2007
DOI: 10.1029/2006jd007722
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Chemical data assimilation estimates of continental U.S. ozone and nitrogen budgets during the Intercontinental Chemical Transport Experiment–North America

Abstract: Global ozone analyses, based on assimilation of stratospheric profile and ozone column measurements, and NOy predictions from the Real‐time Air Quality Modeling System (RAQMS) are used to estimate the ozone and NOy budget over the continental United States during the July–August 2004 Intercontinental Chemical Transport Experiment–North America (INTEX‐A). Comparison with aircraft, satellite, surface, and ozonesonde measurements collected during INTEX‐A show that RAQMS captures the main features of the global an… Show more

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Cited by 110 publications
(128 citation statements)
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References 68 publications
(102 reference statements)
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“…To compare the WRF-Chem forecasts with measurements, background CO mixing ratios need to be included. Time-varying background CO mixing ratios in the Sacramento region were estimated by taking the difference between two regional-scale simulations from the coupled North American Mesoscale (NAM) -Community Multiscale Air Quality (CMAQ) modeling system (Otte et al, 2005): one in which the boundary conditions were obtained from the Real-time Air Quality Modeling System (RAQMS) (Pierce et al, 2007) and one which used fixed boundary conditions. These NAM-CMAQ simulations were run using a parallel version of the Operational NAM-CMAQ that was being tested during the Research at the Nexus of Air Quality and Climate Change experiment conducted in California called CalNex (Cooper et al, 2011; http://www.esrl.noaa.gov/csd/calnex/).…”
Section: Operational Forecastingmentioning
confidence: 99%
“…To compare the WRF-Chem forecasts with measurements, background CO mixing ratios need to be included. Time-varying background CO mixing ratios in the Sacramento region were estimated by taking the difference between two regional-scale simulations from the coupled North American Mesoscale (NAM) -Community Multiscale Air Quality (CMAQ) modeling system (Otte et al, 2005): one in which the boundary conditions were obtained from the Real-time Air Quality Modeling System (RAQMS) (Pierce et al, 2007) and one which used fixed boundary conditions. These NAM-CMAQ simulations were run using a parallel version of the Operational NAM-CMAQ that was being tested during the Research at the Nexus of Air Quality and Climate Change experiment conducted in California called CalNex (Cooper et al, 2011; http://www.esrl.noaa.gov/csd/calnex/).…”
Section: Operational Forecastingmentioning
confidence: 99%
“…BEIS2 biogenic emissions were employed in this study. The RAQMS global model has it own emissions [Pierce et al, 2007], which are mainly based on the EDGAR inventory [Olivier et al, 1996]. An interface component, PREMAQ, which facilitates the transformation of NAM-derived meteorological fields to conform to the CMAQ grid structure, coordinate system, and input data format, has been developed [Otte et al, 2005].…”
Section: A4 University Of Iowa Stem-2k3 Modelmentioning
confidence: 99%
“…[70] STEM-2K3 used time-varying lateral and top boundary conditions provided by RAQMS global chemical transport model forecasts [Pierce et al, 2007] with 2-degree horizontal resolution, and updates every 6 h. During this experiment, the STEM-2K3 used the EPA NEI-2001 emission inventory (compiled by Jeffrey M. Vukovich, Baron AMS, Inc.), and is compatible with the inventory developed for the BAMS MAQSIP-RT 15-km horizontal resolution model described above. This includes the CEMS-based point emissions for NO x .…”
Section: A4 University Of Iowa Stem-2k3 Modelmentioning
confidence: 99%
“…Ozonesonde data have recently been used to evaluate models (Mao et al, 2006;Chai et al, 2007;Pierce et al, 2007;Tarasick et al, 2007;Yu et al, 2007). Mena-Carrasco et al (2007) compared simulated O 3 using their regional air quality model STEM with NASA DC-8 and NOAA WP-3 airborne measurements during International Consortium for Atmospheric Research on Transport and Transformation (ICARTT) 2004 and found a strong positive surface level bias and a negative upper tropospheric bias.…”
Section: Introductionmentioning
confidence: 99%