, the Atlantic meridional overturning circulation (AMOC) tends to be strengthened by volcanic eruptions (Stenchikov et al 2009).”
Bi-decadal variability excited in the coupled ocean–atmosphere system by strong tropical volcanic eruptions (2012, methodology): “In previous studies, the maximum AMOC strengthening occurs between 5 and 15 years after the eruption, with estimates ranging between *1.6 Sv, evaluated as the average for 18 SVEs during the last 600 years (Ottera u et al. 2010), and *2.4 Sv for the Tambora eruption alone ( Stenchikov et al. 2009 ).”