Poéticas del silencio: el Color de lo blanco, de Alvaro Rodríguez y Sacra, de Alexis Naranjo

La presente disertación constituye un breve acercamiento a las poéticas del silencio, constitutivas de El color de lo blanco del poeta colombiano Álvaro Rodríguez Torres y de Sacra del poeta ecuatoriano Alexis Naranjo. Para la aproximación teórica a los textos poéticos, he aplicado ciertas categorías fundamentales de la hermenéutica de Paul Ricoeur. El aporte del pensador francés es interpretar los poemas como un escenario de convergencia entre los niveles semántico, morfosintáctico y fonológico. Así, tras un capítulo introductoria, donde marco la orientación teórica y metodológica de la tesis, he procedido a revisar cada texto de los libros. Dicho estudio lo realicé bajo la premisa de encontrar los distintos elementos compositivos que caracterizan –o caracterizarían- a una determinada poética del silencio. Como parte de las conclusiones preliminares y finales, he propuesto una clasificación de las poéticas del silencio: el despojamiento y la contención. Debo apuntar, además, que las imágenes míticas presentes en cada uno de los textos han sido estudiadas con el propósito de evitar cualquier tipo de digresiones.

El color de la razón y del pensamiento crítico en las Américas

El color de la razón y del pensamiento crítico en las Américas, ha requerido de búsquedas encaminadas a explicar el porqué del color y sus matices. La modernidad europea y latinoamericana, constituyen el escenario en donde hemos visualizado la actuación de imágenes conceptuales que enfatizan el “color” de cada actor y acción. Para el efecto, analizamos “ciertos” aspectos de las propuestas de algunos pensadores, en tres momentos: En el primero a Leopoldo Zea, quien enfatiza la articulación entre la dialéctica del colonialismo y la dependencia, mediada por la dialéctica hegeliana y marxista; y, a Bolívar Echeverría, en lo referente a la relación que se da en América Latina entre modernidad, capitalismo y mestizaje (barroco) o apartheid. En el segundo, la intersección mediada clase/raza manifiesta en las tesis de Aimé Césaire y Frantz Fanon. En el tercero, la “crítica negativa” del paradigma modernidad/colonialidad, elaborada por Aníbal Quijano, Enrique Dussel, Walter Mignolo y Nelson Maldonado, entre otros. La elaboración teórica y la re-construcción de los momentos históricos, simultáneamente concebidos, nos han permitido descifrar el “color” de la razón, como momento necesario para establecer las condiciones que posibilitan un diálogo filosófico intercultural.

Dos textualidades diferentes que rememoran la escena esclavista: color, cuerpo y raza en la novela Jonatás y Manuela de la escritora Argentina Chiriboga y en el video Ecuatoriano Freddy Quiñones, detenido por cruzar con luz roja en Chile

El presente trabajo pretende contribuir en la ampliación de un corpus de estudio sobre la imagen del afrodescendiente. Se trata del análisis de la novela Jonatás y Manuela, de la afroecuatoriana Luz Argentina Chiriboga y del video Ecuatoriano Freddy Quiñones, detenido por cruzar con luz roja en Chile. En ambas narrativas se muestra la subyugación a la que son sometidos los cuerpos de los afrodescendientes. Con este propósito se procura rastrear cómo la percepción del color, asociada a las marcas étnicas y racistas heredadas de los discursos coloniales del siglo XVI al XVIII y los nacionalistas del XIX, se resemantiza en el siglo XX exponiendo las tensiones entre etnia/territorio/cultura a través de sujetos sociales que tradicionalmente han carecido de espacios de visibilidad para su propia representación, como agentes históricos y de acción política. Con esta intención, vale entonces emprender nuestro recorrido junto a las reflexiones de Hering, Cunin, Ariza, Chaves, Ramos, Montelongo, Miranda y Handelsman, quienes exploran las continuidades y discontinuidades que los diferentes discursos canónicos han sustentado alrededor de la percepción del color de piel en relación a la “raza” y a la identidad latinoamericana. Además, de manera simultánea, se analizarán los escenarios de subyugación desde la enunciación, los conceptos de utopía y heterotopía –de Michael Focuault-. De este modo, por razones de organización del corpus de estudio, tanto la novela como el video serán estudiados en cada uno de tres capítulos que componen el presente trabajo desde la configuración del color y del cuerpo en distintos escenarios: primero, el de subyugación que produce perspectivas indicadas.

Predation in Ground-Nesting Birds: an Experimental Study Using Natural Egg-Color Variation

We tested the hypothesis that cryptically colored eggs would suffer less predation than conspicuous eggs in the ground-nesting red-legged partridge, Alectoris rufa. We used A. rufa as a model species because it has a wide range of natural egg colors, the eggs are widely available from breeding farms, and nests are easily mimicked because they are scrapes containing no vegetation. The study was conducted in the spring of 2001 in forest and fallow fields of central Spain in Castilla La Mancha, Ciudad Real. We used 384 clutches of natural eggs that were white, white spotted, brown, or brown spotted. Within clutches, eggs were consistent in color and size; among clutches, color differences were distributed across habitats. Clutches were checked once after 2 wk of exposure. Cryptic coloration had a survival advantage that was dependent on the local suite of predators. Rodent predation was nonselective with respect to clutch color; however, avian predation was significantly higher for conspicuous clutches. In addition, there was an interaction of landscape and egg color for avian predation. In forest landscapes, the clutches with highest survival were brown spotted, whereas in fallow landscapes, brown and brown spotted clutches had higher survival than white and white potted clutches. Thus, both the predator suite and the landscape had significant effects on the value of cryptic egg coloration. Our study is relevant for conservationists and managers in charge of restocking programs in hunting areas. The release of other partridge species or their hybrids could result in hybridization with wild partridges, potentially leading to nonoptimal clutch pigmentation and reduced survival of the native species. We therefore recommend that local authorities, managers, and conservationists be cautious with the use of alien species and hybrids and release only autochthonous species of partridges within their natural ranges.

The response of tropospheric circulation to perturbations in lower-stratospheric temperature

A multiple regression analysis of the NCEP-NCAR reanalysis dataset shows a response to increased solar activity of a weakening and poleward shift of the subtropical jets. This signal is separable from other influences, such as those of El Nino-Southern Oscillation (ENSO) and the North Atlantic Oscillation (NAO), and is very similar to that seen in previous studies using global circulation models (GCMs) of the effects of an increase in solar spectral irradiance. The response to increased stratospheric (volcanic) aerosol is found in the data to be a weakening and equatorward shift of the jets. The GCM studies of the solar influence also showed an impact on tropospheric mean meridional circulation with a weakening and expansion of the tropical Hadley cells and a poleward shift of the Ferrel cells. To understand the mechanisms whereby the changes in solar irradiance affect tropospheric winds and circulation, experiments have been carried out with a simplified global circulation model. The results show that generic heating of the lower stratosphere tends to weaken the subtropical jets and the tropospheric mean meridional circulations. The positions of the jets, and the extent of the Hadley cells, respond to the distribution of the stratospheric heating, with low-latitude heating forcing them to move poleward, and high-latitude or latitudinally uniform heating forcing them equatorward. The patterns of response are similar to those that are found to be a result of the solar or volcanic influences, respectively, in the data analysis. This demonstrates that perturbations to the heat balance of the lower stratosphere, such as those brought about by solar or volcanic activity, can produce changes in the mean tropospheric circulation, even without any direct forcing below the tropopause.

The response of a uniform horizontal temperature gradient to heating

The response of a uniform horizontal temperature gradient to prescribed fixed heating is calculated in the context of an extended version of surface quasigeostrophic dynamics. It is found that for zero mean surface flow and weak cross-gradient structure the prescribed heating induces a mean temperature anomaly proportional to the spatial Hilbert transform of the heating. The interior potential vorticity generated by the heating enhances this surface response. The time-varying part is independent of the heating and satisfies the usual linearized surface quasigeostrophic dynamics. It is shown that the surface temperature tendency is a spatial Hilbert transform of the temperature anomaly itself. It then follows that the temperature anomaly is periodically modulated with a frequency proportional to the vertical wind shear. A strong local bound on wave energy is also found. Reanalysis diagnostics are presented that indicate consistency with key findings from this theory.

Precipitating convection in cold air: virtual potential temperature structure

Simulations of precipitating convection are used to illustrate the importance of the turbulent kinetic energy (TKE) budget in determining the virtual potential-temperature structure of the convecting atmosphere. Two sets of simulations are presented: in one the surface temperature was increased to simulate cold air flowing over a warmer surface and in the second a cooling profile, representing cold-air advection, was imposed. It is shown that the terms in the TKE budgets for both sets of simulations scale in the same way, but that the non-dimensional profiles are different. It is suggested that this is associated with the effects of sublimation of ice. It is shown that the magnitudes of the transport and precipitation terms in the virtual potential temperature budget are determined by the scaling of the TKE budget. Some implications of these results for parametrizations of moist convection are discussed. Copyright © 2007 Royal Meteorological Society

Composition and cure temperature: The influence on properties of final flexible PU cold cure foam parts

Foams are cellular structures, produced by gas bubbles formed during the polyurethane polymerization mixture. Flexible PU foams meet the following two criteria: have a limited resistance to an applied load, being both permeable to air and reversibly deformable. There are two main types of flexible foams, hot and cold cure foams differing in composition and processing temperatures. The hot cure foams are widely applied and represent the main composition of actual foams, while cold cure foams present several processing and property advantages, e.g, faster demoulding time, better humid aging properties and more versatility, as hardness variation with index changes are greater than with hot cure foams. The processing of cold cure foams also is attractive due to the low energy consumption (mould temperature from 30 degrees to 65 degrees C) comparatively to hot cure foams (mould temperature from 30 degrees to 250 degrees C). Another advantage is the high variety of soft materials for low temperature processing moulds. Cold cure foams are diphenylmethane diisocyanate (MDI) based while hot cure foams are toluene diisocyanate (TDI) based. This study is concerned with Viscoelastic flexible foams MDI based for medical applications. Differential Scanning Calorimetry (DSC) was used to characterize the cure kinetics and Dynamical Mechanical Analisys to collect mechanical data. The data obtained from these two experimental procedures were analyzed and associated to establish processing/properties/operation conditions relationships. These maps for the selection of optimized processing/properties/operation conditions are important to achieve better final part properties at lower costs and lead times.

Temperature and moist-stability effects on midlatitude orographic precipitation

Idealized, convection-resolving simulations of moist orographic flows are conducted to investigate the influence of temperature and moist stability on the drying ratio (DR), defined as the fraction of the impinging water mass removed as orographic precipitation. In flow past a long ridge, where most of the air rises over the barrier rather than detouring around it, DR decreases as the surface temperature (Ts) increases, even as the orographic cap cloud becomes statically unstable at higher Ts and develops embedded convection. This behaviour is explained by a few physical principles: (1) the Clausius–Clapeyron equation dictates that the normalized condensation rate decreases as the flow gets warmer, (2) the replacement of ice-phase precipitation growth with warm-rain processes decreases the efficiency by which condensate is converted to precipitation, thereby lowering precipitation efficiency, and (3) embedded convection acts more to vertically redistribute moisture than to enhance precipitation. Over an isolated mountain, the effects of (1) and (2) are counteracted by moisture deflection around the barrier, which is stronger in the colder, more stable flows.

Temperature trends derived from Stratospheric Sounding Unit radiances: the effect of increasing CO2 on the weighting function

Stratospheric Sounding Units (SSU) on the NOAA operational satellites have been the main source of near global temperature trend data above the lower stratosphere. They have been used extensively for comparison with model-derived trends. The SSU senses in the 15 micron band of CO2 and hence the weighting function is sensitive to changes in CO2 concentrations. The impact of this change in weighting function has been ignored in all recent trend analyses. We show that the apparent trends in global mean brightness temperature due to the change in weighting function vary from about -0.4 K/decade to 0.4 K/decade depending on the altitude sensed by the different SSU channels. For some channels, this apparent trend is of a similar size to the trend deduced from SSU data but ignoring the change in weighting function. In the mid-stratosphere, the revised trends are now significantly more negative and in better agreement with model-calculated trends.