Abstract
Abstract. The Weather Research and Forecasting model with Chemistry (WRF/Chem) v3.6.1 with the Carbon Bond 2005 (CB05) gas-phase mechanism is evaluated for its first decadal application during 2001–2010 using the Representative Concentration Pathway 8.5 (RCP 8.5) emissions to assess its capability and appropriateness for long-term climatological simulations. The initial and boundary conditions are downscaled from the modified Community Earth System Model/Community Atmosphere Model (CESM/CAM5) v1.2.2. The meteorological initial and boundary conditions are bias-corrected using the National Center for Environmental Protection's Final (FNL) Operational Global Analysis data. Climatological evaluations are carried out for meteorological, chemical, and aerosol–cloud–radiation variables against data from surface networks and satellite retrievals. The model performs very well for the 2 m temperature (T2) for the 10-year period, with only a small cold bias of −0.3 °C. Biases in other meteorological variables including relative humidity at 2 m, wind speed at 10 m, and precipitation tend to be site- and season-specific; however, with the exception of T2, consistent annual biases exist for most of the years from 2001 to 2010. Ozone mixing ratios are slightly overpredicted at both urban and rural locations with a normalized mean bias (NMB) of 9.7 % but underpredicted at rural locations with an NMB of −8.8 %. PM2.5 concentrations are moderately overpredicted with an NMB of 23.3 % at rural sites but slightly underpredicted with an NMB of −10.8 % at urban/suburban sites. In general, the model performs relatively well for chemical and meteorological variables, and not as well for aerosol–cloud–radiation variables. Cloud-aerosol variables including aerosol optical depth, cloud water path, cloud optical thickness, and cloud droplet number concentration are generally underpredicted on average across the continental US. Overpredictions of several cloud variables over the eastern US result in underpredictions of radiation variables (such as net shortwave radiation – GSW – with a mean bias – MB – of −5.7 W m−2) and overpredictions of shortwave and longwave cloud forcing (MBs of ∼ 7 to 8 W m−2), which are important climate variables. While the current performance is deemed to be acceptable, improvements to the bias-correction method for CESM downscaling and the model parameterizations of cloud dynamics and thermodynamics, as well as aerosol–cloud interactions, can potentially improve model performance for long-term climate simulations.
Highlights
Regional atmospheric models have been developed and applied for high-resolution climate, meteorology, and air quality modeling in the past few decades
Yahya et al.: Decadal evaluation of regional climate and air quality gional climate models such as REMO-HAM (Petikäinen et al, 2012), the regional modeling system known as Providing Regional Climates for Impacts Studies (PRECIS) (Jones et al, 2004; Fan et al, 2014), and a number of European models described in Jacob et al (2007), as well as regional CTMs such as the Community Multiscale Air Quality Model (CMAQ) (Penrod et al, 2014; Xing et al, 2015)
While Grell 3-D ensemble cumulus parameterization contributes in part to the overpredictions of precipitation, most overpredictions occur at high thresholds as shown in Fig. 3d, and they are attributed to possible errors in the Morrison two-moment scheme because the overpredictions of non-convective precipitation dominate the overpredictions of total precipitation
Summary
Regional atmospheric models have been developed and applied for high-resolution climate, meteorology, and air quality modeling in the past few decades. WRF/Chem is used to simulate the “current” climate scenario for 10 years from 2001 to 2010 using the RCP 8.5 emissions and boundary conditions from an updated version of CESM with advanced chemistry and aerosol treatments over the continental US (CONUS) (He and Zhang, 2014; Glotfelty et al, 2016), with a focus on air-quality and climate interactions. Both CESM and WRF/Chem include similar gas-phase chemistry and aerosol treatments. This study assesses whether the RCP 8.5 emissions for the 10-year period are robust enough to produce satisfactory performance against observations with WRF/Chem
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