Patrick Campbell

and 4 more

Parameterization of subgrid-scale variability of land cover characterization (LCC) is an active area of research, and can improve model performance compared to the dominant (i.e., most abundant tile) approach. The “Noah” land surface model implementation in the global Model for Predictions Across Scales-Atmosphere (MPAS-A), however, only uses the dominant LCC approach that leads to oversimplification in regions of highly heterogeneous LCC (e.g., urban/suburban settings). Thus, in this work we implement a subgrid tiled approach as an option in MPAS-A, version 6.0, and assess the impacts of tiled LCC on meteorological predictions for two gradually refining meshes (92-25 and 46-12 km) focused on the conterminous U.S for January and July 2016. Compared to the dominant approach, results show that using the tiled LCC leads to pronounced global changes in 2-m temperature (July global average change ~ -0.4 K), 2-m moisture, and 10-m wind speed for the 92-25 km mesh. The tiled LCC reduces mean biases in 2-m temperature (July U.S. average bias reduction ~ factor of 4) and specific humidity in the central and western U.S. for the 92-25 km mesh, improves the agreement of vertical profiles (e.g., temperature, humidity, and wind speed) with observed radiosondes, and there is a general decrease in error for precipitation in the U.S.; however, there is increased bias and error for incoming solar radiation at the surface. The inclusion of subgrid LCC has implications for reducing systematic warm biases found in numerical weather prediction models.

Wyat Appel

and 4 more

The Community Multiscale Air Quality (CMAQ) model is a state-of-the-science chemical transport model (CTM) capable of simulating the emission, transport and fate of numerous air pollutants. Similarly, the Weather Research and Forecasting (WRF) model is a state-of-the-science meteorological model capable of simulating meteorology at many scales (e.g. global to urban). The coupled WRF-CMAQ system integrates these two models in a “two-way” configuration which allows feedback effects between the chemical (e.g. aerosols) and physical (e.g. solar radiation) states of the atmosphere and more frequent communication between the CTM and meteorological model than is typically done in uncoupled WRF-CMAQ simulations. In this study we apply the various cumulus parameterization (CP) options available in WRF at horizontal grid spacings ranging from regional scale (i.e. 12-km) to urban scale (i.e. 4 and 1 km), focused on the July 2011 DISCOVER-AQ campaign that took place over the Baltimore-Washington D.C region. Of particular interest is the evaluation of the WRF simulated clouds, as analysis of previous WRF-CMAQ simulations using a “standard” 12-km configuration for the model suggest that WRF has difficulty predicting clouds (particularly fair-weather clouds), with decreasing skill at finer horizontal grid spacings. Here we will examine the impact that the WRF CP options have on cloud predictions, using available satellite data to evaluate model the performance. We then examine how changes in the WRF simulated clouds affect CMAQ predictions of ozone and PM2.5 at the various scales.