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dc.contributor.authorFuentes, Jose D.
dc.contributor.authorChamecki, Marcelo
dc.contributor.authorNascimento dos Santos, Rosa Maria
dc.contributor.authorvon Randow, Celso
dc.contributor.authorStoy, Paul C.
dc.contributor.authorKatul, Gabriel
dc.contributor.authorFitzjarrald, David
dc.contributor.authorManzi, Antonio O.
dc.contributor.authorGerken, Tobias
dc.contributor.authorTrowbridge, Amy M.
dc.contributor.authorFreire, Livia Souza
dc.contributor.authorRuiz-Plancarte, Jesus
dc.contributor.authorFurtunato Maia, Jair Max
dc.contributor.authorTota, Julio
dc.contributor.authorDias, Nelson
dc.contributor.authorFisch, Gilberto
dc.contributor.authorSchumacher, Courtney
dc.contributor.authorAcevedo, Otavio C.
dc.contributor.authorMercer, Juliane Rezende
dc.contributor.authorYanez-Serrano, Ana Maria
dc.date.accessioned2017-05-12T19:17:35Z
dc.date.available2017-05-12T19:17:35Z
dc.date.issued2016-12
dc.identifier.citationFuentes, Jose D, Marcelo Chamecki, Rosa Maria Nascimento dos Santos, Celso Von Randow, Paul C Stoy, Katul Gabriel, David Fitzjarrald, Antonio Manzi, Tobias Gerken, Amy Trowbridge, Livia Souza Freire, Jesus Ruiz-Plancarte, Jair Max Furtunato Maia, Julio Tota, Nelson Dias, Gilberto Fisch, Courtney Schumacher, Otavio Acevedo, Juliane Rezende Mercer, and Ana Maria Yanez-Serrano. "Linking meteorology, turbulence, and air chemistry in the Amazon Rain Forest." Bulletin of the American Meteorological Society 97, no. 12 (December 2016): 2329. DOI:https://dx.doi.org/10.1175/BAMS-D-15-00152.1 .en_US
dc.identifier.issn0003-0007
dc.identifier.urihttps://scholarworks.montana.edu/xmlui/handle/1/12832
dc.description.abstractWe describe the salient features of a field study whose goals are to quantify the vertical distribution of plant-emitted hydrocarbons and their contribution to aerosol and cloud condensation nuclei production above a central Amazonian rain forest. Using observing systems deployed on a 50-m meteorological tower, complemented with tethered balloon deployments, the vertical distribution of hydrocarbons and aerosols was determined under different boundary layer thermodynamic states. The rain forest emits sufficient reactive hydrocarbons, such as isoprene and monoterpenes, to provide precursors of secondary organic aerosols and cloud condensation nuclei. Mesoscale convective systems transport ozone from the middle troposphere, enriching the atmospheric boundary layer as well as the forest canopy and surface layer. Through multiple chemical transformations, the ozone-enriched atmospheric surface layer can oxidize rain forest-emitted hydrocarbons. One conclusion derived from the field studies is that the rain forest produces the necessary chemical species and in sufficient amounts to undergo oxidation and generate aerosols that subsequently activate into cloud condensation nuclei.en_US
dc.description.sponsorshipU.S. Department of Energy; National Science Foundation; Universidade do Estado do Amazonia; Institute Nacional de Pesquisas da Amazonia; Central Office of the Large-Scale Biosphere-Atmosphere Experiment in Amazonia;en_US
dc.language.isoen_USen_US
dc.titleLinking meteorology, turbulence, and air chemistry in the Amazon Rain Foresten_US
dc.typeArticleen_US
mus.citation.extentfirstpage2329en_US
mus.citation.issue12en_US
mus.citation.journaltitleBulletin of the American Meteorological Societyen_US
mus.citation.volume97en_US
mus.identifier.categoryLife Sciences & Earth Sciencesen_US
mus.identifier.doi10.1175/BAMS-D-15-00152.1en_US
mus.relation.collegeCollege of Agricultureen_US
mus.relation.departmentLand Resources & Environmental Sciences.en_US
mus.relation.universityMontana State University - Bozemanen_US
mus.data.thumbpage3en_US
mus.contributor.orcidGerken, Tobias|0000-0001-5617-186Xen_US


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