LIGHT-HYDROCARBONS IN THE SURFACE-WATER OF THE MID-ATLANTIC

During a cruise of RV Polarstern over the Atlantic in September/October 1989, C2-C4 hydrocarbons were measured in surface sea water. The ship passed through three different ocean regions divided by divergences at 8-degrees-N and 3-degrees-S. Hydrocarbon concentrations differed considerably in these regions. The highest values were obtained for ethene with mean concentrations of 246 pMol/l between 35-degrees-N and 8-degrees-N, 165 pMol/l between 8-degrees-N and 3-degrees-S, and 63 pMol/l between 3-degrees-S and 30-degrees-S. Low values were found for i- and n-butane and acetylene between 32 pMol/l and 1 pMol/l. The alkene concentrations were in general higher than the concentrations of their saturated homologs. Concentrations decreased with increasing carbon numbers. The various alkenes were well correlated with one another as were the various alkanes. Oceanic emission rates of the light hydrocarbons were calculated from their sea water concentrations using an ocean atmosphere exchange model. The averaged fluxes ranged from about 10(8) molec cm-2 s-1 for the alkenes and ethane to less than 10(7) molec cm-2 s-1 for the C4 alkanes. Acetylene emissions were below 3 x 10(6) molec cm-2 s-1. Based upon these rates budget estimates of NMHC in the ocean surface layer were made with a simple model considering production and destruction processes in the water. The emissions to the atmosphere appear to be the dominant loss process between 35-degrees-N and 8-degrees-N, whereas destruction in the water seems to be dominant in the latitude ranges 8-degrees-N-3-degrees-S and 3-degrees-S-30-degrees-S.