A pervasive role for biomass burning in tropical high ozone/low water structures
- Autores
- Anderson, Daniel C.; Nicely, Julie M.; Salawitch, Ross J.; Canty, Timothy P.; Dickerson, Russell R.; Hanisco, Thomas F.; Wolfe, Glenn M.; Apel, Eric C.; Atlas, Elliot; Bannan, Thomas J.; Bauguitte, Stephane; Blake, Nicola J.; Bresch, James F.; Campos, Teresa L.; Carpenter, Lucy J.; Cohen, Mark D.; Evans, Mathew; Fernandez, Rafael Pedro; Kahn, Brian H.; Kinnison, Douglas E.; Hall, Samuel R.; Harris, Neil R. P.; Hornbrook, Rebecca S.; Lamarque, Jean Francois; Le Breton, Michael; Lee, James D.; Percival, Carl; Pfister, Leonhard; Pierce, R. Bradley; Riemer, Daniel D.; Saiz López, Alfonso; Stunder, Barbara J. B.; Thompson, Anne M.; Ullmann, Kirk; Vaughan, Adam; Weinheimer, Andrew J.
- Año de publicación
- 2016
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- Air parcels with mixing ratios of high O3 and low H2O (HOLW) are common features in the tropical western Pacific (TWP) mid-troposphere (300-700 hPa). Here, using data collected during aircraft sampling of the TWP in winter 2014, we find strong, positive correlations of O3 with multiple biomass burning tracers in these HOLW structures. Ozone levels in these structures are about a factor of three larger than background. Models, satellite data and aircraft observations are used to show fires in tropical Africa and Southeast Asia are the dominant source of high O3 and that low H2O results from large-scale descent within the tropical troposphere. Previous explanations that attribute HOLW structures to transport from the stratosphere or mid-latitude troposphere are inconsistent with our observations. This study suggest a larger role for biomass burning in the radiative forcing of climate in the remote TWP than is commonly appreciated.
Fil: Anderson, Daniel C.. University of Maryland; Estados Unidos
Fil: Nicely, Julie M.. University of Maryland; Estados Unidos
Fil: Salawitch, Ross J.. University of Maryland; Estados Unidos
Fil: Canty, Timothy P.. University of Maryland; Estados Unidos
Fil: Dickerson, Russell R.. University of Maryland; Estados Unidos
Fil: Hanisco, Thomas F.. Nasa Goddard Space Flight Center; Estados Unidos
Fil: Wolfe, Glenn M.. University of Maryland; Estados Unidos
Fil: Apel, Eric C.. Nasa Goddard Space Flight Center; Estados Unidos
Fil: Atlas, Elliot. National Center for Atmospheric Research; Estados Unidos
Fil: Bannan, Thomas J.. Rosenstiel School Of Marine And Atmospheric Science; Estados Unidos
Fil: Bauguitte, Stephane. University of Manchester; Reino Unido
Fil: Blake, Nicola J.. University of California at Irvine; Estados Unidos
Fil: Bresch, James F.. University of California at Irvine; Estados Unidos
Fil: Campos, Teresa L.. National Center for Atmospheric Research; Estados Unidos
Fil: Carpenter, Lucy J.. National Center for Atmospheric Research; Estados Unidos
Fil: Cohen, Mark D.. National Oceanic And Atmospheric Administration; Estados Unidos
Fil: Evans, Mathew. National Oceanic And Atmospheric Administration; Estados Unidos
Fil: Fernandez, Rafael Pedro. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza; Argentina. Universidad Nacional de Cuyo; Argentina
Fil: Kahn, Brian H.. Consejo Superior de Investigaciones Científicas. Instituto de Química Física; España
Fil: Kinnison, Douglas E.. National Center for Atmospheric Research; Estados Unidos
Fil: Hall, Samuel R.. Jet Propulsion Laboratory, California Institute Of Technology; Estados Unidos
Fil: Harris, Neil R. P.. National Center for Atmospheric Research; Estados Unidos
Fil: Hornbrook, Rebecca S.. National Center for Atmospheric Research; Estados Unidos
Fil: Lamarque, Jean Francois. University of Cambridge; Estados Unidos
Fil: Le Breton, Michael. National Center for Atmospheric Research; Estados Unidos
Fil: Lee, James D.. National Center for Atmospheric Research; Estados Unidos
Fil: Percival, Carl. University of Manchester; Reino Unido
Fil: Pfister, Leonhard. University of York; Reino Unido
Fil: Pierce, R. Bradley. University of Manchester; Reino Unido
Fil: Riemer, Daniel D.. University of Miami; Estados Unidos
Fil: Saiz López, Alfonso. Institute of Physical Chemistry Rocasolano; España
Fil: Stunder, Barbara J. B.. National Oceanic And Atmospheric Administration; Estados Unidos
Fil: Thompson, Anne M.. Nasa Goddard Space Flight Center; Estados Unidos
Fil: Ullmann, Kirk. National Center for Atmospheric Research; Estados Unidos
Fil: Vaughan, Adam. University Of York; Estados Unidos
Fil: Weinheimer, Andrew J.. University Of York; Estados Unidos - Materia
-
HOLW Structures
Biomass Burning
OH Hole
Tropical Western Pacific - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- https://creativecommons.org/licenses/by/2.5/ar/
- Repositorio
.jpg)
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/160288
Ver los metadatos del registro completo
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A pervasive role for biomass burning in tropical high ozone/low water structuresAnderson, Daniel C.Nicely, Julie M.Salawitch, Ross J.Canty, Timothy P.Dickerson, Russell R.Hanisco, Thomas F.Wolfe, Glenn M.Apel, Eric C.Atlas, ElliotBannan, Thomas J.Bauguitte, StephaneBlake, Nicola J.Bresch, James F.Campos, Teresa L.Carpenter, Lucy J.Cohen, Mark D.Evans, MathewFernandez, Rafael PedroKahn, Brian H.Kinnison, Douglas E.Hall, Samuel R.Harris, Neil R. P.Hornbrook, Rebecca S.Lamarque, Jean FrancoisLe Breton, MichaelLee, James D.Percival, CarlPfister, LeonhardPierce, R. BradleyRiemer, Daniel D.Saiz López, AlfonsoStunder, Barbara J. B.Thompson, Anne M.Ullmann, KirkVaughan, AdamWeinheimer, Andrew J.HOLW StructuresBiomass BurningOH HoleTropical Western Pacifichttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Air parcels with mixing ratios of high O3 and low H2O (HOLW) are common features in the tropical western Pacific (TWP) mid-troposphere (300-700 hPa). Here, using data collected during aircraft sampling of the TWP in winter 2014, we find strong, positive correlations of O3 with multiple biomass burning tracers in these HOLW structures. Ozone levels in these structures are about a factor of three larger than background. Models, satellite data and aircraft observations are used to show fires in tropical Africa and Southeast Asia are the dominant source of high O3 and that low H2O results from large-scale descent within the tropical troposphere. Previous explanations that attribute HOLW structures to transport from the stratosphere or mid-latitude troposphere are inconsistent with our observations. This study suggest a larger role for biomass burning in the radiative forcing of climate in the remote TWP than is commonly appreciated.Fil: Anderson, Daniel C.. University of Maryland; Estados UnidosFil: Nicely, Julie M.. University of Maryland; Estados UnidosFil: Salawitch, Ross J.. University of Maryland; Estados UnidosFil: Canty, Timothy P.. University of Maryland; Estados UnidosFil: Dickerson, Russell R.. University of Maryland; Estados UnidosFil: Hanisco, Thomas F.. Nasa Goddard Space Flight Center; Estados UnidosFil: Wolfe, Glenn M.. University of Maryland; Estados UnidosFil: Apel, Eric C.. Nasa Goddard Space Flight Center; Estados UnidosFil: Atlas, Elliot. National Center for Atmospheric Research; Estados UnidosFil: Bannan, Thomas J.. Rosenstiel School Of Marine And Atmospheric Science; Estados UnidosFil: Bauguitte, Stephane. University of Manchester; Reino UnidoFil: Blake, Nicola J.. University of California at Irvine; Estados UnidosFil: Bresch, James F.. University of California at Irvine; Estados UnidosFil: Campos, Teresa L.. National Center for Atmospheric Research; Estados UnidosFil: Carpenter, Lucy J.. National Center for Atmospheric Research; Estados UnidosFil: Cohen, Mark D.. National Oceanic And Atmospheric Administration; Estados UnidosFil: Evans, Mathew. National Oceanic And Atmospheric Administration; Estados UnidosFil: Fernandez, Rafael Pedro. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza; Argentina. Universidad Nacional de Cuyo; ArgentinaFil: Kahn, Brian H.. Consejo Superior de Investigaciones Científicas. Instituto de Química Física; EspañaFil: Kinnison, Douglas E.. National Center for Atmospheric Research; Estados UnidosFil: Hall, Samuel R.. Jet Propulsion Laboratory, California Institute Of Technology; Estados UnidosFil: Harris, Neil R. P.. National Center for Atmospheric Research; Estados UnidosFil: Hornbrook, Rebecca S.. National Center for Atmospheric Research; Estados UnidosFil: Lamarque, Jean Francois. University of Cambridge; Estados UnidosFil: Le Breton, Michael. National Center for Atmospheric Research; Estados UnidosFil: Lee, James D.. National Center for Atmospheric Research; Estados UnidosFil: Percival, Carl. University of Manchester; Reino UnidoFil: Pfister, Leonhard. University of York; Reino UnidoFil: Pierce, R. Bradley. University of Manchester; Reino UnidoFil: Riemer, Daniel D.. University of Miami; Estados UnidosFil: Saiz López, Alfonso. Institute of Physical Chemistry Rocasolano; EspañaFil: Stunder, Barbara J. B.. National Oceanic And Atmospheric Administration; Estados UnidosFil: Thompson, Anne M.. Nasa Goddard Space Flight Center; Estados UnidosFil: Ullmann, Kirk. National Center for Atmospheric Research; Estados UnidosFil: Vaughan, Adam. University Of York; Estados UnidosFil: Weinheimer, Andrew J.. University Of York; Estados UnidosNature Publishing Group2016-01info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/160288Anderson, Daniel C.; Nicely, Julie M.; Salawitch, Ross J.; Canty, Timothy P.; Dickerson, Russell R.; et al.; A pervasive role for biomass burning in tropical high ozone/low water structures; Nature Publishing Group; Nature Communications; 7; 1-2016; 1-132041-1723CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/http://www.nature.com/ncomms/2016/160113/ncomms10267/full/ncomms10267.htmlinfo:eu-repo/semantics/altIdentifier/doi/10.1038/ncomms10267info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-10-22T11:19:12Zoai:ri.conicet.gov.ar:11336/160288instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-10-22 11:19:12.829CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
| dc.title.none.fl_str_mv |
A pervasive role for biomass burning in tropical high ozone/low water structures |
| title |
A pervasive role for biomass burning in tropical high ozone/low water structures |
| spellingShingle |
A pervasive role for biomass burning in tropical high ozone/low water structures Anderson, Daniel C. HOLW Structures Biomass Burning OH Hole Tropical Western Pacific |
| title_short |
A pervasive role for biomass burning in tropical high ozone/low water structures |
| title_full |
A pervasive role for biomass burning in tropical high ozone/low water structures |
| title_fullStr |
A pervasive role for biomass burning in tropical high ozone/low water structures |
| title_full_unstemmed |
A pervasive role for biomass burning in tropical high ozone/low water structures |
| title_sort |
A pervasive role for biomass burning in tropical high ozone/low water structures |
| dc.creator.none.fl_str_mv |
Anderson, Daniel C. Nicely, Julie M. Salawitch, Ross J. Canty, Timothy P. Dickerson, Russell R. Hanisco, Thomas F. Wolfe, Glenn M. Apel, Eric C. Atlas, Elliot Bannan, Thomas J. Bauguitte, Stephane Blake, Nicola J. Bresch, James F. Campos, Teresa L. Carpenter, Lucy J. Cohen, Mark D. Evans, Mathew Fernandez, Rafael Pedro Kahn, Brian H. Kinnison, Douglas E. Hall, Samuel R. Harris, Neil R. P. Hornbrook, Rebecca S. Lamarque, Jean Francois Le Breton, Michael Lee, James D. Percival, Carl Pfister, Leonhard Pierce, R. Bradley Riemer, Daniel D. Saiz López, Alfonso Stunder, Barbara J. B. Thompson, Anne M. Ullmann, Kirk Vaughan, Adam Weinheimer, Andrew J. |
| author |
Anderson, Daniel C. |
| author_facet |
Anderson, Daniel C. Nicely, Julie M. Salawitch, Ross J. Canty, Timothy P. Dickerson, Russell R. Hanisco, Thomas F. Wolfe, Glenn M. Apel, Eric C. Atlas, Elliot Bannan, Thomas J. Bauguitte, Stephane Blake, Nicola J. Bresch, James F. Campos, Teresa L. Carpenter, Lucy J. Cohen, Mark D. Evans, Mathew Fernandez, Rafael Pedro Kahn, Brian H. Kinnison, Douglas E. Hall, Samuel R. Harris, Neil R. P. Hornbrook, Rebecca S. Lamarque, Jean Francois Le Breton, Michael Lee, James D. Percival, Carl Pfister, Leonhard Pierce, R. Bradley Riemer, Daniel D. Saiz López, Alfonso Stunder, Barbara J. B. Thompson, Anne M. Ullmann, Kirk Vaughan, Adam Weinheimer, Andrew J. |
| author_role |
author |
| author2 |
Nicely, Julie M. Salawitch, Ross J. Canty, Timothy P. Dickerson, Russell R. Hanisco, Thomas F. Wolfe, Glenn M. Apel, Eric C. Atlas, Elliot Bannan, Thomas J. Bauguitte, Stephane Blake, Nicola J. Bresch, James F. Campos, Teresa L. Carpenter, Lucy J. Cohen, Mark D. Evans, Mathew Fernandez, Rafael Pedro Kahn, Brian H. Kinnison, Douglas E. Hall, Samuel R. Harris, Neil R. P. Hornbrook, Rebecca S. Lamarque, Jean Francois Le Breton, Michael Lee, James D. Percival, Carl Pfister, Leonhard Pierce, R. Bradley Riemer, Daniel D. Saiz López, Alfonso Stunder, Barbara J. B. Thompson, Anne M. Ullmann, Kirk Vaughan, Adam Weinheimer, Andrew J. |
| author2_role |
author author author author author author author author author author author author author author author author author author author author author author author author author author author author author author author author author author author |
| dc.subject.none.fl_str_mv |
HOLW Structures Biomass Burning OH Hole Tropical Western Pacific |
| topic |
HOLW Structures Biomass Burning OH Hole Tropical Western Pacific |
| purl_subject.fl_str_mv |
https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
| dc.description.none.fl_txt_mv |
Air parcels with mixing ratios of high O3 and low H2O (HOLW) are common features in the tropical western Pacific (TWP) mid-troposphere (300-700 hPa). Here, using data collected during aircraft sampling of the TWP in winter 2014, we find strong, positive correlations of O3 with multiple biomass burning tracers in these HOLW structures. Ozone levels in these structures are about a factor of three larger than background. Models, satellite data and aircraft observations are used to show fires in tropical Africa and Southeast Asia are the dominant source of high O3 and that low H2O results from large-scale descent within the tropical troposphere. Previous explanations that attribute HOLW structures to transport from the stratosphere or mid-latitude troposphere are inconsistent with our observations. This study suggest a larger role for biomass burning in the radiative forcing of climate in the remote TWP than is commonly appreciated. Fil: Anderson, Daniel C.. University of Maryland; Estados Unidos Fil: Nicely, Julie M.. University of Maryland; Estados Unidos Fil: Salawitch, Ross J.. University of Maryland; Estados Unidos Fil: Canty, Timothy P.. University of Maryland; Estados Unidos Fil: Dickerson, Russell R.. University of Maryland; Estados Unidos Fil: Hanisco, Thomas F.. Nasa Goddard Space Flight Center; Estados Unidos Fil: Wolfe, Glenn M.. University of Maryland; Estados Unidos Fil: Apel, Eric C.. Nasa Goddard Space Flight Center; Estados Unidos Fil: Atlas, Elliot. National Center for Atmospheric Research; Estados Unidos Fil: Bannan, Thomas J.. Rosenstiel School Of Marine And Atmospheric Science; Estados Unidos Fil: Bauguitte, Stephane. University of Manchester; Reino Unido Fil: Blake, Nicola J.. University of California at Irvine; Estados Unidos Fil: Bresch, James F.. University of California at Irvine; Estados Unidos Fil: Campos, Teresa L.. National Center for Atmospheric Research; Estados Unidos Fil: Carpenter, Lucy J.. National Center for Atmospheric Research; Estados Unidos Fil: Cohen, Mark D.. National Oceanic And Atmospheric Administration; Estados Unidos Fil: Evans, Mathew. National Oceanic And Atmospheric Administration; Estados Unidos Fil: Fernandez, Rafael Pedro. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza; Argentina. Universidad Nacional de Cuyo; Argentina Fil: Kahn, Brian H.. Consejo Superior de Investigaciones Científicas. Instituto de Química Física; España Fil: Kinnison, Douglas E.. National Center for Atmospheric Research; Estados Unidos Fil: Hall, Samuel R.. Jet Propulsion Laboratory, California Institute Of Technology; Estados Unidos Fil: Harris, Neil R. P.. National Center for Atmospheric Research; Estados Unidos Fil: Hornbrook, Rebecca S.. National Center for Atmospheric Research; Estados Unidos Fil: Lamarque, Jean Francois. University of Cambridge; Estados Unidos Fil: Le Breton, Michael. National Center for Atmospheric Research; Estados Unidos Fil: Lee, James D.. National Center for Atmospheric Research; Estados Unidos Fil: Percival, Carl. University of Manchester; Reino Unido Fil: Pfister, Leonhard. University of York; Reino Unido Fil: Pierce, R. Bradley. University of Manchester; Reino Unido Fil: Riemer, Daniel D.. University of Miami; Estados Unidos Fil: Saiz López, Alfonso. Institute of Physical Chemistry Rocasolano; España Fil: Stunder, Barbara J. B.. National Oceanic And Atmospheric Administration; Estados Unidos Fil: Thompson, Anne M.. Nasa Goddard Space Flight Center; Estados Unidos Fil: Ullmann, Kirk. National Center for Atmospheric Research; Estados Unidos Fil: Vaughan, Adam. University Of York; Estados Unidos Fil: Weinheimer, Andrew J.. University Of York; Estados Unidos |
| description |
Air parcels with mixing ratios of high O3 and low H2O (HOLW) are common features in the tropical western Pacific (TWP) mid-troposphere (300-700 hPa). Here, using data collected during aircraft sampling of the TWP in winter 2014, we find strong, positive correlations of O3 with multiple biomass burning tracers in these HOLW structures. Ozone levels in these structures are about a factor of three larger than background. Models, satellite data and aircraft observations are used to show fires in tropical Africa and Southeast Asia are the dominant source of high O3 and that low H2O results from large-scale descent within the tropical troposphere. Previous explanations that attribute HOLW structures to transport from the stratosphere or mid-latitude troposphere are inconsistent with our observations. This study suggest a larger role for biomass burning in the radiative forcing of climate in the remote TWP than is commonly appreciated. |
| publishDate |
2016 |
| dc.date.none.fl_str_mv |
2016-01 |
| dc.type.none.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion http://purl.org/coar/resource_type/c_6501 info:ar-repo/semantics/articulo |
| format |
article |
| status_str |
publishedVersion |
| dc.identifier.none.fl_str_mv |
http://hdl.handle.net/11336/160288 Anderson, Daniel C.; Nicely, Julie M.; Salawitch, Ross J.; Canty, Timothy P.; Dickerson, Russell R.; et al.; A pervasive role for biomass burning in tropical high ozone/low water structures; Nature Publishing Group; Nature Communications; 7; 1-2016; 1-13 2041-1723 CONICET Digital CONICET |
| url |
http://hdl.handle.net/11336/160288 |
| identifier_str_mv |
Anderson, Daniel C.; Nicely, Julie M.; Salawitch, Ross J.; Canty, Timothy P.; Dickerson, Russell R.; et al.; A pervasive role for biomass burning in tropical high ozone/low water structures; Nature Publishing Group; Nature Communications; 7; 1-2016; 1-13 2041-1723 CONICET Digital CONICET |
| dc.language.none.fl_str_mv |
eng |
| language |
eng |
| dc.relation.none.fl_str_mv |
info:eu-repo/semantics/altIdentifier/url/http://www.nature.com/ncomms/2016/160113/ncomms10267/full/ncomms10267.html info:eu-repo/semantics/altIdentifier/doi/10.1038/ncomms10267 |
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openAccess |
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application/pdf application/pdf application/pdf |
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Nature Publishing Group |
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Nature Publishing Group |
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dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar |
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