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            Research Institute of Biomolecular and Chemical Engineering, University of Pannonia, Veszprém, Hungary            
            ELTE Eötvös Loránd University, Institute of Geography and Earth Sciences, Department of Meteorology, Budapest, Hungary            
            MTA-PE Air Chemistry Research Group, Research Institute of Biomolecular and Chemical Engineering, University of Pannonia, Veszprém, Hungary            
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&lt;div class=&quot;title&quot;&gt;&lt;a href=&quot;/gui2/?mode=browse&amp;params=publication;35725820&quot; target=&quot;_blank&quot;&gt;Desert dust and photovoltaic energy forecasts: lessons from 46 Saharan dust events in Hungary (Central Europe)&lt;/a&gt;&lt;/div&gt;    &lt;div&gt;		&lt;span class=&quot;journal-title&quot;&gt;RENEWABLE &amp; SUSTAINABLE ENERGY REVIEWS&lt;/span&gt;

        &lt;span class=&quot;journal-issn&quot;&gt;(&lt;a target=&quot;_blank&quot; href=&quot;https://portal.issn.org/resource/ISSN/1364-0321&quot;&gt;1364-0321&lt;/a&gt; &lt;a target=&quot;_blank&quot; href=&quot;https://portal.issn.org/resource/ISSN/1879-0690&quot;&gt;1879-0690&lt;/a&gt;)&lt;/span&gt;:
		&lt;span class=&quot;journal-volume&quot;&gt;212&lt;/span&gt; 
&lt;span class=&quot;page&quot;&gt;
		Paper 115446.
	
&lt;/span&gt;		 &lt;span class=&quot;year&quot;&gt;(2025)&lt;/span&gt;  
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	&lt;span class=&quot;language&quot; xmlns=&quot;http://www.w3.org/1999/html&quot;&gt;Nyelv:
			Angol
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				&lt;div class=&quot;journal-subject&quot;&gt;Folyóirat szakterülete: Scopus - Renewable Energy, Sustainability and the Environment&amp;nbsp;&amp;nbsp;&amp;nbsp;SJR indikátor:&amp;nbsp;D1&lt;/div&gt;
			&lt;div class=&quot;journal-subject&quot;&gt;Regionális Tudományok Bizottsága IXGJO RTB [1901-]&amp;nbsp;&amp;nbsp;&amp;nbsp;A nemzetközi&lt;/div&gt;
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&lt;div class=&quot;lastModified&quot;&gt;Utolsó módosítás: 2025.02.24. 23:00 Szabó Regina (ELTE TTK admin 5)
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	&lt;pre class=&quot;comment&quot; style=&quot;margin-top: 0; margin-bottom: 0;&quot;&gt;&lt;u&gt;Megjegyzés&lt;/u&gt;: HUN-REN Research Centre for Astronomy and Earth Sciences, Budapest, Hungary            
            Research Institute of Biomolecular and Chemical Engineering, University of Pannonia, Veszprém, Hungary            
            ELTE Eötvös Loránd University, Institute of Geography and Earth Sciences, Department of Meteorology, Budapest, Hungary            
            MTA-PE Air Chemistry Resear...&lt;/pre&gt;
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            ELTE Eötvös Loránd University, Institute of Geography and Earth Sciences, Department of Meteorology, Budapest, Hungary            
            CSFK, MTA Centre of Excellence, Budapest, Hungary            
            Atmospheric Composition Research, Finnish Meteorological Institute, Helsinki, Finland            
            MTA-PE Air Chemistry Research Group, Veszprém, Hungary            
            Research Institute of Biomolecular and Chemical Engineering, University of Pannonia, Veszprém, Hungary            
            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            
            ELTE Eötvös Loránd University, Institute of Geography and Earth Sciences, Department of Environmental and Landscape Geography, Budapest, Hungary            
            Export Date: 8 January 2024            
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;&amp;nbsp;&amp;nbsp;&amp;nbsp;
							&lt;span class=&quot;author-name&quot; &gt;Meinander O
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;&amp;nbsp;&amp;nbsp;&amp;nbsp;
							&lt;span class=&quot;author-name&quot; &gt;Dagsson-Waldhauserova P
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;&amp;nbsp;&amp;nbsp;&amp;nbsp;
							&lt;span class=&quot;author-name&quot; &gt;Csávics A
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							&lt;span class=&quot;author-name&quot; mtid=&quot;10072433&quot;&gt;&lt;a 
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	&lt;pre class=&quot;comment&quot; style=&quot;margin-top: 0; margin-bottom: 0;&quot;&gt;&lt;u&gt;Megjegyzés&lt;/u&gt;: 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            
            Atmospheric Composition Research, Finnish Meteorological Institute, Helsinki, Fi...&lt;/pre&gt;
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      <abstractText>Grain size proxies of aeolian dust deposits have widely been applied in environmental and sedimentary studies. However, large body of research papers are not taking into consideration that a complex grain size distribution curve cannot be an indicator of a single one environmental factor (e.g. wind speed/strength, transportation distance, aridity).

The aim of the present paper is to discuss the main differences of frequently used statistical methods and to provide possible interpretations of the results by applying these various approaches on the high-resolution loess-paleosol profile of Dunaszekcso, South Hungary (Central Europe). Beside single statistical descriptors (mean, median, mode) of grain size and simple indices of size-fraction ratios (U-ratio, Grain Size Index), some more complex algorithms were also used in our paper. The applied parametric curve-fitting, end-member modelling and hierarchical cluster analysis techniques are using the whole spectrum of the measured grain size distributions and provide a more reliable and more representative results even in case of small scale variations.

According to our findings, approaches which provide direct linkage among simple statistical descriptors and single atmospheric or other environmental elements are rather oversimplified as properties aeolian dust deposits are influenced by the integrated effects of several concurrent processes. Differences of more complex decomposition methods arise from the different approach and scope. End-members are determined from the unmixing based on the covariance structure of the whole grain size data-series of the section, while the parametric curve-fitting is based on the one-by-one deconvolution of the grain size distribution curves. End-members of loess-paleosol samples are regarded as representation of the average dust grain size distribution of various temporal sediment clusters of seasonal or other short-term intervals, while (sub) populations by parametric curve-fitting are proposed to illustrate process-related elements of background and dust storm depositional components for each sample. Results of cluster analysis represent similar grouping conditions as end-member modelling with a reduced sedimentary and genetically meaning. (C) 2017 Elsevier Ltd and INQUA. All rights reserved.</abstractText>
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&lt;span title=&quot;Pécsi Tudományegyetem&quot;&gt;PTE&lt;/span&gt;/&lt;span title=&quot;Szentágothai János Kutatóközpont&quot;&gt;SZKK&lt;/span&gt;/Környezeti Analitikai és Geoanalitikai Kutatócsoport&lt;/span&gt; ;&amp;nbsp;&amp;nbsp;&amp;nbsp; &lt;span class=&quot;author-name&quot; mtid=&quot;10002480&quot;&gt;&lt;a href=&quot;/gui2/?type=authors&amp;mode=browse&amp;sel=10002480&quot; target=&quot;_blank&quot;&gt;Szalai Z (&lt;span class=&quot;authorship-author-name&quot;&gt;Szalai Zoltán&lt;/span&gt; &lt;span class=&quot;authorAux-mtmt&quot;&gt; Természetföldrajz&lt;/span&gt;) &lt;/a&gt; &lt;/span&gt; &lt;span class=&quot;author-affil&quot;&gt;&lt;span title=&quot;Csillagászati és Földtudományi Kutatóközpont&quot;&gt;CSFK&lt;/span&gt;/&lt;span title=&quot;Földrajztudományi Intézet&quot;&gt;FTI&lt;/span&gt;/Természetföldrajzi Osztály; &lt;span title=&quot;Eötvös Loránd Tudományegyetem&quot;&gt;ELTE&lt;/span&gt;/&lt;span title=&quot;Természettudományi Kar&quot;&gt;TTK&lt;/span&gt;/&lt;span title=&quot;Földrajz- és Földtudományi Intézet&quot;&gt;FoldrFoldt_I&lt;/span&gt;/&lt;span title=&quot;Földrajztudományi Központ&quot;&gt;Frt_K&lt;/span&gt;/Környezet- és Tájföldrajzi Tanszék&lt;/span&gt; &lt;/div&gt; &lt;/div&gt; &lt;div class=&quot;title&quot;&gt;&lt;a href=&quot;/gui2/?mode=browse&amp;params=publication;30710244&quot; target=&quot;_blank&quot;&gt;On the reliability and comparability of laser diffraction grain size measurements of paleosols in loess records&lt;/a&gt;&lt;/div&gt; &lt;div&gt; &lt;span class=&quot;journal-title&quot;&gt;SEDIMENTARY GEOLOGY&lt;/span&gt; &lt;span class=&quot;journal-issn&quot;&gt;(&lt;a target=&quot;_blank&quot; href=&quot;https://portal.issn.org/resource/ISSN/0037-0738&quot;&gt;0037-0738&lt;/a&gt; &lt;a target=&quot;_blank&quot; href=&quot;https://portal.issn.org/resource/ISSN/1879-0968&quot;&gt;1879-0968&lt;/a&gt;)&lt;/span&gt;: &lt;span class=&quot;journal-volume&quot;&gt;389&lt;/span&gt; &lt;span class=&quot;page&quot;&gt; pp 42-53 &lt;/span&gt; &lt;span class=&quot;year&quot;&gt;(2019)&lt;/span&gt; &lt;/div&gt; &lt;div class=&quot;pub-footer&quot;&gt;  &lt;span class=&quot;language&quot; xmlns=&quot;http://www.w3.org/1999/html&quot;&gt;Nyelv: Angol | &lt;/span&gt; &lt;span class=&quot;identifiers&quot;&gt; &lt;span class=&quot;id identifier oa_none&quot; title=&quot;none&quot;&gt; &lt;a style=&quot;color:blue&quot; title=&quot;10.1016/j.sedgeo.2019.05.011&quot; target=&quot;_blank&quot; href=&quot;https://doi.org/10.1016/j.sedgeo.2019.05.011&quot;&gt; DOI &lt;/a&gt; &lt;/span&gt; &lt;span class=&quot;id identifier oa_CLOSED&quot; title=&quot; Zárt &quot;&gt; &lt;a style=&quot;color:blue&quot; title=&quot;101807&quot; target=&quot;_blank&quot; href=&quot;http://real.mtak.hu/101807&quot;&gt; REAL &lt;/a&gt; &lt;/span&gt; &lt;span class=&quot;id identifier oa_none&quot; title=&quot;none&quot;&gt; &lt;a style=&quot;color:blue&quot; title=&quot;000482506400004&quot; target=&quot;_blank&quot; href=&quot;https://www.webofscience.com/wos/woscc/full-record/000482506400004&quot;&gt; WoS &lt;/a&gt; &lt;/span&gt; &lt;span class=&quot;id identifier oa_none&quot; title=&quot;none&quot;&gt; &lt;a style=&quot;color:blue&quot; title=&quot;85067033305&quot; target=&quot;_blank&quot; href=&quot;http://www.scopus.com/record/display.url?origin=inward&amp;eid=2-s2.0-85067033305&quot;&gt; Scopus &lt;/a&gt; &lt;/span&gt; &lt;/span&gt; &lt;OnlyViewableByAuthor&gt;&lt;div class=&quot;ratings&quot;&gt; &lt;div class=&quot;journal-subject&quot;&gt;Folyóirat szakterülete: Scopus - Geology&amp;nbsp;&amp;nbsp;&amp;nbsp;SJR indikátor:&amp;nbsp;Q1&lt;/div&gt; &lt;div class=&quot;journal-subject&quot;&gt;Folyóirat szakterülete: Scopus - Stratigraphy&amp;nbsp;&amp;nbsp;&amp;nbsp;SJR indikátor:&amp;nbsp;Q1&lt;/div&gt; &lt;div class=&quot;journal-subject&quot;&gt;X. Földtudományok Osztálya XFO&amp;nbsp;&amp;nbsp;&amp;nbsp;A&lt;/div&gt; &lt;/div&gt;&lt;/OnlyViewableByAuthor&gt; &lt;div class=&quot;publication-citation&quot; style=&quot;margin-left: 0.5cm;&quot;&gt; &lt;span title=&quot;Nyilvános idézőközlemények összesen, említések nélkül&quot; class=&quot;citingPub-count&quot;&gt;Nyilvános idéző összesen: 40&lt;/span&gt; | Független: 31 | Függő: 9 | Nem jelölt: 0 | WoS jelölt: 28 | Scopus jelölt:&amp;nbsp;30 | WoS/Scopus jelölt:&amp;nbsp;32 | DOI jelölt:&amp;nbsp;35 &lt;/div&gt;   &lt;div class=&quot;publication-citation&quot;&gt; &lt;a target=&quot;_blank&quot; href=&quot;/api/publication?cond=citations.related;eq;30710244&amp;sort=publishedYear,desc&amp;sort=title&quot;&gt; Idézett közlemények száma: 14 &lt;/a&gt; &lt;/div&gt; &lt;div class=&quot;mtid&quot;&gt;&lt;span class=&quot;long-pub-mtid&quot;&gt;Közlemény: 30710244&lt;/span&gt; | &lt;span class=&quot;status-data status-APPROVED&quot;&gt; Nyilvános &lt;/span&gt; Forrás Idéző | &lt;span class=&quot;type-subtype&quot;&gt;Folyóiratcikk ( Szakcikk ) &lt;/span&gt; | &lt;span class=&quot;pub-category&quot;&gt;Tudományos&lt;/span&gt; | &lt;span class=&quot;publication-sourceOfData&quot;&gt;DOI XML&lt;/span&gt; &lt;/div&gt; &lt;div class=&quot;funder&quot;&gt; (K120620) Támogató: OTKA, (KH130337), (KEP-08/2018) &lt;/div&gt; &lt;div class=&quot;lastModified&quot;&gt;Utolsó módosítás: 2025.06.06. 12:55 Milánkovics Róbert (PTE ÁOK admin 4) &lt;/div&gt; &lt;div class=&quot;lockedBy&quot;&gt;Központi kezelésű 2025.11.17. 11:33 Pécsi Éva (MTMT Közp 2,3, admin) &lt;/div&gt; &lt;/div&gt;&lt;/div&gt;</template2>
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