Significant spatial gradients in new particle formation frequency in Greece during summer

Author:

Aktypis AndreasORCID,Kaltsonoudis ChristosORCID,Patoulias David,Kalkavouras Panayiotis,Matrali Angeliki,Vasilakopoulou Christina N.,Kostenidou Evangelia,Florou Kalliopi,Kalivitis NikosORCID,Bougiatioti Aikaterini,Eleftheriadis KonstantinosORCID,Vratolis Stergios,Gini Maria I.,Kouras AthanasiosORCID,Samara Constantini,Lazaridis Mihalis,Chatoutsidou Sofia-Eirini,Mihalopoulos Nikolaos,Pandis Spyros N.

Abstract

Abstract. Extensive continuous particle number size distribution measurements took place during two summers (2020 and 2021) at 11 sites in Greece for the investigation of the frequency and the spatial extent of new particle formation (NPF). The study area is characterized by high solar intensity and fast photochemistry and has moderate to low fine particulate matter levels during the summer. The average PM2.5 levels were relatively uniform across the examined sites. The NPF frequency during summer varied from close to zero in the southwestern parts of Greece to more than 60 % in the northern, central, and eastern regions. The mean particle growth rate for each station varied between 3.4 and 8 nm h−1, with an average rate of 5.7 nm h−1. At most of the sites there was no statistical difference in the condensation sink between NPF event and non-event days, while lower relative humidity was observed during the events. The high-NPF-frequency sites in the north and northeast were in close proximity to both coal-fired power plants (high emissions of SO2) and agricultural areas with some of the highest ammonia emissions in the country. The southern and western parts of Greece, where NPF was infrequent, were characterized by low ammonia emissions, while moderate levels of sulfuric acid were estimated (107 molec. cm−3) in the west. Although the emissions of biogenic volatile organic compounds were higher in western and southern sectors, they did not appear to lead to enhanced frequency of NPF. The infrequent events at these sites occurred when the air masses had spent a few hours over areas with agricultural activities and thus elevated ammonia emissions. Air masses arriving at the sites directly from the sea were not connected with atmospheric NPF. These results support the hypothesis that ammonia and/or amines limit new particle formation in the study area.

Funder

General Secretariat for Research and Technology

HORIZON EUROPE Research Infrastructures

Publisher

Copernicus GmbH

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