Land atmosphere interactions in Tropical South America and Colombia at multiple timescales

dc.contributorPoveda Jaramillo, Germán
dc.contributorTrenberth, Kevin
dc.contributorVélez, Jorge Julián
dc.contributorSauchyn, David
dc.contributorAristizabal, Edier
dc.contributorCarmona, Alejandra
dc.contributorUniversidad Nacional de Colombia - Sede Medellín
dc.creatorBedoya Soto, Juan Mauricio
dc.date.accessioned2021-01-14T22:30:12Z
dc.date.accessioned2022-09-21T19:06:01Z
dc.date.available2021-01-14T22:30:12Z
dc.date.available2022-09-21T19:06:01Z
dc.date.created2021-01-14T22:30:12Z
dc.date.issued2020-09-15
dc.identifierBedoya-Soto, J.M. (2020). Land Atmosphere Interactions in Tropical South America and Colombia at Multiple Timescales. PhD Thesis. Universidad Nacional de Colombia.
dc.identifierhttps://repositorio.unal.edu.co/handle/unal/78749
dc.identifierUniversidad Nacional de Colombia
dc.identifierRepositorio Institucional Universidad Nacional de Colombia
dc.identifierhttp://repositorio.una.,edu.co
dc.identifier.urihttp://repositorioslatinoamericanos.uchile.cl/handle/2250/3413266
dc.description.abstractIn this thesis, we have studied diverse land-atmosphere interactions (LAI) in Tropical South America (TropSA) and Colombia at several timescales. First, we evaluated the specific role of LAI during the 2009-2011 extreme ENSO phases at continental scale. In particular, we developed a simplified model of LAI on TropSA using graph theory based on linear and non-linear metrics at interannual timescales. Over a specific region of the Central Andes of Colombia (CAC), we explored the seasonal variability of the diurnal cycle of rainfall. A moisture recycling model was implemented to provide evidence supporting the key role of LAI in this variability. The results of the thesis indicate that the strength of land-atmosphere processes in TropSA is influenced by ENSO and depends on the availability of water and energy in soil layers. Soil moisture plays a relevant role at the interannual scale in the coupling between temperature and rainfall through ENSO in this region. The structural model of links developed under the influence of ENSO establishes that surface temperature is a key variable in diagnosing the dynamics of the LAI in TropSA. On shorter space scales, moisture recycling contributes to the understanding of the seasonal dynamics of moisture sources explaining the shifting phase of the diurnal cycle of rainfall through the year over the CAC. The thesis highlights the active role of LAI in the hydroclimatic dynamics of the explored spatiotemporal contexts and the importance to continue improving our understanding of these mechanisms. (Tomado de la fuente)
dc.description.abstractEn esta tesis se han estudiado las interacciones tierra-atmósfera (ITA) sobre Suramérica Tropical (SATrop) y Colombia en múltiples escalas temporales. Evaluamos el papel específico de las ITA durante las fases extremas del ENSO 2009-2011 a escala continental en SATrop y Colombia. Asimismo, desarrollamos un modelo simplificado de las ITA sobre SATrop usando teoría de grafos basado en métricas lineales y no lineales a escala de tiempo interanual. A escala local, exploramos la variabilidad estacional del ciclo diurno de la lluvia en una región específica de los Andes Centrales de Colombia (ACC), e implementamos un modelo de reciclaje de humedad para encontrar evidencias que soporten nuestra hipótesis del papel de las ITA en este contexto. Los resultados de la tesis indican que la potencia de los procesos tierra-atmósfera sobre SATrop está influenciada por ENSO y depende de la disponibilidad de agua y energía en las capas del suelo. La humedad en el suelo tiene un papel relevante a nivel interanual en el acoplamiento entre temperatura y lluvia a través de ENSO en esta región. El modelo estructural de enlaces que se construyó bajo la influencia de ENSO establece que la temperatura superficial es una variable clave para diagnosticar la dinámica de las ITA en SATrop. En la región de estudio sobre los ACC, encontramos que el ciclo diurno es predominantemente unimodal durante todo el año, pero su fase cambia con la fase del ciclo anual. El reciclaje de humedad, como una expresión de las ITA, aporta a la comprensión de la dinámica estacional de este ciclo diurno promedio de lluvia en los ACC. En síntesis, la tesis determinó el papel activo de las ITA en la dinámica hidroclimática de los contextos espacio-temporales explorados y la necesidad de seguir mejorando nuestro entendimiento de estos mecanismos. (Tomado de la fuente)
dc.languageeng
dc.publisherUniversidad Nacional de Colombia
dc.publisherMedellín - Minas - Doctorado en Ingeniería - Recursos Hidráulicos
dc.publisherDepartamento de Geociencias y Medo Ambiente
dc.publisherFacultad de Minas
dc.publisherUniversidad Nacional de Colombia - Sede Medellín
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dc.titleLand atmosphere interactions in Tropical South America and Colombia at multiple timescales
dc.typeTesis


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