Articles | Volume 25, issue 1
https://doi.org/10.5194/acp-25-657-2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-25-657-2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
High-resolution analyses of concentrations and sizes of refractory black carbon particles deposited in northwestern Greenland over the past 350 years – Part 2: Seasonal and temporal trends in refractory black carbon originated from fossil fuel combustion and biomass burning
National Institute of Polar Research, Tachikawa, Tokyo, 190-8518, Japan
SOKENDAI, Shonan Village, Hayama, Kanagawa, 240-0193, Japan
Yoshimi Ogawa-Tsukagawa
National Institute of Polar Research, Tachikawa, Tokyo, 190-8518, Japan
Kaori Fukuda
National Institute of Polar Research, Tachikawa, Tokyo, 190-8518, Japan
Koji Fujita
Graduate School of Environmental Studies, Nagoya University, Nagoya, 464-8601, Japan
Motohiro Hirabayashi
National Institute of Polar Research, Tachikawa, Tokyo, 190-8518, Japan
Remi Dallmayr
National Institute of Polar Research, Tachikawa, Tokyo, 190-8518, Japan
now at: Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany
Jun Ogata
National Institute of Polar Research, Tachikawa, Tokyo, 190-8518, Japan
Nobuhiro Moteki
Department of Chemistry, Graduate School of Science, Tokyo Metropolitan University, Hachioji, Tokyo, 192-0397, Japan
Tatsuhiro Mori
Department of Applied Chemistry, Faculty of Science and Technology, Keio University, Yokohama, Kanagawa, 223-8522, Japan
Sho Ohata
Institute for Space-Earth Environmental Research, Nagoya University, Nagoya, 464-8601, Japan
Yutaka Kondo
National Institute of Polar Research, Tachikawa, Tokyo, 190-8518, Japan
Makoto Koike
Department of Earth and Planetary Science, Graduate School of Science, University of Tokyo, Bunkyo-ku, Tokyo, 113-0033, Japan
Sumito Matoba
Institute of Low Temperature Science, Hokkaido University, Sapporo, 060-0819, Japan
Moe Kadota
Institute of Low Temperature Science, Hokkaido University, Sapporo, 060-0819, Japan
Akane Tsushima
National Institute of Polar Research, Tachikawa, Tokyo, 190-8518, Japan
now at: Graduate School of Integrated Science and Technology, Nagasaki University, Nagasaki, 852-8521, Japan
Naoko Nagatsuka
National Institute of Polar Research, Tachikawa, Tokyo, 190-8518, Japan
now at: Japan Agency for Marine-Earth Science and Technology, Yokosuka, Kanagawa, 237-061, Japan
Teruo Aoki
National Institute of Polar Research, Tachikawa, Tokyo, 190-8518, Japan
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Cited
3 citations as recorded by crossref.
- Evaluation of sample storage methods for single particle analyses of black carbon in snow and ice: Merits and risks of glass and plastic vials for melted sample storage S. Ueda et al. 10.1080/02786826.2025.2542900
- Multiple paleofire proxy metrics from tropical lake sediment and soil in the Greater Serengeti Ecosystem C. Mustaphi et al. 10.1177/09596836251340882
- Technical note: High-resolution analyses of concentrations and sizes of refractory black carbon particles deposited in northwestern Greenland over the past 350 years – Part 1: Continuous flow analysis of the SIGMA-D ice core using the wide-range Single-Particle Soot Photometer and a high-efficiency nebulizer K. Goto-Azuma et al. 10.5194/acp-24-12985-2024
2 citations as recorded by crossref.
- Evaluation of sample storage methods for single particle analyses of black carbon in snow and ice: Merits and risks of glass and plastic vials for melted sample storage S. Ueda et al. 10.1080/02786826.2025.2542900
- Multiple paleofire proxy metrics from tropical lake sediment and soil in the Greater Serengeti Ecosystem C. Mustaphi et al. 10.1177/09596836251340882
Latest update: 28 Aug 2025
Short summary
Monthly ice core records spanning 350 years from Greenland show trends in refractory black carbon (rBC) concentrations and sizes. rBC levels have increased since the 1870s due to the inflow of anthropogenic rBC, with larger diameters than those from biomass burning (BB) rBC. High summer BB rBC peaks may reduce the ice sheet albedo, but BB rBC showed no increase until the early 2000s. These results are vital for validating aerosol and climate models.
Monthly ice core records spanning 350 years from Greenland show trends in refractory black...
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