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Latitudinal and seasonal capacity of the surface oceans as a reservoir of PCBs.

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Latitudinal and seasonal capacity of the surface oceans as a reservoir of PCBs. / Jurado, Elena; Lohmann, Rainer; Meijer, Sandra N. et al.
In: Environmental Pollution, Vol. 128, No. 1-2, 03.2004, p. 149-162.

Research output: Contribution to Journal/MagazineJournal articlepeer-review

Harvard

Jurado, E, Lohmann, R, Meijer, SN, Jones, KC & Dachs, J 2004, 'Latitudinal and seasonal capacity of the surface oceans as a reservoir of PCBs.', Environmental Pollution, vol. 128, no. 1-2, pp. 149-162. https://doi.org/10.1016/j.envpol.2003.08.039

APA

Vancouver

Jurado E, Lohmann R, Meijer SN, Jones KC, Dachs J. Latitudinal and seasonal capacity of the surface oceans as a reservoir of PCBs. Environmental Pollution. 2004 Mar;128(1-2):149-162. doi: 10.1016/j.envpol.2003.08.039

Author

Jurado, Elena ; Lohmann, Rainer ; Meijer, Sandra N. et al. / Latitudinal and seasonal capacity of the surface oceans as a reservoir of PCBs. In: Environmental Pollution. 2004 ; Vol. 128, No. 1-2. pp. 149-162.

Bibtex

@article{69b049a47bd8448e8f02a50dff5f9a45,
title = "Latitudinal and seasonal capacity of the surface oceans as a reservoir of PCBs.",
abstract = "The oceans play an important role as a global reservoir and ultimate sink of persistent organic pollutants (POPs) such as polychlorinated biphenyls congeners (PCBs). However, the physical and biogeochemical variables that affect the oceanic capacity to retain PCBs show an important spatial and temporal variability which have not been studied in detail, so far. The objective of this paper is to assess the seasonal and spatial variability of the ocean's maximum capacity to act as a reservoir of atmospherically transported and deposited PCBs. A level I fugacity model is used which incorporates the environmental variables of temperature, phytoplankton biomass, and mixed layer depth, as determined from remote sensing and from climatological datasets. It is shown that temperature, phytoplankton biomass and mixed layer depth influence the potential PCB reservoir of the oceans, being phytoplankton biomass specially important in the oceanic productive regions. The ocean's maximum capacities to hold PCBs are estimated. They are compared to a budget of PCBs in the surface oceans derived using a level III model that assumes steady state and which incorporates water column settling fluxes as a loss process. Results suggest that settling fluxes will keep the surface oceanic reservoir of PCBs well below its maximum capacity, especially for the more hydrophobic compounds. The strong seasonal and latitudinal variability of the surface ocean's storage capacity needs further research, because it plays an important role in the global biogeochemical cycles controlling the ultimate sink of PCBs. Because this modeling exercise incorporates variations in downward fluxes driven by phytoplankton and the extent of the water column mixing, it predicts more complex latitudinal variations in PCBs concentrations than those previously suggested.",
keywords = "POP, PCB, Global dynamics, Marine pollution, Fugacity model",
author = "Elena Jurado and Rainer Lohmann and Meijer, {Sandra N.} and Jones, {Kevin C.} and Jordi Dachs",
year = "2004",
month = mar,
doi = "10.1016/j.envpol.2003.08.039",
language = "English",
volume = "128",
pages = "149--162",
journal = "Environmental Pollution",
issn = "0269-7491",
publisher = "Elsevier Ltd",
number = "1-2",

}

RIS

TY - JOUR

T1 - Latitudinal and seasonal capacity of the surface oceans as a reservoir of PCBs.

AU - Jurado, Elena

AU - Lohmann, Rainer

AU - Meijer, Sandra N.

AU - Jones, Kevin C.

AU - Dachs, Jordi

PY - 2004/3

Y1 - 2004/3

N2 - The oceans play an important role as a global reservoir and ultimate sink of persistent organic pollutants (POPs) such as polychlorinated biphenyls congeners (PCBs). However, the physical and biogeochemical variables that affect the oceanic capacity to retain PCBs show an important spatial and temporal variability which have not been studied in detail, so far. The objective of this paper is to assess the seasonal and spatial variability of the ocean's maximum capacity to act as a reservoir of atmospherically transported and deposited PCBs. A level I fugacity model is used which incorporates the environmental variables of temperature, phytoplankton biomass, and mixed layer depth, as determined from remote sensing and from climatological datasets. It is shown that temperature, phytoplankton biomass and mixed layer depth influence the potential PCB reservoir of the oceans, being phytoplankton biomass specially important in the oceanic productive regions. The ocean's maximum capacities to hold PCBs are estimated. They are compared to a budget of PCBs in the surface oceans derived using a level III model that assumes steady state and which incorporates water column settling fluxes as a loss process. Results suggest that settling fluxes will keep the surface oceanic reservoir of PCBs well below its maximum capacity, especially for the more hydrophobic compounds. The strong seasonal and latitudinal variability of the surface ocean's storage capacity needs further research, because it plays an important role in the global biogeochemical cycles controlling the ultimate sink of PCBs. Because this modeling exercise incorporates variations in downward fluxes driven by phytoplankton and the extent of the water column mixing, it predicts more complex latitudinal variations in PCBs concentrations than those previously suggested.

AB - The oceans play an important role as a global reservoir and ultimate sink of persistent organic pollutants (POPs) such as polychlorinated biphenyls congeners (PCBs). However, the physical and biogeochemical variables that affect the oceanic capacity to retain PCBs show an important spatial and temporal variability which have not been studied in detail, so far. The objective of this paper is to assess the seasonal and spatial variability of the ocean's maximum capacity to act as a reservoir of atmospherically transported and deposited PCBs. A level I fugacity model is used which incorporates the environmental variables of temperature, phytoplankton biomass, and mixed layer depth, as determined from remote sensing and from climatological datasets. It is shown that temperature, phytoplankton biomass and mixed layer depth influence the potential PCB reservoir of the oceans, being phytoplankton biomass specially important in the oceanic productive regions. The ocean's maximum capacities to hold PCBs are estimated. They are compared to a budget of PCBs in the surface oceans derived using a level III model that assumes steady state and which incorporates water column settling fluxes as a loss process. Results suggest that settling fluxes will keep the surface oceanic reservoir of PCBs well below its maximum capacity, especially for the more hydrophobic compounds. The strong seasonal and latitudinal variability of the surface ocean's storage capacity needs further research, because it plays an important role in the global biogeochemical cycles controlling the ultimate sink of PCBs. Because this modeling exercise incorporates variations in downward fluxes driven by phytoplankton and the extent of the water column mixing, it predicts more complex latitudinal variations in PCBs concentrations than those previously suggested.

KW - POP

KW - PCB

KW - Global dynamics

KW - Marine pollution

KW - Fugacity model

U2 - 10.1016/j.envpol.2003.08.039

DO - 10.1016/j.envpol.2003.08.039

M3 - Journal article

VL - 128

SP - 149

EP - 162

JO - Environmental Pollution

JF - Environmental Pollution

SN - 0269-7491

IS - 1-2

ER -