Bioaerosol field measurements: Challenges and perspectives in outdoor studies Tina Šantl-Temkiv, Branko Sikoparija, Teruya Maki, Federico Carotenuto, Pierre Amato, Maosheng Yao, Cindy E. Morris, Russ Schnell, Ruprecht Jaenicke, Christopher Pöhlker, et al.
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Tina Šantl-Temkiv, Branko Sikoparija, Teruya Maki, Federico Carotenuto, Pierre Amato, et al.. Bioaerosol field measurements: Challenges and perspectives in outdoor studies. Aerosol Science and Technology, Taylor & Francis, 2020, 54, pp.520-546. 10.1080/02786826.2019.1676395. hal-02319383
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Distributed under a Creative Commons Attribution - NonCommercial - NoDerivatives| 4.0 International License Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, To linktothisarticle: To Technology, DOI: Measurements: ChallengesandPerspectivesinOutdoorStudies,AerosolScience P Pierre Amato,MaoshengYao,CindyE.Morris,RussSchnell,RuprechtJaenicke,Christopher citethisarticle: To Huffman ChristopherP Jaenicke, CindyE.Morris,RussSchnell,Ruprecht Amato,MaoshengYao, Pierre Tina Perspectives inOutdoorStudies Challengesand FieldMeasurements: Bioaerosol ö hlker, PaulJ.DeMott,ThomasC.Hill&AlexHuffman(2019):BioaerosolField Š ISSN: 0278-6826(Print)1521-7388(Online)Journalhomepage: ScienceandTechnology Aerosol antl-Temkiv, Branko Sikoparija, Teruya Maki,FedericoCarotenuto, Teruya Sikoparija, Branko antl-Temkiv, View Crossmark data Crossmark View articles related View 33 Article views: Submit yourarticletothisjournal Oct 2019. Accepted authorversionpostedonline:08 2019, 1-79. ,DOI: 10.1080/02786826.2019.1676395 https://www.tandfonline.com/action/journalInformation?journalCode=uast20 10.1080/02786826.2019.1676395 Tina Comment citer cedocument: Full Terms &Conditionsofaccess andusecanbefoundat Full Terms
https://doi.org/10.1080/02786826.2019.1676395 Š antl-Temkiv, BrankoSikoparija,TeruyaMaki,FedericoCarotenuto, ö hlker, PaulJ.DeMott,ThomasC.Hill&Alex hlker,
https://www.tandfonline.com/loi/uast20 Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and 10 Montfavet, France 9 Environmental Sciencesand Engineering,University,Beijing, Peking China 8 7 6 5 Novi Sad, NoviSad, Serbia 4 Change,Climate 3 2 Aarhus, 1 Christopher Pöhlker Amato ŠantlTina Bioaerosol Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, Plant PathologyPlant Res LaboratoryState Key Joint Environmental andPollution Control, Simulation of College of Université NationalItaly Research of Institute (CNR), Council ofBioeconomy (IBE),Italy BioSenseInstitute DepartmentInterdisciplinary Science, Aarhus ofEnvironmental iCLIMATE University for Centre Department Astronomy, ofPhysicsand Stellar Astrophysics Centre Aarhus University,Department ofBioscience, Microbiology Arctic Section and Research Center Institute National OceanicAtmospheric Boulder, and Organization; Colorado, USA P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, 7 Denmark , Maosheng ofEngineering, ScienceandUniversity, Kanazawa Japan Kakuma, Clermont Auvergne, CNRS, SIGMA Clermont, ICCF,Clermont Auvergne,Clermont, SIGMA CNRS, C - Temkiv Field 2019, 1-79. ,DOI: 10.1080/02786826.2019.1676395 Roskilde, Roskilde,
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2019, 1-79. ,DOI: 10.1080/02786826.2019.1676395 airborne airborne in desert habitatsin desert ,
such as plants as such Accepted Manuscript bacteria (Sterflinger and Piñar(Sterflinger 2013)
and animal pathogen transmission, the distribution thedistribution animalofand pathogen allergens transmission, or nosignificant betweenenvironments differences thetwo fungal bacteria Comment citer cedocument: , derived lessextreme from
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Issues Issues
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Accepted Manuscriptrelated measurements tobioaerosol - temporal resolution term temporalterm variations inbioaerosolsfrequently have been observed fungal frequently andcan bacteria to spores after rainfall duringdue increase and (Šikoparija etet al.2018b;Healyet al.2014; Huffman al.2012;Fanget al. Comment citer cedocument: , season . (Joung et al. 2017; Morris et(Joung etal.2017;Rathnayakeet al.2017; al.2017; Conen rological factors rological factors
,
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Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and microbial aerosols, downstream varyingfrom ~10 the atmosphere (e.g. and single diversity ofmicroorganisms Therefore,cultiva damaged,growth orsuitable orappropriate cultivationbecause techniques media were notused. 2007b) bacteriaculturableafter fromcollection the atmosphere <1%e.g. range widely,from cultivated thefact efficiently,areviable that despite they aerosols waters and atmospheric (e.g. long for thereferenceinvestigating inthe methods communities environment, microbial including and2015; Holt Bennett Huffman Xuet al.2011) et 2014; al.2012; (minutes orless) and certainwindows into atmospheric processes emission byat providing data high resolution time sensorstime thatdetectrelativelyand continuously a bioaerosols occurexpression, shorter onago timethan thus scales much thesamplingand could unnoticed. Real 2007) Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, [ [ii: P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, i . ii Finally, the speed of microbial atmosphericFinally, and activity, the speed asgene dilution growth such or
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to ~10 Accepted Manuscript t he Bowers et al.2009;DeLeon
should comprise should high volume filter samplers volumehigh filter samplers 6
Comment citer cedocument: cells (T. Šantl biomass m - 3 independent techn
of air ] - Lighthart 1997) Temkiv et al. 2013; Temkiv et 2013; Temkiv etal.2012) al. In
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for for - Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and use of impingers allows ora samplinginphysiological thus liquid fixative, preserving in bioaerosols organisms, for examplebypassing large vol cultivation allow relevant applications, suchas downstream including viability, physiological state,ice the chemical lower information from suffer strategy devices for resolution lower methods can qualitative or semi spectrometricanalyzers)as acom 2012) et al.2017;Temkivet verify are thatmeasurements notinfluenced by contamination et al.2013;Temkivetal Lever2018; al. et 2015) sterilization contamination issues A areas,characterized biomass withlow impingers Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, erosol concentrators of differenterosol concentrators of design in [ P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, i - v situ (Kim et al.2001) : Preserving storage duringsampling, state the insitu
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Accepted Manuscript- quantitative results at quantitative . Another implication of thelow . , sterile techniques, handling when and . 2012) . the sampling equipment . Comment citer cedocument:
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The . Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and microbial etWeil al.2017;Mazar et al.2016) represent oflocal amixture andlong 2002) electrostatic that state preserveauthentic precipitation) thetheir biologicalrely tomineralthus grains) attached ‘soft’ dust particle (e.g. techniques sampling on quantification ofaerosols. bacterial Microscopic states investigations ofthe(e.g. mixing bioaerosol Lighthart(Turnbull et al.1998; etal. 1993) aerosolsexample arerarely for floating, butoftenattached free clumped or together toother particles, of additional freezing/thawing ofsamples. frozen for uptoseveral days. with frozen ice keep can packs samplescool analyses, future might but culturability affect assessment. (< Cryopreservation Inaddition, numerous microorganismsto grow at therefore altering are known 4°C, quantitati the samples at4°C,whichisacommon short 1998; Nemeck evidence the ice that their Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, [ An additional challenge characterizingmixing theircomplex is to bioaerosols Bacterial state. i: P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, in situ .
Wind
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Emission
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(Suski et(Suski al.2018) modelled .
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transport microbial populations into the into transport populations microbial freeatmosphereand induce ixing process
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or , Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and While While attempted cryopumps Ligler(Andersonet al.1999; et al.1998) etal. 2015)al. Smith 2016; et al.2008,2012;Ayloret al.2011;Gonzalez 2011) dishes cases new to placed indisturbance can thegroundtransport, whileavoiding 2015) Yamaguchial. Kourtev 2012; et et al.2011) by aircraft altitude troposphere, and crucial information identityto provide onthe amount ofbioaerosolsbeing transported spatial variabilityBioaerosol particularly inasinglesample. profiles, spanning thelower across throughair,allow for they of the also collection volumes ofair t spatial dynamics in contamination also plume should betakenexhaust toavoid INPanalys Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, [ also ii: P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, , ,
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controlled balloons controlled both horizontal (i.e. transects)horizontal and vertical(i.e.both profiles) have been have could influencecould (Powers et al. 2018; Lateran et et(Powers al.2016;Techy al.2018; al. Yang 2010; etet al.2008) ] - (Jimenez free areas to ensure representative measurementsfreerepresentative toensure areas Aerial vessels such as high
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Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and multiple scientificmultiple disciplines. scientific need climate change, cover/use change land interests are 2) 2015) and are climate effects, related toseveral which U The increased bioaerosol in interest 4. transcontinental example, viable airborne laboratories since they to are able Maki et al.2008;Kakikawa et al.2008) collect bioaerosols onfilters Harris2014; Yanget and al.2008; etal.Rogers Meier 2002; lower carried troposphere,explore devices balloon can dimensions airborne allowing outdoormeasurements, 2019) opticalgive wouldbe methods able to real Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato,
areguided by a varietyof motivations
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by real (Maki et al. 2017a, 2015, 2013; Chen et al. 2011; Iwasaka 2013;Chenetal. al.2011; (Maki 2017a,2015, et et al.2009; concern of several
some combination of some combination - time time concerning concerning nited States s generally
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Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, cytosolic uponcell content) processes’‘multiplication inthe atmosphere, function of atmosphericresidence d survival, aging,activity their isnecessaryit to to bridge strength distributions, emission thesource vertical thebioaerosol andhorizontal with relatethis environme v distributed [2] such as thunderstorms, caused by wheat harvesting well as orprocessing silage) propagules wind), orrelease passive ofbioaerosolsdue to marine and terrestrial sources question atmosphere challenging to sources [1] etermin
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at the s e 2019, 1-79. ,DOI: 10.1080/02786826.2019.1676395
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In order , (ii and how - are i ) Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, of impact different suchas functions, theirhygroscopicityand their bioaerosol nucleation, allergenic [4] orbacterialassociatedinvasion ofplant, fungal, and species, changes inbio asrelatedassess changes distribution, inbioaerosol togeographyairborne pollination, of agricultur Changes ofasecology plantpathogens, related patterns and indispersal natural toboth bioaerosol through emission driven alterationof landuse by climateactivity. and human been patter proposed that airborne timing focussing onin change, cycl Continued changing climate, and [3] bioaerosols thatas can allergens and serve in clouddroplets, airborne microorganisms
Changes in Atmospheric agingAtmospheric ing has been altered byactivitiesingaltered ( been human has , of arechanging pollination
asability wellhosts. as new their tocolonize surfaces or alterations human 2019, 1-79. ,DOI: 10.1080/02786826.2019.1676395 e, arealso Thus,e, effected. monitoring inavariety requiredecosystem is of types to
Accepted Manuscriptstudies are - distribution depth bioaerosol sites. atdepth studies ‘pristine’ allergies or reproduction Comment citer cedocument: in
the waterthe cycle, required : as a result,as
There is a necessity to understand how atmospheric agingaffectsThere howatmospheric isanecessitytounderstand the , ecology, agriculture, ns in precipitationns in andthe hydrological be influenced cyclemay by :
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. Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, butalso individuals) to viability. relate tonaturally from questions These notonly aerosol dispersed sick (e.g. pathogens can travelwithi role of viral andbacterial aerosol [7] health. mult change,Longer and urban urbanization, pollution. required allergic withclimate from influence of factorsassociated tounderstand diseases physicalan properties atmospheric soot, combustion reac allergies inrecent and inurban decades areas [6] environme and nucleation potential organic and compounds, inorganic activity water availability inthe atmosphere. [5]
Metabolic activity Transport ofTransport humanpathogens of allergiesUrbanization iple factors
outdoor
in airborne microorganisms andin airbornetheir microorganisms thus ability to 2019, 1-79. ,DOI: 10.1080/02786826.2019.1676395
Accepted Manuscriptn ts.
air for lesswell is understood,air ofpathogens dispersal including how fardifferent are Comment citer cedocument:
also required to study the complex relationships thatinfluencealso requiredtostudycomplex the human : d emission rates Additional from topollution. stud d emission plantsexposed
This unique aspect unique beThis should evaluated ofbioaerosols as of afunction intentionally ,
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as well as (i) budgets of atmo budgets of to human hosts to human hosts
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are (e.g. Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and fractionation, efficiency, choi microbiologicalevents theair in are difficult capture. to The research questions interactions they with have can representativea challenge sample divers inlight is ofthe The atmosphere isdynamic Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, ce ofsampling P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, 4.2. of distributions streamline ofthe cloud efforts most for inclusion necessitates cycle,meas expanded of input of bio activation andonbioaerosol ice surfaces nucleation effects colonization. on ice their spatiotemporal distribution thus have health impacts. t hygroscopicity, understanding of [ he hygroscopic of properties 8 ] Climate nucleation nucleation
Technical - INPs andevolution, cloud on cloudradiative formation the hydrological forcing, and 2019, 1-79. ,DOI: 10.1080/02786826.2019.1676395
Accepted Manuscript -
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- Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, organism classe improvedof understanding specific periods at high generally resolution time (but withlow [7] bioaerosols [6] of airborne well established is in Europe pollen that purpose throughdistributed science citizen [5] meteorological, chemical inlargebioaerosol measurements well measurement complement docum campaignsto the to link broad [4]
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Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and collaborative funding opportunities meet community cross and network, disciplines and inorder approachesand exchange to identify ideas Consequently could thatuse techniques, beapplied moreallergen such traditional tofields and as pathogen detection. molecular microbiology techniques currently u particles example, theidea for ofmonitoringnetworksallergen quantifying initiated airborne ideas,and approaches technicalthe different advances studying between disciplines to could designchamber,field laboratory complementary andexperiments inmicrobiology,expertise physics,aerosol meteorology, and chemistry, aerosol bioaerosol engineers strengthemission anddistribution. obtain a mechanistic whichiscrucial understandingofbioaerosolfluxes, forecasting for their future research fields. for carrying out the lackbetween ofcollaboration approachresearch questionsfrom differentAsa result perspectives. proprietaryhave various These somewhatindependently, developed innature. communities and thus behind security clearance development detection of improved against technologies agents ofbiowarfare hidden isfrequently Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, interdisciplinaryefforts, cross P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, eventually
could be applied tostudyingapplied pathogeniccouldclimatic and be oradvanced aspects ofbioaerosols , we D outdoor 2019, 1-79. ,DOI: 10.1080/02786826.2019.1676395 introduce edicated field edicated
Accepted identifyneedor where establishappropriate anew to an platform, researcher Manuscript bioaerosol field studies s,
Comment citer cedocument:
exciting an d information related toagriculturald informationcan related practices orfarming be measurements besupported should by chamber order experiments, in to - community discussion andcommunity promoteof collaboration exchange discussion should communities. communities.
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to Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and charges Planck DigitalLibrarywereMax paid the by (MPDL). Science Scholars Plancksupport by theMax Society(MPG). TechnologicalIII oftheRepublic (project ofSerbia no. Development 44006). (researchgrant 23175) Aarhus University National Research (Grant Foundation DNRF106, no.: agreement tothe Stellar Astrophysics Centre, Louis,Conference September in Missouri 2018. inSt Bioaerosol Working andInternational Group theBioaerosol at StandardizationWorkshop the Aerosol and Perspectives The authors organizers acknowledge “ of issue special this Acknowledgements Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, s
Fund (21725701). and Mathematics and the Max Planck Institute Planck and theMax forand Mathematics Chemi 2019, 1-79. ,DOI: 10.1080/02786826.2019.1676395 ” , including Shanna, including Ratnesar Accepted Manuscript AUFF), by program (AUFF the Nova
. BS recognizesBS The Science Ministry supportfrom ofEducation, and Comment citer cedocument:
JAH JAH
acknowledges by Denver support CollegeNatural University of of
MY is supported by the NSFC Distinguished supported by Young NSFC MY is the - Shumate and Alex Huffman, and Alex Shumate
TST - E
Bioaerosol Research: Methods, - is grateful for the 2015
- FLS s try. - 9
Open accessOpen article processing - 1 0)
as well as and support byThe Danish CP acknowledgesCP
by the Villum Fondenby theVillum
the AAAR AAAR Challenges , Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and Amato, P., Parazols,Sancelme,Laj,Amato, M., P., M.,Mailhot,G.,and (2007b). Delort, P., A.M. Joly,Amato, P., M.,Schaupp, A. Y.,and Attard, O.,Morris, C., Brunet, Delort, E.,Möhler, C.E., Joly,Amato, P., L., M.,Besaury, N.,Moné,L., A., A.I., Oudart, Taib, Deguillaume, Delort, A. Demeer,MartinAmato,Melaouhi, S., P., F., A.,Fontanella, Besaury,L.,Amato, P., M.,Penau Joly, Ludwig,Amann, R.I.,and Schleifer,Phylogenetic W., K.H. (1995). identification detection and insitu Aller, and C.J., Kemp, Kuznetsova, Jahns, P.F. M.R., (2005).surfaceAller, The J.Y., a microlayer as sea References Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, groups and growthgroupsand atlowtemperatures. abilities Microorganismsfrom the phase water troposphe isolated of Atmos. Chem. Phys., (2015). Survivaln andice water. Debroas,(2017). Active microorganisms among D.extremely thrive incloud communities diverse biotransformation micro by Delort, A.M.(20 Metatranscriptomic exploration of inclouds. microbial functioning of microbial individual cells cultivation. without 347. polysaccharidic sea andcomponentsaerosol. proteinaceous of spray Murray, Coffman,P.K., D.J., and (2017). B.J., Knopf, D.A. Size source enrichment andbacterial ofviral aerosols. marine in
J.Y., Radway,T.W., Bothe, Vaillancourt, W.P., Wilson, D.W., J.Y., Kilthau, R.D.,Quinn, J.A.C.,
PLoS One,PLoS
2019, 1-79. ,DOI: 10.1080/02786826.2019.1676395 Accepted Manuscript 07a). A fate A foracids,07a). organic formaldehydecloud in andwater: methanol their
12(8):e0182869.
15(11):6455 Comment citer cedocument: ucleation chamber. activitysimulation as bacteria a in aerosols cloud of - organisms. –
d, B., Deguillaume, L.,B., Deguillaume, A.M. (2019).d, Delort, and
6465.
Atmos. Chem. Phys.,
FEMS Microbiol. Ecol.,FEMS Microbiol. Rev., - Biesse, A.
ric clouds at the Puyatric the de clouds Dôme: Major J. Aerosol Sci.,J. Aerosol
(7):4159 -
resolved characterizationresolved of the 59(1):143 - S., Sancelme,Laj,S., M.,and P., Sci. Rep.,
Atmos. Environ., Atmos. – 4169.
59(2):242
36(5 –
69.
9(1):1
– 6):801 – – 254. 12.
(154):331 –
812. - M., and M., - M. M.
–
Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and Aylor, D.E., Schmale III, D.G., Shields, E.J., Newcomb, M., and Nappo, C.J. (2011) Newcomb,Aylor,III, D.G.,D.E., E.J., and M., SchmaleShields, Nappo, C.J. H.,Niedermeier, Augustin,B., D., Wex, H., Hartmann, Grothe, S., Pummer, Attard, A. E.,Yang,Delort, H., Ignatova,Ariya, O.,Amyot, Nepotchatykh, and P.A., (2002). O., M. Microbiologicaldegradation of Lee,Archer,Lee, S.D.J., Caruso, T.,Maki, T.,C.K.,Cary,Cowan,F.T., K.C., D.A., S.C., and Maestre, (1997).Andreae, Atmospheric M.O.and P.J. Crutzen, Biogeochemical aerosols: sources a Andreae, beforeAerosols pollution. M.O.(2007). Ligler, D.S.,Whelan,Anderson, Cuttino, J.P., G.P., King, K.D., F.S., MacKrell,Bovais, J.F., C.S., Parazols,Sancelme,Laj,Amato, M., P., G., M.,Mailhot, and Delort, P., A. Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, modeling. potato late blight inthe atmosphereLagrangian pathogen aerial and unmanned using vehicles washingwater. Ignatius,T., Voigtländer, K.,and J., Immersion Stratmann,(2013). F. freezing pollen ofbirch Chem. Phys., (2012). Effectsatmospheric ice ofconditions on activity nucleation Pseudomonas. of atmospheric organic compounds. Microbiol., Nat. Pointing, S.B. (2019). limitation to isolatedAnta Airborne microbial transport atmospheric chemistry. biosensor. (1999). BiologicalIndyke,R.J. and Foch, D.K., agent detec 41(37):8253 oceanic source of
Agric. For. Meteorol., F. Anal. Chem. Technol.,F. Anal.Chem. 2019, 1-79. ,DOI: 10.1080/02786826.2019.1676395 –
8263. Accepted12:10667 Manuscript
Atmos. Chem. Phys.,
(4):925 micro
Comment citer cedocument: –
Science (80 Science - – 10677. organisms at for the cloudPuy Dôme water (France). de 932. - M.,
Amato, P., Pöschl, U., Glaux, C.,Koop,T.,and U., Morris, Pöschl, Glaux, Amato, C.E. P.,
151(2):251 Geophys. Res. Lett.,
-
. ).,.
3(4 (13):10989
-- 276(5315):1052 5):307 –
Science(80 260. – – 314. 11003.
29(22):34
– - 1058. . ).,. tion with the use ofan withthe use airbornetion
315(5808):50
- 1 - 34 – - 4. M. (2007c). An important M. (2007c). An important S., Tomsche, L., Tomsche,S., Clauss,
– 51. rctic habitats. soil . Tracking the
Atmos. Environ.,
nd role in role in nd Atmos.
Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and Bigg, E.K. (1996). IceBigg, E.K. forming (1996). nuclei inthe hi Behr Bauer, H., Schuell K.S., Pollard, Barberán,Ladau, Leff,A., Menninger, and J., J.W., R.R., Fierer, H.L., N. Dunn, (2015). Barbaro,T., Zangrando, E., M.,Piazza, R.,Barbante, Kirchgeorg, Vecchiato, R., C.,and A. Gambaro, Banchi,Lazzarin, Stanković,Moretti, D.,Ametrano, F., P., O.,Gabrielli, Verardo, C.G., E., Borney, S., Baldocchi,B.B., D.D.,Hicks,Biosphereand Measuring T.P.(1988). Meyers, Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, enfeld, M.J., Moore, R.H., Hostetler, C.A., Graff, J., Gaube, P., Russell, L.M., Hostetler, R.H., Gaube, Moore, enfeld, C.A.,Graff, Chen, Russell, G.,Doney, J., P., M.J., 48(2):223 Overview. and(NAAMES): Mission Science Motive L.Ziemba,Martin, M.Y.,andAtlantic Aerosol (2019). North The and Ecosystem Marine Study Hu,Y., Sa Hair, Redemann,S., J.W., Janz, J., Morison, F., Anderson, Scarino, Quinn,P.K., B., A.J., Crosbie, Chowdhary, E.,Ferrare, J., R., Carlson, Halsey,Harvey, C., K., Hu, C.,Karp E.L., Westberry,Bates,Bell,T.S., Boss,T.K., T.G.,Br K.D., Bidle, E.S., Liu, Giovannoni,L.M., S., S.C., H.,Proctor, Baetge, C.,Bolaños, N., Davie the urban atmosphericaerosol. Significantof fungal carbon and spores contributions tothemassbalance aerosol totheorganic of 112(18):5756 Continental aerosol.(2015). Sugars inAntarctic uncovers airborneItaly. fungaldiversityofmixed samplesin M.F.,F., M.,Pallavicini, Tassan, A.,and Tretiach, Muggia, L. of B iologically Related Gasesiologically Related Micrometeorological with Methods. – 233. - 2019, 1-79. ,DOI: 10.1080/02786826.2019.1676395 scale ofdust distributions er, E., Weinke, G.,I.L.,Weinke, Hitzenberger, Berger, E.,A., R.,Marr, er, H.(2008). and Puxbaum, Accepted Manuscript– 61.
Comment citer cedocument:
Atmos. Environ.,
Atmos. E - associatedbacteriaand fungi. ghArctic. nviron., ltzman, M.,Siegel, D.A., E.,Shook, Wisthaler,A.,
42(22):5542 -
Tellus, Ser.Tellus, BChem. Phys. Meteorol., Boss, L.,Boss, M.,Menden Kleb,
118:135 Front. Mar.Sci.,
– PLoS One, PLoS – 5549. (2018). metabarcoding DNA 144.
Ecology,
ooks, S.D., Cairns,ooks, S.D., B.,
Proc. Natl. Acad.Natl. Sci., Proc. .
- 13(3):1 Atmosphere Exchanges -
69(5):1331 Martin, C., - – Deuer, S., 20.
– 1340.
Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and Bowers, R.M.,McLetchie,Knight,Fierer, S., (2011). andSpatial N. R., variability ina Bowers, Lauber,Bowers, R.M., C.L., C Wiedinmyer, Bowers, R.M., Boucher, Bretherton, D.,Artaxo,P., O., Feingold, Kerminen,C., Randall, P., G.,Forster, V. andBigg,S., Morris, E.K.,C Soubeyrand, Bigg,Leck, E.K. and Cloud (2001). C. IceBigg,Remote ConcentrationsAreas. E.K. Nucleus (1973). in Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, bacterial atcommunities ahigh their potential toact asatmospheric ice nuclei. Fierer, of airborne Characterization N. (2009). ata communities microbial high Sci. Technol., Seasonal Variability inBacterialand Fungal Diversity the Near of NY,Kingdom USA. York, andNew Xia,V.BexNauels, andP.M.(eds.)]. Y. Midgley Change[Stocker,on Climate D. Qin,G. T.F., ofWorkingIContribution Group Assessment tothe Fifth Zhang, andIn: Clouds X.Y. Aerosols. (2013). ChangePhysical Climate Basis. 2013:The Science Kondo, concentrations ofice andbiological rainfallsuggest nuclei a cause. 106(D23):32,155 The from time differences theice transport with edgewere lessmarked. the range
R.M., McCubbin, I.B., McCubbin, Fierer,R.M., and Seasonal N. variability A.G., Hallar, (2012). inairborne Y., Liao,Y., Lohmann, U., Stevens, Rasch, H.,Satheesh,B., P., Sherwood, and S.K., S., - Clements, N., Emerson, J.B., Wiedinmyer, C., Hannigan, M.P., andClements, Fierer, N.,Emerson, Wiedinmyer, J.B., N. M.P., C.,Hannigan, (2013). 3 but of IFN3 butofat ranged the beginning from the attheend theice pack expedition . of 2019, 1-79. ,DOI: 10.1080/02786826.2019.1676395
Accepted Manuscript 47(21):12097 - 32,166. Comment citer cedocument:
– 12106. - elevation site. -
activecentral Ocean particles over theArctic were typically
.E. (2015). Persistent after ., Hamady,Fall, A.G., M.,Hallar, R.,Knight, and R., -
S.K. M.Plattner, Tignor, Allen, J. Boschung,K. A. Atmos. Environ., Atmos. Appl. Environ.Microbiol., Appl. . CambridgeUniversity Press, Cambridge, United , Report ofthe Interg
J. Atmos. Sci., J. Atmos.
- 50:41 effects ofheavyeffects on rain -
Surface Atmosphere.Surface Atmos. Chem. Phys.,Atmos. – 49.
J. Geophys.J. Res.,
75(15):5121
30:1153 overnmental Panel - elevation site and site elevation irborne bacterial bacterial irborne – 1157. – - 5130. M.,
Environ. 15(5).
in in Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and Buters, J.T.M., Thibaudon, M., Smith, M.,Kennedy,Buters, Thibaudon, M.,Smith, J.T.M., R.,Rantio Buters, Antunes, Galveias,Bergmann, C., J.T.M., A.,K.C.,Thibaudon, M.,Galán, C.,Schmidt AnnesiButers, Prank, R., M.,Pusch, M.,Sofiev, G.,Albertini, J., Burrows, Hoose, S.M., C.,Pös Lawrence,Burrows, M,Elbert, S W., and U.Bacteria Pöschl, (2009). inthe global M.G., atmosphere Tost,H.,Kerkweg,Burrows, M.,Butler,P., Lawrence,T., Jöckel, S. A., Pöschl, U.,and (2009). M.G. Bryan, Granger,N.C., Stewart,D.,B.C. T.G.,and Amethod M., Guzik, (2014). Christner,for sampling British Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, C., and(2018).C., Oteros, and Pollen J. spore monitoring i 136(1):87 geograp L. Variationgrass of thegroup (2015). allergen 5 pollen inrelation pollen ofairborne to content Rantio H., Berger, Celenk, U., Brandao,R., S., particles ordust? 9(23):9263 Part 1:Review and synthesisofliteraturedifferent forecosystems. data ecosystems. Bacteriaglobal inthe atmosphere microbialhigh aerosols altitude balloons. using fungal networks related spores for toallergy source environments. acrosscommunities land - Standards - Lehtimäki,I.,B., Thibaudon, M., M.,Weber, and A.,Reese, G.,Sauliene,Smith, Cecchi, hic location and time in season the HIALINE working group. inseason working the and HIALINE hic location time – – 95. 2019, 1-79. ,DOI: 10.1080/02786826.2019.1676395
9280. - Atmos. Chem. Phys.,Atmos. Chem. Accepted Manuscript Institution (2019). Ambientair
Atmos. Chem. Phys.,
Comment citer cedocument: ISME J.,ISME - use types and their relationship tothe bacterialuse types of potential and their communities relationship chl, U., and Lawrence,chl,Ice U.,and marineBiogenic in M.G.(2013). air: nuclei
5(4):601
(9):9281 -
Part ofemissionsbetween 2:Modeling and transport different .
– Galan, C.,Grewling, B., Ł.,Jackowiak, Kennedy, R., 612. – 9297. - -
Sampling andairborne analysis of pollen Volumetric Hirst method.Volumetric
J. Microbi J.
n theworld. ol. Methods, - Lehtimäki, A.,Albertini, G., Reese, R., - Maesano, I.,Maesano, Antunes, Behrendt, C.,
Clin. Transl. Allergy,Clin.
J. Allergy Clin. Immunol., Clin. J. Allergy
107:161 Atmos. Chem. Phys., Atmos.
BS 16868, – 8.
.
grains and grains and
8(9). - Weber,
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Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and Coluzza, I., Coluzza, Wex,H.,Alpert, M.J., Rossi, Creamean, Bianco, J., P.A., V., Boose,Y., Dellago, C., Christner, Foreman, B.C., andC.E., R., Sands, D.C.(2008). Morris, C.M.,Cai, Chen, B.,Yamada, Kobayashi, F., Y. M.,Kim, Hamilton, Chance, andJ.F.,L.J., Hackenberg,Wilso R.J., Carpenter, Andrews,S.J., S.C., Leyronas,Carotenuto, B., T.,Gioli, F., Georgiadis, Carnelley, andIV. Anderson.,(1887). acid, T.,Haldane, A.M. carbonic J.S., The organic and matter, Triadó Cáliz, J., Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, Felgitsch,L., Fröhlich ice nucleators insnowfall. TetheredBalloon. of Collected CulturableinNorthwest over Bioaerosols Observation Dryland China: a using with ice nucleation ability. (2018). Water Atmos. Chem. Phys., modeling ofsurface 178. micro circulations. strong theairborne patternsgeneral seasonal coupled in toregional microbiome and atmospheric fromEuropeancountries. the HIALINE Results study. L. Cecchi,Prank,Bet pollen from M.,and birch M.,Sofiev, of 5 (2012). v1from Release Jackowiak, B Weber, B., Antunes, Jäger, R., C.,Brandao, C.M., S.,Grewling, Galan, S.,Berger,U., Ł., Celenk,
- organisms air,especially dwellings more and schools. of - Margarit, X.,Camarero,Casamayor, Along L.,and(2018). E.O. 2019, 1-79. ,DOI: 10.1080/02786826.2019.1676395
Proc. Acad. Sci., Natl. ., Sauliene, I., Weichenmeier, I.,I.,., Sauliene, Pusch,G.,Sarioglu, Weichenmeier, H.,Ueffing, H., M.,Behrendt,
Accepted- Manuscript soluble organic composition of the Arctic organicsoluble ofthe composition surface sea microlayerassociation and
Asian J. Atmos.Environ., Asian –
14919 Comment citer cedocument:
- atmosphere microorganisms exchange of inMediterraneangrassland. Nowoisky, J., Herrmann, Kanji, S., Z.A.,H., Jungblut, Nowoisky, J.,
Science, Environ. Sci. Technol.,Environ.Sci. – 14936.
319(5867):1214. 115(48):12229 - H., Iwasaka, H., Y.,and Shi,
5(3):172 C., andC., Morris,(2017). C.E. Measurements and
– DOI: 10.1021/acs.est.7b04072. 12234
–
180. Atmos. Environ., .
Philos. Trans. R.Soc. London., Trans. Philos.
G. - Y. (2011). IdentificationY. (2011).
55:496 Ubiquity ofbiological - term surveyterm unveils Menzl, G.,Moffett,Menzl, – 505
. n, T.W. n, T.W.
Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and Creamean, J., Solomon, Creamean, Iii, Solomon, A., Hanlon, Kirpes,Pickart, J., J., R.,Mcraven, R., Spada, R., N.,Cross, D.S., Crazzolara,A., Miranda, C.,Ebner, M.,Platis, T.,Bange, and A.(2019). Junginger, Anew J., I.,Crawford, Foot, N.H., Robinson, Flynn,V.E.,Gallagher, Huffman,Stanley, M.W., M.J., W.R., J.A., I., Bower,Listowski,Crawford, Ruske, S., M.W., Flynn, Gallagher, K.N.,T.W., C., Choularton, M.J., Mbareche,Lindsley,J.D., Cox, H., indoorfield andBioaerosol sampling. W.G., Duchaine, C.(2019). Conen,V., Yttri, F.,K Yakutin, M. Conen, F.,E.,and Zimmermann, Stopelli, CluesthatdecayingL.(2016). leavesArctic enrich air with Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, continuous springtime measurements an in Arcticoilfield location. 20:17882. L., Marine V.(2018). influences and and Phillips, terrestrial nucleating onice particlesdur boundary layer. multicopter froResults fromand emissions aColorado Kaye,(2014). pineforest: Characterisationof bioaerosol P.H. 14307. detection of airborne fluorescent inAn bioparticles Brough,Lachlan N., Aerosol Sci. Technol., increase when inautumn. leaves fall ice nucleating particles. (Basel).,Atmosphere Researchand Unansweredidentif needs questions Grothe, D.G. (2017).onthe H., future and Perspectives research: Schmale, oficenucleation A., E.,B., C.,Mutzel, U.,Stopelli, Pöschl, Schauperl,M., Scheel, Stratmann, Moritz, F., J.,
m the BEACHON - 2019, 1-79. ,DOI: 10.1080/02786826.2019.1676395 Acceptedbased aerialfor unmanned system pollen andcollection spores inthe atmospher Manuscript
Atmos. Meas. Tech.,Atmos. -
Cope, T., Fleming, Z.L.,Cope, T.,Fleming,Foot, V.E.,and(2017). Stanley, Real W.R. 8(8). Comment citer cedocument:
i n review.
Atmos. Environ.,
- RoMBAS experiment. RoMBAS .E., and Hüglin, C. (2017). Ice(2017). C. .E., and Hüglin, particleconcentrations nucleating
Atmosphere (Basel).,Atmosphere 12(3):1581
129:91 – – 1598. 94. ied from twointernational workshops. tarctica.
Atmos. Chem. Phys.,
8(10).
Atmos. Chem. Phys., Atmos. Chem.
14(16):8559
17(23):14291 – 8578.
- time time ing ing ic
–
Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and DeLeon deL.A., Weger, Šikoparija, B., C.H., C.A.,Kasprzyk, Pashley, I., Skjøth, Grewling, M., Ł., Thibaudon, De(1887). Bary, Comparative A. biology morphology and ofthe and fungi,bacteria mycetozoa Long Damialis, Gioulekas, (2015). A.,Vokou, D.,and D., Halley,J.M. D’Amato,Lanza, G.,Vitale, C., L.,Cuthbertson, Amores Crouzy, T.,Calpini, B., M.,Konzelmann, B.,All Stella, andB. Clot, (2016). Creamean, Smith, Primm, K., Tolbert,E.G., A.,Sheridan, Wendell,J., Jordan, J.M., P.J., M.A.,Hall, Pratt,K.A.,Creamean, Maahn,R.M., Spada, Kirpes, M.,de N.J., Boer, G., and J.M., Schnell, R.C., Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, A.J., Ziemba,L.D., K.T.(2013).A.J., Bergin, M.,Nenes, Microbiome ofKonstantinidis, the A.,and UK andfrom theNetherlands Central andsouthEurope. Magyar, (2016). M. and The D.,Smith, distance long Ambrosia of pollen tothe airborne transport Comparative morphologyandbiology mycetozoa ofthe fungi, andbacteria spore concentrations: Acomparisonpollen. with 16(5):434 and allergicpollution, respiratory diseases: Anupdate. 6(2):29. Characterisation of Arctic Bacterial Communities in the Airabove Svalbard. identification: Towards operational an system. interactions. and (2018b). Schnell, R.C. J., HOVERCAT: springtime inanArctic measurements oilfield location. S.(2018a).China, Marine andonice terrestrial nucleating influences parti - Rodriguez, N.,Lathem,Rodriguez, T.L., Rodriguez
– 40. 2019, 1-79. ,DOI: 10.1080/02786826.2019.1676395
Accepted Manuscript Tech.,Atmos. Meas.
- Arrocha, H., Malard, L.,Arrocha, Els,N.,Sattler, B., Pearce, H.,Malard, andD. (2017). Comment citer cedocument: M., Molino, A., and D’Amato, change,Climate A.,and (2016).M., Molino, M. air
11:3969
– 3985. -
R, L.M., R, Barazesh,B.E., Anderson, J.M., Beyersdorf, A novel aerial evaluationA novel ofaerosol for system
Atm
Fungal Ecol., os. Environ.,
Curr. Opin. Allergy Clin. Immunol., Opin.AllergyCurr. Clin.
Atmos. Chem.Discuss., Phys.
I nt. J.Biometeorol.,
13:150
140:202 - term trends term in – - 156. optical automatic pollen – 212. cles duringcontinuous cles .
Biology (Basel)., 60(12):1829
airborne fungal
1 – 28. – ,
1839.
- cloud cloud
-
Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and Donegan, Seidler, R.,and Por K.,Matyac, C., Dommergue, Tignat P., A.,Amato, Pomata, D.,Riccardi,Di Filippo, P., C. Burrows,Després, J., Huffman, Hoose, S.M., C.,Safatov, V.R.,Alex and Prenni, (2010).DeMott, New P.J. A.J. Need Directions: for thenumbers and defining sources of Hill, T.C.J.,DeMott, P.J., McCluskey, K.A., Prather, Col C.S., Delort, A. Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, recovery,enumeration ofbacteria and phylloplane. applied tothe Front. Microbiol., Zhang,Larose, (2019).Q., andglobalatmospheric Methodstoinvestigate the C. microbiome. K., Vo size aerosol particlesintheatmosphere: Areview. U., andNowoisky, Andreae, Elbert, Primary W., Jaenicke, biological M.O.,Pöschl, R.(2012). J., biological as ice acting aerosols nuclei. 113(21). (2016). Sea as aerosol nucleating spray aunique source particles. ofice Bracero,V.H., andO.L., Bertram,Franc,Bertram, B.F., A.K.,Moffett, Grassian, G.D. T.H., J.L., Martinez, Diaz M Lewis,Dhaniyala, Wentzell, Lee,J.J.B., S., Abbatt, E.R., J., Axson, Ault,A.P., C.M., C.,Sultana, Lee,Irish, Mason, R.H., McMeeking, V.E., T.,Hwang, C.Y.,Rhee, Snider, T.S., J.R., G.R., atmospheric implications. upper troposphere: Speci - segregatedmeasuredaerosol through biomarkers. - M. and Amato, P. (2017). P. Microbiology ofAerosols.Amato, M. and gel, T., Sonke, J.E., Jaffrezo, J.L.,I.,gel, M.,Moreno,Labuschagne,L., T.,Sonke,J.E., Andrade, C.,Martin,
2019, 1-79. ,DOI: 10.1080/02786826.2019.1676395 Accepted Manuscript
10:243. Comment citer cedocument: ., Venero, I.,Venero, Santos ., es andprevalence, composition andstorms, effectsoftropical
Proc. Acad. Sci., Natl. - Perrier, R., Magand, O., Thollot, A., Joly, M., Bouvier,O., Thollot,A.,Joly,Perrier, R.,Magand,L., M., Sellegri,
, Buiarelli, F., C.(2013). and Fungalcontribution Perrino, to
Atmos. Environ., teous, A. (1991).of methods for Evaluation sampling, - Figueroa, G.,Stokes, M.D.,Deane,Figueroa, G.B.,Mayol
Tellus, Ser.Tellus, BChem. Phys. Meteorol.,
110(7):2575
Atmos. Environ.,
44(15):1944 lins, D.B., Sullivan, R.C., Ruppel, M.J., Ruppel, M.J., R.C., D.B.,lins, Sullivan,
– 2580. A.S., Buryak,G., Fröhlich A.S.,
Appl. Environ. Microbiol., Appl. Environ.
– 1945.
Proc. Natl. Acad. Sci Natl. Proc. 64:132
– 140.
64(1).
- -
.,
Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and Fall, A.L. an Failor, Vinatzer,C.L.Monteil, K.C.,Schmale,B.A.,andIce D.G., (2017). nucleation active in bacteria and Dunstan, R.H. (2006).rainEvans, Coombes, Wind, andbacteria: P.J., effect C.A., The ofweather V.,and Grassian,Estillore, A.D.,(2016). J. Trueblood, chemistry V.H. Atmospheric bioaerosols: of I., Essoussi, Ghodhbane Environmental Tay Elbert, W., Ehrenberg,Passat (1847). C.G. Dreischmeier,L.,Budke, Wiehemeier, C., K., BorealKottke, T.,(2017). and cont Koop,T.pollen Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, Phosphate Starvation and LowPhosphate Starvation and Temperature. J., precipitation aregeneticallyand diverse mechanisms. nucleateby ice employing different on themicrobial ofroof composition Sci., Heterogeneous and multip adaptability stonesand toSahara desert monuments. Boudabous,and M.(2010). Gtari, Esterase A.,as an of bioaerosols facilities. at regulated ions. biogenicaerosols theatmosphere: in wet anddry discharged carbohydrates, and spores, inorganic Lebenund Atmosphäre,Berlin. indered. Königliche. ice 57(1):51
- 11(12):2740 nucleating asice nucleating well as
7(11):6604 Atmos. Chem. Phys., d Fall, High R.(1998). d – - 56. lor, P.E., Andreae, U.(2007). offungi M.O.,andprimarylor, P.E., Contribution to Pöschl, Agency Techn (2018). 2019, 1-79. ,DOI: 10.1080/02786826.2019.1676395 Accepted Manuscript – – 2753. 6616. - Gtari, F., Amairi, H., Sghaier, H., Jaouani, A., Brusetti, L.,Gtari, F.,Brusetti, H.,Sghaier, Amairi, H.,Jaouani,A., Daffonchio, D., Comment citer cedocument:
- hase reactions atmosphericand with othergases. trace oxidants 7(17):4569 Staub undBlutStaub - binding ‘antifreeze’binding polysaccharides. - Level Expression of IceLevel of Induced Expression herbicolaIs inErwinia Nuclei by ical Guidance Note (Monitoring) M9: Environmental Guidance Note monitoringical (Monitoring) M9:
- harvested rainwater. – 4588. - Regen: ein großesRegen: ein unsichtbares organisches Wirken
Curr. Microbiol., Curr.
enzymaticGeodermatophilaceae signatureof J. Appl.Microbiol.,
Wate
36(6):370 r Res.,
Sci. Rep.,
40(1):37
– 108(5):1723 376.
7:41890.
– 44.
– 32.
Chem. ISME ain Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and Galan, C.,Antunes Fröhlich Fröhlich Fröhlich Franze, U.(2005). Niessner,by T.,Weller, M.G., air. Protein R.,andPöschl, nitration polluted Fierer,Liu,Z., N., Rodríguez Fang,Z.,Z.,L.Zheng, H.,Wang, Ouyang, X.,and Culturable Hu, airborne (2007). bacteria Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, representativeexposure tothe major of olive allergen Ole e 1. B.,I.,Buters, (2013). G., and Weichenmeier, Airborne olive pollen counts Pusch, J.T.M. are not Kennedy,S., R.,Rantio Sofiev, M.,Albertini, Berger,L., R., L.,Celenk, Jackowiak, S.,Grewling, B., U., Cecchi, Jäger, ecosystem interactions. Després, U.(2016).inthe Earth Bioaerosolssystem: Climate, V.R.,andPöschl, health, and Elbert,Burrows,Yona, Gunthe, W., S.S., H.,Hoor, N., Su, P.,Thines,E.,Hoffmann, S.M., T., 12(4):1057 Ice activity nucleation inthe widespread fungusMortierella soil alpina. 1136. (2012). Biogeographythe air: Fungalover in land diversity and oceans. Bracero, P.,O.L., Begerow, Artaxo, Andreae, R., V.R.,andPöschl, D.,Conrad, U. M.O.,Després, Environ.Sci. Technol., Microbiol., Short environmentsChina. Beijing, in - - - Nowoisky, J., Hill, T.C.J., Pummer, T.C.J., B. Hill, Nowoisky, J., Z., Fraser, Burrows, Xie, S.M., P.A., Engling,G.,Solomon, Nowoisky, M J., Nowoisky, J., Kampf, C.J., Weber, B., Pöhlker, C.,Andreae,Lang C.J., Huffman,M.O., J.A., Kampf, Nowoisky, J., -
term temporal variability andfungal inairborne bacterial populations. –
74(1):200 2019, 1-79. ,DOI: 10.1080/02786826.2019.1676395 1071.
Accepted, C.,Brandao, Garcia Torres, R., C., Manuscript
Comment citer cedocument: –
207.
39(6):1673 - Atmos. Res., - Lehtimäki,I., Sauliene, M., A.,Reese, G., Smith, Hernández, M.,Knight, Henn,Hernandez,Hernández, M.T.(2008). R., M.,and
Microb. Ecol.,
– 1678.
182:346
G., Yordanova,G.D.,Franc, and U.G., Pöschl, (2015). P., – 376.
54(3):487 -
Mozo, H., Caeiro, E., Ferro, H.,Caeiro, R.,Prank,Mozo, M., – 496.
Allergy Eur. J. Allergy Clin. Eur. Allergy
Biogeosciences, Biogeosciences, Thibaudon, M.,Weber,
Appl. Env .P., Mayol.P., iron. in outdoor in outdoor
9:1125
- - – Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and Grewling, Jenerowicz, D.,Czarnecka Bogawski, P., Graham,Maenhaut,B., Taylor, Ebert, Guyon, P.E., W., P., M.,Matthias F.,Gonzalez, Narayan, Castro,M.P.G., Zeller, Walker, P., R.,and DevelopmentL.(2011). an of Leighton,I.D.,Ghosal, Wheeler, S., and (2010). K.E., T.J., Hutcheon, Weber, Spatially P.K. resolved Georgakopoulos,Després,Fröhlich D.G., V., Gehrig, Schwierz, C.(2018). F.,and R.,Maurer, Designing automatically generated new pollen Gantt, B. N.(2013). and Th Meskhidze, Galán, C.,Smith, Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, variability aerosol.Amazonian natural ofthe Van, Glovsky,M.M.,Flagan, and And R.C., Meixner, P., F.X.,Moura,O.L., Artaxo, C.H.E.D., M.A.L.,Grieken,Godoi, R.H.M., Rocha, R. localize potentialpathogen sources. autonomous unmanned aerial collect systemto time 76(10):3275 characterizationandBacillus ofionincorporation water in spores. 737. Biological,chem physical and Ahern, (2009). H.E., Microbiology B.F., Moffett, and and T.C.J. processes: atmospheric Hill, calendars Switzerland. for thepublicin organic aerosol: Areview. Aerobiologia (Bologna)., Brandao,(2014). requirements monitoring: R. Pollen reproducibility minimum and analysis. of Immunol.,
68(6):809 2019, 1-79. ,DOI: 10.1080/02786826.2019.1676395 – M., Thibaudon, M.,Frenguelli, Gehrig, G.,Oteros, Berger, J., and U., B., R., Clot,
Accepted3282. Manuscript
– Comment citer cedocument: 12.
30(4):385
Atmos. Chem. Phys., ical of characterization aerosol particles.
e physical and chemical characteristicse ofmarine physical primary
– J. 395. F. Robot.,
Ae - Nowoisky, J., Psenner, R.,Ariya,Nowoisky, J., Pósfai, P.A., M.,
robiologia (Bologna).,robiologia reae, M.O. (2003). Composition andM.O. (2003). diurnalreae, Composition
J. Geophys. Res. Atmos., - Operacz, M., Šikoparija, B., C.A.,and Operacz, Skjøth, M.,Šikoparija,
13:3979
28(6):961 - stamped samples from the atmospherestamped samplesfrom and – 3996. – 976.
34(3):349
Appl. Environ. Appl. Environ. - Maser, S.,Mayol
108(D24). Biogeosciences, – 362.
Microbiol., - Bracero,
6:721
–
Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and Harris, M.J., Wickramasinghe, N.C., Lloyd, Wickramasinghe,Harris, V,Rajaratnam,Turner, P., N.C., Narlikar, M.P.,Al M.J., J. D., Lovejoy, Harding, inhigh A.D., (2011). C.,andVincent,W.F. T.,Jungblut, arctic Microbes snowand Hara,Zhang,K. andD. (2012). HornerJ.A., Hanson, Fuhrman, C.A., Hader, Wright, and ofpollen J.D., Contribution toatmospheric T.P., Petters, M.D. (2014). ice Grinn Kalberer,Griffiths, Gallimore, Borlace, P.T., P.J., Pope,Herzog, F.D. J.S., M.,and (2012). M., Griffin, (2007).microorganisms movement D.W. Atmospheric ofincloudsdesert dustand Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, samples. Ramadurai, M.K., Wallis, S., andF.cells Detection Hoyle, S., (2002). instratospheric of living forimplications thecold biosphere. Atmos. Environ., biogeographic Processes patterns: microbial shaping landscape. the concentrations. parameters. fungal sporesForecasting inEurope: possibilities and relationships meteorological with D., Fernández Ianovici, V., Sadyś,Rodinkova, C., Tormo N.,Manzano, J.M.M., M.,Skjøth, Lett., Hygroscopiccloudgrowth Alaboratory activation and of pollen: and study. modelling forimplications humanhealth. uninfected areas. (2016). M. MesoscaleSmith, atmosph - Gofroń, A., N Gofroń,
13(4):289 , inProc.SPIE,
2019, 1-79. ,DOI: 10.1080/02786826.2019.1676395 Sci. Total Environ.,Sci. Total
Accepted Manuscript- Rodríguez, S., and S., Airborneand Damialis,Alternaria Cl A.(2019). Rodríguez,
owosad, J., Bosiacka,I.,Linares,B., De J., owosad, Camacho, J., C., Pashley, C.,Belmonte, – Atmos. Chem. Phys.,
295.
47:20 Int. J. Biometeorol.,
Comment citer cedocument: – . 25.
Bacterialabundance andinlong viability
Clin. Microbiol. Clin.
653(November 2018):938 - Devine, M.C., andDevine, Martiny, M.C., Beyond (2012). J.B.H.
Appl. Environ. Microbiol Appl. Environ.
14(11).
60(10):1493 eric transport of ragweederic transport from pollento allergensinfected
Rev., – 1500.
20(3):459
– 946. .,
77(10):3234 –
77.
Nat. Rev. Microbiol., Rev. Nat.
- range transporteddust. – 43. - Molina, R.,Vokou, Molina,
adosporium
Atmos. Sci. . nuclei nuclei
- Mufti, Mufti,
Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and Huffman, J.A., Perring, A.E.,Huffman, Perring, Savage, J.A., N.J. Zhang, Z., T., Niu,H.,Murata, K.,Wu, andHu, W., Bacteria (2018). Hu,M.,Kojima, D. in Hoose, (2012). C.andMöhler, Heterogeneous O. ice onatmospheric nucleation a aerosols: reviewof and Burrows,Hoose, J.E., C.,Kristjánsson, K.D.Holt, K.A.and (2014). Bennett,methodsfor Principlespalynology. automated and Hiranuma, Yamashita, A.,Kiselev,Hoffmann, O., T.,Saito, N., K.,Tajiri, A., C., Möhler, N.,Hoose, L.J., Galloway, Herlihy,J.N., Healy, Pöhlker, O’Connor, D.A., D.J., J.A., C Huffman, Haugen,(1978). Effects D.A. of Hartmann, Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, B., Schneider, J., Sivaprakasam,I.,B.,Zawadowicz,M.A., Crawford, J., Schneider, V., Gallagher, M.,Topping, D., atmospheric Detection,characteristics waters: implications. and results from laboratoryexperiments globalclouds ona scale? icecontribution inclouds. to formation E.,Koop, T.,andJantsch, Murakami,Ic M.(2015). rainwater. fluorescencetime and techniques. microscopy measurements particlesKillarney,Ireland: aerosol ofbiological near Acomparison betweenreal and Instrumentation,Denver, 4th, Colorado, measurements(turbulence and data). windspeed Centuries. IceStratmann, F. ofVariation (2019).NucleatingParticles Arctic Last intheEuropean the Over M., Blunier, T., Brügger, S.O., Schmale, J., Schwikowski, M., Blunier, H.,andT., Brügger, J., Vogel, S.O.,Schmale, M., A.,Wex,
Atmos. Environ., Geophys. Res. Lett., Geophys. Res. 2019, 1-79. ,DOI: 10.1080/02786826.2019.1676395 Accepted Manuscript Comment citer cedocument:
and Mills, A.L.and Mills, Bacterial of (1987). formicaceticin acid utilization and Environ.Res. Lett., . sampling rates and averaging ratesand sampling of meteorological periods
46:1
, Atmosph – 10. , Clot, B., Crouzy, B., Tummon, F., Shoshanim, O., Damit, F., B., O.,Damit, B., Shoshanim, , Clot, Crouzy, Tummon,
S.M. (2010). How biological (2010). important is S.M. in nucleation ice
Nat. Geosci.,Nat.
5(2). eric Chemistry andPhysics pp. 15 pp.
Atmos. Chem. Phys., Atmos. , in Symposium onMeteorological Observations , in
., Pöschl, U.,(2014).., Pöschl, and Ambient Sodeau, J.R. e and potential by cellulose nucleation its –
8(4):273 18.
– 277.
Atmos. Environ.,
14:8055 .
– 8069.
179:201
New Phytol., – 221.
- .
Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and Irish, V.E., Hanna, S.J., Irish, S., M.D.,China, V.E.,Willis, Hanna, S.J., M., Thomas, Cirisan,A.,Si, J.L., J.J.B., Wentzell, Irish,V B.,Hummel, M.,Hoose, Fröhlich C.,Pummer, Schaupp, C., Garland,Huffman, Sinha, B., Snee J.A., R.M., (2017).Huffman, and OnlineTechniques J. Santarpia, and J.A. for Characterization of Quantification Demott, P.J.,Huffman, Prenni, Robinson, Pöhlker, C.,Mason, A.J., R.H., N.H., J.A., Fröhlich Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, nucleatingin the Canadian particlesmarine boundary Arctic layer during inthe summer 2014. Laskin,Leaitch, Murphy, Abbatt, W.R., J.P.D., A., Girard, J.G., and Bertram,A.K. E., Atmos. Chem. Phys., Ice(2017). Miller, Polishchuk,L.A., E., Abbatt,Gosselin, J.P.D., M.,Murray,B.J., Bertram, and A.K. nucleation. Simulating theinfluenceof primaryparticles biological onclouds by aerosol heterogeneous ice fluorescenceduring techniques AMAZE rainforestaerosol particlesintheAmazon characterizedby real and microscopy An Biological Aerosols. nucleiaerosol duringand particlesand afterrain. ice Kreidenweis, Bertram, S.M., (2013). ofbiological A.K.,and U. High concentrations Pöschl, Ruzene, C.,Schmer, B., Harris,Nowoisky, Tobo,Y., Gochis, Després, D.J., E.,Müller J., E., V.R.,Garcia, persp Doughty, Pan, Y.(2019). and D.,Hill, Real S., .E., Elizondo, P., Choul, P., Lizotte,L.A., Charette,C., .E., Elizondo, Chen,Ladino, J., J., M., T.W., Wilson, dreae, U.(2012).distributions M.O.,and Size temporal Pöschl, ofbiological variations ectives. -
Atmos. Chem. Phys.,Atmos. Chem. nucleating particlesinCanadiannucleating Arctic sea 2019, 1-79. ,DOI: 10.1080/02786826.2019.1676395
Accepted Manuscript Technol., Sci. Aerosol , inMicrobiology ofAerosols,
17(17):10583 Comment citer cedocument:
Sinha, B., Sinha, Day,Andreae,Jimenez, J.L., D.A., M.O., Gallagher, M.,
18:15437
–
10595. accepted. - 08. - Pollmann, A., Gunthe, S.S., Artaxo, P., Martin, S.T., Martin, P., S.T., Artaxo, A.,Gunthe, S.S., Pollmann, –
15450.
Atmos. Chem. Phys.,Atmos.
- time sensing bioaerosols:Review and current of time
.
Atmos. Chem. Phys., - - surface microsurface Nowoisky, J., and Möhler, O.Nowoisky, J., (2018).
12(24):119 layer and bulkseawater. layer
13:6151 97 - – time UVtime 12019. - – Germann, I.,Germann, 6164. (2019). Ice(2019).
- -
APS APS
Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and Joly, Sancelme,Abrantes, M.,Amato, P., V., M.,Vinatier, L.,Joly, Deguillaume, M.,Amato, P., Monier Jimenez E.M.,Kim, Jeon, Iwasaka, G. Y.,Shi, (2017). Natural CentralIssanova, of and J. L Abuduwaili, Conditions Asia G.and Tenuta, Hambleton,Isard, Ariatti,J.M., A.,Russo, S., S.A., Barnes,C.W., A.,Gay,and Szabo, D.A., Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, (2015). Survival isolates from ofmicrobial cloudstoward simulated atmospheric stress factors. atmospheric station. of iceactive 0°c nuclei temperatures at near inlow Aircraft System inFranceStates. (sUAS) United and the IceDiversity Activityand a Nucleation Microorganisms Collected With Unmanned of Small Environ., Asian events dust airborne on bacterialanalyses. community by assessed molecular of long atmosphere withballoon the particles over Kosa sourceregions Tobo, Y., a Singapore, 29 Singapore, pp. inthe Desertsin AeolianProceses AsiaandKazakhstan, Storms ofCentral asDust 1357. SporeUsing Trapping,Aerobiological Monitoring, Crop and Modeling. L.J. (2011). Pr Atmos. Chem. Phys., - Sanchez, Aho,K.A., C.,Hanlon, R., Powers, C.,Mor
- range transport.
45(25):4313 nd Hong, C.S. (2009). Mixture of Kosa (Asian dust) and bioaerosols detected (Asian (2009).ofKosa nd Hong,and dust) C.S. Mixture inthe bioaerosols 2019, 1-79. ,DOI: 10.1080/02786826.2019.1676395 Accepted H.J., Impact (2011). Jung, Kim,J.O. M.Y.,Kim,Y.P.,andKa, K.,Kim,of J.H., Manuscript edicting Soybean Rust Incursions into the North American Continental InteriorIncursionsedicting Continental the SoybeanNorth American Rust into - Y., Yamada, F., T.,Naganuma,Y., Kakikawa, B., M.,Kobayashi, Maki, T., Chen,
Atmos. Chem. Phys.,Atmos. 19:1027 Comment citer cedocument: – 4321.
Air Qual. Atmos. Heal.,Air Qual.Atmos. –
– 49. 1039.
, M., Hoose, (2014). C.,andDelort, Quantification , M., A.M.
14(15).
2(1):29
- altitude cloudsDôme at de the Puy M., Deguillaume, L., M., Deguillaume, and Delort, A. –
38. Front. Microbiol., ris, C.E., and Schmale III, Schmale and ris, C.E., D.G. (2018).
- borne measurements: possibility
Plant Dis., Plant
9:1667. and - Cover Changes.Cover
95(11):1346
Atmos. Springer - M. M.
– , Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and Kiselev, D.,Bonacina, (2013).L., J.P. and A Wolf, Chang, (2001).Kim, S., andFroines, C. P.A., Sioutas, Jaques, Versatileaerosol M., J.R., concentration K I.Kasprzyk,M. (2006). and Airborneand fungal Worek, inurbanrural environments Poland. in spores H.,Boose,Ladino,Kanji,L.A., Z.A., Wex, Y.,Burkert Kakikawa,Kobayashi, F.,M., Maki, T.,Yamada, M., Kaarakainen, T.,Rintala, H.,Hyvärinen, A.,Kärkkäinen, P.,Meklin, P Joung, Y.S.,Ge,Buie,Bioaerosol Z., (2017).and generation onsoil. C.R. by raindrops A.M.and (2004). Harrison,R.M. Jones, The effectsofmeteorologicalfactors onatmospheric Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, ellogg, (2006).andglobal D.W. Griffin, Aerobiology ofdesert C.A.transport and the dust. P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, and identification ofpollen grains. individual Aerosol Sci., ultrafine,andambient finecoarseI: particlesDevelopment Partcharacterization. andlaboratory enrichment (VACES system Ecol. Evol., Aerobiologia (Bologna)., Ice(2017). OverviewNucleating of Particles. source Dunhuang. region, Iwasaka,Y., andintheatmosphere Dustborne (2008). microorganisms over Y. an Asiandust diversity and urban rural at landfill, sites. M., andNevalainen, A. Seasonal (2008). inairborne variation concentrations microbialand 8:1 b Atmos. Environ., ioaerosol concentrations – 10.
2019, 1-79. ,DOI: 10.1080/02786826.2019.1676395 21(11):638
32(11):1281 Accepted Manuscript
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Sci. Total Environ.,Sci. Total
CLEAN
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Higashi, G.,Hong, Shi, B., C.,Tobo, T.,Chen, –
- 1(4):195 Soil, Air, Water, Air, Soil, Kohn, M., Cziczo, D.J., and Krämer, D.J., Kohn, M.,Cziczo, M. - lamp based device forlamp based fluorescence detection
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84(3).
3):151 ., Vepsäläinen, A., Hirvonen,
58:1.1
36(7):556
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–
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Nat. Commun.,Nat.
Trends Trends
J.
Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and Ladino,L.A., Yakobi Lee, of (2005). andKuznetsova, theproteinaceous M., Aller, Characterization J. C., inmarine matter Krumins, V.,Mainelis, G.,Kerkhof, D.E.L.J., and(2014). Fennell, Substrate Kraaijeveld,L.A., Hiemstra, and K.,de P.S., M.,Buermans, Weger, J., Ventayol H.,Frank, den García, K.A.,Kourtev, Hill, Shepson, P.B., P.S., and A.(2011). Konopka, cloud Atmospheric Könemann,N., Beall, Rodriguez C.M., T., Savage, Iwata,Kobayashi, Maki, T.,KakK., F., InfluenceBurge,Ko, G., and First,H.A.relative (2000). M.W., of humidity andon particlesize UV IceKnopf, inAtmosphericThe P.A.,and D.A., of Wang,B.Role Alpert, OrganicAerosol (2018). Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, aerosols. Production inanAirborne Bacterium. using next (2015).Dunnen, Efficientand J.T. identification sensitive and quantifi diverse bacterial community. Cruise around Peninsula. theArabian and Pöhl Walter,D.,Lelieveld, Weber, B., Andreae,Pöschl, J., U., P., Yordanova, M.O.,Huffman, J.A., during May poisoning: Kosa observation real cloud of and behavior Y. (2016). of thetoxicity Evaluation eventKosa duststorm) ofa view (Asian of from food 80(4 sensitivity BCG bovis aerosols. and ofSerratia Mycobacterium marcescens Nucleation: A Review. – 5):217
ker,Online Bioaerosol C.(2018).Measurements theAQABA and Dust Research during Mar. Chem., - generation DNA sequencing.
2019, 1-79. ,DOI: 10.1080/02786826.2019.1676395 2011 in Kanazawa, Japan. 2011 inKanazawa, –
Accepted Manuscript 228. - Hancock, J.D., Kilthau, W.P., M., L.A.,Hancock, Mason,Si, R.H., J.D., Miller, Li, J., Schill
Comment citer cedocument:
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Environ. Sci. Technol. Lett., Environ.Sci.
Chem., Air Qual. Atmos. Heal.,Air Qual.Atmos.
Mol. Ecol. Resour.,Mol. Ecol. . -
Caballero, Dorf,F., M.,Harder,H., E., Ditas, 45(30):5399 - time PCR analysesof Kosa PCR time bioaerosols –
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water contains a contains water .
er, Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and Ligler, F.S., Anderson, G.P., Davidson, P.T., Foch, R.J., Ives, Davidson, Foch, Page,Ligler, R.J., P.T., King, G.,Stenger,F.S., G.P., K.D., Anderson, J.T., L Lighthart,B., Marthi,B.T., B.,Ganio, Shaffer, and Lighthart, from B.T.B. chaparralBacterial (1994). andflux Shaffer, the atmosphere into in mid Lighthart,B. ecologyThe (1997). ofbacteriaalfresco atmosp inthe Lever, A.B., Michaud, A.,Eickenbusch, P., M.A., Šantl Torti, (2002).Lee,B.U., Hygroscopic Kim,S.S. and Kim, S.H., growthcoli and ofB. bioaerosols. E. subtilis Leck,Bigg,andE.K. Comparisonof C. (2008). sources the aerosol tropical and natureof withthe Lauber,Pander,Kiselev, A., A., Lateran, Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, D.A., and Whe microbial bioaerosols previously deposited onplants. summer at location. ahigh desert 23(4):263 diverse types. environmentalsample A modularRNA,of and extractionDNA methodforofand theseparation DNApoolsfrom the J. Aerosol Sci., summer high Arctic aerosol. during droplets. oflevitated freezing Ser. Mater. Sci.Eng., altitudevehicle balloonplatform (HAB) sampling. for (UAV) high activeaerosol based laboratoryfield and measurements. Addressing theice mode deposition of Acombination abilities aerosol: nucleating of marine Knopf,C.L., Aller, J.Y., D.A.,Abbatt, (2016). Huffman,Bertram,A.K.,andJ.P.D. J.A., S., Sedan, M.F., Harithuddin, and A.S.M., Azrad,ofunmanned (2016). Sedan, S. S., M.F., Development aerial – 274. 2019, 1-79. ,DOI: 10.1080/02786826.2019.1676395 Accepted Manuscript lan, J.P. (1998). Remote sensinglan, J.P. an using airborne biosensor.
33(12):1721
Comment citer cedocument: 152(1):12018.
T., Handmann, P., and Leisner, andT., Handmann,P., Secondary (2018). formation T. ice –
T 1723. ellus, Ser. BChem. Phys. Meteorol.,
Atmos. Sci.,
Atmos. Environ.,
Front. Microbiol., J. Atmos.Sci.,
28:1267 .M. (1993). Artificialwind .M. (1993).
75(8).
132:1
Aerobiologia (Bologna)., –
1274. 6(476). - Temk
– 10.
here.
iv, T., and Jørgensen,B.B. iv, T.,(2015).
60(1):118
FEMS Microbiol. Ecol.,FEMS - gust of liberation
Environ.Sci. – 126.
9(2
– 3):189
IOP Conf. - – 196.
Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and Madelin, T.M.( Zhou, Yang,Ma, Y., Zhao,S., Zheng, J., andX. (2017). Y., the Assessment impact for of dustevents Lakey,Liu,F., Berkemeier, T., P.S.J., Lindemann, C.D.(1985). andAerial dispersal Upper, ofepiphytic J. over bacteria bean plants. andLindemann, H.A.,Barchet, Upper, as Constantinidou, Plants sources C.D.(1982). J., W.R., of Lin, W. Lin,Lizarraga, (2015).L.,L.A.,Bottomley, Meredith, H., Effectabsorption J. on andofwater Carson Lin,B., andIII, Bozorgmagham, S.D., Schmale A.,Ross, fluctuations Small the D.G. in (2013). Lim,G.E., O’Loingsigh, N.,Munday, T.,De C.I., Allison, Tapper, Deckker, (2011). P.,and N.J. Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, on measles incidence in westernon measles incidence China. in oligomerization u Atmospheric and nitration protein influenced by anthropogenicair chemistry pollutants: Lai,Nowoisky, (2017). Weller, S., U., J., M.G.,Pöschl, andC.J. Shiraiwa,Kampf, M., Env. Microbiol, 1063. airborne bacteria, airbornegradient.along floraan fungal torural urban pollen adhesion. ground level. recoveryacross consecutive offusaria intervals sampling aircraft unmanned with 100mabov Environ., Total Microbiological andmeteorologicalAustr analysis oftwo Technol., - R., Wang,R., P.
32(16):2461 1994). Fungalaerosols:1994). A review. 2019, 1-79. ,DOI: 10.1080/02786826.2019.1676395
Accepted Manuscript (Bologna).,Aerobiologia
412 - 50:1229 J. Colloid InterfaceJ. Colloid Sci., H., Tien, C. H., pon exposure to ozone andpon exposure toozone nitrogen dioxide. including nucleation ice – 413:223 Comment citer cedocument: – 2466. – 1232. - –
J., Chen J., 31.
Tong, A.T., H.,Kunert, Cheng, Meusel,Fröhlich H., Y.,Su,H.,
, W.
29(1):45 Atmos. Environ.,
442:133 - - activebacteria. Y., Yu,Y.
J. Aerosol Sci., – 54. – 139.
-
J. Aerosol Sci., A., and Hsu, L.Hsu, A., and
157:1 alian inApril2009. storms dust
Appl. Environ. Microbiol., Appl. Environ. .
Faraday Discuss., – 9.
- 116:116 Y. (2018). Changes in – 123.
200:413
44(5):1059
– Appl Sci. 427. e
– - Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and Maki, T., Lee,Iwasaka,Maki, T., M.,Kai, Kurosaki, K.,Hong, K.,Onishi, K., Y., C.S., Shinoda, K.C.,Kawai, Lee, K., Maki, T.,Kurosaki,Onishi, Y.,Yamanaka, K.C.,Pointing, S.B.,D., N.,Hasegawa, Jugder, H., A.,Hasegawa,Iwasaka,M., Matsuki, Kobayashi,Maki, T.,Kakikawa,Yamada, M.,H.,and F., Y. Maki, T.,Hara,Kakikawa, K.,Kobayashi, A.,Chen,F., B., Y., Kurosaki, G., Shi, M.,Matsuki, Lee,Iwata,Maki, T.,Hara, A., K., Kai, Pointing, S.B., K.,Kobayashi, K.C.,Kawai, F., Archer, K., S., Mainelis, K.,Adhikari, G.,Willeke, T., and A.,Reponen, Design Grinshpun,(2002). S.A. and Mainelis,Bioaerosol G.(2019). sampling: Mahaffee, Stoll, R.(2016). W.F. and TheFlowin EbbandMonitoring of Airborneand Pathogens: Use Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, dispersalassociated ofbacteria dustandanthropogenic with desert over continental particles and Lacap Y., Archer, S.D.J., Ovoo of during area Gobidesert events. dust Variationsand M.(2017b). Shinoda, thestructure in ofairborne Japan. andorigin(2013).composition Assessment of of an Asian Iwasaka,Hasegawa,and Y.(2015). distributio H., Vertical 17(19):11877 altitudes ove Iwasaka,Hasegawa, atand Y.(2017a).Variationsairborne high in H., communities bacterial Technol., collectionnew efficiency electrostatica precipitator offor collect bioaerosol Sci. Technol., Disease Management Decisions.
Atmos. Environ., -
dust downwind area,Noto Peninsula. downwind dust 36(11):1073 2019, 1-79. ,DOI: 10.1080/02786826.2019.1676395 r the (Japan) NotoPeninsula toAsian dustevents. inresponse
Accepted Manuscript– in review. 11897. Comment citer cedocument:
– 1085.
74:73 ‐ Bugler, D.C.,
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Phytopathology,
classical approaches, and advances perspectives. Hasegawa, H.,and(2019). Pointing, Aeolian S.B.
Air Qual. Atmos. Heal.,Air Qual.Atmos.
Atmos. Environ., airbornefree bacteria troposphere intheover
106(5):420 n ofairborne in communities bacterial – 31.
bacterial communities in Tsogt communities bacterial 119:282
10(3):249 – 293.
Atmos. Chem. Phys., ion.
–
Aerosol Sci. 260.
Aerosol Aerosol -
Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and McCluskey, M.,At Rinaldi, Ovadnevaite, C.S., J., Mazar, Y., theAtmospheric on Cytryn,E., Erel,Y.,and Y. Effect Rudich, (2016). ofDust Storms (2014).Mayol, and M.A.,Herndl,Duarte,Resolving Arrieta, J.M. G.J., the E.,Jiménez, C.M., Li, Chou, M., Mason, R.H.,Si, Dickie,C., J., Marks, Kruczalak, K.,andBacteria R., Jankowska, and M.(2001). K., Michalska, fungi airthe in over Kobayashi, S., Maki, T.,Susuki, M F., Kakikawa, Maki, T.,Puspitasari,Hara, F.,K., Yamada, M Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, Influenced Northe MarineIce and Organic Terrestrial Lohmann, (2018). Z.A.,T.C.J., P.J. U.,O’Dowd,Kreidenweis, C., and Kanji, DeMott, S.M., Microbiome intheEastern Mediterranean. Microbiol., abundance and air with a Bertram,Ice A.K.(2015). nucleating coastal particlesata layer marine site:Correlations boundary Ladino,Leaitch,L.A.,J.D., K., Jones, Schiller, C.L.,Abbatt,Huffman, and J.P.D., W.R., J.A., Gulf andof sea. GdanskBaltic region, Dunhua of adistribution halobacterialatmosphere community (KOSA) inthe Asiandust source ofan Tobo,Y.,C., Hasegawa,H., Ueda,Iwasaka,and Y.(2008). K.,diversityand Phylogenetic vertical (Kosa)dust event. Variations thestructure ina in ofairborne downwind bacterialarea communities an Asian during oceanic surfaces. erosol type and meteorological conditions.
5:1 2019, 1-79. ,DOI: 10.1080/02786826.2019.1676395 Accepted Manuscript – ng City. 9.
J. Geophys. Res.J. Atmos., -
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J. Aerosol Sci.,J.
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488
R., Toom R., ., Kobayashi, F., Hasegawa, H., and Iwasaka,H., and., Kobayashi, F., Hasegawa,(2014). Y.
– J. Geophys. Res. Atmos., 124(10):5579 Environ. Sci. Technol.,Environ. 489:75 ., Yamada, T.,Chen,B., G.,Hong, M.,Higashi, Shi, kinson, J., Belosi, F., J., kinson, Ceburnis, Hill, D.,Marullo, S.,
32(2):237
1(2):81
Atmos. Chem. Phys., - – Sauntry,D., Pöhlker, C.,Yakobi 84.
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50(8):4194
123(11):6196
15:12547 – 202. – 12566. – 6212.
- Hancock, Hancock, n.
Front.
Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and Morris, C.E., Sands, D.C., Glaux, C.,Samsatly,Morris, Sands, Asaad, D.C.,Glaux, Gonçalves, C.E., Moukahel, S., J., and F.L.T., A.R., Morris, Sands, D.C.,Bardin, Vogel, C.E., Leyronas, Ariya, B., M.,Jaenicke, and R., P.A., Psenner, C., Leyronas,Morris, and (2014b). C.E., C., Nicot,Bioaerosols Movement P.C. inthe Atmosphere of and Morris, Georgakopoulos,D.C. (2004 D.G., C.E., and Sands, Huffman,Phillips,Alex Morris, Conen,F., U., J., V.,Pöschl, C.E., and Moran Monaha Möhler, O., Vali,Levin, DeMott, G.,andZ. P.J., atmospheric Microbiology (2007). and processes: the Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, of airborne micro (2011).R. Microbiologyand atmospheric Research challenges processes: conce Ltd,393 UK, pp. Chichester, the Consequencesfor and Climate Microbial Evolution. potential role inprecipitation. through biologicalnucleators inthe atmosphere. ice Bioprecipitation: a feedback cycle linking history, ecosystem dynamics Earth and landuse Chem. Phys., aerosols forestofSaharan theAmazon rain in intrusion plumes. the frequent with dust U., Pöschl, Andreae, P., Artaxo, Pöhlker, N., M.,Ruckteschler, H.,Wang, Su, Wang,Z., Y.,B., Q.,Wang, Weber, S., Wolff, I.,Baars, Heese,Godoi, R., B., H., HMLavrič,L AHolanda,V.,Martin, B.,Ming, S., J. J., 392. between whitecapsandaerosols. marine 10mwinds,ocean role incloudphysics. ofbiological particles - Zuloaga, D., Ditas, F., Walter, D., Saturno, J., Brito,Zuloaga, Ca F., J., D.,Ditas, Walter,D.,J., Saturno, n, E.C., Fairall, C.W., Davidson, K.L.,C.W., (1983). Boyle,n, E.C.,Fairall,Observed and P.J. inter
2019, 1-79. ,DOI: 10.1080/02786826.2019.1676395
Accepted Manuscript18:10055 - organisms ontheatmosphere climate. and organisms Comment citer cedocument: – 10088. –
415. J. Phys. IV,
M., and Pöhlker, C. (2018). Long (2018).C. and Pöhlker, M.,
121:87
Biogeosciences, – 103.
Glob. Chang. Biol., Glob. Chang.
). Ice). active nucleation and bacteria their , inAerosolScience,
Q. J. R. Meteorol. Soc., Meteorol. Q. J. R.
Biogeosciences, rbone, X.,Hrabě Chi, S., Angelis, De 4(6):1059 - Sands, D.C.(2014a). Sands, term oncoarse study mode –
1071. 20(2):341
John WileyJohn & Sons, 8:17
rning theimpact ‐ – – relations relations
25. 109(460):379 351.
Atmos.
– Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and Neufeld,B.K.,A.P., Gugino, Keinath, McGr K.N., Nemergut, E.K.,Hamady,Lozu Costello, D.R., M., Nem Negrin, M.T.,and(2007). and Ronco, M.M.,Delinfluence A.E. Study site Panno, ofbioaerosols in, Negrin,M.T., Terada,Ronco, A.(2009). M., Delof C.G.,andindoor Panno, Characterization Bigg,Morris, Soubeyrand, S., Sands,D.C.,Morris, C.E., Soubeyrand, J.M., C.E., S., E.K., Creamean, Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, eck cucurbit theeasternUnited States using downy mildewaerobiological in an integrated model. (2018).Langston, Ojiambo,P.S. Predicting Keever,B., A.,and risk of T., D.B., Dutta,Sims, the biogeography taxa. ofbacterial L., Stanish, Townsend, C.C., A.R.,Cleveland, Knight, and (2011). patterns R. the Global in 175(13):4062 andPseudomonas syringae lowtemperature. induced limitation is by nutrient strain Aerobiologia (Bologna)., Lathe Plata areaconventional using DNA (Argentina) (fingerprint) and based methods. 109 INC,Nova Science Publishers, 400Oser 1600,Hauppauge, Ave,Ste NY 1 based methods. outdoor 98(6):1109 SensitivityPotential Precipitation BiologicalAerosols. to of Bigg, and E.K., Sands, D.C.( Creamean, J.M., nucleation active bacteria. Bigg, E.K.Urediosporesice (2013). ofrust fungi are - – Marshall, M., LaDuca R.(1993). Fall, High M., Marshall, and R., 125.
bioaerosols and industrial using DNA urban, rural in sites (fingerprint)and conventional
– 2019, 1-79. ,DOI: 10.1080/02786826.2019.1676395 1118.
Accepted– Manuscript 4070. , in Aerosols: Chemistry, Impact Effects, Emvironmental D.Peretz,, inAerosols: andHealth ed,
Comment citer cedocument:
23(4):249
Atmos. Chem. Phys.,
Environ.Microbiol.,
– 258.
ath, M.T., Sikora, E.J., Miller, S.A., Ivey, S.A., Miller, ath, Sikora, M.T., E.J., M.L., pone, C., Jiang, L., Fierer,pone, C.,Jiang, S.K., Schmidt, N., 2017). Mapping Feedback2017). toReveal Rainfall the
13(8):4223
13(1):135 nucleation activenucleation at > - level expression of icelevel nuclei expression ina –
4233. Bull. Am. Meteorol. Soc.,Bull. – 144.
- 1788 10 °c and harbor ice - 3635 USA,pp.
J. Bacteriol.,
Int.
Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and Oteros, J., Bartusel,Oteros, J., A.,Moreno, F.,Behrendt,H.,Schmidt E.,Alessandrini, Núñez, D.A., Leck,Orellana, P.A., E.(2011).Lee, Rauschenberg, C., M.V.,Matrai, Marine Coz, C.D.,A.M.,and I.Oliveira, Delgado, J.L., M.,Ribeiro,H., and(2009).effects The Abreu, Oliveira, Umo, and D.,N.S., O’Sullivan, Ross, T.F., Murray,Whale, B.J., J.D., J.F., Price, H.C.,Atkinson, Leeuw,O’Dowd, production: G.aerosol C.D.and areview de (2007). ofthe Marine current Núñez, A.,de G.A., Paz, Rastrojo,A.,García,Alcamí, A.,Montserrat A.M., Gutiérrez Núñez, A.,Amo G.,Rastrojo,A.,García,A.M.,Alcamí, dePaz, A.,Gutiérrez Noziere, B.forget Don’t (2016). the surface. Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, Traidl 108(33):13612 microgels Biometeorol., airborneconcentrationdiffering areaslevel. sporeintwo fungal inurbanisation atmosphererural ofurban and locationsPortugal. in 1 M.E.(2015).Webb, relevance The biological ofnanoscale icenucleation fragmentsfor inclouds. knowledge. Metagenomics urban appliedenvironments. to MonitoringMoreno, ofairbo D.A. (2016b). Importance, ratios. and variability Moreno,Monitoring D.A. ofairborne (2016a). biolog J. Biomet – 7.
M., Delgado, L.,I. PleosporalesM., Delgado,Fungal Ribeiro,H.,(2010). andfrom inthe Abreu, spores - Hoffmann, C., and Buters, (2019). and Hoffmann, C., Arte J. eorol., ascloud asource thehigh condensation ofin nuclei Arctic.
2019, 1-79. ,DOI: 10.1080/02786826.2019.1676395 Philos. Trans. R.Soc. AM Trans. Philos.
Accepted Manuscript 53(1):61 –
13617. 62(4):655 Comment citer cedocument: –
73. –
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Int. Microbiol., ath. Phys. Eng. Sci., ath. Phys.
Science (80 Science rne biological atmosphere. inoutdoor particles 2: Part
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19(1):1 -
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351(6280):1396 –
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of meteorologicalon of factors
Proc. Natl. Acad. Sci., Natl. Proc. –
12(5):1187 – 80. - 1397. Bustillo, A.M.,and –
1774.
Int. J. - Bustillo, A.,and
– 1194. - Weber, C.,
Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and Papadopoulos, N.G.,I., Agache,Bavbek, Bilo, S., B.M., A., V.,Custovic, Braido, F., Cardona, Palframan,III, H.A.,D.G., Schmale and (2014). M.C., Gruszewski, Woolsey, Detectionof a C.A. Pusch,G.,Weichenmeier,Oteros,I., J., U., Möller, Heimann,R.,Röseler, S.,Traidl Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, Z., Rudzeviciene, C., Rondon, O.,Ruëff, Quirce,C., Raulf Raap, S., U., Pala, G.,L.,M., O’Mahony,S., M., Pfaar, Papi, A.,Passalacqua, O., O’Neil, Pitsios, G.,Perkin, C., A.,Mills, Manole,Mingomataj, F., A., N Mazon, B., Mari, E.,Niggemann, Logan,Lauerma,Lauener, Makrinioti,H.,Mangina, R., Makowska, A., K., Magnan,A., J., P., Kala Hoffmann, Hoffmann H.J., Gevaert, Genuneit,Ferrer, Hamelmann, J., Flohr, Groblewska, P., E., A., C.,Gardner, M., DeJong, N.,DelS., Giacco, Celenk, Calderon,L.O., Caubet, M.,Cardell, CichockaS., J.C., Butiene, Boyman,E., Bonadonna,M., I.,Brockow, Bonini, P., K., J., O., Burney, Buters, P., Annesi Skevaki, Triggiani,M., VanRee, C., R.,Allegri, T.,Flood, Savli, R.,Werfel, S., B., P., Palkonen, J Grattan,DeMonchy, Demoly, Eigenmann,P., Heffler, J., C., J., E., P.,Gayraud, Hellings, P.W., unmanned aircraft system. surrogate a with portable surface biologicalplasmonresonance onboard agent sensor an Allergy Immunol., Schmidt endotoxin. utel, M.,Knol,E.,Lötvall, Muraro,L.K., A., J., Poulsen, G.,Schmid Roberts, yci, A.F., Ö.,Kalpaklioglu, Kleine - Maesano, I., F., Antolin Maesano, Annunziato, - Weber, C.,and Buters, (2015). a Automatic J.T.M.
J. Allergy Clin. Immunol., 2019, 1-79. ,DOI: 10.1080/02786826.2019.1676395 Accepted Manuscript
167(3):158 Comment citer cedocument:
- J. Unmanned Syst., Veh.
Sommergruber, K., Hovhannisyan, L., F.L., V., Jahnsen, Sommergruber,Hovhannisyan, Hox, K., Douladiris, N., Fassio, F., Fauquert, J.L., Fernandez, J., Douladiris, F., M.F., N.,Fassio, J., Rivas, Fernandez, Fauquert, J.L., – - 66. Heimsoth,M., Rhyner, C.,Robson
143(1):369 - Tebbe, J., Konstantinou, G., Kurowski, M., Lau, M., Konstantinou,G.,Kurowski, Tebbe, J., S., F., Rukhadze, M., Rumi, G.,Sackesen, M.,Rumi, F.,A.F., Santos, C., Rukhadze, - Amerigo, D., – 377.
2(4):103
Apfelbacher, C.,Blanca, M.,Bogacka, nd online pollen monitoring. – 118. - Jarosz, E., Cingi, C., Couto, M., E.,Cingi, M., Couto, C., Jarosz, -
Ansley, P., Alves, R.R., Roje, Alves, P., R.R., Ansley, - ilsson, G.,Ollert,ilsson, - Grendelmeier, P., Hoffmann, C., Hoffmann, C.,
Int. Arch. Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and Pei Peel, Finlayson, M.C., B.L., and M H.,EW, DA,Pearce,Bridge, Hughes, W., D.A., N.J., B.,JS, K.A., P.D., Sattler, Psenner, R.,Russell, Pearc L. dansl’atmosphère,Pasteur, existent corpuscules (1862). Surles qui organisés doctrine de examen la Passananti, G.,andV., Delort, M.,Vinatier, Brigante, Siderophores M.(2016). A.M.,Mailhot, incloud Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, - Chih, W., Huey W., Chih, P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, climate classification. Microbiol. Ecol., (2009). O.,andW. G., SM, WJ, theatmosphere Microorganisms Antarctica. in over Front. Microbiol., and Vincent, Aerobiology antarctica (2016). W.F. over L.,Benning,L.G.,Gunde D.H., deBradley, Eguren, G.,Vera,Elster, J.A., G.,Matcher, J.P., Lau,Sattler, Magalhães, B.,B.J., D.J.,Wall, W.L., Adams, Chu, C., C.,Smith, Cary, M.C.Y., Phys.,Chim. des générations spontanées,leçon àle19mai clinique professée de laSociété 1861. Paris, sun waters impactchemistry: complexes and onatmospheric under potential Photoreactivity ofiron in allergy:paper, EFA. incollaborationEAACI with position An Xepapadaki,Boerstra,B., M., Worm, and (2012).P., Akdis,C.A. Whitacker,P., Research needs Stur Seys,I., F.,Sprikkelman,A., Siracusa,A.,Skypala,Spertini, R., S., Spiewak, Sokolowska,M., Santucci, C.,Schmidt A., Scharf, e, D.A., Alekhina, I.A., Terauds,A., Wilmotte, D.A., Quesada, Alekhina, e, A.,Edwards, Dommergue, A., - m, G., Swoboda, I.,m, G.,Swoboda, Terreehorst,I.,E., Traidl Toskala, simulated conditions. 2019, 1-79. ,DOI: 10.1080/02786826.2019.1676395
Accepted Manuscript64. - Jen, S., and S., Chia Jen,
69(2):143
7(FEB):1 Comment citer cedocument:
Hydrol. EarthSyst.Sci., Hydrol. -
Environ. Cimerman, N., Convey, P., Hong, V.H., P., S.B.,Cimerman, Pellizari, N.,Convey, Pointing, S.G., – – 157. 7. cMahon, T.A. (2007). Updated mapcMahon,(2007). ofthe world T.A.Köppen
- -
Yin, L. andYin, Characteristics(2000). outdoorairborne of indoor
Weber, C.,Schnyder, B.,Senna, G.,Sergejeva, Schwarze,J., S., Sci. Technol.,
11:1633
50(17):9324 – -
1644. A new initiative for atmospheric for initiative A new ecology. - Hoffmann, C., Venter,Hoffmann, C., C.,Vlieg –
9332.
Clin. Tra Clin. J., Hughes,J., K.A., Cuthbertson,
nsl. Allergy,
FEMS FEMS
- 2(1):21. Geiger Geiger
Ann. -
Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and Powers, C.W., Hanlon, R., Grothe, H., Prussin, A.J., Marr,L.C., Hanlon,III, Grothe,Powers, C.W., R., H., A.J., andD.G. Prussin, Schmale (2018). G.,Peghaire,Pouzet, Aguès, M.,Baray, E.,Conen, F., J.L., a U.,B.,Huffman,Borrmann, Sinha, Pöschl, Martin, S.S., Farmer, S.T., S., Chen,Q., J.A., D.K., Gunthe, Polymenakou,(2008). Mandalakis,M.,Stephanou, E.G., Particle P.N., andA. Tselepides, size (2012).Pointing, Microbial and S.B. J. controls and colonization in Belnap, dryland systems. andPetters, Petters, S.S. Petters, M.D.(2015). T.P. and Revisiting Wright, samples. ice from nucleation precipitation Perring, Baumgardner, J.P., A.E., Schwarz, M.T.,Spracklen, D.,D.V, Heald, Hernandez, Gao, C.L., Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, Atmosphere (Basel).,Atmosphere processing and variability atof particles Opme,France. biologicalnucleating ice inprecipitation Amazon. Andreae, precipitation nucleiclouds M.O.(2010). and the as in of biogenic Rainforestaerosols Roldin, Rose, P., Petters, D., M.D., Prenni, A.J., J.L., Jimenez, Garland, A.,Mikhailov, G., Manzi, Helas, King, S.M., R.M., E.,Pauliquevis, T., eastern Mediterranean. of airbornedistribution microorganisms and Africanan pathogens intense the during in event dust Microbiol., component aerosols. internally mixed Res. Lett., 120(3):1153 of region Kok,G., McMeeking,R.S., and Fahey,Airborne J.B., G.R.,McQuaid, (2015). D.W. observations fungi home and atsuburban urban al variation influorescentalthe Unitedaerosol variation States. across
Science(80
42(20):8758
10(8):55 2019, 1-79. ,DOI: 10.1080/02786826.2019.1676395 –
Accepted Manuscript 1170.
M.D. (2016). Surfactant effect on cloud condensation nucleiM.D. (2016).effect for two Surfactant oncloudcondensation 1
- 8(11). Comment citer cedocument: – . ).,.
62. – Environ. Health Perspect.,Environ. 8766.
329(5998):1513
s in two seasons. s intwo
J. Geophys. Res., – 1516. Schneider, J., Su, H., Zorn, S.R., Artaxo, P., and H.,Zorn,P., Artaxo, Schneider, Su, S.R., J.,
116(3):29
Sci. Total Environ.,Sci. Total
121(4). nd Amato, P. (2017). P. Atmosphericnd Amato, 2 – 6.
J. Geophys. Res.,
253(1):111 – 118.
Geophys.
-
Nat. Rev.Nat.
Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and Rathnayake, N.,Baker,Z., Metwali, C.M., Jayarathne, G.,Bin,Puspitasari, F.,Shi, Kobayashi, F., C., Hasegaw Maki, T., B.G.,Pummer, AugustinBudke, C., B.G.,Pummer, Bauer, Bernardi,Bleicher, H., S.,andSuspendable J., Grothe,(2012). H. Blades,(2005) Mathison,G.,andR. Prospero, J.M., Naidu, E., Petters, M.D.,Prenni, A.J., Kreidenweis, Heald, S.M., C.L., M Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, 5089. background theMidwestern in locations United States. and Urban E.A.of bioaerosolP.T., relativeenhancement Stone, (2016). PM10 tracers to sourcedust Desert. area, theTaklimakan Phylogenetic sandbacterial in dunesanalysis and of aerosol dust compositions species inanAsian macromolecules.soluble Grothe, T.,and H., U., Fröhlich Pöschl, Koop, Liedl, R.G., Loerting, K.R., T.,Schauperl, M., T.,Moschen, Chem. Phys., macromoleculesareresponsib 19. fungi bacteriaAfrica dust. from and with soil tothe Caribbean nuclei inthebasin. Amazon Wollny, U.(2009).and Relativeofbiogenic Pöschl, A.G., roles emissionsand Saharan asice dust Microbiol., Unmanned (sUAS). and (USV) Aircraft a SurfaceUnmanned System Small Vehicle Coordinated Sampling Microorganisms of Freshwater Over Usingand SaltwaterEnvironments an
9:1668. 2019, 1-79. ,DOI: 10.1080/02786826.2019.1676395
Accepted Manuscript12(5):2541
Comment citer cedocument:
– Atmos. Chem. Phys., 2550.
Nat. Geosci.,Nat. le for activity iceconifer pollen. nucleation and ofbirch -
Bauditz, S., Niedermeier, D., Felgitsch, L., Huber,Bauditz, Niedermeier,Felgitsch, S., D., C.J., Kampf,
Air Qual. Atmos.Heal., Air Qual.
2(6):402
- 15:4077 Nowoisky, J. (2015). Ice (2015). Nowoisky, by water nucleation J. T., Kostle, P.A., Thorne, P.S., O’Shaughnessy,T., Kostle,Thorne, P.S., P.A., – 405.
– J. Geophys. Res. Atmos., 4091.
artin, S.T., Artaxo, P., Garland, P., artin, Artaxo, S.T., R.M., . Interhemispheric. of transport viable
Tollinger, M., Morris, C.E., Wex, H., Morris,Wex, C.E., Tollinger, M., a, H., and Iwasaka, H., and a, Y.(2016).
Aerobiologia (Bologna).,
9(6).
121(9):5071
Front.
Atmos.
21(1):1 - – – Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and Rojo, J., Oteros, J., Pérez Oteros, Rojo, J., J., Rogers,F.C.L.A. and(1937).Geographic National Meier, The Society Rodó, Reponen, K.,Ulevicius, T.,Willeke, (1996). A.,and Effect V.,Reponen, Grinshpun, S.A. ofrelative and Anderson, Conwell, M.(2001). K.L.,Reponen,S.A., J., Aerodynamic T.,Grinshpun, versus Wiest, Renard,I., P.,Canet, Sancelme, M.,Wirgot,L., N.,Deguillaume,A.and Delort, Raupach, R.A., Antonia, M.R., Rathnayake, Metwali C.M., Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, Fernández D., Bonini, E.,Fernández M.,Chiodini, Sánchez K.C., Oliver,Rodrí M.,Albertini, G., R., Thibaudon, stratosphereII.” inthe balloon “Explorer flightof1935 Association disease ofKawasaki windpatterns. withtropospheric Environ., humidityaerodynamic onthe diameterand respiratory of spores. fungal deposition 40(3):119 physical ofspores:Measurementand size for implication respiratory de biosurfactants. of cloud isolatedat (Fran microorganisms the PuyDôme de Appl. Mech. Rev., bioaerosols finecoarse in andparticles. O'Shaughnessy,Influence and E.A. Stone, (2017). P.T., ofrain onthe abundance of X., Ballester,Nakamura, Cayan, and (2011). Y., Uehara, D.,Melish,Burns, M.E., J., R., J.C. - Sánchez, J., Pessi, A.M., Reiniharju, J., Saarto, A.M.,Reiniharju, Pessi, M.C.,Guerrero, J., A.,Sánchez, Calderón, C.,Berra, J.,
– 30(23):3967 - 125. Rodríguez, S Rodríguez, 2019, 1-79. ,DOI: 10.1080/02786826.2019.1676395 Accepted Manuscript
Atmos. Chem. Phys, Atmos. Chem.
44(1):1 - Badia,Ferencova, R.,Cervigón,Z., Gutiérrez P., Comment citer cedocument: – , N.,Jayarathne, Huang, T., J., Kettler, Y.,Thorne, P.S., 3974. ., Tormo –
and (1991). Rajagopalan,S. Rough 25.
- Molina, R.,Damialis,Molina, A., Kolek, F., Traidl
16:12347
- Atmos. Chem. Phys., González, D., García, J., Trigo, D.,García, Myszkowska,González, J., D., M.M., – 12358. guez
QJR Soc., Meteorol. - De la Cruz, D., Sánchez D., laCruz, De ce) stationproductionce) for the of
17(3):2459 - Wall Turbulent Boundary Layers. Boundary Turbulent Wall
- Sci. Rep., US ArmyA - Bustillo, A.M.,Bergmann, position. – 2475. -
M. (2016). Screening
- 1(152). 63:217 Hoffmann, C., ir Corps
Grana, -
Atmos. Reyes, E.,
– 218.
Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and Šantl Santarpia, J.L., Pan, Y. Sahyoun, H.,Gosewinkel, U.,Šantl M.,Wex, V.,Rönkkö,Saari,H., Järvinen, A.,Pirjola,L., Niemi,T.,Kuuluvainen, J. R., S., Aurela,M.,Hillamo, L.M., Russell, L.N., andFrossard, P.K., Hawkins, A.A., Bates, (2010). Quinn, T.S. Carbohydrate Topping,Ruske,I., S., Stanley, Foot, Crawford, D.O., V.E.,Kaye, P.H., W.R., A.P.,and Morse, sorption byRubel, G.O.(1997). of biological watersingle Measurement vapor aerosols Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, Bratbak, G., and Löndahl, J. Bratbak,Löndahl, G.,and J. laboratory tosimulate atmosphericaging. reaction chamber R.G.(2012).Pinnick, Changes influorescence spec quantification of theimpactINP ofbacterialand climate. onweather U.S.(2016).Stratmann, Onthe F., usage and ofclassical Korsholm, nucleation and size Seasonal offluorescentand (2015). andconcentration Keskinen, bioaerosol diurnal J. variations Proc. Acad. Sci., Natl. ofsubmicroncomposition atmospheric theirocean production particlesand from bubblebursting. biological using aerosol Gallagher,Evaluation (2017). ofmachine M.W. learningalgorithms for classificationof primary Technol., groundeffect pollen exposure. ofheight on Radišić,P.,Šikoparija,C.A., B., Celenk,Schmidt S., I., Newbigin,Borycka, E.,Adams K.,Kasprzyk, Severova,Ribeiro, H.,Magyar, E., Makra,L., E.,Caeiro, D.,Alcázar, Udvardy, O.,P.,Galán, C., - Temkiv, B., T.,Amato,Gosewinkel, P., Finster,K.W., A., U.,Thyrhaug, R.,Charton, Chicot, distribution inthedistribution urban environment.
27(4):481 2019, 1-79. ,DOI: 10.1080/02786826.2019.1676395 Accepted Manuscript - L., Hill, S.C., Baker,L., Hill,S.C., B.,L., N., McKee, Cottrell, Ratnesar – 490. Comment citer cedocument:
107(15):6652
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- LIF spectrometer. – 6657. - Temkiv, T.,Nielsen, Finster, N.W., Temkiv, K., J.H., Sørensen, - Flow
Environ.Res.,
Aerosol AirQual.Res., Aerosol - - Rate Impinger the for Rate Studyof Concentration, Groom, B., Apangu, G.P., Frisk,Groom, Skjøt C.A., B., G.P., Apangu, tra of bioaerosols exposed to ozone ina tra toozone ofbioaerosolsexposed -
Weber, C.B., and Buters, J. (2019).Weber, C.B.,NearButers, J. and Atmos. Meas. Tech.,Atmos. Meas.
174:160
Opt. Express, – 169.
Atmos. Environ., Atmos.
15(2):572
20(28):29867. 10:695 - Shumate, S., andShumate, S.,
theory in – – . 581.
708. Aerosol Sci. Aerosol
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Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and Šaulienė, I.,Šaulienė,L.,L., Brdar, Daunys,Vaitkevičius, P., Šukienė, G.,Valiulis, G.,Matavulj, S.,Panic,M., Sattler, H.,and B., Psenner,Bacterialgrowth Puxbaum, R.(2001). cloud droplets. supercooled in Santl Šantl Šantl Šantl Šantl Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, Discuss., Rapid Sikoparija,Crouzy, B., recognitionM. (2019). B.,andB., Automatic pollen the Clot, Sofiev, with Geophys. Res. Lett., Characterization of airborne ice H., Clauss, N.,Ha T.,Woetmann, Arctic Research Villum Site Station. H.(2019).N., Massling,and Biogenic Wex, A., Sourc Fems Micriobiology Ecol., Greenlof bacteria insouthwest Aerobiologia (Bologna)., methanotrophic One,PLoS theMicrobial into U.G. andInventory (2013).AWindow Chemical Hailstones: a Cloud. Storm of Technol., Viability, MetabolicIce Activity, and - - - - - Temkiv, T.,Sahyoun, S.,Augustin M.,Finster, K., Hartmann, Lange,Temkiv, T., Beddows, R., Pilgaard, Gunde M., D.,S.,Dall’Osto, Rauter, Temkiv, U.,Starnawski, T.,Gosewinkel, Lever,(2018). P., Aeolian Finster,K. M.,and dispersal L.,Temkiv, Tina, K.,Hansen,(2013). Finster, B.M.,and U.G. Viable Karlson, Pašić, Temkiv, T.,Finster, K.,Dittmar, T., Hansen,B.M., Thyrhaug, - E parti
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117.
Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and Schumacher, Pöhlker, U., C.,Aalto,Hiltunen, C.J., V.,Petäjä, and P., M., Pöschl, T., Kulmala, Ice (1977).Schnell, R.C. Nuclei inSeawater, Fog Water andtheAir off Marine Coast of Nova III,Schmale Fetters, D.G., S.D., Ross, T.L., Tallapragada, Wood P., III,Schmale C. B.R., D.G., and (2008). application Dingus, Reinholtz, Development of and an Saxena, V.K. andIce Weintraub, D.C.(1987). InvolvementSaxena, V.K. (1983). BiogenicNuclei Evidence ofthe Antarctic in T.T., Mainelis,Savage, Krentz,G.,Pöhlker,Huffman, C.,andJ. C.E.,Könemann, Alex T., N.J., Han, (2018).Savage, and Evaluation Huffman, J.A. N.J. ofa hierarchical agglomerative clustering method Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, semi Huffman, (2013). cycles inboreal fluorescentbiologicalaerosol Seasonal J.A. of particles and 1975.Summer 28(1):1 Fusariumwheat blight head andproduce in mycotoxins. trichothecene Isolates(2012). Fusarium gr of J. F.Robot., autonomous unmanned aerialforaerobiological agriculturalabove vehicle sampling precisefields. J., Phys. Chem., Atmos. Meas. Tech., integrated (WIBS) sensor bioaerosol using size (2017). Systematic characterizationand f data preparation techniques. applied to WIBSlaboratory for d data improved
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2019, 1-79. ,DOI: 10.1080/02786826.2019.1676395
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J.
Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and Šikoparija, B., Šikoparija, B. Šikoparija, Panić, M.,Jakovetić,D.,and B., (2018a). HowO., Radišić, P. Marko,toprepare a pollen Abramidze,Sikoparija, M., B., Smith, C., Galán, Sesartic,Lohmann, A., and T.(2012). Storelvmo, U., BacteriaECHAM5 inthe Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, Pannonian Plain. (2013). M. AmechanismSmith, fortransport long from of Ambrosia distance the pollen reveals characteristics.emission (2018b). Highofairborne temporal above pollen resolution measurements thesource Ambrosia Aerobiologia (Bologna)., calendardaily forforecasting ofAmbrosia, pollenPoaceae? concentrations Betula and (Bologna)., Zemmer, F.(2017). Pollen Vecenaj,Vannini,Velasco J., A., C., Tassan Mazzocco, F., Testoni, Sindt, Smith, Szymanska,Satchwell, M., C., I., J., Šaulienė,Šikoparija, A., Ščevková,J., B., C.,Prentović, RappBenito,M.,Sallin, A.M., Radišić,V., Russo, P., M.,Rachoud, A.,Rodinkova, Pashley,Palamarchuk,S., Oliver,B., G.,Paganoni, C O.,Parati, M., Kofler, Myszkowska,D., Mányoki, V., Magyar,Manzano, G.,Maya J.M., D.,Nowak, M., Ferro,Ianovici,I.,J., E.,Kasprzyk, Hrastovćak, Flori, R., Graber, C., Kmenta, M.J., N.,Józsa, S., Cislaghi, B., G.,Clot, Dahl, Cortonesi,B.,Bella, A.,Della Cristofori, A., Dupuy, Dušička, V., N., K., Bigagli,Bonini,Cerovac,Bucher, M.,Bócsi,Caeiro, V., E., Celenk, S., E.,Chłopek,K., model.
Atmos. Chem. Phys., , Mimić, G., Panić, M., Marko, O., Radišić, P., Pejak Panić, M.,Marko, P., O., G., , Mimić, Radišić, Skjøth, C.A., Alm Kübler, K., Dahl, A., Sommer, J., Grewling, Kübler, C.A.,Alm K., J., L., A.,Sommer, Skjøth, Dahl, and Radišić, P.,
2019, 1-79. ,DOI: 10.1080/02786826.2019.1676395 3
Accepted3(2):191 Manuscript
Agric. For. Meteorol., Comment citer cedocument: – 199.
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180:112 –
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- Groom, B., Albertini, R., Anelli, P., Bastl, Anelli,B., P., R., Groom, Albertini, – 23.
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Aerobiologia
Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and Sterflinger, K. G.(2013). and Piñar, Microbial deterioration of art heritageand cultural works of P., Sofiev, M.,Siljamo, Ranta, H., and Rantio Sofiev, M.and K. Bergmann, Izquierdo,Sofiev, M.,Belmonte,Dahl, Gehrig,(2013). M., P. A.,and R.,Smith, J., R., Siljamo, D.J.,Timonen, H.J., Smith, Birmele,Jaffe, D.A., D.W., M.N.,Perry, Griffin, P.D.,and K.D., Ward, D.J.,Ravichandar, Griffin,Smith, Yu,H., S., J.D., Lusby, Tan, D.W., Jain, Q.,Thissen, J., T.,Nicoll, D.J.,Griffin,Smith, D.W., McPeters,P.D., Ward, R.D., B., Beman,Smith, M.,Gravano, D., Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, Tilting at windmills? Biometeorol., long and Health Impacts, Airborne pollen transport. App Intercontinental (2013).Roberts, M.S. Bacteriaand Dispersalof Archaea byTranspacific Winds. Front. Microbiol., Aircraftdetected from Results NASA anew inthetroposphere: Jaing, C.,andMcGrath, (2018). inearth’s Airborne bacteria stratosphere J. lower resemble taxa P., 27(4):319 survival thestratosphere in global and dispersal. for implications (REDUnmanned Aerial Systems detecting UAV payload. Shedler, S., Martinez, P., Osorio, A., Lechniak, Choi,Shedler, Sabino, Osorio,K.,Iverson, Martinez, P., A.,S., S., J., L., K., Chan, l. Environ.Microbiol., - range air birch transportrange considera pollen: of Theoretical – 332. 2019, 1-79. ,DOI: 10.1080/02786826.2019.1676395
Accepted Manuscript 50(6):392
9(1752). .
Appl. Microbiol. Biotechnol., Comment citer cedocument: – , in 2015 Workshop in2015 Education, andDevelopmentof onResearch, - 402. C. (2013). Allergenic Pollen. Springer Pollen. (2013).C. Allergenic Dordrecht Heidelberg. , inAllergenic Review Pollen:Release, theProduction, A of Distribution
79(4):1134
and Chen, Y. (2015).and validation Developmentof Chen, a Y. and microbe - UAS), UAS),
– 9.
- IEEE, 258 pp.
Lehtimäki, A.(2006). numerical Towards of forecasting
and (2011). Schuerger, Microbial A.C. 97(22):9637 – 264.
tions and a feasibility andtions a study.
– Bioaerosol Collector (ABC).Bioaerosol
46. Aerobiologia (Bologna).,Aerobiologia
Int. J.
-
Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and Tobo, Y., Adachi, K., DeMott, P.J., Hill, T.C.J., Hill, P.J., Tobo, Y., Hamilton,D.S.,Mahowald, Adachi,DeMott, N.M., Nagatsuka, K., N., Weber, D.,Thomson, E.S., Ebert, Bingemer, H.G., M.,and Tuomi, Pettersson,J., J. varianceThe distribution ofairborne urban in (2019). and rural environments. microorganisms Tesson, and S.V.M. Šantl Temkiv, Finster, T.Š., Hansen, K., III,Techy,L.,D.G., Schmaleand (2010). Woolsey, Coordinated aerobiological C.A. ofa sampling Li, Jie Yin,X.,Huang,Tang, Ma,Zhong,Li,S., He,Gu, W., Q., H.,and Y., C., M.,Wang,X. R.J., (2018).Swanson, B.E.and J.A. Development Huffman, characterizationof and an single inexpensive and T.C.J., Kreidenweis, K.J., Hill, Suski, DeMott,Levin, P.J., (2018). Miller, A., S.M. E.J.T., Ho S.C., Sullivan, Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, Ohata, S., Uetake, J., Kondo,Y.,Ohata, and Koike, S.,Uetake, J., M.(2019). Intensification observedemissions. ofnucleation ship ice inocean Environ.Pollut., Air diversity as assesseda stormcloud by of hailstones. Robot., plant pathogen atmosphere inthelower autonomous usingunmanned aerial two vehicles. of temperature. anemophilous pollen(2019).of Water and six species: hygroscopicgrowtheffect adsorption The particle fluorescence spectrometerbioaerosolmonitoring. for 13771. Agricultural h production inclouds. borneAquatic 9(November):1 and Microalgae.
27(3):335 2019, 1-79. ,DOI: 10.1080/02786826.2019.1676395 ose, C.,Leisner, Kiselev,and A.,Initiation Nenes,A.(2018).ofsecondary T., ice
Accepted Manuscript ofice emissions arvesting
Atmos. Chem. Phys., Atmos. Chem.
247:898 – 343. -
Temkiv,Ice T.(2018).NucleationAeolian in Activityand DispersalSuccess Comment citer cedocument: Atmos. Chem. Phys.,
– 906. B.M., Nielsen, N.W., andB.M.,N.W., Karlson,(2012). Nielsen,The U.G. microbial
19:22 - nucleating particles.
47 18(3):1593 – 2258. – 14.
FEMS Microbiol. Ecol., –
1610. Glacially sourced dust asdust Glacially a potentially sourced
Atmos. Chem. Phys.,Atmos. Chem. Opt. Expres
Sci. Rep., s,
26(3):3646
8(1):1111. 81(3):684 B.C. (2018).
18:13755 – –
95. 3660.
J. F.
–
- Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and Vesala, T., Kljun, N., Rannik, Ü., Rinne, J., Vesala, J., Ü., Rinne, Sogachev, T., Kljun,N.,Rannik, Sabelfeld, A.,Markkanen,Foken,and T., K., T., Vaïtilingom,L., Deguillaume, M., V., Sancelme,Chaumerliac, Vinatier,and Delort, M.,Amato, N., P., Vaitilingom,L., Deguillaume, M., V., Sancelme,Chaumerliac, Vinatier,and Delort, M.,Amato, N., P., United Kreidenweis, Demott, R. (2019). and Uetake,P.J., Tobo,Y.,T.C.J., Misumi, Uji,Y.,Hill, S.M., J., Le Lindeque,Bennett,Turnbull, P.C., P.M., J., A.M.,and (1998). Parks, S.R. Airborne Roux, Lighthart,Tong, inB.and distribution (2000).andsize Y. bacterial annual particleconcentration The Prenni, T.C.J., Tobo, Y.,A.J., Swoboda Hill, Demott, P.J., Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, Leclerc, M.Y. (2008). Flux and concentrationLeclerc, Flux M.Y.(2008). footprint budget clouds. in A. budget clouds. in A. https://sustainabledevelopment.un.org/ Microbiol., Seasonal changes ofairborne over communities Toky localmeteorology. and influence of Microbiol, movement ofanthrax spores frominthe EtoshaNational sites Namibia. carcass Park, 32(5):393 the ambient a atmospherearea rural ofthe in Valle Willamette Chem. Phys., Kreidenweis, (2014). Organic S.M. matter significantnucleating particles. sourceofice - - - Nations (2015). M. (2013). impact Potential ofmicrobial activity ontheoxidan M. (2012). impact Potential ofmicrobial activity ontheoxidan –
403. 84(4):667 accepted. 2019, 1-79. ,DOI: 10.1080/02786826.2019.1676395
Accepted Manuscript 14(16):8521
Proc. Natl. Acad. Sci. U.S.A., Proc. Natl. Acad. Sci., Proc. Natl. U.N. SustainableDevelopment Goals. Available at –
Comment citer cedocument: 676. –
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110(2):559 matters formatters ice of origin. agricultural nuclei soil
Nat. Geosci., Nat.
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12(4):253 – 64. y, Oregon.
t capacitycarbonand organic t capacitycarbonand organic – 258.
Aerosol Sci. Technol.,Aerosol
Environ.
J Appl
Front. Atmos.
Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and Wang, D.B.,G.B.,Moore, M.D., Beall, X.,Deane, Collins, K.A.,O.S.,Stokes, Ryder, C.M., Wang, Harder,Kelly, B., T.H.,L., Kovarik, D.S.,China,S., Piens, M.,Arey,B.W., S.T., Keiluweit, Waggoner,The(1973). removal Hel P.E.of Von Der(2009). S. LossF., CalculatorBorrmann, Particle Weiden, S.L.,Drewnick, and Diehl,Borrmann,von Blohn, K.,and(2005). S. N.,Mitra, The ability S.K., nucleating ice ofpollen: Vinatier, V.,Joly, Wirgot,L.,Abrantes, N.,M.,Sancelme, M.,Deguillaume, M., and Delort, A.M. Villa, T.F., F.,L.,and F. Salimi, Morton,K.,Morawska,Gonzalez, Development (2016). and Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, Sci., drops controlling in mix the Santander,Burrows, Sultana, C.M., S.M., M.V., and Prather, The (2017). and role K.A. of film jet Geosci.,Nat. Laskin, A.(2016).Gilles, M.K.,andgenerated organic Airborne soil particles by pr 63(10):1252 2:479 software the oftheperformance assessment for tool ofaerosol inlet systems. types. III: andPart studies inimmersion contact laboratory New freezing modesincluding more pollen 9323. by isolated microorganisms at the puystation. de Dôme waters(2016). impact Siderophorescloud onatmospheric and potential chemistry: in Production 16(12):2202. validation of system a UAVmeasurements.air based forpollution Pollut.,
114(27):6978
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2019, 1-79. ,DOI: 10.1080/02786826.2019.1676395 –
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50(17):9315 ecipitation. -
A new A new
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Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and Wilkinson, D.M.,Koumoutsaris, Mitchell,Wilkinson, E.A.D.,Bey, andI. Modelling S., (2012). theeffect ofsize and Putaud, Ogren,Wiedensohler, W., A.,J.P., (2014). Birmili, Recommendations J. f Gallagher,Whitehead, Robinson, J.D., Dorsey, N.,Gabey, M.W., Coe,H., J.R., McFiggans,G., A.M., Darbyshire, Barbosa,Whitehead, J.D., Crawford, J., I., E.,Brito, Gallagher, R., H.M.J., Stern, M.W., H.,Huang,L.,Wex, Zhang, Becagli, Hung, R., H.,Traversi, W., Moffett, Sheesley, C.E., S., R.J., Werchan,T., Goergen, M.,Sehlinger, F.,Bergmann, and K. T.,DeL.,Weil, Pavarini, Albanese, Filippo,M., C., Donati,Carotenuto, C.,Pindo, M., D., F., Pasqui, K.,Zou,Wei, Z.,yu,Zheng,Li, Y., Shen, F., C. Yao, Y.,Hu, Wu, M.,and M.(2016). Wu, J., Ambient Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, Sampling. above South in a rainforest tropical Flynn, M 9743. the central duringto dry from wet thetransition Amazon season. Kaye, Coe,H.,a P., Allan,Artaxo, P.H., J.D., at different Arctic locations. Herenz, F. and P., Stratmann, (2019). varia Annual Löffler,Lubitz,Barrett, H.,Hünerbein,J., Bossi,Linke, R.,Skov, A., O.,Hartmann, T.E.,M., M., sampling device. Microbiome, i L., Barbante, Poto, J., Gabrieli, C.,Sattler, B.,F. D.,Legal Cavalieri, and (2017). Miglietta, 550:751 bioaerosol observed particle and duringsunny haze dynamics mmigrants: Invasionmmigrants: alien microbial of during communities duststorms. winterdesert occurring
– .J., Ryder, J., Nemitz, E.,and Nemitz, Davies, Ryder, and(2010). J., F. dynamics Aerosolfluxes andwithin .J., 759. , inAerosolScience: andApplications, Technology 2019, 1-79. ,DOI: 10.1080/02786826.2019.1676395
5(1):32.
Accepted Manuscript
Allergo J. Int., Allergo
Comment citer cedocument:
Atmos. Chem. Phys.,
27(1)
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Atmos. Chem. Phys.,
1 bility ofice particleconcentrations nucleating – 31. -
C. (2018).C. pollator: a The personal pollen
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Atmos. Chem. Phys.,
10:9369 – 9382.
Sci. Total Environ.,Sci. Total or Aerosol
16:9727 –
Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and Wu, Y.,Calis,A., Wu, Y. Wu, Wright, Hader, McMeeking, T.P., Petters, J.D., M.D. (2014).a G.R.,and High as Relative Humidity Womack, A.M.,Bohannan, biogeography and Biodiversity B.J.M., Green,and J.L. (2010). Ishida, Womack, P.E., A.M.,Artaxo, F.Y., Saleska, Wiedemann, R.C., Mueller, S.R., Bohan K.T., R.,El Wolf, Wirgot, N., Wilson, Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, Taipei metropolis. Characteristics, ofambient andspatial determinants, variations fungal inthesubtropical levels IceTriggerRelease forNuclei. Widespread of atmosphere. atmosphere rainforest. the over Amazon andB.J.M., Green, Characterization of(2015). inthe active J.L. and communities total fungal environments. ofbacteriaPrévôt, (2017). A.S.H. Contribution the energetic metabolism ofthecloud microbiome. Nature, A marineand (2015). Murray,B.J. ofatmospheric biogenic source ice O.,Yakobi Wurl, J.P.S., Polishchuk,Najera, E.,Rae, Tempr Schiller,M., S., C.L.,Si, J.J., Kilthau, C., Mason,McFiggans, R.H., W.P., J.A., Carslaw,Judd, K.S., Huffman,L.A., G.,Miller, on theaerialmicroorganisms. of dispersal - H., T.W., Ladino, Burrows,L.A., M.N.,Brooks,I.M., Alpert,Browse, Breckels, J., P.A., S.M.,
Chan, C. Vinatier,L.,Deguillaume, V., M.,and Sancelme, (2017). Delort, H2O2 A.M. modulates -
Haddad, Dällenbach,I., Bal Slowik, K.,Bruns, J.G., J., E., Vasilescu, 525(7568):234 2019, 1-79. ,DOI: 10.1080/02786826.2019.1676395
Philos. Trans. R.Soc. BBiol.Sci., Trans. Philos.
Luo,Lutton,Lin, Y.,Y., Chen,Rivenson, C., M., H.C., Zhang, X.,Koydemir, Y., Accepted Manuscript
Atmos. Environ., - C., Rao, C.Y., Lee, Rao,C.Y., C., C.
Atmos. Environ., Comment citer cedocument: – 238. - Hancock, J.D., Abbatt, J.P.D., Aller, J.Y., Bertram, Aller,Hancock, J.Y., Abbatt,A.K., Knopf, J.P.D., D.A., J.D.,
160:97
41(12):2500 - – T., Hsu, H. T., Hsu,
106. Biogeosciences,
J. Biogeogr.,
Aerosol Sci. Technol.,Aerosol
- 365(1558). like particles to PM2.5 aerosol inurban andlike particles rural aerosol toPM2.5 – 2509. -
H., Chiu, Y. H., Chiu, Atmos. Chem. Phys.,
39(1):89
12:6337
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nan, nan, Version postprint perspectives in outdoor studies. Aerosol Science and Technology, In press, Published Online:8 October Huffman, J. A.(Auteur de correspondance) (2019). Bioaerosol fieldmeasurements: Challenges and Ziska, L.H., Makra, L.,Ziska,Harry,L.H.,Bruffaerts, Makra, F., N.,Hendrickx, Saarto, S.K., M.,Coates, A., Thibaudon, L.D., Chen,G., G.,Hudgins,Ziemba, Corr,Diskin, A.J., C.A., Crumeyrolle, Beyersdorf, S.N., C., Lichtveld,I.,Zavala, Ebersviller, J., S.,Carson, J.L., K.,Jaspers, H.E.,Sexton, Walters,G.W., Jeffries, Yao, M.(2018). Repr Yang,Kawaguchi, Y.,Yokobori, J., S., Yamamoto, among Y.,Yokoyama,Matsuki,H.(2015). N.,Matsuki, and Relationships indoor, H., Ichijo,Yamaguchi, Sakotani, A.,Baba,and Nasu,Global T., T., dispersion M.(2012).bacteri N., of Xu, Z.,F., Y.,Shen, Wu, Šantl-Temkiv, T.(Auteur decorrespondance), Sikoparija, B.,Maki, T.,Carotenuto, F.,Amato, P., Yao, M.,Morris,C. E.,Schnell,R., Jaenicke,R., Pöhlker,C.,DeMott, P.J.,Hill, Bonini, M., Oh, J.W., Bonini,Sullivan, M.,Oh,J.W., K., Ford,L.,Bro M., Oliver,A., Vokou, A., Charalampopoulos, G., Guđjohnsen, D.,Heiđmarsson, S., E., Damialis, usingIntegrated a Bioaerosol Wideband Sensor. andB.E. Anderson, ofbioaerosol Airborne (2016). the over Southeast States observations United Martin, Mi R., alternative exposure aerosol studies. invitro methodfor K.G., The and(2014). Gil W. Vizuete, Aerosol Sci., stratospherecollectedusing in2005. by a balloon Matsuzaka,Investigation Y.,Namiki, and M., otherscultivable (2008).microorganisms of inthe outdoor, and personal airbornepollencounts. Japanese cedar cells on Asian dust. engineering: andfuture. present, Past, MicroscopyLearning. and Deep Wang,Z., Ozcan, H.,Göröcs, Label and A.(2018). 2019, 1-79. ,DOI: 10.1080/02786826.2019.1676395
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