FN Archimer Export Format PT J TI Diurnal Variability of Persistent Organic Pollutants in the Atmosphere over the Remote Southern Atlantic Ocean BT AF GIOIA, Rosalinda MACLEOD, Matthew CASTRO-JIMENEZ, Javier NIZZETTO, Luca DACHS, Jordi LOHMANN, Rainer JONES, Kevin C. AS 1:1,2;2:3;3:4;4:1,5;5:4;6:6;7:1; FF 1:;2:;3:;4:;5:;6:;7:; C1 Univ Lancaster, Lancaster Environm Ctr, Lancaster LA1 4YQ, England. Cefas Lowestoft Lab, Ctr Environm Fisheries & Aquaculture Sci, Lowestoft NR33 0HT, Suffolk, England. Swiss Fed Inst Technol, CH-8093 Zurich, Switzerland. CSIC, IDAEA, Dept Environm Chem, E-08034 Barcelona, Spain. Norwegian Inst Water Res, NO-0349 Oslo, Norway. Univ Rhode Isl, Grad Sch Oceanog, Narragansett, RI 02882 USA. C2 UNIV LANCASTER, UK CEFAS, UK ETH ZURICH, SWITZERLAND CSIC, SPAIN NIVA, NORWAY UNIV RHODE ISL, USA IN DOAJ IF 0.226 TC 1 UR https://archimer.ifremer.fr/doc/00645/75721/76676.pdf https://archimer.ifremer.fr/doc/00645/75721/76677.pdf LA English DT Article DE ;persistent organic pollutants (POPs);diurnal cycle;polychlorinated biphenyls (PCBs);polycyclic aromatic hydrocarbons (PAHs);South Atlantic AB A diel (24-h) cycle with daytime atmospheric concentrations higher than nighttime concentrations by a factor of 1.5-3 was observed for several low molecular weight polychlorinated biphenyls (PCBs) and polycyclic aromatic hydrocarbons (PAHs) in remote areas of the tropical South Atlantic during a cruise in October-November 2005. In contrast, high molecular weight PCBs and PAHs did not display diurnal variability. A model which has successfully explained diel variability of persistent organic pollutants (POPs) over land could not reproduce the observed diel cycle by considering variability in temperature, atmospheric OH radical concentrations, atmospheric boundary layer height and wind speed as causal factors. We used the model to conduct two bounding scenarios to explore the possibility that phytoplankton biomass turn-over in the surface ocean drives the observed variability in air concentrations. The model could only qualitatively reproduce the field observations of diel variability for low chlorinated PCB congeners when the ocean acts as a source of pollutants to the atmosphere, and when variability in biomass drives variability in the capacity of the surface ocean. PY 2014 PD SEP SO Atmosphere SN 2073-4433 PU Mdpi VL 5 IS 3 UT 000343111900008 BP 622 EP 634 DI 10.3390/atmos5030622 ID 75721 ER EF