975 resultados para Sullivan, Timothy Daniel, 1862-1913.
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El desarrollo de la presente tesis busca la comprensión del aporte que brindan los conceptos: inteligencia emocional y liderazgo transformador en la formación y desarrollo de equipos efectivos de trabajo. Ambos elementos son relevantes para lograr una buena gestión de trabajo individual y de equipo, que favorezca la eficiencia organizacional y las relaciones interpersonales. Desde la perspectiva laboral, tanto el liderazgo transformador como la inteligencia emocional generan en las personas sentido de pertenencia a la organización, promueven su desarrollo profesional y personal, mejoran su satisfacción y actitud logrando un adecuado trabajo de equipo. La inteligencia emocional es la capacidad de entender los sentimientos propios y de los demás para generar respuestas adecuadas. El liderazgo transformador es el conjunto de habilidades y destrezas de un individuo para gestionar, estimular o motivar a un equipo favoreciendo el cumplimiento de objetivos comunes. Finalmente, a través de la correlación entre las variables inteligencia emocional y liderazgo transformador, se buscará entender el nivel de efectividad de los equipos de alto rendimiento en la fuerza comercial de microfinanzas CREDI FE Zona Quito.
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En esta investigación, la autora propone un análisis de la performance latinoamericana desde la concepción del cuerpo como político, lo que implica analizar el cuerpo dentro de su existencia histórica antes que biológica, cobrando gran importancia el contexto y las experiencias vividas como detonantes de estas prácticas artísticas, que muchas veces conllevan acciones de dolor físico, las cuales, dentro de la concepción política del cuerpo, se convierten en actos de memoria. Estos planteamientos de los usos sociales y políticos del cuerpo son analizados en las performances de Daniel Brittany Chávez, Regina José Galindo, María José Machado y Daniel Coka.
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Dendrodrilus rubidus were sampled from a mine spoil soil at Coniston Copper Mine, an abandoned Cu mine in Cumbria, UK and a Cu-free control site. Earthworms were maintained for 14 d in both Kettering loam and a Moorland soil amended with Cu nitrate. Mortality, condition index, weight change and tissue concentration were determined. In both soils D. rubidus native to the mine site were able to tolerate significantly higher soil Cu concentrations (MWRT, p <= 0.001), and exhibited significantly less change in weight (t-test, p <= 0.001) and a lower loss in condition (t-test, p <= 0.001) than control earthworms. For a given soil Cu concentration tissue Cu concentrations were greater in the mine site earthworms. Low cocoon production and viability from the mine site population prevented the determination of toxicity parameters on the F1 generation and may be an indicator of the cost of tolerance to the population. (c) 2007 Elsevier Ltd. All rights reserved.
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During the twentieth century sea surface temperatures in the Atlantic Ocean exhibited prominent multidecadal variations. The source of such variations has yet to be rigorously established—but the question of their impact on climate can be investigated. Here we report on a set of multimodel experiments to examine the impact of patterns of warming in the North Atlantic, and cooling in the South Atlantic, derived from observations, that is characteristic of the positive phase of the Atlantic Multidecadal Oscillation (AMO). The experiments were carried out with six atmospheric General Circulation Models (including two versions of one model), and a major goal was to assess the extent to which key climate impacts are consistent between the different models. The major climate impacts are found over North and South America, with the strongest impacts over land found over the United States and northern parts of South America. These responses appear to be driven by a combination of an off-equatorial Gill response to diabatic heating over the Caribbean due to increased rainfall within the region and a Northward shift in the Inter Tropical Convergence Zone (ITCZ) due to the anomalous cross-equatorial SST gradient. The majority of the models show warmer US land temperatures and reduced Mean Sea Level Pressure during summer (JJA) in response to a warmer North Atlantic and a cooler South Atlantic, in line with observations. However the majority of models show no significant impact on US rainfall during summer. Over northern South America, all models show reduced rainfall in southern hemisphere winter (JJA), whilst in Summer (DJF) there is a generally an increase in rainfall. However, there is a large spread amongst the models in the magnitude of the rainfall anomalies over land. Away from the Americas, there are no consistent significant modelled responses. In particular there are no significant changes in the North Atlantic Oscillation (NAO) over the North Atlantic and Europe in Winter (DJF). Additionally, the observed Sahel drying signal in African rainfall is not seen in the modelled responses. Suggesting that, in contrast to some studies, the Atlantic Multidecadal Oscillation was not the primary driver of recent reductions in Sahel rainfall.