Non-methane hydrocarbon (C<sub>2</sub>–C<sub>8</sub>) sources and sinks around the Arabian Peninsula

<p>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 Penin...

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Bibliographic Details
Main Authors: E. Bourtsoukidis, L. Ernle, J. N. Crowley, J. Lelieveld, J.-D. Paris, A. Pozzer, D. Walter, J. Williams
Format: Article
Language:English
Published: Copernicus Publications 2019-05-01
Series:Atmospheric Chemistry and Physics
Online Access:https://www.atmos-chem-phys.net/19/7209/2019/acp-19-7209-2019.pdf
Description
Summary:<p>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&amp;G), yet it is among the least studied. Atmospheric mixing ratios of <span class="inline-formula">C<sub>2</sub></span>–<span class="inline-formula">C<sub>8</sub></span> 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&thinsp;ppb of alkanes was detected. The ratio between <span class="inline-formula"><i>i</i></span>-pentane and <span class="inline-formula"><i>n</i></span>-pentane was found to be <span class="inline-formula">0.93±0.03</span>&thinsp;ppb&thinsp;ppb<span class="inline-formula"><sup>−1</sup></span> over the Arabian Gulf, which is indicative of widespread O&amp;G activities, while it was <span class="inline-formula">1.71±0.06</span>&thinsp;ppb&thinsp;ppb<span class="inline-formula"><sup>−1</sup></span> in the Suez Canal, which is a characteristic signature of ship emissions. We provide evidence that international shipping contributes to ambient <span class="inline-formula">C<sub>3</sub></span>–<span class="inline-formula">C<sub>8</sub></span> 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 (<span class="inline-formula"><i>b</i><sub>AG</sub>=0.16</span>) and along the northern part of the Red Sea (<span class="inline-formula"><i>b</i><sub>RSN</sub>=0.22</span>), but stronger dependencies are found in unpolluted regions such as the Gulf of Aden (<span class="inline-formula"><i>b</i><sub>GA</sub>=0.58</span>) and the Mediterranean Sea (<span class="inline-formula"><i>b</i><sub>MS</sub>=0.48</span>). 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.</p>
ISSN:1680-7316
1680-7324