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http://hdl.handle.net/10261/139661
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dc.contributor.author | Anderson, D. C. | es_ES |
dc.contributor.author | Nicely, J. M. | es_ES |
dc.contributor.author | Salawitch, R. J. | es_ES |
dc.contributor.author | Canty, T. P. | es_ES |
dc.contributor.author | Dickerson, R. R. | es_ES |
dc.contributor.author | Hanisco, T. F. | es_ES |
dc.contributor.author | Wolfe, G. M. | es_ES |
dc.contributor.author | Apel, E. C. | es_ES |
dc.contributor.author | Atlas, Elliot L. | es_ES |
dc.contributor.author | Bannan, T. | es_ES |
dc.contributor.author | Bauguitte, S. | es_ES |
dc.contributor.author | Blake, N. J. | es_ES |
dc.contributor.author | Bresch, J. F. | es_ES |
dc.contributor.author | Campos, T. L. | es_ES |
dc.contributor.author | Carpenter, L. J. | es_ES |
dc.contributor.author | Cohen, M. D. | es_ES |
dc.contributor.author | Evans, M. | es_ES |
dc.contributor.author | Fernández, Rafael P. | es_ES |
dc.contributor.author | Kahn, B. H. | es_ES |
dc.contributor.author | Kinnison, Douglas E. | es_ES |
dc.contributor.author | Hall, S. R. | es_ES |
dc.contributor.author | Harris, Neil R. P. | es_ES |
dc.contributor.author | Hornbrook, Rebecca S. | es_ES |
dc.contributor.author | Lamarque, Jean-François | es_ES |
dc.contributor.author | Le Breton, M. | es_ES |
dc.contributor.author | Lee, J. D. | es_ES |
dc.contributor.author | Percival, C. | es_ES |
dc.contributor.author | Pfister, L. | es_ES |
dc.contributor.author | Pierce, Robert Bradley | es_ES |
dc.contributor.author | Riemer, D. D. | es_ES |
dc.contributor.author | Saiz-Lopez, A. | es_ES |
dc.contributor.author | Stunder, B. J. B. | es_ES |
dc.contributor.author | Thompson, A. M. | es_ES |
dc.contributor.author | Ullmann, K. | es_ES |
dc.contributor.author | Vaughan, A. | es_ES |
dc.contributor.author | Weinheimer, A. J. | es_ES |
dc.date.accessioned | 2016-10-31T13:26:24Z | - |
dc.date.available | 2016-10-31T13:26:24Z | - |
dc.date.issued | 2016 | - |
dc.identifier | doi: 10.1038/ncomms10267 | - |
dc.identifier | issn: 2041-1723 | - |
dc.identifier.citation | Nature Communications 7 (2016) | es_ES |
dc.identifier.uri | http://hdl.handle.net/10261/139661 | - |
dc.description.abstract | Air parcels with mixing ratios of high O and low HO (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 O 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 O and that low HO 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. | - |
dc.publisher | Nature Publishing Group | es_ES |
dc.relation.isversionof | Publisher's version | - |
dc.rights | openAccess | - |
dc.title | A pervasive role for biomass burning in tropical high ozone/low water structures | es_ES |
dc.type | artículo | es_ES |
dc.identifier.doi | 10.1038/ncomms10267 | - |
dc.date.updated | 2016-10-31T13:26:24Z | - |
dc.description.version | Peer Reviewed | - |
dc.language.rfc3066 | eng | - |
dc.relation.csic | Sí | es_ES |
dc.identifier.pmid | 26758808 | - |
dc.type.coar | http://purl.org/coar/resource_type/c_6501 | es_ES |
item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
item.fulltext | With Fulltext | - |
item.cerifentitytype | Publications | - |
item.openairetype | artículo | - |
item.grantfulltext | open | - |
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ncomms10267.pdf | 1,78 MB | Adobe PDF | Visualizar/Abrir |
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