Abstract
Abstract. Atmospheric non-methane hydrocarbons (NMHCs) have been extensively studied around the globe due to their importance to atmospheric chemistry and their utility in emission source and chemical sink identification. This study reports on shipborne NMHC measurements made around the Arabian Peninsula during the AQABA (Air Quality and climate change in the Arabian BAsin) ship campaign. The ship traversed the Mediterranean Sea, the Suez Canal, the Red Sea, the northern Indian Ocean, and the Arabian Gulf, before returning by the same route. The Middle East is one of the largest producers of oil and gas (O&G), yet it is among the least studied. Atmospheric mixing ratios of C2–C8 hydrocarbons ranged from a few ppt in unpolluted regions (Arabian Sea) to several ppb over the Suez Canal and Arabian Gulf (also known as the Persian Gulf), where a maximum of 166.5 ppb of alkanes was detected. The ratio between i-pentane and n-pentane was found to be 0.93±0.03 ppb ppb−1 over the Arabian Gulf, which is indicative of widespread O&G activities, while it was 1.71±0.06 ppb ppb−1 in the Suez Canal, which is a characteristic signature of ship emissions. We provide evidence that international shipping contributes to ambient C3–C8 hydrocarbon concentrations but not to ethane, which was not detected in marine traffic exhausts. NMHC relationships with propane differentiated between alkane-rich associated gas and methane-rich non-associated gas through a characteristic enrichment of ethane over propane atmospheric mixing ratios. Utilizing the variability–lifetime relationship, we show that atmospheric chemistry governs the variability of the alkanes only weakly in the source-dominated areas of the Arabian Gulf (bAG=0.16) and along the northern part of the Red Sea (bRSN=0.22), but stronger dependencies are found in unpolluted regions such as the Gulf of Aden (bGA=0.58) and the Mediterranean Sea (bMS=0.48). NMHC oxidative pair analysis indicated that OH chemistry dominates the oxidation of hydrocarbons in the region, but along the Red Sea and the Arabian Gulf the NMHC ratios occasionally provided evidence of chlorine radical chemistry. These results demonstrate the utility of NMHCs as source/sink identification tracers and provide an overview of NMHCs around the Arabian Peninsula.
Highlights
Anthropogenic activities are estimated to be responsible for the release of 169 Mt of non-methane hydrocarbons (NMHCs) into the atmosphere each year (Huang et al, 2017)
To investigate regional variations in atmospheric chemistry and abundance of NMHCs, the track was subdivided into eight regions: Mediterranean Sea (MS), Suez Canal (SC; including Great Bitter Lake and the Gulf of Suez), Red Sea North (RSN), Red Sea South (RSS), Gulf of Aden (GA), Arabian Sea (AS), Gulf of Oman (GO), and Arabian Gulf (AG)
The enhancement ratio of 1.71 ppb ppb−1 that was observed over the Suez Canal and Arabian Gulf points towards a characteristic value for ship emissions, found to be similar to our ship exhaust emission ratios and identical to the ratio slope observed in the Texas ship channel (Blake et al, 2014)
Summary
Anthropogenic activities are estimated to be responsible for the release of 169 Mt of non-methane hydrocarbons (NMHCs) into the atmosphere each year (Huang et al, 2017). NMHCs are important in atmospheric chemistry as precursors of tropospheric ozone and particle formation, both of which have negative impacts on air quality, human health, and climate (Lelieveld et al, 2015; Seinfeld and Pandis, 2016; EEA, 2018). Ozone production is known to be efficient in Oil and Gas (O&G) basins (Edwards et al, 2014; Wei et al, 2014; Field et al, 2015) when the high NMHC concentrations react with the hydroxyl radical (OH) under low nitrogen oxide (NOx) regimes leading to carbonyls which photolyse to recycle the OH oxidant (Rohrer et al, 2014). E. Bourtsoukidis et al.: NMHCs around the Arabian Peninsula evated ozone concentrations (Parrish et al, 2004; Lelieveld et al, 2009; Perring et al, 2013; Helmig et al, 2014)
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