Dust in Svalbard: local sources versus long-range transported dust (SVALDUST)

This is chapter 3 of the State of Environmental Science in Svalbard (SESS) report 2022. Dust consists of fine and coarse particles that travel in the atmosphere and are deposited on the Earth’s surface. Dust particles deposited on snow and ice can cause snow darkening and contribute to melting. In t...

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Main Authors: Di Mauro, Biagio, Cappeletti, David, Moroni, Beatrice, Mazzola, Mauro, Gilardoni, Stefania, Luks, Bartłomiej, Nawrot, Adam, Lewandowski, Marek, Dagsson Waldhauserova, Pavla, Meinander, Outi, Wittmann, Monika, Kaspari, Susan, Khan, Alia
Other Authors: orcid:0000-0001-6608-3951, Ilmatieteen laitos, Finnish Meteorological Institute
Format: Other/Unknown Material
Language:English
Published: Svalbard Integrated Arctic Earth Observing System 2023
Subjects:
Online Access:http://hdl.handle.net/10138/566904
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author Di Mauro, Biagio
Cappeletti, David
Moroni, Beatrice
Mazzola, Mauro
Gilardoni, Stefania
Luks, Bartłomiej
Nawrot, Adam
Lewandowski, Marek
Dagsson Waldhauserova, Pavla
Meinander, Outi
Wittmann, Monika
Kaspari, Susan
Khan, Alia
author2 orcid:0000-0001-6608-3951
Ilmatieteen laitos
Finnish Meteorological Institute
author_facet Di Mauro, Biagio
Cappeletti, David
Moroni, Beatrice
Mazzola, Mauro
Gilardoni, Stefania
Luks, Bartłomiej
Nawrot, Adam
Lewandowski, Marek
Dagsson Waldhauserova, Pavla
Meinander, Outi
Wittmann, Monika
Kaspari, Susan
Khan, Alia
author_sort Di Mauro, Biagio
collection HELDA – University of Helsinki Open Repository
description This is chapter 3 of the State of Environmental Science in Svalbard (SESS) report 2022. Dust consists of fine and coarse particles that travel in the atmosphere and are deposited on the Earth’s surface. Dust particles deposited on snow and ice can cause snow darkening and contribute to melting. In this chapter, we summarise existing knowledge on local and long-range dust sources in Svalbard, and describe current methodologies for studying dust from both an observational and modelling perspective. Dust science in Svalbard is still in its infancy; future research will help to disentangle the complex role of dust in the Svalbard environment.
format Other/Unknown Material
genre Arktinen alue
Svalbard
Spitsbergen
genre_facet Arktinen alue
Svalbard
Spitsbergen
geographic Svalbard
geographic_facet Svalbard
id ftunivhelsihelda:oai:helda.helsinki.fi:10138/566904
institution Open Polar
language English
op_collection_id ftunivhelsihelda
op_relation 10.5281/zenodo.7377518
The State of Environmental Science in Svalbard - an annual report
2022
978-82-93871-06-4
89669
http://hdl.handle.net/10138/566904
URN:NBN:fi-fe20231108143566
op_rights CC BY 4.0
publishDate 2023
publisher Svalbard Integrated Arctic Earth Observing System
record_format openpolar
spelling ftunivhelsihelda:oai:helda.helsinki.fi:10138/566904 2025-01-16T20:55:08+00:00 Dust in Svalbard: local sources versus long-range transported dust (SVALDUST) Di Mauro, Biagio Cappeletti, David Moroni, Beatrice Mazzola, Mauro Gilardoni, Stefania Luks, Bartłomiej Nawrot, Adam Lewandowski, Marek Dagsson Waldhauserova, Pavla Meinander, Outi Wittmann, Monika Kaspari, Susan Khan, Alia orcid:0000-0001-6608-3951 Ilmatieteen laitos Finnish Meteorological Institute 2023-11-08T10:50:14Z 62-77 application/pdf http://hdl.handle.net/10138/566904 en eng Svalbard Integrated Arctic Earth Observing System 10.5281/zenodo.7377518 The State of Environmental Science in Svalbard - an annual report 2022 978-82-93871-06-4 89669 http://hdl.handle.net/10138/566904 URN:NBN:fi-fe20231108143566 CC BY 4.0 atmosphere (earth) Svalbard dust snow Spitsbergen glaciers climate changes fine particles melting ilmakehä pöly lumi Huippuvuoret jäätiköt ilmatonmuutokset pienhiukkaset sulaminen arktinen alue A3 Kirjan tai muun kokoomateoksen osa A3 Book section, Chapters in research books 2023 ftunivhelsihelda 2023-11-09T00:01:12Z This is chapter 3 of the State of Environmental Science in Svalbard (SESS) report 2022. Dust consists of fine and coarse particles that travel in the atmosphere and are deposited on the Earth’s surface. Dust particles deposited on snow and ice can cause snow darkening and contribute to melting. In this chapter, we summarise existing knowledge on local and long-range dust sources in Svalbard, and describe current methodologies for studying dust from both an observational and modelling perspective. Dust science in Svalbard is still in its infancy; future research will help to disentangle the complex role of dust in the Svalbard environment. Other/Unknown Material Arktinen alue Svalbard Spitsbergen HELDA – University of Helsinki Open Repository Svalbard
spellingShingle atmosphere (earth)
Svalbard
dust
snow
Spitsbergen
glaciers
climate changes
fine particles
melting
ilmakehä
pöly
lumi
Huippuvuoret
jäätiköt
ilmatonmuutokset
pienhiukkaset
sulaminen
arktinen alue
Di Mauro, Biagio
Cappeletti, David
Moroni, Beatrice
Mazzola, Mauro
Gilardoni, Stefania
Luks, Bartłomiej
Nawrot, Adam
Lewandowski, Marek
Dagsson Waldhauserova, Pavla
Meinander, Outi
Wittmann, Monika
Kaspari, Susan
Khan, Alia
Dust in Svalbard: local sources versus long-range transported dust (SVALDUST)
title Dust in Svalbard: local sources versus long-range transported dust (SVALDUST)
title_full Dust in Svalbard: local sources versus long-range transported dust (SVALDUST)
title_fullStr Dust in Svalbard: local sources versus long-range transported dust (SVALDUST)
title_full_unstemmed Dust in Svalbard: local sources versus long-range transported dust (SVALDUST)
title_short Dust in Svalbard: local sources versus long-range transported dust (SVALDUST)
title_sort dust in svalbard: local sources versus long-range transported dust (svaldust)
topic atmosphere (earth)
Svalbard
dust
snow
Spitsbergen
glaciers
climate changes
fine particles
melting
ilmakehä
pöly
lumi
Huippuvuoret
jäätiköt
ilmatonmuutokset
pienhiukkaset
sulaminen
arktinen alue
topic_facet atmosphere (earth)
Svalbard
dust
snow
Spitsbergen
glaciers
climate changes
fine particles
melting
ilmakehä
pöly
lumi
Huippuvuoret
jäätiköt
ilmatonmuutokset
pienhiukkaset
sulaminen
arktinen alue
url http://hdl.handle.net/10138/566904