Seasonal and Diurnal Variability of Monoterpenes in the Eastern Mediterranean Atmosphere

Author:

Tzitzikalaki Evangelia1ORCID,Kalivitis Nikos1,Kouvarakis Giorgos1,Mihalopoulos Nikos12ORCID,Kanakidou Maria134ORCID

Affiliation:

1. Environmental Chemical Processes Laboratory, Department of Chemistry, University of Crete, Voutes Campus, P.O. Box 2208, 70013 Heraklion, Greece

2. Institute of Environmental Research & Sustainable Development, National Observatory of Athens, 15236 Palea Penteli, Greece

3. Laboratory for Modeling and Observations of the Earth System (LAMOS), Institute of Environmental Physics (IUP), University of Bremen, 28359 Bremen, Germany

4. Center of Studies on Air quality and Climate Change (C-STACC), ICE-HT, FORTH, 26504 Patras, Greece

Abstract

Monoterpenes significantly affect air quality and climate as they participate in tropospheric ozone formation, new particle formation (NPF), and growth through their oxidation products. Vegetation is responsible for most biogenic volatile organic compound (BVOC) emissions released into the atmosphere, yet the contribution of shrub and regional transport to the ambient monoterpene mixing ratios is not sufficiently documented. In this study, we present one-year systematic observations of monoterpenes in the Eastern Mediterranean at a remote coastal site, affected mainly by the typical phrygana vegetation found on the Island of Crete in Greece. A total of 345 air samples were collected in absorption tubes and analyzed by a GC-FID system during three intensive campaigns (in spring 2014, summer 2014, and spring 2015) in addition to the systematic collection of one diurnal cycle per week from October 2014 to April 2015. Limonene, α-pinene and 1,8-cineol have been detected. The mixing ratios of α-pinene during spring and summer show a cycle that is typical for biogenic compounds, with high levels during the night and early morning, followed by an abrupt decrease around midday, which results from the strong photochemical depletion of this compound. Limonene was the most abundant monoterpene, with average mixing ratios of 36.3 ± 66 ppt. The highest mixing ratios were observed during autumn and spring, with a maximum mixing ratio in the early afternoon. The spring and autumn maxima could be attributed to the seasonal behavior of vegetation growth at Finokalia. The green period starts in late autumn when phrygana vegetation grows because of the rainfall; the temperature is still high at this time, as Finokalia is located in the southeast part of Europe. Statistical analyses of the observations showed that limonene and α-pinene have different sources, and none of the studied monoterpenes is correlated with the anthropogenic sources. Finally, the seasonality of the new particle formation (NPF) events and monoterpene mixing ratios show similarities, with a maximum occurring in spring, indicating that monoterpenes may contribute to the production of new particles.

Funder

PANhellenic infrastructure for Atmospheric Composition and climatE change

Competitiveness, Entrepreneurship and Innovation

European Regional Development Fund) and the HORIZON project Edu4Climate

Publisher

MDPI AG

Subject

Atmospheric Science,Environmental Science (miscellaneous)

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