Photochemical grid model estimates of lateral boundary contributions to ozone and particulate matter across the continental United States

被引:23
|
作者
Baker, Kirk R. [1 ]
Emery, Chris [2 ]
Dolwick, Pat [1 ]
Yarwood, Greg [2 ]
机构
[1] US EPA, Res Triangle Pk, NC 27711 USA
[2] Ramboll Environ, Novato, CA 94998 USA
关键词
Boundary contribution; Boundary inflow; Source apportionment; OSAT; RTRAC; PSAT; RELEVANT BACKGROUND OZONE; SOURCE APPORTIONMENT; DRY DEPOSITION; IMPLEMENTATION;
D O I
10.1016/j.atmosenv.2015.10.055
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Multiple approaches to characterize lateral boundary contributions to photochemical model predicted ozone (O-3) and particulate matter less than 2.5 microns in diameter (PM2.5) are available in the Comprehensive Air quality Model with extensions (CAMx). Here, three approaches are used for O-3: (1) a comprehensive source apportionment scheme for chemical boundary conditions and emissions (OSAT), (2) chemically reactive tracers (RTRAC), and (3) chemically inert tracers. Two approaches are used for PM2.5: (1) particulate source apportionment (PSAT) and (2) chemically inert tracers. The inert tracer approach resulted in higher O-3 lateral boundary contribution estimates because the method does not account for any O-3 destruction reactions. OSAT and RTRAC estimate generally similar monthly average contributions during the warmer months although RTRAC estimates higher urban area contribution during the cold months because this RTRAC implementation did not treat O-3 titration by NO. Accurate representation of lateral boundary O-3 impacts must include appropriate accounting for O-3 destruction reactions. OSAT and RTRAC were configured to estimate the contribution to modeled O-3 from each of the four lateral faces of the model domain. RTRAC was configured to further stratify the western and northern boundaries by groups of vertical layers. The RTRAC approach showed that the largest O-3 contributions to the continental U.S. are from the mid-troposphere, with less contribution from the upper troposphere/lower stratosphere. Inert tracers compared more closely to reactive tracers on average for PM2.5 compared to O-3. This close agreement for PM2.5 indicates most of the lateral boundary contribution is from PM2.5 rather than precursor inflow. A strong relationship exists between model predicted PM2.5 boundary contribution and model overestimates of nitrate and organic carbon at IMPROVE monitor locations suggesting global model estimates of these species were overestimated at some places and times. Published by Elsevier Ltd.
引用
收藏
页码:49 / 62
页数:14
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