WRF-Chem simulations in the Amazon region during wet and dry season transitions: evaluation of methane models and wetland inundation maps

V. Beck, C. Gerbig, T. Koch, M. M. Bela, K. M. Longo, S. R. Freitas, J. O. Kaplan, C. Prigent, P. Bergamaschi, M. Heimann
2013 Atmospheric Chemistry and Physics  
<p><strong>Abstract.</strong> The Amazon region, being a large source of methane (CH<sub>4</sub>), contributes significantly to the global annual CH<sub>4</sub> budget. For the first time, a forward and inverse modelling framework on regional scale for the purpose of assessing the CH<sub>4</sub> budget of the Amazon region is implemented. Here, we present forward simulations of CH<sub>4</sub> as part of the forward and inverse modelling framework based on a modified version of the Weather
more » ... f the Weather Research and Forecasting model with chemistry that allows for passive tracer transport of CH<sub>4</sub>, carbon monoxide, and carbon dioxide (WRF-GHG), in combination with two different process-based bottom-up models of CH<sub>4</sub> emissions from anaerobic microbial production in wetlands and additional datasets prescribing CH<sub>4</sub> emissions from other sources such as biomass burning, termites, or other anthropogenic emissions. We compare WRF-GHG simulations on 10 km horizontal resolution to flask and continuous CH<sub>4</sub> observations obtained during two airborne measurement campaigns within the Balanço Atmosférico Regional de Carbono na Amazônia (BARCA) project in November 2008 and May 2009. In addition, three different wetland inundation maps, prescribing the fraction of inundated area per grid cell, are evaluated. Our results indicate that the wetland inundation maps based on remote-sensing data represent the observations best except for the northern part of the Amazon basin and the Manaus area. WRF-GHG was able to represent the observed CH<sub>4</sub> mixing ratios best at days with less convective activity. After adjusting wetland emissions to match the averaged observed mixing ratios of flights with little convective activity, the monthly CH<sub>4</sub> budget for the Amazon basin obtained from four different simulations ranges from 1.5 to 4.8 Tg for November 2008 and from 1.3 to 5.5 Tg for May 2009. This corresponds to an average CH<sub>4</sub> flux of 9–31 mg m<sup>−2</sup> d<sup>−1</sup> for November 2008 and 8–36 mg m<sup>−2</sup> d<sup>−1</sup> for May 2009.</p>
doi:10.5194/acp-13-7961-2013 fatcat:bjhsgrv4d5hjtgslogpw2p6zu4