Category: Model Improvements Completed Studies

  • Investigating Sources of Ammonia Uncertainty in Modeling the Salt lake City PM2.5 Nonattainment Area

    This study will investigate the existing emission inventory of ammonia (NH3) sources and compare modeled NH3 concentrations to those observed during recent field studies in order to identify and correct missing NH3 sources. In addition to improving the inventory, this study will add new NH3 emission pathways to the photochemical model. Principal Investigators: Chris Emery…

  • Wintertime Atmospheric Modeling

    Wintertime meteorological conditions in Utah are difficult to portray using conventional atmospheric-modeling approaches. To improve the accuracy of simulations of pollution along the Wasatch Front and Cache Valley, models need to better simulate the complex meteorological features associated with the cold-air pools that form during winter in the valleys of northern Utah. Specifically, models need…

  • Meteorological Modeling of 3 Wintertime Episodes

    Following the completion of the Winter Modeling Improvements study funded by DAQ with the original legislative research funding, DAQ contracted with the same research group for a targeted modeling project. The purpose of this was to model three past inversion episodes using the model improvements that resulted from the original study. The study was completed…

  • Chemical Mechanisms at Low Temperatures

    Wintertime ozone in the Uinta Basin is unique and requires improvements to the photochemical models used for winter conditions. Current chemical mechanisms within the modeling system assume a summertime temperature of 300 K (80° F) when performing important chemical reactions, far different from the wintertime temperatures in the Basin. In order to properly model the…

  • CAMx Snow Cover Treatment

    Wintertime ozone is a serious air quality issue in the Uinta Basin. The situation is unique and requires improvements to the photochemical models used for winter conditions. High concentrations of wintertime ozone occur over snow-covered surfaces. Snow cover influences wintertime ozone by increasing surface albedo and thus increasing photolysis rates, inhibiting the surface deposition of…

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