Conditions influencing incoming global solar radiation in Hornsund (Spitsbergen) in spring 2015

This article analyses the conditions affecting the incoming global solar radiation in Hornsund (Spitsbergen) in spring of 2015. Incoming solar radiation turned out to be average for the season under analysis, as compared with longer-term data. The clearness index (KT) was 0.46, and was mainly determ...

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Main Authors: Uscka-Kowalkowska Joanna, Markowicz Krzysztof M., Przybylak Rajmund, Araźny Andrzej
Format: Article
Language:English
Published: Polish Academy of Sciences 2017-09-01
Series:Polish Polar Research
Subjects:
Online Access:http://www.degruyter.com/view/j/popore.2017.38.issue-3/popore-2017-0021/popore-2017-0021.xml?format=INT
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spelling doaj-e8b862ec690c4e7dae568ea6115404322020-11-25T03:48:10ZengPolish Academy of SciencesPolish Polar Research2081-82622017-09-0138333334910.1515/popore-2017-0021popore-2017-0021Conditions influencing incoming global solar radiation in Hornsund (Spitsbergen) in spring 2015Uscka-Kowalkowska Joanna0Markowicz Krzysztof M.1Przybylak Rajmund2Araźny Andrzej3Department of Meteorology and Climatology, Faculty of Earth Sciences, Nicolaus Copernicus University, Lwowska 1, 87-100Toruń, PolandInstitute of Geophysics, Faculty of Physics, University of Warsaw, Pasteura 7, 02-093Warsaw, PolandDepartment of Meteorology and Climatology, Faculty of Earth Sciences, Nicolaus Copernicus University, Lwowska 1, 87-100Toruń, PolandDepartment of Meteorology and Climatology, Faculty of Earth Sciences, Nicolaus Copernicus University, Lwowska 1, 87-100Toruń, PolandThis article analyses the conditions affecting the incoming global solar radiation in Hornsund (Spitsbergen) in spring of 2015. Incoming solar radiation turned out to be average for the season under analysis, as compared with longer-term data. The clearness index (KT) was 0.46, and was mainly determined by the extent of cloudiness. As a result of differences in the length of day, sunshine duration in May was greater than in April. Incoming solar radiation to the earth’s surface is also affected by the atmospheric optical properties. The average value of aerosol optical depth (AOD) at 500 nm in Hornsund in spring of 2015 was 0.087. In the analysed period, increased values of AOD at 500 nm (up to 0.143) were observed, although these are not record values. Over April and May, the greatest part of optical depth was comprised of anthropogenic aerosols (41%), followed by marine aerosols (26%), desert dust (21%) and biomass-burning aerosols (12%). This indicates the significant role of the anthropogenic factor in the climatic conditions of Spitsbergen.http://www.degruyter.com/view/j/popore.2017.38.issue-3/popore-2017-0021/popore-2017-0021.xml?format=INTArcticSpitsbergenglobal solar radiationcloudinesssunshine durationaerosol optical depth
collection DOAJ
language English
format Article
sources DOAJ
author Uscka-Kowalkowska Joanna
Markowicz Krzysztof M.
Przybylak Rajmund
Araźny Andrzej
spellingShingle Uscka-Kowalkowska Joanna
Markowicz Krzysztof M.
Przybylak Rajmund
Araźny Andrzej
Conditions influencing incoming global solar radiation in Hornsund (Spitsbergen) in spring 2015
Polish Polar Research
Arctic
Spitsbergen
global solar radiation
cloudiness
sunshine duration
aerosol optical depth
author_facet Uscka-Kowalkowska Joanna
Markowicz Krzysztof M.
Przybylak Rajmund
Araźny Andrzej
author_sort Uscka-Kowalkowska Joanna
title Conditions influencing incoming global solar radiation in Hornsund (Spitsbergen) in spring 2015
title_short Conditions influencing incoming global solar radiation in Hornsund (Spitsbergen) in spring 2015
title_full Conditions influencing incoming global solar radiation in Hornsund (Spitsbergen) in spring 2015
title_fullStr Conditions influencing incoming global solar radiation in Hornsund (Spitsbergen) in spring 2015
title_full_unstemmed Conditions influencing incoming global solar radiation in Hornsund (Spitsbergen) in spring 2015
title_sort conditions influencing incoming global solar radiation in hornsund (spitsbergen) in spring 2015
publisher Polish Academy of Sciences
series Polish Polar Research
issn 2081-8262
publishDate 2017-09-01
description This article analyses the conditions affecting the incoming global solar radiation in Hornsund (Spitsbergen) in spring of 2015. Incoming solar radiation turned out to be average for the season under analysis, as compared with longer-term data. The clearness index (KT) was 0.46, and was mainly determined by the extent of cloudiness. As a result of differences in the length of day, sunshine duration in May was greater than in April. Incoming solar radiation to the earth’s surface is also affected by the atmospheric optical properties. The average value of aerosol optical depth (AOD) at 500 nm in Hornsund in spring of 2015 was 0.087. In the analysed period, increased values of AOD at 500 nm (up to 0.143) were observed, although these are not record values. Over April and May, the greatest part of optical depth was comprised of anthropogenic aerosols (41%), followed by marine aerosols (26%), desert dust (21%) and biomass-burning aerosols (12%). This indicates the significant role of the anthropogenic factor in the climatic conditions of Spitsbergen.
topic Arctic
Spitsbergen
global solar radiation
cloudiness
sunshine duration
aerosol optical depth
url http://www.degruyter.com/view/j/popore.2017.38.issue-3/popore-2017-0021/popore-2017-0021.xml?format=INT
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