Japan Geoscience Union Meeting 2025

Presentation information

[J] Oral

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

[A-AS11] Atmospheric Chemistry

Sun. May 25, 2025 3:30 PM - 5:00 PM Exhibition Hall Special Setting (6) (Exhibition Hall 7&8, Makuhari Messe)

convener:Shinichi Enami(University of Tsukuba), Hitoshi Irie(Center for Environmental Remote Sensing, Chiba University), Shigeyuki Ishidoya(Advanced Industrial Science and Technology), Tomoki Nakayama(Graduate School of Fisheries and Environmental Sciences, Nagasaki University), Chairperson:Kohei Ikeda(National Institute for Environmental Studies)

4:00 PM - 4:15 PM

[AAS11-03] Validation of NO2 vertical profile from remote sensing and estimation of emission rates using airborne measurements

*Yongjoo Choi1, Yugo Kanaya2, Jongbyeok Jun1, Giyeol Lee1, Beom-Keun Seo3, Lim-Seok Chang4 (1.Hankuk University of Foreign Studies, 2.Japan Agency for Marine-Earth Science and Technology , 3.Hanseo University, 4.National Institute of Environmental Research)

Keywords:airborne measurement, MAX-DOAS, NO2 vertical profile, emission rates

During the Airborne and Satellite Investigation of Asian Air Quality (ASIA-AQ) campaign, we conducted airborne measurements using a C90GT aircraft for two distinct research purposes: (1) estimation of emission rates of NO2 from emission sources and (2) validation of NO2 vertical distribution based on ground-based multi-axis differential optical absorption spectroscopy (MAX-DOAS) observations and Geostationary Environment Monitoring Spectrometer (GEMS) satellite data. For emission rate estimation, research flights were conducted over cattle sheds (using zigzag flight patterns) located on the west coast and in the central part of the Korean Peninsula, respectively. The measured NO2 concentrations were used to estimate emission rates by applying our ensemble model, which combines mass balance and Gaussian footprint methods. For validation of the NO2 vertical distribution, the spiral flights (varying the flight altitude up to 3 km) were conducted three times a day (morning, noon, and afternoon) to capture the temporal evolution of the NO2 layer. These results will help validate bottom-up emission inventories and improve the accuracy of NO2 tropospheric vertical column density estimates from GEMS by updating NO2 vertical profiles to better reflect real-world conditions.