2006
DOI: 10.1016/j.atmosenv.2006.01.020
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Comparison of ozone simulations using MM5 and CALMET/MM5 hybrid meteorological fields for the July/August 2000 CCOS episode

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Cited by 32 publications
(11 citation statements)
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“…For these components, the models tend to over-predict the relatively moderate concentrations observed during IOP1 and underpredict the extremely high concentrations observed during IOP3. This behavior could be due in part to limitations of using prognostic meteorological fields in simulating air quality for stagnant periods on domains with complex topography (Hu et al, 2009;Jackson et al, 2006). However, overprediction of PM during IOP1 and under-prediction during IOP3 has also been reported for air quality simulations based on objective-analyses meteorological fields (Ying et al 2008) despite evidence that objective-analyses fields may result in better air quality model performance (Jackson et al 2006;Hu et al 2009).…”
Section: Particle Mass Size Distributionsmentioning
confidence: 93%
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“…For these components, the models tend to over-predict the relatively moderate concentrations observed during IOP1 and underpredict the extremely high concentrations observed during IOP3. This behavior could be due in part to limitations of using prognostic meteorological fields in simulating air quality for stagnant periods on domains with complex topography (Hu et al, 2009;Jackson et al, 2006). However, overprediction of PM during IOP1 and under-prediction during IOP3 has also been reported for air quality simulations based on objective-analyses meteorological fields (Ying et al 2008) despite evidence that objective-analyses fields may result in better air quality model performance (Jackson et al 2006;Hu et al 2009).…”
Section: Particle Mass Size Distributionsmentioning
confidence: 93%
“…This behavior could be due in part to limitations of using prognostic meteorological fields in simulating air quality for stagnant periods on domains with complex topography (Hu et al, 2009;Jackson et al, 2006). However, overprediction of PM during IOP1 and under-prediction during IOP3 has also been reported for air quality simulations based on objective-analyses meteorological fields (Ying et al 2008) despite evidence that objective-analyses fields may result in better air quality model performance (Jackson et al 2006;Hu et al 2009). Kelly et al (2010) reported that concentration peaks in modeled size distributions for inorganic particle components occurred in the adjacent larger diameter bin to the observed peaks when CMAQ's lognormal distributions were mapped to the discrete bins of impactor measurements in Tampa.…”
Section: Particle Mass Size Distributionsmentioning
confidence: 93%
“…Meteorological observations have been acquired at the ground stations of the Osservatorio Geofisico of the University of Modena and Reggio Emilia (Modena, Italy) and of the Regional Environmental Agency (ARPA). Meteorological simulated data comprise of mesoscale vertical wind profiles and mixing height: these data have been provided by ARPA using CALMET model (Deserti et al 2001), which requires input meteorological ground measurements and radio sounding profiles of temperature and wind speed [CALMET is often used to generate meteorological field also for air quality models, even coupled with larger-scale models (Yim et al 2007;Cox et al 2005;Chandrasekar et al 2003;Jackson et al 2006)]. Ground elevation data have been provided by Shuttle Radar Topography Mission through United States Geological Service (USGS), sampled at 3 arc-seconds, while land use-land surface cover dataset is extracted from the European CORINE Land Cover 2000 dataset (European Environment Agency) in raster format with a spatial resolution of 100 9 100 m.…”
Section: Modelling Of the Plume Dispersion In Atmospherementioning
confidence: 99%
“…In this study, CALMET was configured with five domains ( Figure 2) as well as sharp gradients in land surface characteristics that are smaller than the typical resolutions used in MM5 simulations (around 1-4 km [21][22][23][24]). The result of this is that the effects of the terrain and land surface characteristics on the meteorological fields are not always captured in the MM5 simulations.…”
Section: The Calmet Diagnostic Meteorological Modelmentioning
confidence: 99%