Japan Geoscience Union Meeting 2023

Presentation information

[J] Oral

A (Atmospheric and Hydrospheric Sciences ) » A-AS Atmospheric Sciences, Meteorology & Atmospheric Environment

[A-AS07] Atmospheric Chemistry

Mon. May 22, 2023 1:45 PM - 3:00 PM Exhibition Hall Special Setting (2) (Exhibition Hall 8, Makuhari Messe)

convener:Yosuke Sakamoto(Kyoto University Graduate School of Global Environmental Studies), Risa Uchida(Japan Automobile Research Institute), Shigeyuki Ishidoya(Advanced Industrial Science and Technology), Yoko Iwamoto(Graduate School of Integrated Sciences for Life, Hiroshima University), Chairperson:Yoko Iwamoto(Graduate School of Integrated Sciences for Life, Hiroshima University), Risa Uchida(Japan Automobile Research Institute), Yosuke Sakamoto(Kyoto University Graduate School of Global Environmental Studies)

2:30 PM - 2:45 PM

[AAS07-14] Wet deposition rate of black carbon in low stratus over north Pacific, estimated from aircraft observation

Yoshihiro Kuribara1, *Kazuyuki Kita1, Kenta Minamio1, Nobuhiro Moteki2, Tatsuhiro Mori3, Temma Saito2, Taikichiro Omi2, Makoto Koike2 (1.Faculty of Science, Ibaraki University, 2.University of Tokyo, 3.Keio University)

Keywords:Black carbon aerosol, wet deposition, stratus

Black carbon (BC) is critically significant for meteorological and climate processes because of its strong absorption of solar radiation and its cloud/ice nuclei ability. Wet deposition is major removal process of BC and its efficiency in clouds is critical for understanding its concentration decrease during transport. In this study, BC wet deposition efficiency in low stratus over north Pacific was directly estimated from BC and carbon monoxide (CO) data derived aircraft observation.
AF2022 aircraft observation campaign was conducted from19 July to2 August, 2022, over north Pacific southeast of Hokkaido. BC, CO concentrations as well as cloud water content data directly measured from the aircraft were used in this study.
On 29 and 30 July, higher BC and CO concentrations were measured under/in/over low clouds at 6 areas lower than 3000m. These higher CO and BC air masses in/over clouds were transported from east Siberia and probably affected by biomass burning there. BC wet deposition rates at each area were estimated from decrease of BC per CO concentrations (DBC/DCO) in clouds. The estimated BC deposition rate in the clouds were between 50 and 70% and well correlated with the cloud water content values.