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• W2072229602 abstract "Freshwater environments contribute more than 20% of total CH 4 flux to the atmosphere, and the lakes are one of the major natural sources of atmospheric CH 4 , mainly in boreal lakes. So, we present and analyze the temporal and spatial variations of CH 4 VMRs over Lake Baikal, the only freshwater body, the unique large and high latitude lake, based on the retrieved monthly CH 4 data from SCIAMACHY spectra. The result showed that monthly CH 4 concentrations in atmosphere extended between 1744.780ppb and 1818.495ppb. The value in March was a relative higher value, and then increased from April to August. After this growing, the CH 4 concentration decreased to September. But, there was an increased trend in October. Overall, the temporal pattern liked the ocean pattern during the growing season, and was in line with permafrost in other time. Moreover, the spatial distribution of CH 4 VMRs showed that the values were higher in North Lake Baikal, followed by South, Center. The crucial controlling factor for the seasonal variation of CH 4 concentration and spatial difference was both temperature, the amount of organic matter in the sediment and stability of hydrate. This exerted a direct influence on diatom and CH 4 source plus (hydrate). Furthermore, the monthly CH 4 concentrations by air transport were few for the size of basin over Lake Baikal and mountain barriers. So the source over Lake Baikal was itself. Based the average annual mean (8 months) atmospheric CH 4 concentration and the area of the Lake Baikal (31494Km2), the annual CH 4 flux (at all atmospheric altitude levels) was roughly estimated to be 40.03Mg yr (−1) (mean) during the period (March-October, 2003)." @default.
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• W2072229602 date "2010-06-01" @default.
• W2072229602 modified "2023-09-23" @default.
• W2072229602 title "The distribution characteristics of atmospheric methane over Lake Baikal, Siberia by SCIAMACHY remotely sensed data" @default.
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• W2072229602 doi "https://doi.org/10.1109/geoinformatics.2010.5567624" @default.
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