Impacts of transported background pollutants on summertime western US air quality: Model evaluation, sensitivity analysis and data assimilation
The impacts of transported background (TBG) pollutants on western US ozone (Oâ©â) distributions in summer 2008 are studied using the multi-scale Sulfur Transport and dEposition Modeling system. Forward sensitivity simulations show that TBG contributes Ë30â35 ppb to the surface Monthly mean Daily maximum 8-h Average Oâ (MDA8) over Pacific Southwest (US Environmental Protection Agency (EPA) Region 9, including California, Nevada and Arizona) and Pacific Northwest (EPA Region 10, including Washington, Oregon and Idaho), and ~10â17 ppm-h to the secondary standard metric "W126 monthly index" over EPA Region 9 and Ë3-4 ppm-h over Region 10. The strongest TBG impacts on W126 occur over the grass/shrub-covered regions. Among TBG pollutants, Oâ is the major contributor to surface Oâ, while peroxyacetyl nitrate is the most important Oâ precursor species. W126 shows larger responses than MDA8 to perturbations in TBG and stronger non-linearity to the magnitude of perturbations. The TBG impacts on both metrics overall negatively correlate to model vertical resolution and positively correlate to the horizontal resolution. The mechanisms that determine TBG contributions and their variation are analyzed using trajectories and the receptor-based adjoint sensitivity analysis, which demonstrate the connection between the surface Oâ and Oâ aloft (at Ë1â4 km) 1â2 days earlier. The probabilities of airmasses originating from Mt. Bachelor (2.7 km) and 2.5 km above Trinidad Head (THD) entraining into the boundary layer reach daily maxima of 66% and 34% at Ë03:00 p.m. Pacific Daylight Time (PDT), respectively, and stay above 50% during 09:00 a.m.-04:00 p.m. PDT for those originating 1.5 km above California's South Coast. Assimilation of the surface in-situ measurements significantly reduced the errors in the modeled surface Oâ during a long-range transport episode by ~5 ppb on average (up to ~17 ppb) and increased the estimated TBG contributions by Ë3 ppb. Available Oâ vertical profiles from Tropospheric Emission Spectrometer (TES), Ozone Monitoring Instrument (OMI) and THD sonde identified this transport event, but assimilation of these observations in this case did not efficiently improve the Oâ distributions except near the sampling locations, due to their limited spatiotemporal resolution and/or possible uncertainties.
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https://n2t.org/ark:/85065/d7vt1sx5
eng
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publication
2016-01-01T00:00:00Z
publication
2013-01-14T00:00:00Z
Copyright Author(s) 2013. This work is distributed under the Creative Commons Attribution 3.0 License.
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