Ar. Bandy et al., CARBON-DISULFIDE MEASUREMENTS IN THE ATMOSPHERE OF THE WESTERN NORTH-ATLANTIC AND THE NORTHWESTERN SOUTH-ATLANTIC OCEANS, JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 98(D12), 1993, pp. 23449-23457
Carbon disulfide (CS2) measurements were made over the western and equ
atorial North Atlantic Ocean and the northwestern and equatorial South
Atlantic Ocean. Carbon disulfide was in the range 0.4-50 pptrv in the
atmosphere of the western North Atlantic Ocean. Emissions from anthro
pogenic sources and wet lands were found to be important although anth
ropogenic sources were 4-6 times larger than biogenic sources. The flu
x of CS2 from eastern North America between 30 and 39-degrees latitude
was estimated to be 2 x 10(8)g yr-1 of sulfur. The anthropogenic cont
ribution was 1.8 x 10(8)g yr-1 of sulfur whereas the contribution of m
arshes was 0.2 x 10(8)g yr-1 of sulfur. Sources of CS2 at high latitud
es in the northern hemisphere were comparatively weak. Carbon disulfid
e levels in the western South Atlantic Ocean between -5 and 1-degrees
latitude were in the range 0.2-6 pptrv. Most of the CS2 appeared to co
me from biomass burning in Africa. Carbon disulfide was much higher cl
ose to shore suggesting that the South American continent was a signif
icant source although too few data were available to quantify it. On f
erry flights from Wallops, Virginia to Natal, Brazil, CS2 levels at th
e ferry altitude of about 6 kin averaged 1.2 pptrv. This background CS
2 was adequate to account for all the OCS in the atmosphere.