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Methane airborne measurements and comparison to global models during BARCA
Author(s) -
Beck Veronika,
Chen Huilin,
Gerbig Christoph,
Bergamaschi Peter,
Bruhwiler Lori,
Houweling Sander,
Röckmann Thomas,
Kolle Olaf,
Steinbach Julia,
Koch Thomas,
Sapart Célia J.,
Veen Carina,
Frankenberg Christian,
Andreae Meinrat O.,
Artaxo Paulo,
Longo Karla M.,
Wofsy Steven C.
Publication year - 2012
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2011jd017345
Subject(s) - amazon rainforest , sciamachy , environmental science , atmospheric sciences , amazon basin , structural basin , climatology , troposphere , geology , ecology , biology , paleontology
Tropical regions, especially the Amazon region, account for large emissions of methane (CH 4 ). Here, we present CH 4 observations from two airborne campaigns conducted within the BARCA (Balanço Atmosférico Regional de Carbono na Amazônia) project in the Amazon basin in November 2008 (end of the dry season) and May 2009 (end of the wet season). We performed continuous measurements of CH 4 onboard an aircraft for the first time in the Amazon region, covering the whole Amazon basin with over 150 vertical profiles between altitudes of 500 m and 4000 m. The observations support the finding of previous ground‐based, airborne, and satellite measurements that the Amazon basin is a large source of atmospheric CH 4 . Isotope analysis verified that the majority of emissions can be attributed to CH 4 emissions from wetlands, while urban CH 4 emissions could be also traced back to biogenic origin. A comparison of five TM5 based global CH 4 inversions with the observations clearly indicates that the inversions using SCIAMACHY observations represent the BARCA observations best. The calculated CH 4 flux estimate obtained from the mismatch between observations and TM5‐modeled CH 4 fields ranges from 36 to 43 mg m −2 d −1 for the Amazon lowland region.

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