Figure 5.2: Annual average
source strength in kg km-2 hr-1 for each of the aerosol
types considered here (a to g) with total aerosol optical depth (h). Shown are
(a) the column average H2 SO4 production rate from anthropogenic
sources, (b) the column average H2 SO4 production rate from
natural sources (DMS and SO2 from volcanoes), (c) anthropogenic sources
of organic matter, (d) natural sources of organic matter, (e) anthro-pogenic sources
of black carbon, (f) dust ources for dust with diameters less than 2 µm,
(g) sea salt sources for sea salt with diameters less than 2 µm, and (h)
total optical depth for the sensitivity case CHAM/GRANTOUR model (see Section
5.4.1.4).
