Wang Siyuan, Apel Eric C, Hornbrook Rebecca S, Hills Alan, Emmons Louisa K, Tilmes Simone, Lamarque Jean-François, Jimenez Jose L, Campuzano-Jost Pedro, Nault Benjamin A, Crounse John D, Wennberg Paul O, Ryerson Thomas B, Thompson Chelsea R, Peischl Jeff, Moore Fred, Nance David, Hall Brad, Elkins James, Tanner David, Gregory Huey L, Hall Samuel R, Ullmann Kirk, Orlando John J, Tyndall Geoff S, Flocke Frank M, Ray Eric, Hanisco Thomas F, Wolfe Glenn M, St Clair Jason, Commane Róisín, Daube Bruce, Barletta Barbara, Blake Donald R, Weinzierl Bernadett, Dollner Maximilian, Conley Andrew, Vitt Francis, Wofsy Steven C, Riemer Daniel D
Advanced Study Program (ASP), National Center for Atmospheric Research, Boulder CO, 80301.
Atmospheric Chemistry Observations and Modeling, National Center for Atmospheric Research, Boulder CO, 80301.
Geophys Res Lett. 2019 May 28;46(10):5601-5613. doi: 10.1029/2019GL082034. Epub 2019 Apr 29.
We report airborne measurements of acetaldehyde (CHCHO) during the first and second deployments of the National Aeronautics and Space Administration (NASA) Atmospheric Tomography Mission (ATom). The budget of CHCHO is examined using the Community Atmospheric Model with chemistry (CAM-chem), with a newly-developed online air-sea exchange module. The upper limit of the global ocean net emission of CHCHO is estimated to be 34 Tg a (42 Tg a if considering bubble-mediated transfer), and the ocean impacts on tropospheric CHCHO are mostly confined to the marine boundary layer. Our analysis suggests that there is an unaccounted CHCHO source in the remote troposphere and that organic aerosols can only provide a fraction of this missing source. We propose that peroxyacetic acid (PAA) is an ideal indicator of the rapid CHCHO production in the remote troposphere. The higher-than-expected CHCHO measurements represent a missing sink of hydroxyl radicals (and halogen radical) in current chemistry-climate models.
我们报告了美国国家航空航天局(NASA)大气层析任务(ATom)首次和第二次部署期间对乙醛(CH₃CHO)的空中测量结果。使用具有化学功能的社区大气模型(CAM-chem)以及新开发的在线海气交换模块对CH₃CHO的收支情况进行了研究。CH₃CHO全球海洋净排放的上限估计为34 Tg a(若考虑气泡介导的传输则为42 Tg a),海洋对对流层CH₃CHO的影响主要局限于海洋边界层。我们的分析表明,在偏远对流层存在一个未被计入的CH₃CHO源,且有机气溶胶只能提供该缺失源的一部分。我们提出过氧乙酸(PAA)是偏远对流层中CH₃CHO快速生成的理想指标。高于预期的CH₃CHO测量结果表明当前化学气候模型中存在羟基自由基(和卤素自由基)的缺失汇。