Limited temperature response to the very large AD 1258 volcanic eruption

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Aerosol size confines climate response to volcanic super‐eruptions (2010, background): “Another possible reason for the weak response could be the decrease of volcanic radiative forcing due to aerosol growth effects for very large eruptions [Pinto et al., 1989; Timmreck et al., 2009 ], which has been neglected in previous studies.”
Climate and carbon-cycle variability over the last millennium (2010, background): “…for the largest eruption of the last millennium (1258 AD) demonstrate thatReff variations matter and that aerosol particle sizes substantially larger than those observed after Pinatubo yield temperature changes consistent with reconstructions (Timmreck et al., 2009; and references therein).”
Technical details concerning development of a 1200 yr proxy index for global volcanism (2012, background): “Aerosol size affects lifetime and scattering properties (Pinto et al., 1989), significantly affecting in particular the climate impact of very large eruptions (e.g. Timmreck et al., 2009).”
Importance of tropospheric volcanic aerosol for indirect radiative forcing of climate (2012, background): “Recent advances include the use of global aerosol microphysics models due to a growing awareness that the evolution of the particle size distribution is critical to determining the magnitude of simulated climate forcings (e.g., Timmreck et al., 2009, 2010).”