04 May 2022
04 May 2022
Status: this preprint is currently under review for the journal ACP.

Vehicle-based in-situ observations of the water vapor isotopic composition across China: spatial and seasonal distributions and controls

Di Wang1,2,3, Lide Tian1,3, Camille Risi2, Xuejie Wang1,3, Jiangpeng Cui4, Gabriel J. Bowen5, Kei Yoshimura6, Zhongwang Wei7, and Laurent Z. X. Li2 Di Wang et al.
  • 1Institute of International Rivers and Eco-security, Yunnan University, Kunming 650500, Yunnan, China
  • 2Laboratoire de Météorologie Dynamique, IPSL, CNRS, Sorbonne Université, Paris 75006, France
  • 3Yunnan Key Laboratory of International Rivers and Transboundary Eco–security, Kunming 650500, Yunnan, China
  • 4Sino-French Institute for Earth System Science, College of Urban and Environmental Sciences, Peking University, Beijing 100871, China
  • 5Department of Geology and Geophysics, and Global Change and Sustainability Center, University of Utah, Salt Lake City, Utah 84108, USA
  • 6Institute of Industrial Science, The University of Tokyo, Tokyo113-8654, Japan
  • 7School of Atmospheric Sciences, Sun Yat-sen University, Guangzhou 510275, Guangdong, China

Abstract. Stable water isotopes are natural tracers in the hydrological cycle and have been applied in hydrology, atmospheric science, ecology, and paleoclimatology. However, the factors controlling the isotopic distribution, both at spatial and temporal scales, are debated in East Asia. For the first time, we made large scale (order 10000 km) continuous observations of near-surface vapor isotopes across China in both pre-monsoon and monsoon seasons, using a newly-designed vehicle-based vapor isotope monitoring system. For both seasons, the observed variations along the sampling route are mainly due to spatial variations, and marginally influenced by synoptic-scale variations. The data thus documents the spatial and seasonal variability of vapor isotopes. The spatial variations of vapor δ18O are mainly controlled by Rayleigh distillation during the pre-monsoon period, but significantly influenced by different moisture sources, continental recycling processes and convection during moisture transport during the monsoon period. The seasonal variation of vapor δ18O reflects the influence of the summer monsoon convective precipitation in southern China, and a dependence on temperature in the North. The spatial and seasonal variations in d-excess reflect the different moisture sources and the influence of continental recycling. The isotope-incorporated global spectral model (Iso-GSM) successfully captures the spatial variation of vapor δ18O during the pre-monsoon period owing to the large latitudinal contrast in humidity and temperature, the overall performance is weaker during the monsoon period. These results provides an overview of the spatial distribution and seasonal variability of water isotopic composition in East Asia and their controlling factors, and emphasize the need to interpret proxy records in the context of the regional system and moisture sources.

Di Wang et al.

Status: open (until 23 Jun 2022)

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Di Wang et al.

Data sets

Vehicle-based in-situ measurements of the water vapor isotopic composition across China Lide Tian, Di Wang

Di Wang et al.


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Short summary
To better understand the spatial and temporal distribution of vapor isotopes, we present two vehicle-based spatially continuous snapshots of the near-surface vapor isotopes in China during the pre-monsoon and monsoon periods. These observations are explained well by different moisture sources and processes along the air mass trajectories. Our results suggest that proxy records need to be interpreted in the context of regional systems and sources of moisture.