Table 2. Annual DMS Flux (TgS/yr) per 10 Degree Latitudinal Band After This Study (L10) and the Kettle and Andreae [2000] (K00) Climatology, Computed With the Nightingale et al. [2000] Parameterization of the Piston Velocitya


Latitude	K00	L10

	Nightingale et al. [2000]
90degree-80degreeN	0.0	0.0
80degree-70degreeN	0.2	0.1
70degree-60degreeN	0.2	0.2
60degree-50degreeN	0.7	0.9
50degree-40degreeN	1.4	1.5
40degree-30degreeN	1.5	1.5
30degree-20degreeN	1.4	1.4
20degree-10degreeN	2.4	2.6
10degree-0degreeN	2.3	2.6
0degree-10degreeS	1.9	2.2
10degree-20degreeS	2.3	3.5
20degree-30degreeS	1.9	3.0
30degree-40degreeS	1.9	2.7
40degree-50degreeS	2.4	2.8
50degree-60degreeS	2.0	2.1
60degree-70degreeS	1.2	0.9
70degree-80degreeS	0.2	0.1
80degree-90degreeS	0.0	0.0
Total	24.0	28.1

	Liss and Merlivat [1986]
	K00	L10
Total	15.0	17.6

	Wanninkhof [1992]
	K00	L10
Total	29.4	34.4

aTotal global DMS fluxes calculated using the Liss and Merlivat [1986] and Wanninkhof [1992] parameterizations are provided for comparison.