TY - JOUR
T1 - Studies on Arctic aerosols and clouds during the ArCS project
AU - Koike, M.
AU - Goto-Azuma, K.
AU - Kondo, Y.
AU - Matsui, H.
AU - Mori, T.
AU - Moteki, N.
AU - Ohata, S.
AU - Okamoto, H.
AU - Oshima, N.
AU - Sato, K.
AU - Takano, T.
AU - Tobo, Y.
AU - Ukita, J.
AU - Yoshida, A.
N1 - Funding Information:
We thank the staff of the Norwegian Polar Institute for their maintenance of the cloud and aerosol measurements at the Zeppelin Observatory. We also thank the staffs of the National Oceanic and Atmospheric Administration (USA), the Arctic and Antarctic Research Institute (Russia), and Environment and Climate Change Canada for their maintenance of the COSMOS instruments. We are grateful for support from the Alfred Wegener Institute (Germany) and the PAMARCMiP 2018 team members during the ground-based and aircraft experiments. Useful discussion and support from the ArCS project team are gratefully acknowledged. MK thanks Ikuyo Oshima for contributions to the data analysis. HO and KS thank Shuichiro Katagiri and Kohei Ota for their contributions to the radar data analysis.
Funding Information:
The ArCS Project (Arctic Challenge for Sustainability Project, JPMXD1300000000 ) reported here was supported by the Ministry of Education, Culture, Sports, Science, and Technology (MEXT) in Japan. Parts of the studies reported in this paper were also supported by the Environment Research and Technology Development Fund ( JPMEERF20172003 , JPMEERF20202003 , and JPMEERF20205001 ) of the Environmental Restoration and Conservation Agency of Japan , by Japan Society for the Promotion of Science KAKENHI grants ( JP15K13570 , JP16H06020 , JP16H01770 , JP16H01772 , JP17H06139 , JP17H04709 , JP18K03745 , JP18H03363 , JP18H05292 , JP19K20441 , JP19H01972 , and JP19H05699 ), by the Japan Aerospace Exploration Agency for EarthCARE Research Announcement, by the Collaborative Research Program of the Research Institute for Applied Mechanics, Kyushu University, and by a grant for the Global Environmental Research Coordination System of the Ministry of the Environment, Japan.
Funding Information:
We thank the staff of the Norwegian Polar Institute for their maintenance of the cloud and aerosol measurements at the Zeppelin Observatory. We also thank the staffs of the National Oceanic and Atmospheric Administration (USA), the Arctic and Antarctic Research Institute (Russia), and Environment and Climate Change Canada for their maintenance of the COSMOS instruments. We are grateful for support from the Alfred Wegener Institute (Germany) and the PAMARCMiP 2018 team members during the ground-based and aircraft experiments. Useful discussion and support from the ArCS project team are gratefully acknowledged. MK thanks Ikuyo Oshima for contributions to the data analysis. HO and KS thank Shuichiro Katagiri and Kohei Ota for their contributions to the radar data analysis. The ArCS Project (Arctic Challenge for Sustainability Project, JPMXD1300000000) reported here was supported by the Ministry of Education, Culture, Sports, Science, and Technology (MEXT) in Japan. Parts of the studies reported in this paper were also supported by the Environment Research and Technology Development Fund (JPMEERF20172003, JPMEERF20202003, and JPMEERF20205001) of the Environmental Restoration and Conservation Agency of Japan, by Japan Society for the Promotion of Science KAKENHI grants (JP15K13570, JP16H06020, JP16H01770, JP16H01772, JP17H06139, JP17H04709, JP18K03745, JP18H03363, JP18H05292, JP19K20441, JP19H01972, and JP19H05699), by the Japan Aerospace Exploration Agency for EarthCARE Research Announcement, by the Collaborative Research Program of the Research Institute for Applied Mechanics, Kyushu University, and by a grant for the Global Environmental Research Coordination System of the Ministry of the Environment, Japan.
Publisher Copyright:
© 2020 Elsevier B.V. and NIPR
PY - 2021/3
Y1 - 2021/3
N2 - Aerosols and clouds play important roles in the Arctic climate. Conversely, aerosol emissions and cloud formation are affected by changes in the Arctic climate. This paper reviews studies of aerosols and clouds performed during the Arctic Challenge for Sustainability (ArCS) project carried out by the National Institute of Polar Research (NIPR) in Japan and collaborating institutions. The ArCS project included intensive studies of black carbon aerosols (BC). We installed Continuous Soot Monitoring System (COSMOS) instruments to measure atmospheric BC at four locations in the Arctic, establishing the Arctic BC COSMOS Measurement Network (ABCM-net). We also measured BC concentrations in snowpack in extensive areas of the Arctic and showed that previous studies have greatly overestimated BC in snowpack. We developed and improved new aerosol models that achieved better agreements with measurements of BC in the Arctic atmosphere, snowpack, and falling snow. We made new estimates of radiative forcing of BC in the Arctic atmosphere and snow/ice surfaces that lower their albedo. In addition to these researches on BC, we made accurate measurements of ice nucleating particles (INPs) at Ny-Ålesund, Svalbard, showing that their concentrations increased in summer as a result of dust particle emissions from glacial outwash sediments. This high ice nucleating ability was likely due to the presence of organic substances mixed with the dust particles. We also made continuous cloud radar measurements and the first continuous in-situ measurements of cloud microphysical properties in the Arctic at Ny-Ålesund. Results from these cloud measurements and their relationship with aerosols are described.
AB - Aerosols and clouds play important roles in the Arctic climate. Conversely, aerosol emissions and cloud formation are affected by changes in the Arctic climate. This paper reviews studies of aerosols and clouds performed during the Arctic Challenge for Sustainability (ArCS) project carried out by the National Institute of Polar Research (NIPR) in Japan and collaborating institutions. The ArCS project included intensive studies of black carbon aerosols (BC). We installed Continuous Soot Monitoring System (COSMOS) instruments to measure atmospheric BC at four locations in the Arctic, establishing the Arctic BC COSMOS Measurement Network (ABCM-net). We also measured BC concentrations in snowpack in extensive areas of the Arctic and showed that previous studies have greatly overestimated BC in snowpack. We developed and improved new aerosol models that achieved better agreements with measurements of BC in the Arctic atmosphere, snowpack, and falling snow. We made new estimates of radiative forcing of BC in the Arctic atmosphere and snow/ice surfaces that lower their albedo. In addition to these researches on BC, we made accurate measurements of ice nucleating particles (INPs) at Ny-Ålesund, Svalbard, showing that their concentrations increased in summer as a result of dust particle emissions from glacial outwash sediments. This high ice nucleating ability was likely due to the presence of organic substances mixed with the dust particles. We also made continuous cloud radar measurements and the first continuous in-situ measurements of cloud microphysical properties in the Arctic at Ny-Ålesund. Results from these cloud measurements and their relationship with aerosols are described.
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U2 - 10.1016/j.polar.2020.100621
DO - 10.1016/j.polar.2020.100621
M3 - Article
AN - SCOPUS:85096827513
SN - 1873-9652
VL - 27
JO - Polar Science
JF - Polar Science
M1 - 100621
ER -