Open AccessModeling the distribution of the volcanic aerosol cloud from the 1783–1784 Laki eruption
Author(s) -
Oman Luke,
Robock Alan,
Stenchikov Georgiy L.,
Thordarson Thorvaldur,
Koch Dorothy,
Shindell Drew T.,
Gao Chaochao
Publication year - 2006
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2005jd006899
Subject(s) - sulfate aerosol , aerosol , atmospheric sciences , sulfate , vulcanian eruption , stratosphere , radiative forcing , volcano , troposphere , climatology , environmental science , latitude , geology , northern hemisphere , meteorology , chemistry , geography , geochemistry , organic chemistry , geodesy
We conducted simulations of the atmospheric transformation and transport of the emissions of the 1783–1784 Laki basaltic flood lava eruption (64.10°N, 17.15°W) using the NASA Goddard Institute for Space Studies modelE climate model coupled to a sulfur cycle chemistry model. The model simulations successfully reproduced the aerosol clouds of the 1912 Katmai and 1991 Mount Pinatubo eruptions, giving us confidence in the Laki simulations. Simulations of the Laki eruption produce peak zonal mean sulfate (SO 4 ) concentrations of over 70 ppbv during August and into September 1783 in the upper troposphere and lower stratosphere at high latitudes. While the majority of the sulfate aerosol was removed during the fall and early winter, a significant aerosol perturbation remained into 1784. The peak SO 2 gas loading was just over 37 megatons (Mt) in late June with the sulfate loading peaking in late August 1783 at 60 Mt over the average of 3 runs. This yielded a peak sulfate aerosol (75% H 2 SO 4 , 25% H 2 O) loading of over 80 Mt with the total aerosol produced during the entire eruption being about 165 Mt. The resulting sulfate deposition compares well with ice cores taken across Greenland. The top of atmosphere net radiative forcing peaks at −27 W/m 2 over the high latitudes during late summer 1783 and produces a global mean forcing of −4 W/m 2 . The model results confirm that Northern Hemisphere high‐latitude volcanic eruptions produce aerosols that remain mostly confined north of 30°N latitude.