Publication Date:
2019
Description:
Abstract
Air quality models provide spatial fields of wet deposition (WD) and dry deposition (DD) that explicitly account for the transport and transformation of emissions from thousands of sources. However, many sources of uncertainty in the air quality model including errors in emissions and meteorological inputs (particularly precipitation) and incomplete descriptions of the chemical and physical processes governing deposition, can lead to bias and error in the simulation of WD. We present an approach to bias‐correct Community Multiscale Air Quality (CMAQ) model output over the contiguous United States using observation‐based gridded precipitation data generated by the Parameter‐elevation Regressions on Independent Slopes Model (PRISM), and WD observations at the National Atmospheric Deposition Program National Trends Network (NADP/NTN) sites. A cross‐validation analysis shows that the adjusted annual accumulated WD for NO3‐, NH4+, and SO42‐ from 2002 to 2012 has less bias and higher correlation with observed values than the base model output without adjustment. Temporal trends in observed WD are captured well by the adjusted model simulations across the entire CONUS. Consistent with previous trend analyses, WD NO3‐ and SO42‐ are shown to decrease during this period in the eastern half of the U.S., particularly in the Northeast, while remaining nearly constant in the West. Trends in WD of NH4+ are more spatially and temporally heterogeneous, with some positive trends in the Great Plains and Central Valley of CA and slightly negative trends in the South.
Print ISSN:
2169-897X
Electronic ISSN:
2169-8996
Topics:
Geosciences
,
Physics
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