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Spatial Distribution of Multi-Fractal Scaling Behaviours of Atmospheric XCO(2) Concentration Time Series during 2010–2018 over China

Exploring the spatial distribution of the multi-fractal scaling behaviours in atmospheric CO(2) concentration time series is useful for understanding the dynamic mechanisms of carbon emission and absorption. In this work, we utilise a well-established multi-fractal detrended fluctuation analysis to...

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Detalles Bibliográficos
Autores principales: Ma, Yiran, He, Xinyi, Wu, Rui, Shen, Chenhua
Formato: Online Artículo Texto
Lenguaje:English
Publicado: MDPI 2022
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9222844/
https://www.ncbi.nlm.nih.gov/pubmed/35741538
http://dx.doi.org/10.3390/e24060817
Descripción
Sumario:Exploring the spatial distribution of the multi-fractal scaling behaviours in atmospheric CO(2) concentration time series is useful for understanding the dynamic mechanisms of carbon emission and absorption. In this work, we utilise a well-established multi-fractal detrended fluctuation analysis to examine the multi-fractal scaling behaviour of a column-averaged dry-air mole fraction of carbon dioxide (XCO(2)) concentration time series over China, and portray the spatial distribution of the multi-fractal scaling behaviour. As XCO(2) data values from the Greenhouse Gases Observing Satellite (GOSAT) are insufficient, a spatio-temporal thin plate spline interpolation method is applied. The results show that XCO(2) concentration records over almost all of China exhibit a multi-fractal nature. Two types of multi-fractal sources are detected. One is long-range correlations, and the other is both long-range correlations and a broad probability density function; these are mainly distributed in southern and northern China, respectively. The atmospheric temperature and carbon emission/absorption are two possible external factors influencing the multi-fractality of the atmospheric XCO(2) concentration. Highlight: (1) An XCO(2) concentration interpolation is conducted using a spatio-temporal thin plate spline method. (2) The spatial distribution of the multi-fractality of XCO(2) concentration over China is shown. (3) Multi-fractal sources and two external factors affecting multi-fractality are analysed.