A monthly and latitudinally varying volcanic forcing dataset in simulations of 20th century climate

Atmospheric sciences Meteorology and Atmospheric Dynamics: Numerical modeling and data assimilation Meteorology and Atmospheric Dynamics: Climatology 13. Climate action Volcanic effects Climate dynamics 01 natural sciences 0105 earth and related environmental sciences
DOI: 10.1029/2003gl016875 Publication Date: 2003-06-30T09:31:54Z
ABSTRACT
A new monthly volcanic forcing dataset is included in a coupled GCM for a more physically consistent treatment of the stratospheric sulfate aerosol history from explosive volcanism. The volcanic forcing is different from previous versions in that there is an individual evolution of the aerosol for each event. Thus the seasonal and latitudinal dependence of the volcanic aerosol can affect global climate in a more realistic way prior to the satellite period, compared to earlier volcanic forcing datasets. Negative radiative forcing from volcanic activity is greatest in the early 20th century prior to 1915 and in the late 20th century after 1960. The combination of volcanic and solar forcing contributes to an early‐20th century warming, followed by relative cooling in late 20th century. Consequently, the addition of natural forcing factors to the anthropogenic GHG forcing in late 20th century is required to simulate the observed late 20th century warming.
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