Home > Research > Publications & Outputs > Diurnal variability of persistent organic pollu...

Links

Text available via DOI:

View graph of relations

Diurnal variability of persistent organic pollutants in the atmosphere over the remote Southern Atlantic Ocean

Research output: Contribution to Journal/MagazineJournal articlepeer-review

Published

Standard

Diurnal variability of persistent organic pollutants in the atmosphere over the remote Southern Atlantic Ocean. / Gioia, Rosalinda; MacLeod, Matthew; Castro-Jiménez, Javier et al.
In: Atmosphere, Vol. 5, No. 3, 22.08.2014, p. 622-634.

Research output: Contribution to Journal/MagazineJournal articlepeer-review

Harvard

Gioia, R, MacLeod, M, Castro-Jiménez, J, Nizzetto, L, Dachs, J, Lohmann, R & Jones, KC 2014, 'Diurnal variability of persistent organic pollutants in the atmosphere over the remote Southern Atlantic Ocean', Atmosphere, vol. 5, no. 3, pp. 622-634. https://doi.org/10.3390/atmos5030622

APA

Gioia, R., MacLeod, M., Castro-Jiménez, J., Nizzetto, L., Dachs, J., Lohmann, R., & Jones, K. C. (2014). Diurnal variability of persistent organic pollutants in the atmosphere over the remote Southern Atlantic Ocean. Atmosphere, 5(3), 622-634. https://doi.org/10.3390/atmos5030622

Vancouver

Gioia R, MacLeod M, Castro-Jiménez J, Nizzetto L, Dachs J, Lohmann R et al. Diurnal variability of persistent organic pollutants in the atmosphere over the remote Southern Atlantic Ocean. Atmosphere. 2014 Aug 22;5(3):622-634. doi: 10.3390/atmos5030622

Author

Gioia, Rosalinda ; MacLeod, Matthew ; Castro-Jiménez, Javier et al. / Diurnal variability of persistent organic pollutants in the atmosphere over the remote Southern Atlantic Ocean. In: Atmosphere. 2014 ; Vol. 5, No. 3. pp. 622-634.

Bibtex

@article{ac23e16130444316a32b14d2e10e0bee,
title = "Diurnal variability of persistent organic pollutants in the atmosphere over the remote Southern Atlantic Ocean",
abstract = "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.",
author = "Rosalinda Gioia and Matthew MacLeod and Javier Castro-Jim{\'e}nez and Luca Nizzetto and Jordi Dachs and Rainer Lohmann and Jones, {Kevin C.}",
year = "2014",
month = aug,
day = "22",
doi = "10.3390/atmos5030622",
language = "English",
volume = "5",
pages = "622--634",
journal = "Atmosphere",
issn = "2073-4433",
publisher = "MDPI AG",
number = "3",

}

RIS

TY - JOUR

T1 - Diurnal variability of persistent organic pollutants in the atmosphere over the remote Southern Atlantic Ocean

AU - Gioia, Rosalinda

AU - MacLeod, Matthew

AU - Castro-Jiménez, Javier

AU - Nizzetto, Luca

AU - Dachs, Jordi

AU - Lohmann, Rainer

AU - Jones, Kevin C.

PY - 2014/8/22

Y1 - 2014/8/22

N2 - 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.

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.

U2 - 10.3390/atmos5030622

DO - 10.3390/atmos5030622

M3 - Journal article

AN - SCOPUS:84906355114

VL - 5

SP - 622

EP - 634

JO - Atmosphere

JF - Atmosphere

SN - 2073-4433

IS - 3

ER -