JpGU-AGU Joint Meeting 2020

講演情報

[E] 口頭発表

セッション記号 A (大気水圏科学) » A-AS 大気科学・気象学・大気環境

[A-AS07] 大気化学

コンビーナ:齋藤 尚子(千葉大学環境リモートセンシング研究センター)、中山 智喜(長崎大学 大学院水産・環境科学総合研究科)、豊田 栄(東京工業大学物質理工学院)、内田 里沙(一般財団法人 日本自動車研究所)

[AAS07-12] Greenhouse gases and air quality monitoring system for urban anthropogenic emission estimation around Jakarta megacity

*西橋 政秀1向井 人史1寺尾 有希夫1橋本 茂1Rizaldi Boer2Muhammad Ardiansyah2Bregas Budianto2Adi Rakhman2Gito Sugih Immanuel2Rudi Nugroho3Nawa Suwedi3Anies Marufatin3Muhammad Agus Salim3Dodo Gunawan4Eka Suharguniyawan4Asep Firman Ilahi4Muharam Syam Nugraha4Ronald Christian Wattimena4Bayu Feriaji4Qoriana Maulani4小田 知宏5Thomas Lauvaux6 (1.国立環境研究所、2.ボゴール農科大学、3.インドネシア技術評価応用庁、4.インドネシア気象気候地球物理庁、5.USRA/NASA、6.LSCE)

キーワード:温室効果ガス、大気質、都市観測、CO2シミュレーション、インドネシア

National Institute for Environmental Studies (NIES) has implemented an international joint research project for greenhouse gases (GHGs) and air quality monitoring with three institutes in Indonesia, IPB, BPPT, and BMKG since 2015/2016. The purpose of this project is to quantify anthropogenic emissions from Jakarta megacity and characterize them in terms of socioeconomic activities in the city. In order to respond to the Paris Climate Agreement, it is important for a monitoring project like ours not only to be capable of monitoring the increasing anthropogenic emissions by rapid economic growth in a developing country, but also to assess future those reduction impacts resulted from mitigation strategies implemented. It is also important to observe GHGs and related air pollutants with high accuracy in Indonesia because such kinds of observations are very limited in Southeast Asia.

We have maintained continuous monitoring systems of CO2, CH4, CO, NOx, SO2, O3, aerosol concentrations (PM2.5, PM10, BC) and the chemical components (NO3-, SO42-) of PM2.5 and PM10, and meteorological parameters at three sites: Serpong (Jakarta suburb), Bogor (center of Bogor city), and Cibeureum (mountainous area, background-like site) since 2016/2017. We have also performed automatic flask sampling of ambient air once a week. The air samples are used to analyze N2O, SF6, and carbon isotopes (13C, 14C) in CO2 at NIES and to validate CO2, CH4, and CO data obtained from the continuous measurement.

We have also conducted high-resolution atmospheric CO2 simulations using the Weather Research and Forecasting model coupled to Chemistry (WRF-Chem). We used two emission inventories to prescribe the surface emissions: ODIAC (Open-source Data Inventory for Anthropogenic CO2) as fossil fuel CO2 (ffCO2) and MsTMIP (Multi-scale Synthesis and Terrestrial Model Intercomparison Project) as biogenic CO2 (bioCO2).

We analyzed the intersite differences of daytime CO2 mole fractions (dCO2) between the urban sites (Serpong, Bogor) and the background-like site (Cibeureum) in the dry season (July-August 2017) and the rainy season (January-February 2018). The observed dCO2 at Serpong was 8.7 and 0.9 ppm in the dry and rainy seasons, respectively. The simulated dCO2 at Serpong shows similar decreasing trend, which is 8.5 and 3.1 ppm in the dry and rainy seasons, respectively. While the simulated CO2 values at Serpong are slightly overestimated in the rainy season possibly due to the poor reproducibility of meteorological fields (wind environment near the surface), the simulation indicates two main factors of the seasonal differences in dCO2: one is the reduction of ffCO2 at Serpong in the rainy season (3.3 ppm) and another one is the reduction of bioCO2 uptake by photosynthesis at Cibeureum in the rainy season (2.9 ppm). The seasonal differences in dCO2 observed and simulated at Bogor are similar to those of Serpong, but smaller.
In our presentation, we will also present the relationship between CO2 and the other species.