El benestar psicològic en l'adolescència: la perspectiva de les ciències de la complexitat

El benestar psicològic, entès com la vessant psicològica que forma part del concepte més ampli de qualitat de vida, constitueix un àmbit d'estudi en expansió. Tot i tenir un passat més breu en comparació amb d'altres constructes psicosocials, cada vegada investigadors de les més diverses disciplines s'afegeixen a la llista d'estudiosos que fan del benestar psicològic un dels seus objectes d'investigació. Amb tot, l'estudi del benestar psicològic en l'adolescència constitueix probablement un dels àmbits en els quals la necessitat de seguir avançant es fa més evident. El seu estudi en subjectes adolescents té, a més, un doble interès. Per una part, els canvis i transicions que nois i noies experimenten durant l'adolescència comporten amb freqüència que sigui un període estressant per a molts d'ells/es, amb implicacions importants per al seu benestar psicològic. Aprofundir en el seu coneixement durant aquest període té un interès més enllà de l'estrictament científic i permet el disseny de programes de prevenció més ajustats a les problemàtiques que els/les adolescents puguin estar experimentant. L'exploració dels elements del benestar psicològic constitueix una de les estratègies d'aproximació al seu estudi. En aquesta tesi doctoral s'han seleccionat alguns dels elements que de la literatura científica es desprèn que tenen una connexió més estreta amb el benestar psicològic i que són la satisfacció amb la vida globalment i amb àmbits específics de la vida, l'autoestima, el suport social percebut, la percepció de control i els valors. Tot i que existeix un consens elevat en considerar que l'exploració d'aquests elements és de primera necessitat de cares a aprofundir en l'estructura del benestar psicològic, generalment han estat estudiats de forma separada, malgrat no falten intents d'integració teòrica. Les limitacions més importants que presenta l'estudi del benestar psicològic i el dels seus elements en l'actualitat són bàsicament de caràcter epistemològic i fan referència a la dificultat de trobar visions comunes (tant a nivell de definicions com de teories explicatives) compartides per una majoria d'investigadors socials. Aquestes limitacions justifiquen l'interès per dirigir l'atenció vers un altre tipus d'explicacions del benestar psicològic, qualitativament diferents a les disponibles, que no es refugiïn ni en reduccionismes ni en explicacions causals rígides. Les teories de la complexitat suposen una alternativa productiva en aquest sentit ja que aquelles característiques a través de les quals la complexitat ve donada (borrositat de límits, punts de catàstrofe, dimensions fractals, processos caòtics i no lineals), són, en definitiva, les mateixes propietats que caracteritzen als fenòmens psicosocials. I això inclou el de benestar psicològic. Les dades de les que disposem, obtingudes mitjançant un estudi transversal, impedeixen fer una aproximació al benestar psicològic des de totes les propietats de la complexitat esmentades a excepció de la característica de la no linealitat. L'objectiu general de la tesi ha estat el de construir un model de benestar psicològic a partir de les dades obtingudes que permetés: 1) Evidenciar relacions entre variables que fins aquests moments no han pogut ser massa explorades, 2) Contemplar aquestes relacions més enllà de la seva unidireccionalitat, i 3) Entendre el benestar psicològic en l'adolescència des d'un punt de vista més integrador i holista i, consegüentment, oferir una manera més comprehensiva d'aproximar-se a aquest fenomen. Aquesta tesi ha de ser entesa com un primer pas, fonamentalment metodològic, per l'elaboració futura de conceptualizacions sobre el benestar psicològic en l'adolescència que es basin en els principis que ens aporten les ciències de la complexitat. Malgrat els resultats obtinguts no estan absents de limitacions, obren noves perspectives d'anàlisi del benestar psicològic en l'adolescència.

Lo extraficcional en La casa de los locos y La Señorita Ecuador, las primeras novelas de Alfredo Pareja Diezcanseco (Del Fabulador)

El autor analiza, en las dos primeras novelas escritas por Pareja Diezcanseco, elementos externos de la estructura del mundo novelado, proporcionados por la voz extraficcional (prefacios, epílogos, notas de pie de página). La casa de los locos es la sátira de una sociedad en anarquía, que presenta la actuación caótica de las clases sociales dirigentes y prefigura a los sodalios deformes de Las pequeñas estaturas, en ella es de gran importancia el «liminar», en el que la voz extraficcional presenta su poética de la escritura: ésta puede ser un arma de combate cultural e ideológico. En La Señorita Ecuador, uno de los elementos extraficcionales, el epílogo, aclara y justifica la designación del texto como novela. Estos elementos constituyen, en ambos textos, indispensable contrapunto para entender el sentido y la crítica social implícitos en las ficciones textuales.

“Mi delirio sobre el Chimborazo”: anuncios y fundación (Dossier: Bicentenario, rastros y revelaciones de la Independencia)

El autor reflexiona sobre el poema escrito por Bolívar en 1823. Plantea que, ante la sobrecogedora belleza del volcán, y enfrentado a un destino complejo y caótico, el héroe revive eternos temores. Serrano lo asimila al Cristo del sermón de la montaña, cuando pretende reencontrarse con los elementos, reinsertarse en el mundo que está redefiniéndose en los campos de batalla. En la cima del Chimborazo, Bolívar dialoga con el tiempo, voz en la que el autor destaca las resonancias bíblicas. Resalta que el héroe, perturbado por los acontecimientos políticos, está poseído por una “pasión violenta”, por un proyecto político que deviene en obsesión: la idea de construir una gran nación liberada. Serrano concibe a la voz del Viejo como la representante de un orden mítico que pervive (el guardián del mundo mineral y espiritual), que interpela a un sujeto que, otra vez como el Cristo, duda. El final abierto del texto, para el autor, sugiere que solo en el sueño o el delirio es posible reconocer nuestra condición de “míseros mortales”.

Francisco Granizo: el poeta que invoca el momento primigenio (In memoriam)

Michelena Otero, Sofía Gabriela","ECUADOR","SIGLO XX","2011","Este artículo está dedicado a uno de los poetas más lúcidos y coherentes de la poesía ecuatoriana: Francisco Granizo Ribadeneira (Quito, 1925-2009). En una primera parte, se desarrollan algunos aspectos biográficos del poeta, esto permitirá que los lectores se acerquen de una manera mucho más humana y familiar a la vida de Granizo, conozcan al niño y al hombre que fue y, así, se intuyan ciertas características que están reflejadas en su poesía. Granizo nunca mencionó nada de su vida personal, nadie lo buscó para saber de él ni de su trabajo académico y diplomático, por esta razón es importante hacerlo aquí, para reivindicar su labor de poeta y de hombre de cultura. Luego se realiza un análisis de los tres ejes temáticos relevantes en la poesía de Granizo. En primer lugar, el amor, ese eterno desencuentro con el ser amado que representa y se fusiona al tiempo con la naturaleza, con Dios, con el momento primigenio y, al final, con la muerte. En segundo lugar, el misticismo, ese ímpetu religioso que gobierna la relación hombre-Dios y que obliga a que la voz poemática permanezca en una constante búsqueda de lo absoluto, es decir, del Origen. Y, en tercer lugar, la blasfemia, ese momento caótico, desesperante y contradictorio que surge como una consecuencia del fracaso amoroso y místico.

The diabatic contour advective semi-Lagrangian model

This article describes a novel algorithmic development extending the contour advective semi-Lagrangian model to include nonconservative effects. The Lagrangian contour representation of finescale tracer fields, such as potential vorticity, allows for conservative, nondiffusive treatment of sharp gradients allowing very high numerical Reynolds numbers. It has been widely employed in accurate geostrophic turbulence and tracer advection simulations. In the present, diabatic version of the model the constraint of conservative dynamics is overcome by including a parallel Eulerian field that absorbs the nonconservative ( diabatic) tendencies. The diabatic buildup in this Eulerian field is limited through regular, controlled transfers of this field to the contour representation. This transfer is done with a fast newly developed contouring algorithm. This model has been implemented for several idealized geometries. In this paper a single-layer doubly periodic geometry is used to demonstrate the validity of the model. The present model converges faster than the analogous semi-Lagrangian models at increased resolutions. At the same nominal spatial resolution the new model is 40 times faster than the analogous semi-Lagrangian model. Results of an orographically forced idealized storm track show nontrivial dependency of storm-track statistics on resolution and on the numerical model employed. If this result is more generally applicable, this may have important consequences for future high-resolution climate modeling.

A cell by cell anisotropic adaptive mesh ALE scheme for the numerical solution of the Euler equations

In this paper a cell by cell anisotropic adaptive mesh technique is added to an existing staggered mesh Lagrange plus remap finite element ALE code for the solution of the Euler equations. The quadrilateral finite elements may be subdivided isotropically or anisotropically and a hierarchical data structure is employed. An efficient computational method is proposed, which only solves on the finest level of resolution that exists for each part of the domain with disjoint or hanging nodes being used at resolution transitions. The Lagrangian, equipotential mesh relaxation and advection (solution remapping) steps are generalised so that they may be applied on the dynamic mesh. It is shown that for a radial Sod problem and a two-dimensional Riemann problem the anisotropic adaptive mesh method runs over eight times faster.

Impact of Tibetan Orography and Heating on the Summer Flow over Asia

The influence on the summer flow over Asia of both the orographic and thermal forcing of the Tibetan Plateau is investigated using a sequence of idealised experiments with a global primitive equation model. The zonally averaged flow is prescribed and both realistic and idealised orography and heating are used. There is some similarity between the responses to the two forcings when applied separately. The upper tropospheric Tibetan anticyclone is predominantly forced by the heating but also weakly by the orography. Below this, both forcings tend to give air descending in an equatorward anticyclonic circulation down the isentropes to the west and rising in a similar poleward circulation to the east. However the heating-only response has a strong ascending southwesterly flow that is guided around the south and south-east of the orography when it is included. On the northern side, the westerly flow over the orography gives ascent on the upslope and descent on the downslope. It is found that heating over the Plateau leads to a potential vorticity (PV) minimum and that if it is sufficiently strong the flow is unstable, producing a quasi-biweekly oscillation. During this oscillation the Tibetan anticyclone changes between a single centre over the southwestern side of the Plateau and a split/double structure with centres over China and the Middle East. These characteristics are similar to observed variability in the region. Associated with this quasi-biweekly oscillation are significant variations in the strength of the ascent over the Plateau and the Rossby wave pattern over the North Pacific. The origin of the variability is instability associated with the zonally extended potential vorticity PV minimum on a θ-surface, as proposed by Hsu and Plumb (2000). This minimum is due to the tendency to reduce the PV above the heating over the Plateau and to advection by the consequent anticyclone of high PV around from the east and low PV to the west. The deep convection to the south and southeast of the Plateau tends to suppress the quasi-biweekly oscillation because the low PV produced above it acts to reduce the meridional PV gradient reversal. The occurrence of the oscillation depends on the relative magnitude of the heating in the two regions.

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

Wind-tunnel modelling of dispersion from a scalar area source in urban-like roughness

A wind-tunnel study was conducted to investigate ventilation of scalars from urban-like geometries at neighbourhood scale by exploring two different geometries a uniform height roughness and a non-uniform height roughness, both with an equal plan and frontal density of λ p = λ f = 25%. In both configurations a sub-unit of the idealized urban surface was coated with a thin layer of naphthalene to represent area sources. The naphthalene sublimation method was used to measure directly total area-averaged transport of scalars out of the complex geometries. At the same time, naphthalene vapour concentrations controlled by the turbulent fluxes were detected using a fast Flame Ionisation Detection (FID) technique. This paper describes the novel use of a naphthalene coated surface as an area source in dispersion studies. Particular emphasis was also given to testing whether the concentration measurements were independent of Reynolds number. For low wind speeds, transfer from the naphthalene surface is determined by a combination of forced and natural convection. Compared with a propane point source release, a 25% higher free stream velocity was needed for the naphthalene area source to yield Reynolds-number-independent concentration fields. Ventilation transfer coefficients w T /U derived from the naphthalene sublimation method showed that, whilst there was enhanced vertical momentum exchange due to obstacle height variability, advection was reduced and dispersion from the source area was not enhanced. Thus, the height variability of a canopy is an important parameter when generalising urban dispersion. Fine resolution concentration measurements in the canopy showed the effect of height variability on dispersion at street scale. Rapid vertical transport in the wake of individual high-rise obstacles was found to generate elevated point-like sources. A Gaussian plume model was used to analyse differences in the downstream plumes. Intensified lateral and vertical plume spread and plume dilution with height was found for the non-uniform height roughness

Boundary-layer ventilation by baroclinic lifecycles

Ventilation of the boundary layer has an important effect on local and regional air quality and is a prerequisite for long-range pollution transport. Once in the free troposphere, pollutants can alter the chemical composition of the troposphere and impact on the Earth's radiative forcing. Idealised baroclinic life cycles, LC1 and LC2, have been simulated in a three-dimensional dry hemispheric model in the presence of boundary-layer turbulent fluxes. A passive tracer is added to the simulations to represent pollution emitted at, or near, the surface. A simple conveyor-belt diagnostic is developed to objectively identify regions of the boundary layer that can be ventilated by either warm or cold conveyor belts. Transport of pollutants within and above the boundary layer is examined on synoptic scales. Three different physical mechanisms are found to interact with each other to ventilate pollutants out of the boundary layer. These mechanisms are turbulent mixing within the boundary layer, horizontal advection due to Ekman convergence and divergence within the boundary layer, and advection by the warm conveyor belt. The mass of tracer ventilated by the two life cycles is remarkably similar given the differences in frontal structure, suggesting that the large-scale baroclinicity is an effective constraint on ventilation.

Application of the Lighthill-Ford theory of spontaneous imbalance to clear-air turbulence forecasting

A new method of clear-air turbulence (CAT) forecasting based on the Lighthill–Ford theory of spontaneous imbalance and emission of inertia–gravity waves has been derived and applied on episodic and seasonal time scales. A scale analysis of this shallow-water theory for midlatitude synoptic-scale flows identifies advection of relative vorticity as the leading-order source term. Examination of leading- and second-order terms elucidates previous, more empirically inspired CAT forecast diagnostics. Application of the Lighthill–Ford theory to the Upper Mississippi and Ohio Valleys CAT outbreak of 9 March 2006 results in good agreement with pilot reports of turbulence. Application of Lighthill–Ford theory to CAT forecasting for the 3 November 2005–26 March 2006 period using 1-h forecasts of the Rapid Update Cycle (RUC) 2 1500 UTC model run leads to superior forecasts compared to the current operational version of the Graphical Turbulence Guidance (GTG1) algorithm, the most skillful operational CAT forecasting method in existence. The results suggest that major improvements in CAT forecasting could result if the methods presented herein become operational.

The moist boundary layer under a mid-latitude weather system

Mid-latitude weather systems are key contributors to the transport of atmospheric water vapour, but less is known about the role of the boundary layer in this transport. We expand a conceptual model of dry boundary-layer structure under synoptic systems to include moist processes, using idealised simulations of cyclone waves to investigate the three-way interaction between the boundary layer, atmospheric moisture and large-scale dynamics. Forced by large-scale thermal advection, boundary-layer structures develop over large areas, analogous to the daytime convective boundary layer, the nocturnal stable boundary layer and transitional regimes between these extremes.

Observed trends and teleconnections of the Siberian high: A recently declining center of action

This study investigates variability in the intensity of the wintertime Siberian high (SH) by defining a robust SH index (SHI) and correlating it with selected meteorological fields and teleconnection indices. A dramatic trend of -2.5 hPa decade(-1) has been found in the SHI between 1978 and 2001 with unprecedented (since 1871) low values of the SHI. The weakening of the SH has been confirmed by analyzing different historical gridded analyses and individual station observations of sea level pressure (SLP) and excluding possible effects from the conversion of surface pressure to SLP. SHI correlation maps with various meteorological fields show that SH impacts on circulation and temperature patterns extend far outside the SH source area extending from the Arctic to the tropical Pacific. Advection of warm air from eastern Europe has been identified as the main mechanism causing milder than normal conditions over the Kara and Laptev Seas in association with a strong SH. Despite the strong impacts of the variability in the SH on climatic variability across the Northern Hemisphere, correlations between the SHI and the main teleconnection indices of the Northern Hemisphere are weak. Regression analysis has shown that teleconnection indices are not able to reproduce the interannual variability and trends in the SH. The inclusion of regional surface temperature in the regression model provides closer agreement between the original and reconstructed SHI.

Long-term change, interannual and intra-seasonal variability in climate and glacier mass balance in the Central Greater Caucasus, Russia

Long-term trends, interannual and intra-seasonal variability in the mass-balance record from Djankuat glacier, central Greater Caucasus, Russia, are related to local climate change, synoptic and large-scale anomalies in atmospheric circulation. A clear warming signal emerged in the central Greater Caucasus in the early 1990s, leading to a strong increase in ablation. In the absence of a compensating change in winter accumulation, the net mass balance of Djankuat has declined. The highest value of seasonal ablation on record was registered in the summer of 2000. At the beginning of the 21st century these trends reversed. Ablation was below average even in the summer of 2003, which was unusually warm in western Europe. Precipitation and winter accumulation were high, allowing for a partial recovery of net mass balance. The interannual variability in the components of mass balance is weakly related to the North Atlantic Oscillation (NAO) and the Scandinavian teleconnection patterns, but there is a clear link with the large-scale circulation anomalies represented by the Rossby pattern. Five synoptic categories have been identified for the ablation season of 2005, revealing a strong separation between components of radiation budget, air temperature and daily melt. Air temperature is the main control over melt. The highest values of daily ablation are related to the strongly positive NAO which forces high net radiation, and to the warm and moist advection from the Black Sea.

Modelling monsoons: understanding and predicting current and future behaviour

The global monsoon system is so varied and complex that understanding and predicting its diverse behaviour remains a challenge that will occupy modellers for many years to come. Despite the difficult task ahead, an improved monsoon modelling capability has been realized through the inclusion of more detailed physics of the climate system and higher resolution in our numerical models. Perhaps the most crucial improvement to date has been the development of coupled ocean-atmosphere models. From subseasonal to interdecadal time scales, only through the inclusion of air-sea interaction can the proper phasing and teleconnections of convection be attained with respect to sea surface temperature variations. Even then, the response to slow variations in remote forcings (e.g., El Niño—Southern Oscillation) does not result in a robust solution, as there are a host of competing modes of variability that must be represented, including those that appear to be chaotic. Understanding the links between monsoons and land surface processes is not as mature as that explored regarding air-sea interactions. A land surface forcing signal appears to dominate the onset of wet season rainfall over the North American monsoon region, though the relative role of ocean versus land forcing remains a topic of investigation in all the monsoon systems. Also, improved forecasts have been made during periods in which additional sounding observations are available for data assimilation. Thus, there is untapped predictability that can only be attained through the development of a more comprehensive observing system for all monsoon regions. Additionally, improved parameterizations - for example, of convection, cloud, radiation, and boundary layer schemes as well as land surface processes - are essential to realize the full potential of monsoon predictability. A more comprehensive assessment is needed of the impact of black carbon aerosols, which may modulate that of other anthropogenic greenhouse gases. Dynamical considerations require ever increased horizontal resolution (probably to 0.5 degree or higher) in order to resolve many monsoon features including, but not limited to, the Mei-Yu/Baiu sudden onset and withdrawal, low-level jet orientation and variability, and orographic forced rainfall. Under anthropogenic climate change many competing factors complicate making robust projections of monsoon changes. Absent aerosol effects, increased land-sea temperature contrast suggests strengthened monsoon circulation due to climate change. However, increased aerosol emissions will reflect more solar radiation back to space, which may temper or even reduce the strength of monsoon circulations compared to the present day. Precipitation may behave independently from the circulation under warming conditions in which an increased atmospheric moisture loading, based purely on thermodynamic considerations, could result in increased monsoon rainfall under climate change. The challenge to improve model parameterizations and include more complex processes and feedbacks pushes computing resources to their limit, thus requiring continuous upgrades of computational infrastructure to ensure progress in understanding and predicting current and future behaviour of monsoons.