Threshold wind speed and turbulence under LLJs events at Ipero - Brazil

dc.contributor.authorBEU, CASSIA M.L.pt_BR
dc.contributor.authorLANDULFO, EDUARDOpt_BR
dc.contributor.editorCOMERON, ADOLFOpt_BR
dc.contributor.editorKASSIANOV, EVGUENI I.pt_BR
dc.contributor.editorSCHAFER, KLAUSpt_BR
dc.contributor.editorPICARD, RICHARD H.pt_BR
dc.contributor.editorWEBER, KONRADINpt_BR
dc.contributor.editorSINGH, UPENDRA N.pt_BR
dc.coverageInternacionalpt_BR
dc.creator.eventoSPIE REMOTE SENSINGpt_BR
dc.date.accessioned2020-03-30T17:28:29Z
dc.date.available2020-03-30T17:28:29Z
dc.date.eventoSeptember 9-12, 2019pt_BR
dc.description.abstractThe threshold wind speed is a useful criterion in determining whether strong turbulence is generated within the Stable Boundary Layer (SBL), the layer where all surface emissions remain con ned during the night. Con dence turbulence estimates are extremely important for atmospheric transport and dispersion simulations, although due to its complex dinamics many aspects of the SBL are neglected by numerical models that, in turn, are the inputs and boundary conditions for the transport and dispersion simulations. Turbulence is especially important during severe episodies like hazardous material accidental releases, for example. Turbulence intensity can a ect the dispersion speed, released material concentration, and its reach. For many decades, remote sensing has been an important tool in lling the gap of information and providing advances in the atmospheric sciences. The doppler lidar is increasingly being used for micrometeoroly and Planetary Boundary Layer (PBL) studies because of its autonomy and long range capability, in contrast with traditional techniques as radioprobes and captive balloons. After 1 year of continuous measurements with a doppler lidar, it was possible to determine the threshold wind speed for Ipero, Sao Paulo, Brazil. Besides threshold wind speed, it was observed that the SBL turbulence has a straight relationship with the Low-Level Jets (LLJs) that frequently occur over the region. The vertical turbulence distribution depends greatly on the LLJ characteristics, which in turn is highly variable during its life cycle. The strong turbulence regime is associated to the stronger LLJs, that presents a more de ned pattern. In contrast, weak LLJs (that generate weaker SBL turbulence) present more dispersive characteristics in respect to the entire dataset. These di erences are seen both for the LLJ height as for the turbulence vertical pro le. These results will contribute for the atmospheric modeling and dispersion simulations, as well for the environmental studies at Ipero.pt_BR
dc.format.extent1115212-1 - 1115212-10pt_BR
dc.identifier.citationBEU, CASSIA M.L.; LANDULFO, EDUARDO. Threshold wind speed and turbulence under LLJs events at Ipero - Brazil. In: COMERON, ADOLFO (ed.); KASSIANOV, EVGUENI I. (ed.); SCHAFER, KLAUS (ed.); PICARD, RICHARD H. (ed.); WEBER, KONRADIN (ed.); SINGH, UPENDRA N. (ed.). In: SPIE REMOTE SENSING, September 9-12, 2019, Strasbourg, France. <b>Proceedings...</b> Bellingham, WA, USA: SPIE, 2019. p. 1115212-1 - 1115212-10. (Proceedings of SPIE Vol. 11152, Remote Sensing of Clouds and the Atmosphere XXIV). DOI: <a href="https://dx.doi.org/10.1117/12.2532281">10.1117/12.2532281</a>. Disponível em: http://repositorio.ipen.br/handle/123456789/30994.
dc.identifier.doi10.1117/12.2532281pt_BR
dc.identifier.orcid0000-0002-9691-5306pt_BR
dc.identifier.orcidhttps://orcid.org/0000-0002-9691-5306
dc.identifier.urihttp://repositorio.ipen.br/handle/123456789/30994
dc.localBellingham, WA, USApt_BR
dc.local.eventoStrasbourg, Francept_BR
dc.publisherSPIEpt_BR
dc.relation.ispartofseriesProceedings of SPIE Vol. 11152, Remote Sensing of Clouds and the Atmosphere XXIVpt_BR
dc.rightsclosedAccesspt_BR
dc.subjectwind
dc.subjectearth atmosphere
dc.subjectdispersions
dc.subjectjets
dc.subjectboundary layers
dc.titleThreshold wind speed and turbulence under LLJs events at Ipero - Brazilpt_BR
dc.typeTexto completo de eventopt_BR
dspace.entity.typePublication
ipen.autorEDUARDO LANDULFO
ipen.autorCASSIA MARIA LEME BREU
ipen.codigoautor503
ipen.codigoautor14140
ipen.contributor.ipenauthorEDUARDO LANDULFO
ipen.contributor.ipenauthorCASSIA MARIA LEME BREU
ipen.date.recebimento20-03
ipen.event.datapadronizada2019pt_BR
ipen.identifier.ipendoc26791pt_BR
ipen.notas.internasProceedingspt_BR
ipen.type.genreArtigo
relation.isAuthorOfPublicatione4dff370-e8c1-4437-846a-ef18a3ad606b
relation.isAuthorOfPublicationfb9e40b7-9758-4b4d-8605-17381305051f
relation.isAuthorOfPublication.latestForDiscoveryfb9e40b7-9758-4b4d-8605-17381305051f
sigepi.autor.atividadeLANDULFO, EDUARDO:503:920:Npt_BR
sigepi.autor.atividadeBEU, CASSIA M.L.:14140:920:Spt_BR

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