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Spatio-temporal variability of the Atmospheric Boundary Layer in the Aburrá Valley: characterization, processes, multiscale interactions and impacts

dc.rights.licenseAtribución-NoComercial-SinDerivadas 4.0 Internacional
dc.contributor.advisorHoyos Ortiz, Carlos David
dc.contributor.advisorRotach, Mathias
dc.contributor.authorHerrera Mejía, Laura
dc.date.accessioned2022-03-15T15:46:09Z
dc.date.available2022-03-15T15:46:09Z
dc.date.issued2021-08-23
dc.identifier.urihttps://repositorio.unal.edu.co/handle/unal/81221
dc.descriptionilustraciones, diagramas, mapas, tablas
dc.description.abstractBoundary-Layer Meteorology refers to the theoretical, numerical, and experimental framework that focuses on studying the interactions between the earth's surface and the lower troposphere. These interactions are crucial for several applications in various temporal and spatial scales. A better understanding of these interactions implies studying the structure and variability of the Atmospheric Boundary-Layer as a result of processes that are better described in the realm of a combination of fluid dynamics and thermodynamics. By definition, the ABL is turbulent, which means that the processes of mixing and exchange of energy, momentum, and scalars from the Surface Layer to the rest of the atmosphere depend on turbulence, both thermal and mechanic. In this sense, the small-scale physical processes depicted by the different terms in Turbulent Kinetic Energy budget equation modulate the characteristics of large-scale phenomena. One of the main challenges in studying the ABL dynamics is the high heterogeneity of the underlying forcing imposed by the earth's surface. Ranging from abrupt changes in orography to a wide variety of land uses and roughness elements, complex terrain is the rule rather than the exception, especially when dealing with processes involving anthropogenic modified environments. Nevertheless, most of our understanding of turbulence in the ABL is based on an idealized picture of real-life scenarios, e.g., horizontally homogeneous and flat terrains, implying that most of the exchange is vertical, and horizontal contributions are small and negligible. The main goal of this work is to identify and gain insight into the main processes between the synoptic- and micro-scale ends of the spectrum of atmospheric motions (including their cross-scale interactions) that modulate the ABL structure and dynamics over a complex and highly urbanized low-latitude valley. The Aburrá Valley is located in the Colombian Andes. The work follows an experimental approach, using multiple data sources, in order to evaluate the potential contribution of these phenomena on the boundary-layer variability in the study area. The intention is to shed some light on open questions regarding boundary-layer characteristics and some of their environmental implications over such complex terrain. The structure of this document was decided considering that, once in final form, Chapters 3, 4 and 5 will be submitted to be considered for publication in peer reviewed journals (Chapter 2 is already published). For this reason, this thesis includes four main self-contained chapters (Chapters 2 to 5) with the results of the evaluation of the boundary-layer dynamics in a highly complex terrain at different spatio-temporal scales and some of the interactions between them.
dc.description.abstractLa Meteorología de la Capa Límite hace referencia al marco teórico, numérico y experimental que se enfoca en estudiar las interacciones entre la superficie terrestre y la tropósfera baja. Estas interacciones son fundamentales para muchas aplicaciones en varias escalas espacio-temporales. Un mejor entendimiento de dichas interacciones implica el estudio de la estructura y variabilidad de la Capa Límite Atmosférica como resultado de procesos que son mejor descritos en el ámbito de una combinación de dinámica de fluidos y termodinámica. Por definición, la Capa Límite es turbulenta, lo cual significa que los procesos de mezcla e intercambio de energía, momentum y escalares, desde la Capa Superficial al resto de la atmósfera, dependen de la turbulencia, tanto térmica como mecánica.En este sentido, los procesos físicos de pequeña escala descritos por los términos en la ecuación de balance de la energía cinética turbulenta modulen las características de los fenómenos a mayor escala. Uno de los más grandes desafíos a la hora de estudiar las dinámicas de la Capa Límite es la alta heterogeneidad de la superficie terrestre, que van desde cambios abruptos en la orografía, hasta una amplia variedad de usos del suelo y elementos rugosos. Así, los terrenos complejos más que la excepción son la regla, especialmente cuando se trabajan con procesos que involucran modificaciones antrópicas al ambiente. Sin embargo, la gran mayoría de nuestro conocimiento en turbulencia en la Capa límite es basado en una imagen idealizada de los escenarios de la vida real, es decir, terrenos planos y horizontalmente homogéneos, lo cual implica que la mayoría de los intercambios aon verticales, y las contribuciones horizontales son pequeñas y pueden ser despreciadas. El principal objetivo de esta investigación es identificar y comprender los principales procesos de las diferentes escalas atmosféricas de movimiento (incluidas las interacciones entre escalas) los cuales modulan la estructura y dinámica de la Capa Límite en el Valle de Aburrá, ell cual es un valle altamente urbanizado ubicado en los Andes Colombianos. El trabajo sigue un enfoque experimental, usando múltiples fuentes de datos, con el objetivo de evaluar la potencial contribución de estos fenómenos en la variabilidad de la Capa límite en la zona de estudio. La intención es dar algo de luz sobre preguntas que siguen abiertas relacionadas con las características de la capa límite y algunas de sus implicaciones ambientales en un terreno tan complejo. (Texto tomado de la fuente)
dc.format.extentviii, 171 páginas
dc.format.mimetypeapplication/pdf
dc.language.isoeng
dc.publisherUniversidad Nacional de Colombia - Sede Medellín
dc.publisherUniversidad Nacional de Colombia
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/
dc.subject.ddc550 - Ciencias de la tierra::551 - Geología, hidrología, meteorología
dc.titleSpatio-temporal variability of the Atmospheric Boundary Layer in the Aburrá Valley: characterization, processes, multiscale interactions and impacts
dc.typeTrabajo de grado - Doctorado
dc.type.driverinfo:eu-repo/semantics/doctoralThesis
dc.type.versioninfo:eu-repo/semantics/acceptedVersion
dc.publisher.programMedellín - Minas - Doctorado en Ingeniería - Recursos Hidráulicos
dc.coverage.countryValle del Aburrá, Medellín (Colombia)
dc.description.degreelevelDoctorado
dc.description.degreenameDoctor en Ingeniería
dc.description.researchareaMeteorología de capa límite
dc.identifier.instnameUniversidad Nacional de Colombia
dc.identifier.reponameRepositorio Institucional Universidad Nacional de Colombia
dc.identifier.repourlhttps://repositorio.unal.edu.co/
dc.publisher.departmentDepartamento de Geociencias y Medo Ambiente
dc.publisher.facultyFacultad de Minas
dc.publisher.placeMedellín, Colombia
dc.publisher.branchUniversidad Nacional de Colombia - Sede Medellín
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dc.rights.accessrightsinfo:eu-repo/semantics/openAccess
dc.subject.lembPlanetary boundary layer
dc.subject.lembCapa límite planetaria
dc.subject.lembBoundary layer (Meteorology)
dc.subject.lembCapa límite (Meteorología)
dc.subject.proposalBoundary-Layer
dc.subject.proposalAtmospheric Turbulence
dc.subject.proposalComplex terrain
dc.subject.proposalAir-quality
dc.subject.proposalMicrometeorology
dc.subject.proposalAtmospheric Boundary Layer
dc.subject.proposalEddy covariance
dc.subject.proposalRemote sensing
dc.subject.proposalMeteorology
dc.subject.proposalAtmospheric stability
dc.subject.proposalCapa Límite Atmosférica
dc.subject.proposalCalidad del aire
dc.subject.proposalTerrenos complejos
dc.subject.proposalTurbulencia atmosférica
dc.subject.proposalSensores remotos
dc.subject.proposalMeteorología
dc.subject.proposalEstabilidad atmosférica
dc.title.translatedVariabilidad espacio-temporal de la Capa Límite atmosférica en el Valle de Aburrá: caracterización, procesos, interacciones multi-escala e impactos
dc.type.coarhttp://purl.org/coar/resource_type/c_db06
dc.type.coarversionhttp://purl.org/coar/version/c_ab4af688f83e57aa
dc.type.contentText
dc.type.redcolhttp://purl.org/redcol/resource_type/TD
oaire.accessrightshttp://purl.org/coar/access_right/c_abf2
oaire.awardtitleSistema de Alerta Temprana de Medellín y el Valle de Aburrá - SIATA
oaire.fundernameOeAD Austria - Mach grant
oaire.fundernameÁrea metropolitana del Valle de Aburrá
dcterms.audience.professionaldevelopmentEstudiantes
dcterms.audience.professionaldevelopmentInvestigadores
dcterms.audience.professionaldevelopmentMaestros
dcterms.audience.professionaldevelopmentPúblico general
dc.description.curricularareaÁrea Curricular de Medio Ambiente


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