Articles | Volume 17, issue 20
https://doi.org/10.5194/acp-17-12779-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/acp-17-12779-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Do contemporary (1980–2015) emissions determine the elemental carbon deposition trend at Holtedahlfonna glacier, Svalbard?
Meri M. Ruppel
CORRESPONDING AUTHOR
Department of Environmental Sciences, University of Helsinki, Helsinki, 00790, Finland
Joana Soares
Finnish Meteorological Institute (FMI), Helsinki, 00560, Finland
Air Quality Research Division, Environment and Climate Change Canada, Toronto, M3H 5T4, Canada
Jean-Charles Gallet
Norwegian Polar Institute, Tromsø, 9296, Norway
Elisabeth Isaksson
Norwegian Polar Institute, Tromsø, 9296, Norway
Tõnu Martma
Department of Geology, Tallinn University of Technology, Tallinn, 19086, Estonia
Jonas Svensson
Department of Environmental Sciences, University of Helsinki, Helsinki, 00790, Finland
Finnish Meteorological Institute (FMI), Helsinki, 00560, Finland
Jack Kohler
Norwegian Polar Institute, Tromsø, 9296, Norway
Christina A. Pedersen
Norwegian Polar Institute, Tromsø, 9296, Norway
Sirkku Manninen
Department of Environmental Sciences, University of Helsinki, Helsinki, 00790, Finland
Atte Korhola
Department of Environmental Sciences, University of Helsinki, Helsinki, 00790, Finland
Johan Ström
Department of Environmental Science and Analytical Chemistry ACES (Atmospheric Science Unit), Stockholm University, Stockholm, 11418, Sweden
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Cited
14 citations as recorded by crossref.
- An 800-year high-resolution black carbon ice core record from Lomonosovfonna, Svalbard D. Osmont et al. 10.5194/acp-18-12777-2018
- Elemental and water-insoluble organic carbon in Svalbard snow: a synthesis of observations during 2007–2018 C. Zdanowicz et al. 10.5194/acp-21-3035-2021
- Black carbon deposited in Hariqin Glacier of the Central Tibetan Plateau record changes in the emission from Eurasia M. Wang et al. 10.1016/j.envpol.2020.115778
- Observed and Modeled Black Carbon Deposition and Sources in the Western Russian Arctic 1800–2014 M. Ruppel et al. 10.1021/acs.est.0c07656
- Individual Particle Characteristics, Optical Properties and Evolution of an Extreme Long‐Range Transported Biomass Burning Event in the European Arctic (Ny‐Ålesund, Svalbard Islands) B. Moroni et al. 10.1029/2019JD031535
- Tracing devastating fires in Portugal to a snow archive in the Swiss Alps: a case study D. Osmont et al. 10.5194/tc-14-3731-2020
- Variability in black carbon mass concentration in surface snow at Svalbard M. Bertò et al. 10.5194/acp-21-12479-2021
- Organic Compounds, Radiocarbon, Trace Elements and Atmospheric Transport Illuminating Sources of Elemental Carbon in a 300‐Year Svalbard Ice Core M. Ruppel et al. 10.1029/2022JD038378
- Interactions between the atmosphere, cryosphere, and ecosystems at northern high latitudes M. Boy et al. 10.5194/acp-19-2015-2019
- Sources of black carbon in the atmosphere and in snow in the Arctic L. Qi & S. Wang 10.1016/j.scitotenv.2019.07.073
- Increase in precipitation scavenging contributes to long-term reductions of light-absorbing aerosol in the Arctic D. Heslin-Rees et al. 10.5194/acp-24-2059-2024
- Climate change is rapidly deteriorating the climatic signal in Svalbard glaciers A. Spolaor et al. 10.5194/tc-18-307-2024
- Deposition of Polychlorinated Biphenyls to Firn and Ice Cores at Opposite Polar Sites: Site M, Dronning Maud Land, Antarctica, and Holtedahlfonna, Svalbard M. Hermanson et al. 10.1021/acsearthspacechem.0c00227
- A Holocene black carbon ice-core record of biomass burning in the Amazon Basin from Illimani, Bolivia D. Osmont et al. 10.5194/cp-15-579-2019
14 citations as recorded by crossref.
- An 800-year high-resolution black carbon ice core record from Lomonosovfonna, Svalbard D. Osmont et al. 10.5194/acp-18-12777-2018
- Elemental and water-insoluble organic carbon in Svalbard snow: a synthesis of observations during 2007–2018 C. Zdanowicz et al. 10.5194/acp-21-3035-2021
- Black carbon deposited in Hariqin Glacier of the Central Tibetan Plateau record changes in the emission from Eurasia M. Wang et al. 10.1016/j.envpol.2020.115778
- Observed and Modeled Black Carbon Deposition and Sources in the Western Russian Arctic 1800–2014 M. Ruppel et al. 10.1021/acs.est.0c07656
- Individual Particle Characteristics, Optical Properties and Evolution of an Extreme Long‐Range Transported Biomass Burning Event in the European Arctic (Ny‐Ålesund, Svalbard Islands) B. Moroni et al. 10.1029/2019JD031535
- Tracing devastating fires in Portugal to a snow archive in the Swiss Alps: a case study D. Osmont et al. 10.5194/tc-14-3731-2020
- Variability in black carbon mass concentration in surface snow at Svalbard M. Bertò et al. 10.5194/acp-21-12479-2021
- Organic Compounds, Radiocarbon, Trace Elements and Atmospheric Transport Illuminating Sources of Elemental Carbon in a 300‐Year Svalbard Ice Core M. Ruppel et al. 10.1029/2022JD038378
- Interactions between the atmosphere, cryosphere, and ecosystems at northern high latitudes M. Boy et al. 10.5194/acp-19-2015-2019
- Sources of black carbon in the atmosphere and in snow in the Arctic L. Qi & S. Wang 10.1016/j.scitotenv.2019.07.073
- Increase in precipitation scavenging contributes to long-term reductions of light-absorbing aerosol in the Arctic D. Heslin-Rees et al. 10.5194/acp-24-2059-2024
- Climate change is rapidly deteriorating the climatic signal in Svalbard glaciers A. Spolaor et al. 10.5194/tc-18-307-2024
- Deposition of Polychlorinated Biphenyls to Firn and Ice Cores at Opposite Polar Sites: Site M, Dronning Maud Land, Antarctica, and Holtedahlfonna, Svalbard M. Hermanson et al. 10.1021/acsearthspacechem.0c00227
- A Holocene black carbon ice-core record of biomass burning in the Amazon Basin from Illimani, Bolivia D. Osmont et al. 10.5194/cp-15-579-2019
Latest update: 20 Nov 2024
Short summary
Black carbon (BC) deposition enhances Arctic warming and melting. We present Svalbard ice core BC data from 2005 to 2015, comparing the results with chemical transport model data. The ice core and modelled BC deposition trends clearly deviate from measured and observed atmospheric concentration trends, and thus meteorological processes such as precipitation and scavenging efficiency seem to have a stronger influence on the BC deposition trend than BC emission or atmospheric concentration trends.
Black carbon (BC) deposition enhances Arctic warming and melting. We present Svalbard ice core...
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