High Latitude Dust Transport Altitude Pattern Revealed from Deposition on Snow, Svalbard

High Latitude Dust (HLD) deposition in the surface snow layer in two distant locations in Svalbard (Hornsund and Pyramiden) were collected during the June/July 2019 field campaign and examined in the laboratory. Despite the differences in their climate and topography, both locations are characterise...

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Main Authors: Jan Kavan, Kamil Láska, Adam Nawrot, Tomasz Wawrzyniak
Format: Article
Language:English
Published: MDPI AG 2020-12-01
Series:Atmosphere
Subjects:
Online Access:https://www.mdpi.com/2073-4433/11/12/1318
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spelling doaj-1c1aee495e964b63a1846148d27ac2f32020-12-07T00:01:34ZengMDPI AGAtmosphere2073-44332020-12-01111318131810.3390/atmos11121318High Latitude Dust Transport Altitude Pattern Revealed from Deposition on Snow, SvalbardJan Kavan0Kamil Láska1Adam Nawrot2Tomasz Wawrzyniak3Department of Geography, Faculty of Science, Masaryk University, Kotlářská 2, 611 37 Brno, Czech RepublicDepartment of Geography, Faculty of Science, Masaryk University, Kotlářská 2, 611 37 Brno, Czech RepublicInstitute of Geophysics, Polish Academy of Sciences, 64 Księcia Janusza Str., 01-452 Warsaw, PolandInstitute of Geophysics, Polish Academy of Sciences, 64 Księcia Janusza Str., 01-452 Warsaw, PolandHigh Latitude Dust (HLD) deposition in the surface snow layer in two distant locations in Svalbard (Hornsund and Pyramiden) were collected during the June/July 2019 field campaign and examined in the laboratory. Despite the differences in their climate and topography, both locations are characterised by very similar spatial patterns of the deposition. On the one hand, strong linear negative relationship between the altitude of the sample taken and its concentration was found in low altitude (below 300 m a.s.l.), suggesting a strong influence of local HLD sources. On the other hand, almost constant concentrations were found at higher elevated sampling sites (above 300 m a.s.l.). This suggests a predominantly long-range transport in high altitude areas. The importance of local sources in the lower altitude corresponds well with the generally higher concentrations of HLD in the Pyramiden area. This region has a drier, continental climate and more deglaciated bare land surfaces, which favour more sediment to be uplifted in comparison with the more maritime climate of Hornsund area in the southern part of Svalbard. The spatial division between the local and long-range transport is supported by the proportion of certain lithophile elements in the altitude gradient.https://www.mdpi.com/2073-4433/11/12/1318High Latitude DustsnowaltitudeSvalbardArctic
collection DOAJ
language English
format Article
sources DOAJ
author Jan Kavan
Kamil Láska
Adam Nawrot
Tomasz Wawrzyniak
spellingShingle Jan Kavan
Kamil Láska
Adam Nawrot
Tomasz Wawrzyniak
High Latitude Dust Transport Altitude Pattern Revealed from Deposition on Snow, Svalbard
Atmosphere
High Latitude Dust
snow
altitude
Svalbard
Arctic
author_facet Jan Kavan
Kamil Láska
Adam Nawrot
Tomasz Wawrzyniak
author_sort Jan Kavan
title High Latitude Dust Transport Altitude Pattern Revealed from Deposition on Snow, Svalbard
title_short High Latitude Dust Transport Altitude Pattern Revealed from Deposition on Snow, Svalbard
title_full High Latitude Dust Transport Altitude Pattern Revealed from Deposition on Snow, Svalbard
title_fullStr High Latitude Dust Transport Altitude Pattern Revealed from Deposition on Snow, Svalbard
title_full_unstemmed High Latitude Dust Transport Altitude Pattern Revealed from Deposition on Snow, Svalbard
title_sort high latitude dust transport altitude pattern revealed from deposition on snow, svalbard
publisher MDPI AG
series Atmosphere
issn 2073-4433
publishDate 2020-12-01
description High Latitude Dust (HLD) deposition in the surface snow layer in two distant locations in Svalbard (Hornsund and Pyramiden) were collected during the June/July 2019 field campaign and examined in the laboratory. Despite the differences in their climate and topography, both locations are characterised by very similar spatial patterns of the deposition. On the one hand, strong linear negative relationship between the altitude of the sample taken and its concentration was found in low altitude (below 300 m a.s.l.), suggesting a strong influence of local HLD sources. On the other hand, almost constant concentrations were found at higher elevated sampling sites (above 300 m a.s.l.). This suggests a predominantly long-range transport in high altitude areas. The importance of local sources in the lower altitude corresponds well with the generally higher concentrations of HLD in the Pyramiden area. This region has a drier, continental climate and more deglaciated bare land surfaces, which favour more sediment to be uplifted in comparison with the more maritime climate of Hornsund area in the southern part of Svalbard. The spatial division between the local and long-range transport is supported by the proportion of certain lithophile elements in the altitude gradient.
topic High Latitude Dust
snow
altitude
Svalbard
Arctic
url https://www.mdpi.com/2073-4433/11/12/1318
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