Bowen Chang, Haoran Liu, Muping Chen, C T Zhang, Chengzhi Xing, Hu Q, Wei Tan, Qihua Li, Xiangguang Ji, C H Liu
High Resolution Image Download MS PowerPoint Slide Formaldehyde (HCHO) is a hazardous atmospheric pollutant; however, spatiotemporal discrepancies between tropospheric column density (C HCHO ) and surface concentration (S HCHO ) hinder the accurate derivation of surface concentrations from satellite observations. Based on 2.5 years of vertical profile measurements from 18 sites within China’s hyperspectral remote sensing network, this study demonstrates that HCHO is predominantly enriched below 0.2 km. Its diurnal variation exhibits a midday-evening bimodal pattern driven by boundary layer dynamics, photochemistry, and anthropogenic emissions. Using Generalized Additive Models (GAMs), we identify the dominant drivers of C HCHO and S HCHO across urban, suburban, and background environments. C HCHO is consistently governed by regional photochemistry (31–52% contribution), whereas S HCHO is primarily controlled by anthropogenic emissions in urban areas (29%) and shifts toward photochemical dominance in suburban (42%) and background (51%) regions. Discrepancies in the response magnitudes of C HCHO and S HCHO to strong emissions and photochemical activity substantially weaken their correlation. By integrating vertical profiles with height-resolved GAMs, we further characterize altitude-dependent mechanisms governing column-to-surface conversion. HCHO below 0.2 km is regulated by local emissions and photochemistry, transitions to photochemical dominance in the middle layer, and becomes increasingly influenced by seasonal variability, large-scale meteorology, and biogenic activity in the upper layer (>1.0 km).