Japan Geoscience Union Meeting 2018

Presentation information

[EJ] Oral

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

[A-AS06] Atmospheric Chemistry

Thu. May 24, 2018 10:45 AM - 12:15 PM A05 (Tokyo Bay Makuhari Hall)

convener:Yoko Iwamoto(Graduate School of Biosphere Science, Hiroshima University), Tomoki Nakayama(Graduate School of Fisheries and Environmental Sciences, Nagasaki University), Sakae Toyoda(東京工業大学物質理工学院, 共同), Nawo Eguchi(Kyushu University), Chairperson:Saitoh Naoko(Chiba University)

11:45 AM - 12:00 PM

[AAS06-15] First MAX-DOAS observation of glyoxal and formaldehyde in Southeast Asia and South Asia.

*Hossain Mohammed Syedul Hoque1, Hitoshi Irie1, Alessandro Damiani1, Manish Naja2 (1.Center for Environmental Remote Sensing (CEReS), Chiba University, Japan, 2.Aryabhatta Research Institute of Observational Sciences (ARIES), Nainital, India)

We present the Multi-Axis Differential Optical Absorption Spectroscopy (MAX-DOAS) measurements of formaldehyde (HCHO) and glyoxal (CHOCHO) performed at Phimai in Thailand (15.18° N,102.56° E) and at Pantnagar in India (29.03° N,79.47° E). Our MAX-DOAS instruments have been operating in Phimai and Pantnagar since September 2014 and January 2017, respectively. Vertical profiles of eight components were retrieved separately using the Japanese MAX-DOAS profile retrieval algorithm, version 2. Here we focus on formaldehyde (HCHO) and glyoxal (CHOCHO) and study their volume mixing ratios (VMRs) in the lowest layer (0-1 km) of the retrieved vertical profiles. We estimated the ratio of CHOCHO to HCHO concentrations (RGF), which is suggested to be an important tracer indicating changes in volatile organic compound (VOC) emissions. In Phimai, higher concentrations of HCHO and CHOCHO were observed during the dry season, reflecting the influence of biomass burning. The annual mean RGF for the Phimai site was estimated to be 0.032 ± 0.008. The estimated RGF for the dry season (0.028 ± 0.007) was lower than that of the wet season (0.040 ± 0.010). This change in the RGF is consistent with results reported from satellite retrievals, suggesting a higher RGF for strong biogenic emissions. Similarly, in Pantnagar, biomass burning influence during spring and autumn led to higher concentrations of HCHO and CHOCHO. RGF estimated for the spring (0.030 ± 0.007) and autumn (0.026 ± 0.006) season in Pantnagar was lower, consistent with the RGF response observed in Phimai in the dry season. The RGF response observed in Phimai and Pantnagar was in contrast to some field studies suggesting higher RGF during biomass burning activities. Such discrepancies might be due to the differences in the emission from a biomass burning event. The overall discrepancies observed among satellite measurements and field studies are yet under discussion. Findings of such studies are expected to be used to reduce model uncertainties related to VOC chemistry in study regions.