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Simulations of atmospheric methane for Cape Grim, Tasmania, to constrain southeastern Australian methane emissions

机译:塔斯马尼亚州格里姆角的大气甲烷模拟,以限制澳大利亚东南部的甲烷排放

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摘要

This study uses two climate models and six scenarios of prescribed methane emissions to compare modelled and observed atmospheric methane between 1994 and 2007, for Cape Grim, Australia (40.7° S, 144.7° E). The model simulations follow the TransCom-CH4 protocol and use the Australian Community Climate and Earth System Simulator (ACCESS) and the CSIRO Conformal-Cubic Atmospheric Model (CCAM). Radon is also simulated and used to reduce the impact of transport differences between the models and observations. Comparisons are made for air samples that have traversed the Australian continent. All six emission scenarios give modelled concentrations that are broadly consistent with those observed. There are three notable mismatches, however. Firstly, scenarios that incorporate interannually varying biomass burning emissions produce anomalously high methane concentrations at Cape Grim at times of large fire events in southeastern Australia, most likely due to the fire methane emissions being unrealistically input into the lowest model level. Secondly, scenarios with wetland methane emissions in the austral winter overestimate methane concentrations at Cape Grim during wintertime while scenarios without winter wetland emissions perform better. Finally, all scenarios fail to represent a~methane source in austral spring implied by the observations. It is possible that the timing of wetland emissions in the scenarios is incorrect with recent satellite measurements suggesting an austral spring (September–October–November), rather than winter, maximum for wetland emissions. © Author(s) 2015.
机译:这项研究使用了两种气候模式和六种甲烷的预定排放情景,以比较1994年至2007年澳大利亚格里姆角(40.7°S,144.7°E)的模拟甲烷和观测到的大气甲烷。模型模拟遵循TransCom-CH4协议,并使用澳大利亚共同体气候和地球系统模拟器(ACCESS)和CSIRO保形立方大气模型(CCAM)。还对进行了模拟,并用于减少模型和观测值之间的输运差异的影响。对穿越澳大利亚大陆的空气样本进行了比较。所有六个排放情景都给出了与观察到的浓度基本一致的模拟浓度。但是,存在三个明显的不匹配。首先,在澳大利亚东南部发生大火事件时,结合了年际变化的生物质燃烧排放量的情景会在格里姆角产生异常高的甲烷浓度,这很可能是由于甲烷排放量不切实际地输入了最低模型水平。其次,南方冬季湿地甲烷排放的情景高估了格里姆角冬季的甲烷浓度,而冬季无湿地排放的情景则表现更好。最后,所有的观测结果都不能代表南极春季的甲烷源。情景中的湿地排放时间可能不正确,因为最近的卫星测量表明,湿地排放的最大春季是春季(9月至10月至11月),而不是冬季。 ©作者2015。

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