Atmospheric CO <sub>2</sub> dynamics in a coastal megacity: spatiotemporal patterns, sea–land breeze impacts, and anthropogenic–biogenic emission partitioning

Abstract. Attributing observed carbon dioxide (CO2) to fossil-fuel emissions versus biogenic fluxes is essential for assessing urban mitigation, but in coastal megacities it is complicated by anthropogenic–biogenic coupling and sea–land breeze (SLB) circulation. Here we analyze Guangzhou using multi-site in situ CO2 and CO measurements (January 2023–September 2024), transport footprints, and a site-specific ΔCO / ΔCO2 (RCO) relationship to resolve spatiotemporal variability, quantify SLB effects, and partition fossil-fuel (CO2ff) and biogenic (CO2bio) contributions without assimilating emission inventories. Along a coastal–urban–suburban gradient, the coastal site shows the largest seasonal amplitude, the vegetated site exhibits strong summertime diurnal amplitude, and the urban core is combustion-dominated. These gradients reveal a “coastal CO2 dome” that – unlike urban domes often conceptualized as core-anchored – is seasonally displaced, with peak concentrations shifting away from the core due to the interplay of coastal ventilation and biogenic exchange. SLB effects are seasonal: SLB ventilates CO2 in spring–winter but promotes summertime accumulation (+2.08 ppm) under stable stratification, accompanied by pronounced CO enhancements, consistent with trapped/recirculated combustion plumes. Regression-derived urban RCO is consistent with post-2013 broad tightening of coal/industrial and vehicle-emission controls. Winter-afternoon urban CO2ff attribution remains robust to transport-model configurations and measurement/background uncertainty. Summer-afternoon CO2bio shows substantial biogenic uptake, offsetting ∼ 60 % of concurrent CO2ff. These results demonstrate that coastal dynamics and urban greening reshape observed CO2 signals, highlighting that biogenic–anthropogenic decoupling and SLB-aware sampling are essential for the robust evaluation of carbon mitigation in coastal megacities.

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Publication Details

Journal
Atmospheric chemistry and physics
Published
2026-03-03
DOI
https://doi.org/10.5194/acp-26-3253-2026
Citations
1
Primary Topic
Atmospheric and Environmental Gas Dynamics
Type
article
Field-Weighted Citation Impact
36.62

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Atmospheric CO 2 dynamics in a coastal megacity: spatiotemporal patterns, sea–land breeze impacts, and anthropogenic–biogenic emission partitioning

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article

Atmospheric CO 2 dynamics in a coastal megacity: spatiotemporal patterns, sea–land breeze impacts, and anthropogenic–biogenic emission partitioning

Xiufeng Lian, Chunlei Cheng, Chenglei Pei, Shaojie Song, Junjie Li, Bo Huang, Zhen Zhou, Jinwen Zhang, Yongjian Liang, Cheng Wu, Yingyan Huang, Mei Li
article en
1 citations

Abstract

Abstract. Attributing observed carbon dioxide (CO2) to fossil-fuel emissions versus biogenic fluxes is essential for assessing urban mitigation, but in coastal megacities it is complicated by anthropogenic–biogenic coupling and sea–land breeze (SLB) circulation. Here we analyze Guangzhou using multi-site in situ CO2 and CO measurements (January 2023–September 2024), transport footprints, and a site-specific ΔCO / ΔCO2 (RCO) relationship to resolve spatiotemporal variability, quantify SLB effects, and partition fossil-fuel (CO2ff) and biogenic (CO2bio) contributions without assimilating emission inventories. Along a coastal–urban–suburban gradient, the coastal site shows the largest seasonal amplitude, the vegetated site exhibits strong summertime diurnal amplitude, and the urban core is combustion-dominated. These gradients reveal a “coastal CO2 dome” that – unlike urban domes often conceptualized as core-anchored – is seasonally displaced, with peak concentrations shifting away from the core due to the interplay of coastal ventilation and biogenic exchange. SLB effects are seasonal: SLB ventilates CO2 in spring–winter but promotes summertime accumulation (+2.08 ppm) under stable stratification, accompanied by pronounced CO enhancements, consistent with trapped/recirculated combustion plumes. Regression-derived urban RCO is consistent with post-2013 broad tightening of coal/industrial and vehicle-emission controls. Winter-afternoon urban CO2ff attribution remains robust to transport-model configurations and measurement/background uncertainty. Summer-afternoon CO2bio shows substantial biogenic uptake, offsetting ∼ 60 % of concurrent CO2ff. These results demonstrate that coastal dynamics and urban greening reshape observed CO2 signals, highlighting that biogenic–anthropogenic decoupling and SLB-aware sampling are essential for the robust evaluation of carbon mitigation in coastal megacities.

Atmospheric chemistry and physicsVol. 26(4)
Nankai University (CN), Beijing Jiaotong University (CN), Guangzhou Experimental Station (CN), Guangdong-Hongkong-Macau Joint Laboratory of Collaborative Innovation for Environmental Quality (CN), Guangdong Province Environmental Monitoring Center (CN)
National Natural Science Foundation of China, National Oceanic and Atmospheric Administration
Life below water
Openalex Percentile: Top 0%
Atmospheric and Environmental Gas Dynamics
36.62
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