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            <front>

                <journal-meta>
                                    <journal-id></journal-id>
            <journal-title-group>
                                                <journal-title></journal-title>
            </journal-title-group>
                            <issn pub-type="ppub">2667-419X</issn>
                                                                                                        <publisher>
                    <publisher-name>Eskisehir Technical University</publisher-name>
                </publisher>
                    </journal-meta>
                <article-meta>
                                        <article-id pub-id-type="doi">10.20290/estubtdb.543355</article-id>
                                                                <article-categories>
                                            <subj-group  xml:lang="en">
                                                            <subject>Engineering</subject>
                                                    </subj-group>
                                            <subj-group  xml:lang="tr">
                                                            <subject>Mühendislik</subject>
                                                    </subj-group>
                                    </article-categories>
                                                                                                                                                        <title-group>
                                                                                                                        <trans-title-group xml:lang="tr">
                                    <trans-title>ANALYSIS OF DUST EVENT IN TURKMENISTAN AND ITS SOURCE REGIONS</trans-title>
                                </trans-title-group>
                                                                                                                                                                                                <article-title>ANALYSIS OF DUST EVENT IN TURKMENISTAN AND ITS SOURCE REGIONS</article-title>
                                                                                                    </title-group>
            
                                                    <contrib-group content-type="authors">
                                                                        <contrib contrib-type="author">
                                                                    <contrib-id contrib-id-type="orcid">
                                        https://orcid.org/0000-0001-5305-6145</contrib-id>
                                                                <name>
                                    <surname>Oğuz</surname>
                                    <given-names>Kahraman</given-names>
                                </name>
                                                                    <aff>Turkish State Meteorological Service</aff>
                                                            </contrib>
                                                                                </contrib-group>
                        
                                        <pub-date pub-type="pub" iso-8601-date="20200228">
                    <day>02</day>
                    <month>28</month>
                    <year>2020</year>
                </pub-date>
                                        <volume>8</volume>
                                        <issue>1</issue>
                                        <fpage>61</fpage>
                                        <lpage>72</lpage>
                        
                        <history>
                                    <date date-type="received" iso-8601-date="20190322">
                        <day>03</day>
                        <month>22</month>
                        <year>2019</year>
                    </date>
                                                    <date date-type="accepted" iso-8601-date="20200203">
                        <day>02</day>
                        <month>03</month>
                        <year>2020</year>
                    </date>
                            </history>
                                        <permissions>
                    <copyright-statement>Copyright © 2010, </copyright-statement>
                    <copyright-year>2010</copyright-year>
                    <copyright-holder></copyright-holder>
                </permissions>
            
                                                                                                <trans-abstract xml:lang="tr">
                            <p>Dust transports cause significantincreases in atmospheric concentration and surface PM10 particulate matter. Inrecent years, Asian countries have experienced dust transport frequently. Dusttransport has a significant negative impact on human health, the economy andthe environment. This study includes the analysis of source regions and dusttransport dated in 27-29 May 2018 over Turkmenistan. In the study, a generaldust situation of Turkmenistan region has been studied by using MODIS AOD data.Then, the meteorological conditions and the pathway of this dust transportevent on were examined. The preliminary analysis using synoptic analyzes andsatellite data showed that the dust transport is coming through Uzbekistan andKazakhstan. The transport took place on the south direction and affected mostof Turkmenistan on 27 May 2018. Observed AOD data in the region increasedsignificantly and took its maximum on 27 May 2018. The effect of this movementin Turkmenistan lasted until 30 May 2018. The global CAMS dust model hasgenerally estimated dust transport event even some overestimations. MSG/RGBsatellite products were examined detailly in order to analyze the sourceregions of this dust transport. The analyzes showed the main source region ofthis dust transport as Aral lake.</p></trans-abstract>
                                                                                                                                    <abstract><p>Dust transports cause significantincreases in atmospheric concentration and surface PM10 particulate matter. Inrecent years, Asian countries have experienced dust transport frequently. Dusttransport has a significant negative impact on human health, the economy andthe environment. This study includes the analysis of source regions and dusttransport dated in 27-29 May 2018 over Turkmenistan. In the study, a generaldust situation of Turkmenistan region has been studied by using MODIS AOD data.Then, the meteorological conditions and the pathway of this dust transportevent on were examined. The preliminary analysis using synoptic analyzes andsatellite data showed that the dust transport is coming through Uzbekistan andKazakhstan. The transport took place on the south direction and affected mostof Turkmenistan on 27 May 2018. Observed AOD data in the region increasedsignificantly and took its maximum on 27 May 2018. The effect of this movementin Turkmenistan lasted until 30 May 2018. The global CAMS dust model hasgenerally estimated dust transport event even some overestimations. MSG/RGBsatellite products were examined detailly in order to analyze the sourceregions of this dust transport. The analyzes showed the main source region ofthis dust transport as Aral lake.</p></abstract>
                                                            
            
                                                                                        <kwd-group>
                                                    <kwd>Dust event</kwd>
                                                    <kwd>  Dust source regions</kwd>
                                                    <kwd>  Turkmenistan</kwd>
                                                    <kwd>  Dust model</kwd>
                                                    <kwd>  Observed AOD</kwd>
                                            </kwd-group>
                            
                                                <kwd-group xml:lang="tr">
                                                    <kwd>Dust event</kwd>
                                                    <kwd>  dust source regions</kwd>
                                                    <kwd>  Turkmenistan</kwd>
                                                    <kwd>  dust model</kwd>
                                                    <kwd>  observed AOD</kwd>
                                            </kwd-group>
                                                                                                                                        </article-meta>
    </front>
    <back>
                            <ref-list>
                                    <ref id="ref1">
                        <label>1</label>
                        <mixed-citation publication-type="journal">[1] Banacos PC and Ekster ML. The association of the elevated mixed layer with 	significant severe weather events in the Northeast United States. Wea. Forecasting 2010; 25: 1082-1102.</mixed-citation>
                    </ref>
                                    <ref id="ref2">
                        <label>2</label>
                        <mixed-citation publication-type="journal">[2] Dündar C, Oğuz K and Güllü G. Evaluation of Sand and Dust Storms (SDS) over Eastern Mediterranean Basin. 10. National Conference on Environmental 	Engineering; 12-14 September 2013; Hacettepe University, Ankara, Turkey.</mixed-citation>
                    </ref>
                                    <ref id="ref3">
                        <label>3</label>
                        <mixed-citation publication-type="journal">[3] Goudie AS and Middleton NJ. Saharan dust storms: nature and consequences. Earth-Science Reviews 2001; 56; 179–204.</mixed-citation>
                    </ref>
                                    <ref id="ref4">
                        <label>4</label>
                        <mixed-citation publication-type="journal">[4] Indoitu R, Orlovsky L and Orlovsky N. Dust storms in Central Asia: spatial and temporal variations. J Arid Environ 2012; 85; 62–70.</mixed-citation>
                    </ref>
                                    <ref id="ref5">
                        <label>5</label>
                        <mixed-citation publication-type="journal">[5] IPCC 2007 Summary for policymakers in Climate Change 2007: the Physical Science Basis; Cambridge University Press, New York, NY, USA.</mixed-citation>
                    </ref>
                                    <ref id="ref6">
                        <label>6</label>
                        <mixed-citation publication-type="journal">[6] Jickells TD, An ZS, Andersen KK, Baker AR, Bergametti G, Brooks N, Cao JJ, Boyd PW, Duce RA, Hunter KA, Kawahata H, Kubilay N, laRoche J, Liss PS, Mahowald N, 	Prospero JM, Ridgwell AJ, Tegen I and Torres R. Global iron connections between desert dust, ocean biogeochemistry, and climate. Science 2005; 308; 5718 67–	71.</mixed-citation>
                    </ref>
                                    <ref id="ref7">
                        <label>7</label>
                        <mixed-citation publication-type="journal">[7] Kalnay et al. The NCEP/NCAR 40-year reanalysis Project. Bull. Amer. Meteor. Soc. 1996; 77; 437-470.</mixed-citation>
                    </ref>
                                    <ref id="ref8">
                        <label>8</label>
                        <mixed-citation publication-type="journal">[8] Lensky IM and Rosenfeld D. Clouds-Aerosols-Precipitation Satellite Analysis Tool (CAPSAT). Atmos. Chem. Phys. 2008; 8; 6739–6753.</mixed-citation>
                    </ref>
                                    <ref id="ref9">
                        <label>9</label>
                        <mixed-citation publication-type="journal">[8] Lohmann U and Feichter J Global indirect aerosol effects: a review. Atmospheric Chemistry and Physics 2005; 5 3; 715–737.</mixed-citation>
                    </ref>
                                    <ref id="ref10">
                        <label>10</label>
                        <mixed-citation publication-type="journal">[9] Moore BJ, Neiman PJ, Ralph FM and Barthold F. Physical processes associated with heavy ﬂooding rainfall in Nashville, Tennessee, and vicinity during 1–2 May 2010: 	The role of an atmospheric river andmesoscale convective systems. Mon. Weather 	Rev. 2012; 140; 358–378.</mixed-citation>
                    </ref>
                                    <ref id="ref11">
                        <label>11</label>
                        <mixed-citation publication-type="journal">[10] Naruse T, Sakai H and Inoue K. Aeolian dust origin of fine quartz in selected soils. Japan Quat Res (Tokyo) 1986; 24; 295–300.</mixed-citation>
                    </ref>
                                    <ref id="ref12">
                        <label>12</label>
                        <mixed-citation publication-type="journal">[11] Notaro M, Alkolibi F, Fadda E, and Bakhrjy F. Trajectory analysis of Saudi Arabian dust storms. J. Geophys. Res. Atmos. 2013; 118; 6028–6043.</mixed-citation>
                    </ref>
                                    <ref id="ref13">
                        <label>13</label>
                        <mixed-citation publication-type="journal">[12] Orlovsky L, Orlovsky N and Durdyev A. Dust storms in Turkmenistan. Journal of Arid Environments 2005; 60; 83–97.</mixed-citation>
                    </ref>
                                    <ref id="ref14">
                        <label>14</label>
                        <mixed-citation publication-type="journal">[13] Prospero JM, Ginoux P, Torres O, Nicholson S, Gill TE. Environmental characterization of global sources of atmospheric soil dust derived from the NIMBUS&amp;TOMS absorbing aerosol product. Rev. Geophys. 2002; 40; 1 2-1-2-31.</mixed-citation>
                    </ref>
                                    <ref id="ref15">
                        <label>15</label>
                        <mixed-citation publication-type="journal">[14] Rolph GD 2012 Real-time Environmental Applications and DisplaysYstem (READY) website (http://ready.arl.noaa.gov); NOAA AirResources Laboratory, Silver Spring, 	MD.</mixed-citation>
                    </ref>
                                    <ref id="ref16">
                        <label>16</label>
                        <mixed-citation publication-type="journal">[15] Solomos S, Ansmann A, Mamouri RE, Binietoglou I, Patlakas P, Marinou E and 	Amiridis V. Remote sensing and modelling analysis of the extreme dust storm 	hitting the Middle East and eastern Mediterranean in September 2015. Atmos. Chem. Phys. 2017; 17; 4063-4079.</mixed-citation>
                    </ref>
                                    <ref id="ref17">
                        <label>17</label>
                        <mixed-citation publication-type="journal">[16] Shen H, Abuduwaili J, Ma L and Samat A. Remote sensing-based land surface change identification and prediction in the Aral Sea bed, Central Asia. International Journal 	of Environmental Science and Technology 2018; 1-16.</mixed-citation>
                    </ref>
                                    <ref id="ref18">
                        <label>18</label>
                        <mixed-citation publication-type="journal">[17] https://www.arl.noaa.gov/hysplit/hysplit/</mixed-citation>
                    </ref>
                                    <ref id="ref19">
                        <label>19</label>
                        <mixed-citation publication-type="journal">[18] https://modis.gsfc.nasa.gov/about/</mixed-citation>
                    </ref>
                            </ref-list>
                    </back>
    </article>
