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http://hdl.handle.net/10261/197047
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dc.contributor.author | Gordillo Vázquez, Francisco J. | es_ES |
dc.contributor.author | Pérez-Invernón, Francisco J. | es_ES |
dc.contributor.author | Huntrieser, H. | es_ES |
dc.contributor.author | Smith, A. K. | es_ES |
dc.date.accessioned | 2019-12-19T08:37:40Z | - |
dc.date.available | 2019-12-19T08:37:40Z | - |
dc.date.issued | 2019 | - |
dc.identifier.citation | Earth and Space Science (2019) | es_ES |
dc.identifier.issn | 2333-5084 | - |
dc.identifier.uri | http://hdl.handle.net/10261/197047 | - |
dc.description | This is an open access article under the terms of the Creative Commons Attribution‐NonCommercial‐NoDerivs License, which permits use and distribution in any medium, provided the original work is properly cited, the use is non‐commercial and no modifications or adaptations are made.-- Data presented here are available from figshare repository (https://bit.ly/2ww816g).Alternatively, requests for data and codes used to generate figures, graphs, plots, or tables may be made to the authors F. J. G. V (vazquez@iaa.es) or F. J. P. I. (fjpi@iaa.es). | es_ES |
dc.description.abstract | We present simulations performed with six lightning parameterizations implemented in the Community Atmosphere Model (CAM5). The amount of lightning-produced nitrogen oxides (LNOx) by the various schemes considered is estimated. We provide some insight on how the lightning NO injected in the atmosphere influences the global concentrations of key chemical species such as OH, HO2, H2O2, NOx, O-3, SO2, CO, and HNO3. The vertical global averaged densities of HO2, H2O2, CO, and SO2 are depleted due to lightning while those of NO, NO2, O-3, OH, and HNO3 increase. Our results indicate that the parameterizations based on the upward ice flux (ICEFLUX) exhibit the largest global and midlatitude spatial correlations (0.73 and 0.632 for ICEFLUX and 0.72 and 0.553 for cloud top height) with respect to satellite global flash rate observations. Five out of the six lightning schemes investigated exhibit larger LNOx per flash in the midlatitudes than in the tropics. In particular, it is found that the ICEFLUX midlatitude LNOx per flash exhibits the largest difference with respect to its predicted tropical LNOx per flash, in agreement with available observations. When using CAM5, the ICEFLUX lightning parameterization could be considered a reliable lightning scheme (within its intrinsic uncertainties) in terms of its geographical distribution. Both ICEFLUX and cloud top height results agree with the enhancements of NO2 and O-3 produced by lightning over tropical Atlantic and Africa and the weaker lightning background over the tropical Pacific reported by Martin et al. (2007) in the periods and locations (upper troposphere) where lightning is expected to dominate the trace gas observations.©2019. The Authors. | es_ES |
dc.description.sponsorship | This work was supported by the Spanish Ministry of Science and Innovation, MINECO under Project ESP2017-86263-C4-4-R and by the EU through the H2020 Science and Innovation with Thunderstorms (SAINT) project (Ref. 722337) and the FEDER program. F. J. P. I. acknowledges support by a PhD research contract, Code BES-2014-069567 and by the EU through the European Research Council (ERC) under the European Union's H2020 programm/ERC Grant 681257. F. J. G. V. acknowledges support from the Spanish Ministry of Education and Culture under the Salvador de Madariaga Program PRX17/00078. Authors F. J. G. V. and F. J. P. I. acknowledge financial support from the State Agency for Research of the Spanish MCIU through the "Center of Excellence Severo Ochoa" award for the Instituto de Astrofisica de Andalucia (SEV-2017-0709). H. H. acknowledges support from the DLR project KliSAW. The National Center for Atmospheric Research is sponsored by the National Science Foundation. The CESM project is supported by the National Science Foundation and the Office of Science (BER) of the U.S. Department of Energy. Computing resources were provided by the Climate Simulation Laboratory at NCAR's Computational and Information Systems Laboratory (CISL), sponsored by the National Science Foundation and other agencies. | es_ES |
dc.publisher | American Geophysical Union | es_ES |
dc.relation | info:eu-repo/grantAgreement/MINECO/Plan Estatal de Investigación Científica y Técnica y de Innovación 2013-2016/ESP2017-86263-C4-4-R | es_ES |
dc.relation | info:eu-repo/grantAgreement/EC/H2020/722337 | es_ES |
dc.relation | info:eu-repo/grantAgreement/EC/H2020/681257 | es_ES |
dc.relation | info:eu-repo/grantAgreement/MINECO/Plan Estatal de Investigación Científica y Técnica y de Innovación 2013-2016/BES-2014-069567 | es_ES |
dc.relation | info:eu-repo/grantAgreement/MINECO/Plan Estatal de Investigación Científica y Técnica y de Innovación 2013-2016/SEV-2017-0709 | es_ES |
dc.relation.isversionof | Publisher's version | es_ES |
dc.rights | openAccess | es_ES |
dc.title | Comparison of Six Lightning Parameterizations in CAM5 and the Impact on Global Atmospheric Chemistry | es_ES |
dc.type | artículo | es_ES |
dc.identifier.doi | 10.1029/2019EA000873 | - |
dc.description.peerreviewed | Peer reviewed | es_ES |
dc.relation.publisherversion | http://dx.doi.org/10.1029/2019EA000873 | es_ES |
dc.rights.license | https://creativecommons.org/licenses/by-nc-nd/4.0/ | es_ES |
dc.contributor.funder | Ministerio de Ciencia e Innovación (España) | es_ES |
dc.contributor.funder | European Commission | es_ES |
dc.contributor.funder | European Research Council | es_ES |
dc.contributor.funder | Ministerio de Educación y Cultura (España) | es_ES |
dc.contributor.funder | Ministerio de Ciencia, Innovación y Universidades (España) | es_ES |
dc.contributor.funder | German Centre for Air and Space Travel | es_ES |
dc.contributor.funder | National Science Foundation (US) | es_ES |
dc.relation.csic | Sí | es_ES |
oprm.item.hasRevision | no ko 0 false | * |
dc.identifier.funder | http://dx.doi.org/10.13039/100000001 | es_ES |
dc.identifier.funder | http://dx.doi.org/10.13039/501100000781 | es_ES |
dc.identifier.funder | http://dx.doi.org/10.13039/501100000780 | es_ES |
dc.identifier.funder | http://dx.doi.org/10.13039/501100004837 | es_ES |
dc.identifier.funder | http://dx.doi.org/10.13039/501100002946 | es_ES |
dc.type.coar | http://purl.org/coar/resource_type/c_6501 | es_ES |
item.openairetype | artículo | - |
item.grantfulltext | open | - |
item.cerifentitytype | Publications | - |
item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
item.fulltext | With Fulltext | - |
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