Saharan, Aral-Caspian and Middle East dust travels to Finland (1980-2022).


Journal

Environment international
ISSN: 1873-6750
Titre abrégé: Environ Int
Pays: Netherlands
ID NLM: 7807270

Informations de publication

Date de publication:
10 2023
Historique:
received: 22 06 2023
revised: 13 09 2023
accepted: 28 09 2023
medline: 1 11 2023
pubmed: 8 10 2023
entrez: 7 10 2023
Statut: ppublish

Résumé

Studies on atmospheric dust and long-range transport of mineral dust have been a focus of atmospheric science in recent years. With its wide range of direct and indirect effects, mineral dust is one of the most uncertain elements in the mechanisms of climate change, and a deeper understanding of its role is essential for understanding future processes. The aim of our research was to provide the first systematic data on the so far episodically documented northward transport mineral dust from arid-semiarid areas. So, in this paper, we present dust storm events from lower latitudes reaching the Finnish atmosphere, based on the MERRA-2 model Dust Column Mass Density data and after a multistep verification procedure using independent data source. In total, 86 long-range dust storm events were identified between 1980 and 2022, when air masses loaded with dust reached Finland. Based on backward-trajectories different sources were identified: 59 were Saharan, 22 were Aral-Caspian, and five were associated with Middle Eastern source areas. Considerable variation in inter-annual frequencies was observed among the source areas, which may be due to changes in circulation conditions and the effects of human activity (agriculture and land use changes in Aral Sea region). There is a clear maximum of dust events in spring (60%), followed by summer and autumn (where 10 of the 11 autumn episodes were from the Sahara). However, the number and proportion of scarce winter events have more than doubled since 2010 compared to the preceding 30 years, but no autumn events were registered during this period. This clear temporal variation coincides with changes in dust transport observed in other regions of Europe, driven by greater atmospheric meridionality associated with climate change and driven by reduced temperature difference between low and high latitudes due to enhanced temperature increases at Arctic regions.

Identifiants

pubmed: 37804716
pii: S0160-4120(23)00516-0
doi: 10.1016/j.envint.2023.108243
pii:
doi:

Substances chimiques

Dust 0
Air Pollutants 0
Minerals 0

Types de publication

Journal Article Research Support, Non-U.S. Gov't

Langues

eng

Sous-ensembles de citation

IM

Pagination

108243

Informations de copyright

Copyright © 2023 The Authors. Published by Elsevier Ltd.. All rights reserved.

Déclaration de conflit d'intérêts

Declaration of Competing Interest The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.

Auteurs

György Varga (G)

HUN-REN Research Centre for Astronomy and Earth Sciences, Budapest, Hungary; ELTE Eötvös Loránd University, Institute of Geography and Earth Sciences, Department of Meteorology, Budapest, Hungary; CSFK, MTA Centre of Excellence, Budapest, Hungary; Research Institute of Biomolecular and Chemical Engineering, University of Pannonia, Veszprém, Hungary. Electronic address: varga.gyorgy@csfk.org.

Outi Meinander (O)

Atmospheric Composition Research, Finnish Meteorological Institute, Helsinki, Finland.

Ágnes Rostási (Á)

MTA-PE Air Chemistry Research Group, Veszprém, Hungary; Research Institute of Biomolecular and Chemical Engineering, University of Pannonia, Veszprém, Hungary.

Pavla Dagsson-Waldhauserova (P)

Faculty of Environmental and Forest Sciences, Agricultural University of Iceland, Reykjavik, Iceland; Faculty of Environmental Sciences, Department of Water Resources and Environmental Modeling, Czech University of Life Sciences Prague, Prague, Czech Republic.

Adrienn Csávics (A)

HUN-REN Research Centre for Astronomy and Earth Sciences, Budapest, Hungary; ELTE Eötvös Loránd University, Institute of Geography and Earth Sciences, Department of Meteorology, Budapest, Hungary; CSFK, MTA Centre of Excellence, Budapest, Hungary.

Fruzsina Gresina (F)

HUN-REN Research Centre for Astronomy and Earth Sciences, Budapest, Hungary; ELTE Eötvös Loránd University, Institute of Geography and Earth Sciences, Department of Meteorology, Budapest, Hungary; CSFK, MTA Centre of Excellence, Budapest, Hungary; ELTE Eötvös Loránd University, Institute of Geography and Earth Sciences, Department of Environmental and Landscape Geography, Budapest, Hungary.

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Classifications MeSH