Abstract. Formaldehyde (HCHO) and nitrogen dioxide (NO2) concentrations and profiles were retrieved from ground-based multi-axis differential optical absorption spectroscopy (MAX-DOAS) observations during January 2017–December 2018 at three sites in Asia: (1) Phimai (15.18∘ N, 102.5∘ E), Thailand; (2) Pantnagar (29∘ N, 78.90∘ E) in the Indo-Gangetic Plain (IGP), India; and (3) Chiba (35.62∘ N, 140.10∘ E), Japan. Retrievals were performed using the Japanese MAX-DOAS profile retrieval algorithm ver. 2 (JM2). The observations were used to evaluate the NO2 and HCHO partial columns and
profiles (0–4 km) simulated using the global chemistry transport model
(CTM) CHASER (Chemical Atmospheric General Circulation Model for Study of Atmospheric Environment and Radiative Forcing). The NO2 and HCHO concentrations at all three sites
showed consistent seasonal variation throughout the investigated period.
Biomass burning affected the HCHO and NO2 variations at Phimai during
the dry season and at Pantnagar during spring (March–May) and post-monsoon
(September–November). Results found for the HCHO-to-NO2 ratio
(RFN), an indicator of high ozone sensitivity, indicate that the transition region (i.e., 1 < RFN < 2) changes regionally, echoing the recent finding for RFN effectiveness. Moreover, reasonable estimates of transition regions can be derived, accounting for the NO2–HCHO chemical feedback. The model was evaluated against global NO2 and HCHO columns data
retrieved from Ozone Monitoring Instrument (OMI) observations before
comparison with ground-based datasets. Despite underestimation, the model
well simulated the satellite-observed global spatial distribution of
NO2 and HCHO, with respective spatial correlations (r) of 0.73 and 0.74. CHASER demonstrated good performance, reproducing the MAX-DOAS-retrieved HCHO and NO2 abundances at Phimai, mainly above 500 m from the surface.
Model results agree with the measured variations within the 1-sigma (1σ)
standard deviation of the observations. Simulations at higher resolution
improved the modeled NO2 estimates for Chiba, reducing the mean bias
error (MBE) for the 0–2 km height by 35 %, but resolution-based
improvements were limited to surface layers. Sensitivity studies show that
at Phimai, pyrogenic emissions contribute up to 50 % and 35 % to HCHO and NO2 concentrations, respectively.