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  • Acp 13 3271 2013

    Rights statement: © Author(s) 2013. This work is distributed under the Creative Commons Attribution 3.0 License

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The role of the global cryosphere in the fate of organic contaminants

Research output: Contribution to Journal/Magazine › Journal article › peer-review

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The role of the global cryosphere in the fate of organic contaminants. / Grannas, A. M.; Bogdal, C.; Hageman, K. J. et al.
In: Atmospheric Chemistry and Physics , Vol. 13, No. 6, 20.03.2013, p. 3271-3305.

Research output: Contribution to Journal/Magazine › Journal article › peer-review

Harvard

Grannas, AM, Bogdal, C, Hageman, KJ, Halsall, C, Harner, T, Hung, H, Kallenborn, R, Klan, P, Kanova, J, Meyer, T & Wania, F 2013, 'The role of the global cryosphere in the fate of organic contaminants', Atmospheric Chemistry and Physics , vol. 13, no. 6, pp. 3271-3305. https://doi.org/10.5194/acp-13-3271-2013

APA

Grannas, A. M., Bogdal, C., Hageman, K. J., Halsall, C., Harner, T., Hung, H., Kallenborn, R., Klan, P., Kanova, J., Meyer, T., & Wania, F. (2013). The role of the global cryosphere in the fate of organic contaminants. Atmospheric Chemistry and Physics , 13(6), 3271-3305. https://doi.org/10.5194/acp-13-3271-2013

Vancouver

Grannas AM, Bogdal C, Hageman KJ, Halsall C, Harner T, Hung H et al. The role of the global cryosphere in the fate of organic contaminants. Atmospheric Chemistry and Physics . 2013 Mar 20;13(6):3271-3305. doi: 10.5194/acp-13-3271-2013

Author

Grannas, A. M. ; Bogdal, C. ; Hageman, K. J. et al. / The role of the global cryosphere in the fate of organic contaminants. In: Atmospheric Chemistry and Physics . 2013 ; Vol. 13, No. 6. pp. 3271-3305.

Bibtex

@article{d8b41564ef4440e0800a5b0e6d1335d6,
title = "The role of the global cryosphere in the fate of organic contaminants",
abstract = "The cryosphere is an important component of global organic contaminant cycles. Snow is an efficient scavenger of atmospheric organic pollutants while a seasonal snowpack, sea ice, glaciers and ice caps are contaminant reservoirs on time scales ranging from days to millennia. Important physical and chemical processes occurring in the various cryospheric compartments impact contaminant cycling and fate. A variety of interactions and feedbacks also occur within the cryospheric system, most of which are susceptible to perturbations due to climate change. In this article, we review the current state of knowledge regarding the transport and processing of organic contaminants in the global cryosphere with an emphasis on the role of a changing climate. Given the complexity of contaminant interactions with the cryosphere and limitations on resources and research capacity, interdisciplinary research and extended collaborations are essential to close identified knowledge gaps and to improve our understanding of contaminant fate under a changing climate.",
author = "Grannas, {A. M.} and C. Bogdal and Hageman, {K. J.} and Crispin Halsall and T. Harner and H. Hung and R. Kallenborn and P. Klan and J. Kanova and T. Meyer and F. Wania",
note = "{\textcopyright} Author(s) 2013. This work is distributed under the Creative Commons Attribution 3.0 License",
year = "2013",
month = mar,
day = "20",
doi = "10.5194/acp-13-3271-2013",
language = "English",
volume = "13",
pages = "3271--3305",
journal = "Atmospheric Chemistry and Physics ",
issn = "1680-7316",
publisher = "Copernicus GmbH (Copernicus Publications) on behalf of the European Geosciences Union (EGU)",
number = "6",

}

RIS

TY - JOUR

T1 - The role of the global cryosphere in the fate of organic contaminants

AU - Grannas, A. M.

AU - Bogdal, C.

AU - Hageman, K. J.

AU - Halsall, Crispin

AU - Harner, T.

AU - Hung, H.

AU - Kallenborn, R.

AU - Klan, P.

AU - Kanova, J.

AU - Meyer, T.

AU - Wania, F.

N1 - © Author(s) 2013. This work is distributed under the Creative Commons Attribution 3.0 License

PY - 2013/3/20

Y1 - 2013/3/20

N2 - The cryosphere is an important component of global organic contaminant cycles. Snow is an efficient scavenger of atmospheric organic pollutants while a seasonal snowpack, sea ice, glaciers and ice caps are contaminant reservoirs on time scales ranging from days to millennia. Important physical and chemical processes occurring in the various cryospheric compartments impact contaminant cycling and fate. A variety of interactions and feedbacks also occur within the cryospheric system, most of which are susceptible to perturbations due to climate change. In this article, we review the current state of knowledge regarding the transport and processing of organic contaminants in the global cryosphere with an emphasis on the role of a changing climate. Given the complexity of contaminant interactions with the cryosphere and limitations on resources and research capacity, interdisciplinary research and extended collaborations are essential to close identified knowledge gaps and to improve our understanding of contaminant fate under a changing climate.

AB - The cryosphere is an important component of global organic contaminant cycles. Snow is an efficient scavenger of atmospheric organic pollutants while a seasonal snowpack, sea ice, glaciers and ice caps are contaminant reservoirs on time scales ranging from days to millennia. Important physical and chemical processes occurring in the various cryospheric compartments impact contaminant cycling and fate. A variety of interactions and feedbacks also occur within the cryospheric system, most of which are susceptible to perturbations due to climate change. In this article, we review the current state of knowledge regarding the transport and processing of organic contaminants in the global cryosphere with an emphasis on the role of a changing climate. Given the complexity of contaminant interactions with the cryosphere and limitations on resources and research capacity, interdisciplinary research and extended collaborations are essential to close identified knowledge gaps and to improve our understanding of contaminant fate under a changing climate.

U2 - 10.5194/acp-13-3271-2013

DO - 10.5194/acp-13-3271-2013

M3 - Journal article

VL - 13

SP - 3271

EP - 3305

JO - Atmospheric Chemistry and Physics

JF - Atmospheric Chemistry and Physics

SN - 1680-7316

IS - 6

ER -