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Identification of Potential Methane Source Regions in Europe Using δ 13 C CH4 Measurements and Trajectory Modeling
Author(s) -
Varga T.,
Fisher R. E.,
France J. L.,
Haszpra L.,
Jull A. J. T.,
Lowry D.,
Major I.,
Molnár M.,
Nisbet E. G.,
László E.
Publication year - 2021
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
eISSN - 2169-8996
pISSN - 2169-897X
DOI - 10.1029/2020jd033963
Subject(s) - methane , environmental science , atmospheric sciences , seasonality , atmospheric methane , context (archaeology) , air pollution , climatology , meteorology , chemistry , geography , geology , statistics , mathematics , organic chemistry , archaeology
The methane emissions from the Hungarian Pannonian Basin are not well qualified, due to a lack of measurements of CH 4 mole fraction and δ 13 C CH4 in the air. This study reports methane measurements in air samples from Hungary, placing them in the context of regional and global background data, to investigate the inputs to the methane burden in Central Europe. CH 4 mole fraction and δ 13 C CH4 from the Hungarian tall tower station, Hegyhátsál, and additional data from Mace Head (Ireland) and Zeppelin (Svalbard) are used with back trajectory modeling to identify central European source areas and their seasonal variation between the summer vegetation and winter heating periods. Methane measurements in air masses sampled in the European interior, have significantly higher maxima and seasonal amplitudes than at the Mace Head and Zeppelin European background sites. The mean CH 4 mole fraction value is about 80 ppb higher than the comparable marine background, and values above 2,000 ppb were frequently observed between February 2013 and December 2015. The mean δ 13 C CH4 value −47.5 ± 0.3‰ (2σ) was comparable to values at all three monitoring sites, but specific pollution events were detected at Hegyhátsál. Concentration weighted trajectory modeling, meteorological parameters, stable carbon isotopic composition (δ 13 C CH4 ), and Miller‐Tans analysis show that the main factors influencing CH 4 at the Hegyhátsál, apart from diurnal and seasonal changes in the planetary boundary layer, are emissions from residential heating and industrial CH 4 emissions during the winter.