Abstract

Airborne measurements of volatile organic compounds (VOCs) were performed during CalNex 2010 (California Research at the Nexus of Air Quality and Climate Change) in the Los Angeles (LA) basin in May–June 2010 and during ITCT2k2 (Intercontinental Transport and Chemical Transformation) in May 2002. While CO2 enhancements in the basin were similar between the two years, the ΔCO/ΔCO2 ratio had decreased by about a factor of two. The ΔVOC/ΔCO emission ratios stayed relatively constant between the two years. This indicates that, relative to CO2, VOCs in the LA basin also decreased by about a factor of two since 2002. These data are compared with the results from various previous field campaigns dating back as early as 1960 and from the extensive air quality monitoring system in the LA basin going back to 1980. The results show that the mixing ratios of VOCs and CO have decreased by almost two orders of magnitude during the past five decades at an average annual rate of about 7.5%. Exceptions to this trend are the small alkanes ethane and propane, which have decreased slower due to the use and production of natural gas. A comparison with trends in London, UK shows that, due to stricter regulations at the time, VOC mixing ratios in LA decreased earlier than in London, albeit at a slower rate, such that typical mixing ratios in both cities in 2008 were at about the same level.

Highlights

  • [2] Since the 1950s, the Los Angeles (LA) basin has been well known for its photochemically induced air pollution or urban smog with high ozone levels [Haagen-Smit, 1952; Renzetti, 1956]

  • [4] Volatile organic compounds (VOCs) in the LA basin are mainly emitted by anthropogenic sources with vehicular traffic as the most important source

  • VOCs are oxidized in the atmosphere typically by reactions with the hydroxyl radical (OH) and produce a variety of secondary pollutants such as O3, in the presence of sunlight and nitrogen oxide (NOx), and secondary organic aerosol (SOA)

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Summary

Introduction

[2] Since the 1950s, the Los Angeles (LA) basin has been well known for its photochemically induced air pollution or urban smog with high ozone levels [Haagen-Smit, 1952; Renzetti, 1956]. While the air quality in the LA basin has improved significantly, it is still designated as an ozone non-attainment area. [6] In this paper we describe ambient VOC trends in the LA basin using three different data sources: (1) two NOAA aircraft campaigns in the LA basin: ITCT2k2 (Intercontinental Transport and Chemical Transformation) in 2002 and CalNex (Research at the Nexus of Air Quality and Climate Change) in 2010, (2) historical data sets from field intensives that are available from the literature and (3) data from the CARB monitoring network. Details on the measurement procedures, sampling intervals and data availability for VOCs, CO, ozone, NO2 and organic carbon (OC) that are used in this analysis are publicly available through CARB (CARB, online publication, 2011). We will most often use these maximum values for the trend analysis, but we will use annual averages if necessary for comparisons

VOC Decrease in the LA Basin
VOC Measurements From Field Campaigns in the LA Basin Since 1960
Literature
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