Central America - Fuego & Santiaguito: NPP-OMPS TROPOMI N20-OMPS
Colombia - Cotopaxi, Machin, Ruiz & Sangay: OMI NPP-OMPS TROPOMI N20-OMPS
DRCongo - Nyamuragira & Nyiragongo: OMI NPP-OMPS TROPOMI N20-OMPS
Halmahera - Dukono: OMI NPP-OMPS TROPOMI N20-OMPS
Hawaii - Kilauea: OMI NPP-OMPS TROPOMI N20-OMPS
Indonesia - Lewotobi: OMI NPP-OMPS TROPOMI N20-OMPS
Italy - Etna: OMI NPP-OMPS TROPOMI N20-OMPS
Java - Semeru: OMI NPP-OMPS TROPOMI N20-OMPS
Mexico - El Chichon & Popocatepetl: OMI NPP-OMPS TROPOMI N20-OMPS
Northern Chile - Lastarria: OMI NPP-OMPS TROPOMI N20-OMPS
Papau New Guinea - Bagana: OMI NPP-OMPS TROPOMI N20-OMPS
Peru - Ubinas & Sabancaya: OMI NPP-OMPS TROPOMI N20-OMPS
Philippines - Kanlaon: OMI NPP-OMPS TROPOMI N20-OMPS
South Sandwich Islands - Michael: OMI NPP-OMPS TROPOMI N20-OMPS
Vanuatu - Aoba & Yasur: OMI NPP-OMPS TROPOMI N20-OMPS
The SO2 mass for all significant explosive eruptions in our database (VEI 3+) was converted to sulfate mass in this plot using a typical SO2/sulfate mass ratio (assuming complete conversion of SO2 to sultate aerosol with composition 75 wt% H2SO4 - 25 wt% H2O). To simulate the decay of sulfate aerosol mass with time we assumed a fixed, latitude-dependent e-folding time. |