La atmósfera nocturna en un área urbana tropical de terreno complejo. Caso de estudio: el Valle de Aburrá (Colombia)

Ilustraciones, mapas

Autores:
Ramírez Cardona, Álvaro
Tipo de recurso:
Fecha de publicación:
2022
Institución:
Universidad Nacional de Colombia
Repositorio:
Universidad Nacional de Colombia
Idioma:
spa
OAI Identifier:
oai:repositorio.unal.edu.co:unal/82085
Acceso en línea:
https://repositorio.unal.edu.co/handle/unal/82085
https://repositorio.unal.edu.co/
Palabra clave:
550 - Ciencias de la tierra::551 - Geología, hidrología, meteorología
000 - Ciencias de la computación, información y obras generales::004 - Procesamiento de datos Ciencia de los computadores
Calidad del aire
Meteorología dinámica
Estado atmosférico - Efectos de la actividad solar
Meteorología urbana y de montañas
Patrones de circulación
Capa límite nocturna
Estabilidad atmosférica
Terreno complejo
Area urbana tropical
Número de Richardson aproximado
Urban and mountain meteorology
Urban and mountain meteorology
Circulation patterns
Nocturnal boundary layer
Atmospheric stability
Complex terrain
Tropical urban area
Bulk Richardson number
Rights
openAccess
License
Reconocimiento 4.0 Internacional
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oai_identifier_str oai:repositorio.unal.edu.co:unal/82085
network_acronym_str UNACIONAL2
network_name_str Universidad Nacional de Colombia
repository_id_str
dc.title.spa.fl_str_mv La atmósfera nocturna en un área urbana tropical de terreno complejo. Caso de estudio: el Valle de Aburrá (Colombia)
dc.title.translated.eng.fl_str_mv The nocturnal atmosphere in a tropical urban area of complex terrain. Case study: Aburrá Valley (Colombia)
title La atmósfera nocturna en un área urbana tropical de terreno complejo. Caso de estudio: el Valle de Aburrá (Colombia)
spellingShingle La atmósfera nocturna en un área urbana tropical de terreno complejo. Caso de estudio: el Valle de Aburrá (Colombia)
550 - Ciencias de la tierra::551 - Geología, hidrología, meteorología
000 - Ciencias de la computación, información y obras generales::004 - Procesamiento de datos Ciencia de los computadores
Calidad del aire
Meteorología dinámica
Estado atmosférico - Efectos de la actividad solar
Meteorología urbana y de montañas
Patrones de circulación
Capa límite nocturna
Estabilidad atmosférica
Terreno complejo
Area urbana tropical
Número de Richardson aproximado
Urban and mountain meteorology
Urban and mountain meteorology
Circulation patterns
Nocturnal boundary layer
Atmospheric stability
Complex terrain
Tropical urban area
Bulk Richardson number
title_short La atmósfera nocturna en un área urbana tropical de terreno complejo. Caso de estudio: el Valle de Aburrá (Colombia)
title_full La atmósfera nocturna en un área urbana tropical de terreno complejo. Caso de estudio: el Valle de Aburrá (Colombia)
title_fullStr La atmósfera nocturna en un área urbana tropical de terreno complejo. Caso de estudio: el Valle de Aburrá (Colombia)
title_full_unstemmed La atmósfera nocturna en un área urbana tropical de terreno complejo. Caso de estudio: el Valle de Aburrá (Colombia)
title_sort La atmósfera nocturna en un área urbana tropical de terreno complejo. Caso de estudio: el Valle de Aburrá (Colombia)
dc.creator.fl_str_mv Ramírez Cardona, Álvaro
dc.contributor.advisor.none.fl_str_mv Jiménez Mejía, José Fernando (Thesis advisor)
dc.contributor.author.none.fl_str_mv Ramírez Cardona, Álvaro
dc.subject.ddc.spa.fl_str_mv 550 - Ciencias de la tierra::551 - Geología, hidrología, meteorología
000 - Ciencias de la computación, información y obras generales::004 - Procesamiento de datos Ciencia de los computadores
topic 550 - Ciencias de la tierra::551 - Geología, hidrología, meteorología
000 - Ciencias de la computación, información y obras generales::004 - Procesamiento de datos Ciencia de los computadores
Calidad del aire
Meteorología dinámica
Estado atmosférico - Efectos de la actividad solar
Meteorología urbana y de montañas
Patrones de circulación
Capa límite nocturna
Estabilidad atmosférica
Terreno complejo
Area urbana tropical
Número de Richardson aproximado
Urban and mountain meteorology
Urban and mountain meteorology
Circulation patterns
Nocturnal boundary layer
Atmospheric stability
Complex terrain
Tropical urban area
Bulk Richardson number
dc.subject.lemb.none.fl_str_mv Calidad del aire
Meteorología dinámica
Estado atmosférico - Efectos de la actividad solar
dc.subject.proposal.spa.fl_str_mv Meteorología urbana y de montañas
Patrones de circulación
Capa límite nocturna
Estabilidad atmosférica
Terreno complejo
Area urbana tropical
Número de Richardson aproximado
dc.subject.proposal.eng.fl_str_mv Urban and mountain meteorology
Urban and mountain meteorology
Circulation patterns
Nocturnal boundary layer
Atmospheric stability
Complex terrain
Tropical urban area
Bulk Richardson number
description Ilustraciones, mapas
publishDate 2022
dc.date.accessioned.none.fl_str_mv 2022-08-24T21:50:28Z
dc.date.available.none.fl_str_mv 2022-08-24T21:50:28Z
dc.date.issued.none.fl_str_mv 2022-08-24
dc.type.spa.fl_str_mv Trabajo de grado - Maestría
dc.type.driver.spa.fl_str_mv info:eu-repo/semantics/masterThesis
dc.type.version.spa.fl_str_mv info:eu-repo/semantics/acceptedVersion
dc.type.content.spa.fl_str_mv Text
dc.type.redcol.spa.fl_str_mv http://purl.org/redcol/resource_type/TM
status_str acceptedVersion
dc.identifier.uri.none.fl_str_mv https://repositorio.unal.edu.co/handle/unal/82085
dc.identifier.instname.spa.fl_str_mv Universidad Nacional de Colombia
dc.identifier.reponame.spa.fl_str_mv Repositorio Institucional Universidad Nacional de Colombia
dc.identifier.repourl.spa.fl_str_mv https://repositorio.unal.edu.co/
url https://repositorio.unal.edu.co/handle/unal/82085
https://repositorio.unal.edu.co/
identifier_str_mv Universidad Nacional de Colombia
Repositorio Institucional Universidad Nacional de Colombia
dc.language.iso.spa.fl_str_mv spa
language spa
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spelling Reconocimiento 4.0 Internacionalhttp://creativecommons.org/licenses/by-nc/4.0/info:eu-repo/semantics/openAccesshttp://purl.org/coar/access_right/c_abf2Jiménez Mejía, José Fernando (Thesis advisor)bef708a01979fda20e25724833fbcba8600Ramírez Cardona, Álvaro82f7baf0dba28d0c5c06f357cce73c622022-08-24T21:50:28Z2022-08-24T21:50:28Z2022-08-24https://repositorio.unal.edu.co/handle/unal/82085Universidad Nacional de ColombiaRepositorio Institucional Universidad Nacional de Colombiahttps://repositorio.unal.edu.co/Ilustraciones, mapasEsta investigación caracterizó la estructura térmica y dinámica de la capa límite nocturna para el año 2017 en el Valle de Aburrá–Colombia, un área urbana tropical con topografía compleja. Se utilizaron registros provenientes de un radiómetro de microondas, un radar perfilador de vientos, un ceilómetro, estaciones meteorológicas y el modelo WRF-ARW acoplado al modelo de parametrización urbana SLUCM. Este último fue ejecutado con seis esquemas de parametrización distintos de la capa límite atmosférica, para 33 noches distribuidas en el periodo de estudio. Un análisis exploratorio fue ejecutado para identificar procesos espacio-temporales usando variables de estado como los vientos, el número de Richardson aproximado, la temperatura potencial virtual y la intensidad de retrodispersión. Mediante un análisis de sensibilidad de los registros se encontró que el espesor de la capa límite nocturna corresponde a un número de Richardson crítico de 0,5. Además se evaluó el modelo para las horas de la noche y se encontró un desempeño aceptable del esquema de parametrización MYNN. También se identificaron patrones de circulación asociados a un jet de bajo nivel, inversiones térmicas, vientos catabáticos y acoplamiento de los vientos alisios con los vientos orográficos. Se observó que los trimestres junio-julio-agosto y septiembre-octubre-noviembre son más estables dinámicamente, mientras que los trimestres de diciembre-enero-febrero y marzo-abril-mayo lo son más desde el punto de vista estático. Finalmente, se concluye que los espesores de la capa límite nocturna en el Valle de Aburrá son relativamente bajos, con condiciones de velocidades significantes al principio de la noche, pero al final de la noche con velocidades muy cercanas a cero y con una estabilidad atmosférica cada vez fortaleciéndose más por el enfriamiento radiativo. (texto tomado de la fuente)This research characterized the thermal structure and dynamics of the nocturnal boundary layer for the year 2017 in the Aburrá Valley-Colombia, a tropical urban area with complex topography. Records from a microwave radiometer, a wind profiler radar, a ceilometer, meteorological stations, and the WRF-ARW model coupled to the SLUCM urban parameterization model were used. This last one was run with six different atmospheric boundary layer parameterization schemes, for 33 nights distributed in the study period. An exploratory analysis was performed to detect spatio-temporal processes using state variables such as winds, bulk Richardson number, virtual potential temperature and backscatter. Through a sensitivity analysis of the records, it was found that the thickness of the nocturnal boundary layer corresponds to a critical Richardson number of 0,5. In addition, the model was evaluated during night hours and an acceptable performance of the MYNN parameterization scheme was found. Circulation patterns associated with a low-level jet, thermal inversions, katabatic winds and coupling of trade winds with orographic winds were also identified. It was observed that the quarters of june-july-august and september-october-november are more dynamically stable, and whereas those of the december-january-february and march-april-may are more statically stable. Finally, it is concluded that the thicknesses of the nocturnal boundary layer in the Aburrá Valley are relatively low, with significant velocities at the beginning of the night, but at the end of the night with velocities very close to zero and with atmospheric stability becoming increasingly stronger due to radiative cooling.MaestríaMagíster en Ingeniería - Recursos HidráulicosMeteorología urbana y de montañasÁrea Curricular de Medio Ambiente89 páginasapplication/pdfspaUniversidad Nacional de ColombiaMedellín - Minas - Maestría en Ingeniería - Recursos HidráulicosDepartamento de Geociencias y Medo AmbienteFacultad de MinasMedellínUniversidad Nacional de Colombia - Sede Medellín550 - Ciencias de la tierra::551 - Geología, hidrología, meteorología000 - Ciencias de la computación, información y obras generales::004 - Procesamiento de datos Ciencia de los computadoresCalidad del aireMeteorología dinámicaEstado atmosférico - Efectos de la actividad solarMeteorología urbana y de montañasPatrones de circulaciónCapa límite nocturnaEstabilidad atmosféricaTerreno complejoArea urbana tropicalNúmero de Richardson aproximadoUrban and mountain meteorologyUrban and mountain meteorologyCirculation patternsNocturnal boundary layerAtmospheric stabilityComplex terrainTropical urban areaBulk Richardson numberLa atmósfera nocturna en un área urbana tropical de terreno complejo. Caso de estudio: el Valle de Aburrá (Colombia)The nocturnal atmosphere in a tropical urban area of complex terrain. Case study: Aburrá Valley (Colombia)Trabajo de grado - Maestríainfo:eu-repo/semantics/masterThesisinfo:eu-repo/semantics/acceptedVersionTexthttp://purl.org/redcol/resource_type/TMAcevedo, O. C., Mahrt, L., Puhales, F. S., Costa, F. D., Medeiros, L. E., & Degrazia, G. A. (2016). Contrasting structures between the decoupled and coupled states of the stable boundary layer. Quarterly Journal of the Royal Meteorological Society, 142(695), 693–702. https://doi.org/10.1002/qj.2693Acevedo, O. C., Moraes, O. L. L., Degrazia, G. A., & Medeiros, L. E. (2006). Intermittency and the exchange of scalars in the nocturnal surface layer. Boundary-Layer Meteorology, 119(1), 41–55. https://doi.org/10.1007/s10546-005-9019-3Adler, B., Babia, K., Kalthoff, N., Lohou, F., Lothon, M., Dione, C., Pedruzo-Bagazgoitia, X., & Andersen, H. (2019). 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Journal of Geophysical Research: Atmospheres, 123(4), 2017–2036. https://doi.org/10.1002/2017JD027041EstudiantesInvestigadoresMaestrosMedios de comunicaciónPúblico generalResponsables políticosLICENSElicense.txtlicense.txttext/plain; charset=utf-81748https://repositorio.unal.edu.co/bitstream/unal/82085/1/license.txt8a4605be74aa9ea9d79846c1fba20a33MD51ORIGINAL1152442900.2022.pdf1152442900.2022.pdfTesis de Maestría en Medio Ambiente y Desarrolloapplication/pdf9776393https://repositorio.unal.edu.co/bitstream/unal/82085/2/1152442900.2022.pdf1c83118486b8522a7bb75719c43042a2MD52THUMBNAIL1152442900.2022.pdf.jpg1152442900.2022.pdf.jpgGenerated Thumbnailimage/jpeg3662https://repositorio.unal.edu.co/bitstream/unal/82085/3/1152442900.2022.pdf.jpgd133230c2fcde2a6fdeaf96da8090768MD53unal/82085oai:repositorio.unal.edu.co:unal/820852023-08-07 23:03:57.403Repositorio Institucional Universidad Nacional de Colombiarepositorio_nal@unal.edu.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