The Arctic region is threatened by contamination deriving from both long-range pollution and local human activities. Polycyclic Aromatic Hydrocarbons (PAHs) are environmental tracers of emission, transport and deposition processes. A first campaign has been conducted at Ny-Ålesund, Svalbard, from October 2018 to May 2019, monitoring weekly concentrations of PAHs in Arctic surface snow. The trend of the 16 high priority PAH compounds showed that long-range inputs occurred mainly in the winter, with concentrations ranging from 0.8 ng L-1 to 37 ng L-1. In contrast to this, the most abundant analyte retene, showed an opposite seasonal trend with highest values in autumn and late spring (up to 97 ng L-1), while in winter this compound remained below 3 ng L-1. This is most likely due to local contributions from outcropping coal deposits and stockpiles. Our results show a general agreement with the atmospheric signal, although significant skews can be attributed to post-depositional processes, wind erosion, melting episodes and redistribution. © 2023 The Authors

The seasonal change of PAHs in Svalbard surface snow

Marco Vecchiato
;
Carlo Barbante;Elena Barbaro;Warren R. L. Cairns;David Cappelletti;Federico Dallo;Marianna D'Amico;Andrea Gambaro;Mauro Mazzola;Ivan Sartorato;Federico Scoto;Clara Turetta;Massimiliano Vardè;Andrea Spolaor
2024

Abstract

The Arctic region is threatened by contamination deriving from both long-range pollution and local human activities. Polycyclic Aromatic Hydrocarbons (PAHs) are environmental tracers of emission, transport and deposition processes. A first campaign has been conducted at Ny-Ålesund, Svalbard, from October 2018 to May 2019, monitoring weekly concentrations of PAHs in Arctic surface snow. The trend of the 16 high priority PAH compounds showed that long-range inputs occurred mainly in the winter, with concentrations ranging from 0.8 ng L-1 to 37 ng L-1. In contrast to this, the most abundant analyte retene, showed an opposite seasonal trend with highest values in autumn and late spring (up to 97 ng L-1), while in winter this compound remained below 3 ng L-1. This is most likely due to local contributions from outcropping coal deposits and stockpiles. Our results show a general agreement with the atmospheric signal, although significant skews can be attributed to post-depositional processes, wind erosion, melting episodes and redistribution. © 2023 The Authors
2024
Istituto di Scienze Polari - ISP
Istituto di Scienze dell'Atmosfera e del Clima - ISAC
Inglese
Volume 340, Part 1, 1 January 2024
122864
1
9
9
https://www.sciencedirect.com/science/article/pii/S0269749123018663?pes=vor
Esperti anonimi
PAHs
Snow
Arctic
Winter
Retene
Deadline for manuscript submissions: closed (25 July 2022)Received 27 July 2023, Revised 13 October 2023, Accepted 1 November 2023, Available online 2 November 2023, Version of Record 11 November 2023. Open access. This project has received funding from the European Union's Horizon 2020 research and innovation programme under grant agreement no. 689443 via ERA_PLANET Strand 4 project iCUPE (Integrative and Comprehensive Understanding on Polar Environments).
Internazionale
Elettronico
21
info:eu-repo/semantics/article
262
Vecchiato, Marco; Barbante, Carlo; Barbaro, Elena; Burgay, François; Cairns, Warren R. L.; Callegaro, Alice; Cappelletti, David; Dallo, Federico; D'Am...espandi
01 Contributo su Rivista::01.01 Articolo in rivista
open
   The European network for observing our changing planet
   ERA-PLANET
   EU
   H2020
   689443
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/20.500.14243/454800
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