Table 2.
Volcanic eruptions analyzed from the CMIP5/PMIP3 past1000 ensemble. Aerosol mass is from Gao et al.[2008]. Aerosol flux is from Crowley et al.(2008).
| Eruption Year (C.E) | Volcano | Latitude | Stratospheric Sulfate Aerosol Mass (Tg) | Total Sulfate Aerosol Flux (kg km−2) |
|---|---|---|---|---|
| 1167G | Kirishima | 31°N | 52.12 | 10.9 |
| 1227 | Zaozan | 38°N | 67.52 | 51.2 |
| 1258 | Samalas | 8°S | 257.91 | 196.9 |
| 1275G | Quilotoa | 1°S | 63.72 | 10 |
| 1284 | Unidentified | ? | 54.69 | 15.1 |
| 1452 | Kuwae | 17°S | 137.50 | 59.1 |
| 1600 | Huaynaputina | 17°S | 56.59 | 45.7 |
| 1641G | Parker | 6°N | 51.60 | 17.6 |
| 1673C | Gamkonora | 1°N | 16.13 | 20.1 |
| 1694C | Unidentified | ? | 27.1 | 28.3 |
| 1809 | Unidentified | ? | 53.74 | 40.6 |
| 1815 | Tambora | 8°S | 109.72 | 84.8 |
| 1835C | Cosigüina | 13°N | 40.16 | 22.7 |
C
Volcano was used only in CEA-forced runs.
G
Volcano was used only in GRA-forced runs.
Eruptions in years without a superscript were analyzed for all runs.