Influence of Air Mass Advection on the Amount of Global Solar Radiation Reaching the Earth’s Surface in Poland, Based on the Analysis of Backward Trajectories (1986–2015)

The paper aims to analyse the relationship between the amount of global solar radiation (GSR) reaching the Earth’s surface in Poland and the direction of air mass advection, using 72-h backward trajectories (1986–2015). The study determined average daily sums of GSR related to groups of trajectories...

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Published in:Meteorology
Main Author: Kinga Kulesza
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2023
Subjects:
Online Access:https://doi.org/10.3390/meteorology2010003
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spelling ftmdpi:oai:mdpi.com:/2674-0494/2/1/3/ 2023-08-20T04:08:26+02:00 Influence of Air Mass Advection on the Amount of Global Solar Radiation Reaching the Earth’s Surface in Poland, Based on the Analysis of Backward Trajectories (1986–2015) Kinga Kulesza 2023-01-09 application/pdf https://doi.org/10.3390/meteorology2010003 EN eng Multidisciplinary Digital Publishing Institute https://dx.doi.org/10.3390/meteorology2010003 https://creativecommons.org/licenses/by/4.0/ Meteorology; Volume 2; Issue 1; Pages: 37-51 global solar radiation atmospheric circulation backward trajectories HYSPLIT CM SAF Poland Text 2023 ftmdpi https://doi.org/10.3390/meteorology2010003 2023-08-01T08:12:31Z The paper aims to analyse the relationship between the amount of global solar radiation (GSR) reaching the Earth’s surface in Poland and the direction of air mass advection, using 72-h backward trajectories (1986–2015). The study determined average daily sums of GSR related to groups of trajectories with certain similarities in shape. It was found that the average daily sums of GSR during air mass inflow from all the directions (clusters) identified were significantly different from the average daily sum in the multi-year period. A significant increase in the amount of GSR over Poland is accompanied by air mass inflow from the north and east. The frequency of these advection directions is 27% of all days. The western directions of advection prompt different GSR sums: from slightly increased during advection from the north-west, to significantly decreased during advection from the west (from the central and western part of the North Atlantic). Special attention was given to days with extremely large (above the 0.95 percentile) and with the largest (above the 0.99 percentile) GSR sums. These are prompted by two main types of synoptic conditions: the Azores High ridge covering Central and Southern Europe; and the high-pressure areas which appear in Northern and Central Europe. Text North Atlantic MDPI Open Access Publishing Meteorology 2 1 37 51
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic global solar radiation
atmospheric circulation
backward trajectories
HYSPLIT
CM SAF
Poland
spellingShingle global solar radiation
atmospheric circulation
backward trajectories
HYSPLIT
CM SAF
Poland
Kinga Kulesza
Influence of Air Mass Advection on the Amount of Global Solar Radiation Reaching the Earth’s Surface in Poland, Based on the Analysis of Backward Trajectories (1986–2015)
topic_facet global solar radiation
atmospheric circulation
backward trajectories
HYSPLIT
CM SAF
Poland
description The paper aims to analyse the relationship between the amount of global solar radiation (GSR) reaching the Earth’s surface in Poland and the direction of air mass advection, using 72-h backward trajectories (1986–2015). The study determined average daily sums of GSR related to groups of trajectories with certain similarities in shape. It was found that the average daily sums of GSR during air mass inflow from all the directions (clusters) identified were significantly different from the average daily sum in the multi-year period. A significant increase in the amount of GSR over Poland is accompanied by air mass inflow from the north and east. The frequency of these advection directions is 27% of all days. The western directions of advection prompt different GSR sums: from slightly increased during advection from the north-west, to significantly decreased during advection from the west (from the central and western part of the North Atlantic). Special attention was given to days with extremely large (above the 0.95 percentile) and with the largest (above the 0.99 percentile) GSR sums. These are prompted by two main types of synoptic conditions: the Azores High ridge covering Central and Southern Europe; and the high-pressure areas which appear in Northern and Central Europe.
format Text
author Kinga Kulesza
author_facet Kinga Kulesza
author_sort Kinga Kulesza
title Influence of Air Mass Advection on the Amount of Global Solar Radiation Reaching the Earth’s Surface in Poland, Based on the Analysis of Backward Trajectories (1986–2015)
title_short Influence of Air Mass Advection on the Amount of Global Solar Radiation Reaching the Earth’s Surface in Poland, Based on the Analysis of Backward Trajectories (1986–2015)
title_full Influence of Air Mass Advection on the Amount of Global Solar Radiation Reaching the Earth’s Surface in Poland, Based on the Analysis of Backward Trajectories (1986–2015)
title_fullStr Influence of Air Mass Advection on the Amount of Global Solar Radiation Reaching the Earth’s Surface in Poland, Based on the Analysis of Backward Trajectories (1986–2015)
title_full_unstemmed Influence of Air Mass Advection on the Amount of Global Solar Radiation Reaching the Earth’s Surface in Poland, Based on the Analysis of Backward Trajectories (1986–2015)
title_sort influence of air mass advection on the amount of global solar radiation reaching the earth’s surface in poland, based on the analysis of backward trajectories (1986–2015)
publisher Multidisciplinary Digital Publishing Institute
publishDate 2023
url https://doi.org/10.3390/meteorology2010003
genre North Atlantic
genre_facet North Atlantic
op_source Meteorology; Volume 2; Issue 1; Pages: 37-51
op_relation https://dx.doi.org/10.3390/meteorology2010003
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/meteorology2010003
container_title Meteorology
container_volume 2
container_issue 1
container_start_page 37
op_container_end_page 51
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