JpGU-AGU Joint Meeting 2017

Presentation information

[JJ] Poster

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

[A-AS11] [JJ] Atmospheric Chemistry

Wed. May 24, 2017 3:30 PM - 5:00 PM Poster Hall (International Exhibition Hall HALL7)

convener:Hitoshi Irie(Center for Environmental Remote Sensing, Chiba University), Toshinobu Machida(National Institute for Environmental Studies), Hiroshi Tanimoto(National Institute for Environmental Studies), Yoko Iwamoto(Graduate School of Biosphere Science, Hiroshima University)

[AAS11-P13] Causes leading to enhancements in sulfur dioxide concentration observed by MAX-DOAS in Kyusyu

*Takaya Okuzaki1, Hitoshi Irie2 (1.Graduate School of Advanced Integration Science, Chiba University, 2.Center for Environmental Remote Sensing, Chiba University)

Keywords:SO2, MAX-DOAS, valcano

We performed continuous observations of sulfur dioxide (SO2) using the Multi-Axis Differential Optical Absorption Spectroscopy (MAX-DOAS) at Kasuga in Kyushu, Japan. Spectra measured at 310-320 nm were analyzed with the DOAS method to retrieve mean SO2 concentrations for a 0-1 km layer with a horizontal scale of about 10 km. This spatial scale is expected to provide useful inputs for data assimilation. First, we focused on data acquired in July-August 2014. In the period, seven days were identified as the SO2 level was high (>5 ppbv). Back trajectory analysis indicates that there were two categories; the one from a volcanic origin (the Aso volcano and the Sakurajima volcano) and the other from a continental origin (China and Korea). Based on these results, we performed quantitative analysis using data obtained from January 2014 to September 2016. The mean and the median of the daily maximum SO2 concentrations in the period were 3.3 and 2.1 ppbv, respectively. We investigated the dependence of the observed SO2 level on the size of the range to judge whether the observed air masses passed over volcanoes and found that the higher SO2 concentrations were observed in air masses that passed closer to volcanoes. The mean of the daily maximum SO2 values affected by the Aso volcano was about 6 ppbv, which is larger than that for the Sakurajima volcano (4 ppbv), suggesting that the influence of the Aso volcano was larger. To consider the continental effect, we analyzed relations between SO2 and the length of residence time over China or Korea and between SO2 and the time required for reaching Kasuga from China or Korea. However, no significant correlation was observed. In this case, the mean of the daily maximum SO2 values was about 2.4 ppbv. The results were unchanged even if only influences of urban areas in China or Korea were considered. These results suggest that the impact of long-range transport of air pollution from China or Korea on enhancements in SO2 concentration was smaller than that of volcanoes in Kyusyu. In this presentation, we will also discuss results of analysis including the explosive eruptions of the Aso volcano occurred on 8 October, 2016.