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Assessing the impact of large volcanic eruptions of the last millennium (850–1850 CE) on Australian rainfall regimes

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Figure

Table 2. The six largest tropical eruptions of the last millenniumand their total global stratospheric sulfate injection (Tg) as recordedby Gao et al
Figure 1. Evaluation of GISS model ENSO variability against Reynold’s Optimum Interpolation Sea Surface Temperature (OISST, 1982–The meridional extent used to construct the NINO3 index is typically 5for GISS SST
Figure 2. Time series of volcanic forcing from Gao et al. (2008)(a) and Crowley and Unterman (2012) (b)
Figure 3. Global SST anomalies (K) in response to the CR forcings, showing multi-ensemble mean response over JASON averaged acrossall analysed eruptions for years 0 to +5 after eruption.
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