Characteristics of Atmospheric CO2 at Shangri-La Regional Atmospheric Background Station in Southwestern China: Insights from Recent Observations (2019–2022)

Southwestern China serves as a critical region for carbon sources and sinks, influenced by both natural ecosystems and anthropogenic activities. The Shangri-La atmospheric background station (28.01° N, 99.73° E), the only regional station in southwestern China, provides essential data for understanding CO2 dynamics. This study analyzes hourly CO2 mole fractions from 2019 to 2022. Background signals were extracted using the Robust Extraction of Baseline Signal (REBS) algorithm, and air-mass trajectories were analyzed using HYSPLIT model and Potential Source Contribution Function (PSCF) and Concentration Weighted Trajectory (CWT) methods. The REBS-derived background CO2 concentration increased from ~409 ppm in 2019 to ~417 ppm in 2022, yielding a growth rate of 1.9 ± 0.1 ppm yr−1, slightly lower than the 2010–2014 rate reported previously and consistent with the recent global slowdown associated with ENSO-driven carbon–climate variability. A coherent seasonal cycle, with spring maxima and late-summer minima, reflects the combined influence of biospheric uptake and monsoonal inflow. Comparison with the global marine boundary layer and Waliguan records shows similar phase and amplitude, confirming the representativeness of Shangri-La as a regional background site, albeit with a one-month phase lag to Waliguan station due to regional climatic and phenological differences. Trajectory and wind analyses identify southern Indo-Myanmar and Sichuan–Yunnan regions as major transport corridors influencing high-CO2 events. Overall, the results highlight that regional transport rather than local emissions dominates CO2 variability at Shangri-La. The derived background and transport signals thus provide an updated and internally consistent characterization of carbon-cycle variability over the southeastern Tibetan Plateau, offering critical observational support for future regional carbon budget assessments.

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Journal
Atmosphere
Published
2025-12-19
DOI
https://doi.org/10.3390/atmos17010003
Primary Topic
Atmospheric and Environmental Gas Dynamics
Type
article
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article

Characteristics of Atmospheric CO2 at Shangri-La Regional Atmospheric Background Station in Southwestern China: Insights from Recent Observations (2019–2022)

Xiaochuan Duan, Ronglian Zhou, Xiaorui Song, Wei He et al.
Atmosphere
Atmospheric and Environmental Gas Dynamics
article

Characteristics of Atmospheric CO2 at Shangri-La Regional Atmospheric Background Station in Southwestern China: Insights from Recent Observations (2019–2022)

Xiaochuan Duan, Ronglian Zhou, Xiaorui Song, Wei He, Yan Yin, Xiaoli Li, Xiaoqing Peng, Ciyong Zhima
article en

Abstract

Southwestern China serves as a critical region for carbon sources and sinks, influenced by both natural ecosystems and anthropogenic activities. The Shangri-La atmospheric background station (28.01° N, 99.73° E), the only regional station in southwestern China, provides essential data for understanding CO2 dynamics. This study analyzes hourly CO2 mole fractions from 2019 to 2022. Background signals were extracted using the Robust Extraction of Baseline Signal (REBS) algorithm, and air-mass trajectories were analyzed using HYSPLIT model and Potential Source Contribution Function (PSCF) and Concentration Weighted Trajectory (CWT) methods. The REBS-derived background CO2 concentration increased from ~409 ppm in 2019 to ~417 ppm in 2022, yielding a growth rate of 1.9 ± 0.1 ppm yr−1, slightly lower than the 2010–2014 rate reported previously and consistent with the recent global slowdown associated with ENSO-driven carbon–climate variability. A coherent seasonal cycle, with spring maxima and late-summer minima, reflects the combined influence of biospheric uptake and monsoonal inflow. Comparison with the global marine boundary layer and Waliguan records shows similar phase and amplitude, confirming the representativeness of Shangri-La as a regional background site, albeit with a one-month phase lag to Waliguan station due to regional climatic and phenological differences. Trajectory and wind analyses identify southern Indo-Myanmar and Sichuan–Yunnan regions as major transport corridors influencing high-CO2 events. Overall, the results highlight that regional transport rather than local emissions dominates CO2 variability at Shangri-La. The derived background and transport signals thus provide an updated and internally consistent characterization of carbon-cycle variability over the southeastern Tibetan Plateau, offering critical observational support for future regional carbon budget assessments.

AtmosphereVol. 17(1)
China Meteorological Administration (CN), Beijing Meteorological Bureau (CN)
Openalex Percentile: Top 62%
Atmospheric and Environmental Gas Dynamics
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