Journal cover Journal topic
Atmospheric Chemistry and Physics An interactive open-access journal of the European Geosciences Union
doi:10.5194/acp-2017-237
© Author(s) 2017. This work is distributed
under the Creative Commons Attribution 3.0 License.
Research article
16 Mar 2017
Review status
This discussion paper is under review for the journal Atmospheric Chemistry and Physics (ACP).
Tagged tracer simulations of black carbon in the Arctic: Transport, source contributions, and budget
Kohei Ikeda1, Hiroshi Tanimoto1, Takafumi Sugita1, Hideharu Akiyoshi1, Yugo Kanaya2, Chunmao Zhu2, and Fumikazu Taketani2 1National Institute for Environmental Studies, Tsukuba, 305-8506, Japan
2Japan Agency for Marine-Earth Science and Technology, Yokohama, 236-0001, Japan
Abstract. We implemented a tagged tracer method of black carbon (BC) into a global chemistry-transport model GEOS-Chem, examined the pathways and efficiency of long-range transport from a variety of anthropogenic and biomass burning emission sources to the Arctic, and quantified the source contributions of individual emissions. Firstly, we evaluated the simulated BC by comparing it with observations at the Arctic sites and found that the simulated seasonal variations were improved by implementing an aging parameterization and reducing the wet scavenging rate by ice clouds. For tagging BC, we added BC tracers distinguished by source types (anthropogenic and biomass burning) and regions; the global domain was divided into 16 and 27 regions for anthropogenic and biomass burning emissions, respectively. Our simulations showed that BC emitted from Europe and Russia was transported to the Arctic mainly in the lower troposphere during winter and spring. In particular, BC transported from Russia was widely spread over the Arctic in winter and spring, leading to a dominant contribution of 62 % to the Arctic BC near the surface as the annual mean. In contrast, BC emitted from East Asia was found to be transported in the middle troposphere into the Arctic mainly over the Okhotsk Sea and East Siberia during winter and spring. We identified an important window area, which allowed a strong incoming of East Asian BC to the Arctic (130°–180° E and 3–8 km altitude at 66° N). The model demonstrated that the contribution from East Asia to the Arctic had a maximum at about 5 km altitude due to uplifting during the long-range transport in early spring. The efficiency of BC transport from East Asia to the Arctic was smaller than that from other large source regions such as Europe, Russia and North America. However, the East Asian contribution was most important for BC in the middle troposphere (41 %) and BC burden over the Arctic (27 %) because of the large emissions from this region. These results suggested that the main sources of the Arctic BC differed with altitude. The contribution of all the anthropogenic sources to Arctic BC concentrations near the surface was dominant (90 %) on an annual basis. The contributions of biomass burning in boreal regions (Siberia, Alaska and Canada) to the annual total BC deposition onto the Arctic were estimated to be 12–15 %, which became the maximum during summer.

Citation: Ikeda, K., Tanimoto, H., Sugita, T., Akiyoshi, H., Kanaya, Y., Zhu, C., and Taketani, F.: Tagged tracer simulations of black carbon in the Arctic: Transport, source contributions, and budget, Atmos. Chem. Phys. Discuss., doi:10.5194/acp-2017-237, in review, 2017.
Kohei Ikeda et al.
Kohei Ikeda et al.
Kohei Ikeda et al.

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Short summary
Black carbon (BC), also known as soot particles, plays a key role in Arctic warming, hence the understandings of the major source regions and types are important for its mitigation. We found that Russia was the dominant contributor to the Arctic BC at the surface level, while East Asian contribution was the largest in the middle troposphere and the burden over the Arctic, suggesting that the BC emission reduction from Russia and East Asia can help mitigate the warming in the Arctic.
Black carbon (BC), also known as soot particles, plays a key role in Arctic warming, hence the...
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