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A Measurement‐Model Fusion Approach for Improved Wet Deposition Maps and Trends

Air quality models provide spatial fields of wet deposition (WD) and dry deposition 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 inpu...

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Autores principales: Zhang, Yuqiang, Foley, Kristen M., Schwede, Donna B., Bash, Jesse O., Pinto, Joseph P., Dennis, Robin L.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: John Wiley and Sons Inc. 2019
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6559167/
https://www.ncbi.nlm.nih.gov/pubmed/31218153
http://dx.doi.org/10.1029/2018JD029051
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author Zhang, Yuqiang
Foley, Kristen M.
Schwede, Donna B.
Bash, Jesse O.
Pinto, Joseph P.
Dennis, Robin L.
author_facet Zhang, Yuqiang
Foley, Kristen M.
Schwede, Donna B.
Bash, Jesse O.
Pinto, Joseph P.
Dennis, Robin L.
author_sort Zhang, Yuqiang
collection PubMed
description Air quality models provide spatial fields of wet deposition (WD) and dry deposition 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 model output over the contiguous United States using observation‐based gridded precipitation data generated by the Parameter‐elevation Regressions on Independent Slopes Model and WD observations at the National Atmospheric Deposition Program National Trends Network sites. A cross‐validation analysis shows that the adjusted annual accumulated WD for NO(3) (−), NH(4) (+), and SO(4) (2−) 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 contiguous United States. Consistent with previous trend analyses, WD NO(3) (−) and SO(4) (2−) are shown to decrease during this period in the eastern half of the United States, particularly in the Northeast, while remaining nearly constant in the West. Trends in WD of NH(4) (+) 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.
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spelling pubmed-65591672019-06-17 A Measurement‐Model Fusion Approach for Improved Wet Deposition Maps and Trends Zhang, Yuqiang Foley, Kristen M. Schwede, Donna B. Bash, Jesse O. Pinto, Joseph P. Dennis, Robin L. J Geophys Res Atmos Research Articles Air quality models provide spatial fields of wet deposition (WD) and dry deposition 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 model output over the contiguous United States using observation‐based gridded precipitation data generated by the Parameter‐elevation Regressions on Independent Slopes Model and WD observations at the National Atmospheric Deposition Program National Trends Network sites. A cross‐validation analysis shows that the adjusted annual accumulated WD for NO(3) (−), NH(4) (+), and SO(4) (2−) 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 contiguous United States. Consistent with previous trend analyses, WD NO(3) (−) and SO(4) (2−) are shown to decrease during this period in the eastern half of the United States, particularly in the Northeast, while remaining nearly constant in the West. Trends in WD of NH(4) (+) 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. John Wiley and Sons Inc. 2019-04-08 2019-04-16 /pmc/articles/PMC6559167/ /pubmed/31218153 http://dx.doi.org/10.1029/2018JD029051 Text en ©2019. The Authors. This is an open access article under the terms of the http://creativecommons.org/licenses/by-nc-nd/4.0/ License, which permits use and distribution in any medium, provided the original work is properly cited, the use is non‐commercial and no modifications or adaptations are made.
spellingShingle Research Articles
Zhang, Yuqiang
Foley, Kristen M.
Schwede, Donna B.
Bash, Jesse O.
Pinto, Joseph P.
Dennis, Robin L.
A Measurement‐Model Fusion Approach for Improved Wet Deposition Maps and Trends
title A Measurement‐Model Fusion Approach for Improved Wet Deposition Maps and Trends
title_full A Measurement‐Model Fusion Approach for Improved Wet Deposition Maps and Trends
title_fullStr A Measurement‐Model Fusion Approach for Improved Wet Deposition Maps and Trends
title_full_unstemmed A Measurement‐Model Fusion Approach for Improved Wet Deposition Maps and Trends
title_short A Measurement‐Model Fusion Approach for Improved Wet Deposition Maps and Trends
title_sort measurement‐model fusion approach for improved wet deposition maps and trends
topic Research Articles
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6559167/
https://www.ncbi.nlm.nih.gov/pubmed/31218153
http://dx.doi.org/10.1029/2018JD029051
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