Please use this identifier to cite or link to this item: https://apo.ansto.gov.au/dspace/handle/10238/7521
Title: Simulations of atmospheric methane for Cape Grim, Tasmania, to constrain southeastern Australian methane emissions
Authors: Loh, ZH
Law, RM
Haynes, KD
Krummel, PB
Steele, LP
Fraser, PJ
Chambers, SD
Williams, AG
Keywords: Climate models
Emissions trading
Atmospheres
Australia
Methane
Wetlands
Issue Date: 13-Jan-2014
Publisher: Copernicus Publications
Citation: Loh, Z. M., Law, R. M., Haynes, K. D., Krummel, P. B., Steele, L. P., Fraser, P. J., Chambers, D. D., Williams, A. G. (2014). Simulations of atmospheric methane for Cape Grim, Tasmania, to constrain South East Australian methane emissions. Atmospheric Chemistry and Physics Discussions, 14, 21189-21221. doi:10.5194/acp-15-305-2015
Abstract: 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.
Gov't Doc #: 7103
URI: http://dx.doi.org/10.5194/acp-15-305-2015
http://apo.ansto.gov.au/dspace/handle/10238/7521
ISSN: 1680-7316
Appears in Collections:Journal Articles

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