Abstract

This study examined the model-derived and observed ozone production efficiency (OPE = ∆Ox/∆NOz) in one rural location, Pinnacle State Park (PSP) in Addison, New York (NY), and one urban location, Queens College (QC) in Flushing, NY, in New York State (NYS) during photo-chemically productive hours (11 a.m.–4 p.m. Eastern Standard Time (EST)) in summer 2016. Measurement data and model predictions from National Oceanic and Atmospheric Administration National Air Quality Forecast Capability (NOAA NAQFC)—Community Multiscale Air Quality (CMAQ) model versions 4.6 (v4.6) and 5.0.2 (v5.0.2) were used to assess the OPE at both sites. CMAQ-predicted and observed OPEs were often in poor agreement at PSP and in reasonable agreement at QC, with model-predicted and observed OPEs, ranging from approximately 5–11 and 10–13, respectively, at PSP; and 4–7 and 6–8, respectively, at QC. The observed relationship between OPE and oxides of nitrogen (NOx) was studied at PSP to examine where the OPE downturn may have occurred. Summer 2016 observations at PSP did not reveal a distinct OPE downturn, but they did indicate that the OPE at PSP remained high (10 or greater) regardless of the [NOx] level. The observed OPEs at QC were found by using species-specific reactive odd nitrogen (NOy) instruments and an estimated value for nitrogen dioxide (NO2), since observed OPEs determined using non-specific NOx and NOy instruments yielded observed OPE results that (1) varied from approximately 11–25, (2) sometimes had negative [NOz] concentrations, and (3) were inconsistent with CMAQ-predicted OPE. This difference in observed OPEs at QC depending on the suite of instruments used suggests that species-specific NOx and NOy instruments may be needed to obtain reliable urban OPEs.

Highlights

  • Lower tropospheric ozone (O3 ) production occurs due to a sequence of photochemical reactions involving volatile organic compounds (VOCs) in the presence of oxides of nitrogen (NOx = nitric oxide (NO) + nitrogen dioxide (NO2 )) [1]

  • 2016, where the was defined as the slope of the plot of observed ozone production efficiency (OPE) were often in poor agreement at Pinnacle State Park (PSP)

  • This study examined estimated OPE (∆Ox /∆NOz ) at one rural site, PSP, and one urban site, Queens College (QC), in New York State (NYS) from June–September 2016 and August–September 2016, respectively

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Summary

Introduction

Lower tropospheric ozone (O3 ) production occurs due to a sequence of photochemical reactions involving volatile organic compounds (VOCs) in the presence of oxides of nitrogen (NOx = nitric oxide (NO) + nitrogen dioxide (NO2 )) [1]. O3 concentrations ([O3 ]) are controlled through reducing anthropogenic emissions of VOCs, NOx , or both VOCs and NOx [2]. It is important to understand how VOCs and NOx lead to O3 formation [2]. The concept of ozone production efficiency (OPE) helps gain such an understanding. OPE is defined as the number of O3 molecules formed for every molecule of NOx oxidized [3]. The OPE is often an effective metric for scaling regional

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