000890231 001__ 890231
000890231 005__ 20240712101031.0
000890231 0247_ $$2doi$$a10.1080/16000889.2019.1695349
000890231 0247_ $$2ISSN$$a0280-6509
000890231 0247_ $$2ISSN$$a1600-0889
000890231 0247_ $$2Handle$$a2128/27049
000890231 0247_ $$2WOS$$aWOS:000600212000001
000890231 037__ $$aFZJ-2021-00818
000890231 082__ $$a550
000890231 1001_ $$0P:(DE-HGF)0$$aZanatta, Marco$$b0$$eCorresponding author
000890231 245__ $$aAirborne survey of trace gases and aerosols over the Southern Baltic Sea: from clean marine boundary layer to shipping corridor effect
000890231 260__ $$aAbingdon$$bTaylor & Francis$$c2020
000890231 3367_ $$2DRIVER$$aarticle
000890231 3367_ $$2DataCite$$aOutput Types/Journal article
000890231 3367_ $$0PUB:(DE-HGF)16$$2PUB:(DE-HGF)$$aJournal Article$$bjournal$$mjournal$$s1611658249_22258
000890231 3367_ $$2BibTeX$$aARTICLE
000890231 3367_ $$2ORCID$$aJOURNAL_ARTICLE
000890231 3367_ $$00$$2EndNote$$aJournal Article
000890231 520__ $$aThe influence of shipping on air quality over the Southern Baltic Sea was investigated by characterizing the horizontal and vertical distribution of aerosols and trace gases using airborne measurements in the summer of 2015. Generally, continental and anthropogenic emissions affected the vertical distribution of atmospheric pollutants, leading to pronounced stratification in and above the marine boundary layer and controlling the aerosol extinction. Marine traffic along the shipping corridor “Kadet Fairway” in the Arkona Basin is shown to influence the presence and properties of both trace gases and aerosol particles in the lowest atmospheric layer. Total particle number concentration and NOy mixing ratio increased in the corridor plumes, relative to background, by a factor 1.55 and 3.45, respectively. Titration, triggered by the enhanced presence of nitrogen compounds, led to a median ozone depletion of 19% in the corridor plumes. The enforcement of the Sulphur Emission Control Area (SECA) might be responsible for the minor sulphur dioxide increase (20%) in the corridor plumes. Ship traffic caused a minor enhancement of black carbon mass concentration, estimated to be around 10%. The study of individual ship plumes indicated that ship emitted aerosol was substantially different from background aerosol: fresh ship exhaust was preferentially enriched in aerosol particles with diameters below 100 nm and in black carbon particles with core diameters above 300-400 nm. With the present work the impact of marine traffic on the concentration and properties of atmospheric components within the marine boundary layer over the open water of the Southern Baltic Sea is assessed with airborne observations for the first time. Due to the high uncertainty affecting the estimations of ship emissions, this dataset represents a valuable reference for the assessment of ship emission inventories and related environmental-climatic impacts on the Southern Baltic Sea
000890231 536__ $$0G:(DE-HGF)POF3-243$$a243 - Tropospheric trace substances and their transformation processes (POF3-243)$$cPOF3-243$$fPOF III$$x0
000890231 588__ $$aDataset connected to CrossRef
000890231 7001_ $$0P:(DE-HGF)0$$aBozem, Heiko$$b1
000890231 7001_ $$0P:(DE-HGF)0$$aKöllner, Franziska$$b2
000890231 7001_ $$0P:(DE-Juel1)130949$$aSchneider, Johannes$$b3$$ufzj
000890231 7001_ $$0P:(DE-HGF)0$$aKunkel, Daniel$$b4
000890231 7001_ $$0P:(DE-HGF)0$$aHoor, Peter$$b5
000890231 7001_ $$0P:(DE-Juel1)164186$$ade Faria, Julia$$b6$$ufzj
000890231 7001_ $$0P:(DE-Juel1)136669$$aPetzold, Andreas$$b7$$ufzj
000890231 7001_ $$0P:(DE-Juel1)159541$$aBundke, Ulrich$$b8$$ufzj
000890231 7001_ $$0P:(DE-HGF)0$$aHayden, Katherine$$b9
000890231 7001_ $$0P:(DE-HGF)0$$aStaebler, Ralf M.$$b10
000890231 7001_ $$0P:(DE-HGF)0$$aSchulz, Hannes$$b11
000890231 7001_ $$0P:(DE-HGF)0$$aHerber, Andreas B.$$b12
000890231 773__ $$0PERI:(DE-600)2026992-4$$a10.1080/16000889.2019.1695349$$gVol. 72, no. 1, p. 1 - 24$$n1$$p1 - 24$$tTellus / B$$v72$$x1600-0889$$y2020
000890231 8564_ $$uhttps://juser.fz-juelich.de/record/890231/files/Airborne%20survey%20of%20trace%20gases%20and%20aerosols%20over%20the%20Southern%20Baltic%20Sea%20from%20clean%20marine%20boundary%20layer%20to%20shipping%20corridor%20effect.pdf$$yOpenAccess
000890231 909CO $$ooai:juser.fz-juelich.de:890231$$pdnbdelivery$$pVDB$$pVDB:Earth_Environment$$pdriver$$popen_access$$popenaire
000890231 9101_ $$0I:(DE-588b)5008462-8$$6P:(DE-Juel1)130949$$aForschungszentrum Jülich$$b3$$kFZJ
000890231 9101_ $$0I:(DE-588b)5008462-8$$6P:(DE-Juel1)164186$$aForschungszentrum Jülich$$b6$$kFZJ
000890231 9101_ $$0I:(DE-588b)5008462-8$$6P:(DE-Juel1)136669$$aForschungszentrum Jülich$$b7$$kFZJ
000890231 9101_ $$0I:(DE-588b)5008462-8$$6P:(DE-Juel1)159541$$aForschungszentrum Jülich$$b8$$kFZJ
000890231 9131_ $$0G:(DE-HGF)POF3-243$$1G:(DE-HGF)POF3-240$$2G:(DE-HGF)POF3-200$$3G:(DE-HGF)POF3$$4G:(DE-HGF)POF$$aDE-HGF$$bErde und Umwelt$$lAtmosphäre und Klima$$vTropospheric trace substances and their transformation processes$$x0
000890231 9141_ $$y2020
000890231 915__ $$0StatID:(DE-HGF)0200$$2StatID$$aDBCoverage$$bSCOPUS$$d2020-09-04
000890231 915__ $$0StatID:(DE-HGF)0160$$2StatID$$aDBCoverage$$bEssential Science Indicators$$d2020-09-04
000890231 915__ $$0StatID:(DE-HGF)1050$$2StatID$$aDBCoverage$$bBIOSIS Previews$$d2020-09-04
000890231 915__ $$0StatID:(DE-HGF)1190$$2StatID$$aDBCoverage$$bBiological Abstracts$$d2020-09-04
000890231 915__ $$0StatID:(DE-HGF)0600$$2StatID$$aDBCoverage$$bEbsco Academic Search$$d2020-09-04
000890231 915__ $$0StatID:(DE-HGF)0100$$2StatID$$aJCR$$bTELLUS B : 2018$$d2020-09-04
000890231 915__ $$0LIC:(DE-HGF)CCBYNC4$$2HGFVOC$$aCreative Commons Attribution-NonCommercial CC BY-NC 4.0
000890231 915__ $$0StatID:(DE-HGF)0501$$2StatID$$aDBCoverage$$bDOAJ Seal$$d2020-09-04
000890231 915__ $$0StatID:(DE-HGF)0500$$2StatID$$aDBCoverage$$bDOAJ$$d2020-09-04
000890231 915__ $$0StatID:(DE-HGF)0113$$2StatID$$aWoS$$bScience Citation Index Expanded$$d2020-09-04
000890231 915__ $$0StatID:(DE-HGF)0700$$2StatID$$aFees$$d2020-09-04
000890231 915__ $$0StatID:(DE-HGF)0150$$2StatID$$aDBCoverage$$bWeb of Science Core Collection$$d2020-09-04
000890231 915__ $$0StatID:(DE-HGF)9900$$2StatID$$aIF < 5$$d2020-09-04
000890231 915__ $$0StatID:(DE-HGF)0510$$2StatID$$aOpenAccess
000890231 915__ $$0StatID:(DE-HGF)0030$$2StatID$$aPeer Review$$bDOAJ : Blind peer review$$d2020-09-04
000890231 915__ $$0StatID:(DE-HGF)0561$$2StatID$$aArticle Processing Charges$$d2020-09-04
000890231 915__ $$0StatID:(DE-HGF)1150$$2StatID$$aDBCoverage$$bCurrent Contents - Physical, Chemical and Earth Sciences$$d2020-09-04
000890231 915__ $$0StatID:(DE-HGF)0300$$2StatID$$aDBCoverage$$bMedline$$d2020-09-04
000890231 915__ $$0StatID:(DE-HGF)0199$$2StatID$$aDBCoverage$$bClarivate Analytics Master Journal List$$d2020-09-04
000890231 9201_ $$0I:(DE-Juel1)IEK-8-20101013$$kIEK-8$$lTroposphäre$$x0
000890231 9801_ $$aFullTexts
000890231 980__ $$ajournal
000890231 980__ $$aVDB
000890231 980__ $$aUNRESTRICTED
000890231 980__ $$aI:(DE-Juel1)IEK-8-20101013
000890231 981__ $$aI:(DE-Juel1)ICE-3-20101013