Preprints
https://doi.org/10.5194/egusphere-2025-5852
https://doi.org/10.5194/egusphere-2025-5852
11 Dec 2025
 | 11 Dec 2025
Status: this preprint is open for discussion and under review for Biogeosciences (BG).

The Spatial and Temporal Distribution Patterns of XCH₄ in Iran: New Insights from TROPOMI Observations

Ali Rahimi, Manuchehr Farajzadeh, Yousef Ghavidel, and Christoffer Karoff

Abstract. The unprecedented increase in methane concentration, as the second most important greenhouse gas after carbon dioxide, poses a serious challenge to climate change mitigation policies, while accurate and comprehensive monitoring remains insufficient in many countries, including Iran. This study investigates the spatial and temporal patterns of column-averaged methane in Iran using satellite-based observations from Tropospheric Monitoring Instrument on the Sentinel-5P satellite during 2019–2024 and compares them with data from the Emissions Database for Global Atmospheric Research database. On average, XCH₄ concentrations across Iran increased from 1872.6 ± 11.9 ppb in 2019 to 1918.6 ± 11.2 ppb in 2024, representing a +46.1 ± 16.4 ppb rise over six years. All uncertainty estimates represent standard deviations, with a mean value of 12.3 ppb. Statistical and spatial analyses, including Global Moran’s I (0.914–0.982, p < 0.01), Local Moran’s I, and the Getis-Ord Gi* hotspot analysis, confirmed that methane concentrations in Iran exhibit a significant clustering pattern. Hotspots were mainly observed in Class 1: Northern Agro-Hotspots (Gilan, Mazandaran, and Golestan), Class 2: Central Urban-Dense Hotspots, and Class 3: Southern Industrial-Fossil Hotspots, whereas Class 4: Low-Emission Provinces and Class 5: Very-Low-Emission Provinces exhibited lower concentrations with sparse hotspots, located mostly in western and eastern Iran. The highest seasonal averages were recorded in summer (1914.3 ± 13.1 ppb) and autumn (1910.5 ± 13.5 ppb). Comparison with EDGAR data indicates that several major emission sources are underestimated, and spatial overlaps with the observed hotspots did not exceed 5 % in any month. Satellite observations reveal discrepancies in hotspot locations and emission magnitudes, emphasizing that relying solely on modeled inventories may misrepresent methane emissions.

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Ali Rahimi, Manuchehr Farajzadeh, Yousef Ghavidel, and Christoffer Karoff

Status: open (until 22 Jan 2026)

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Ali Rahimi, Manuchehr Farajzadeh, Yousef Ghavidel, and Christoffer Karoff
Ali Rahimi, Manuchehr Farajzadeh, Yousef Ghavidel, and Christoffer Karoff
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Latest update: 11 Dec 2025
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Short summary
Methane in Iran increased from 1873 ppb in 2019 to 1919 ppb in 2024. Hotspots lie in rice areas of the north, the urban-industrial centre, and oil-gas zones in the south, while west and east stay low. The TROPOspheric Monitoring Instrument (TROPOMI) detects many scattered sources that the EDGAR v8.1 inventory smooths into broad areas. Merging TROPOMI, EDGAR, weather, and land-use data sharpens source maps, reveals model gaps, and guides targeted national and regional emission cuts.
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