L’intégration des jeunes immigrants : une analyse des politiques à la jeunesse orientées vers la population immigrante au Québec

Ce mémoire porte sur l’intégration des jeunes immigrants au Québec. Il questionne la prise en compte de ces jeunes dans le cadre des politiques publiques de la province, à savoir celles de l’intégration des immigrants et la politique à la jeunesse du Québec. Le but est de savoir comment ces politiques abordent l’intégration des jeunes immigrants de première et de deuxième génération. À partir d’un tour d’horizon sur la littérature disponible, le travail permet de constater les différents problèmes d’intégration vécus par ces jeunes, notamment dans le milieu scolaire et sur le marché du travail. Les politiques dont il est question ici décrivent les obstacles et difficultés des jeunes immigrants. Elles proposent des mesures d’intégration pour les jeunes d’origine immigrante. La démarche qualitative est l’option privilégiée pour la réalisation de cette recherche de nature qualitative et exploratoire. Elle permet l’étude des documents de politique ci-mentionnés par rapport notre question de recherche. L’analyse documentaire est la principale méthode utilisée sur la base de laquelle, les dimensions de l’intégration des immigrants au Québec comme le français, les valeurs éducatives et l’emploi sont analysées en tant qu’enjeux soulevés par les documents de politique. Les constats qui en découlent permettent d’observer plusieurs résultats à propos des jeunes concernés par cette étude. Les résultats de l’étude démontrent que ces politiques mettent l’accent sur le français comme facteur incontournable de l’intégration. Ce faisant, elles insistent sur l’investissement du gouvernement dans l’apprentissage de cette langue par les jeunes immigrants. D’autres résultats révèlent que la grande majorité des jeunes nouveaux arrivants au Québec ces dernières années connaissent bien le français, d’ailleurs ils sont sélectionnés sur cette base. Cependant, cette majorité n’est pas intégrée sur le marché du travail. Par ailleurs, les politiques prônent une intervention auprès des jeunes axée sur la création par la société d’accueil des conditions favorables à leur intégration, tout en minimisant l’importance de leurs trajectoires migratoires ainsi que l’expérience acquise au pays d’origine. Ces prises en compte sont pourtant nécessaires à l’intégration. Au fond, les politiques proposent une intégration qui s’apparente à l’assimilation, ce qui est aux antipodes du modèle d’intégration interculturaliste adopté par le Québec.

‘Sudden Stratospheric Warming and its Influence on the Tropical Atmosphere'

The stratospheric warming events are categorized into major and minor warming depending on the temperature increase in the polar stratosphere. The warming is called a ‘major’, when the polar temperature increases poleward from 60 degree latitude and followed by a reversal in the zonal wind at 10 hPa (~32 Km). Usually major warming events are associated with the displacement of polar vortex from high to mid latitudes or the splitting of vortices in to two. The warming is called a "Minor", when the polar temperature increases more than 25 degree in a period of a week or less, at any stratospheric level with less intensified easterly wind anomalies. The stratospheric warmings generated during the transition period of winter to spring are called final warmings. The warming events observed in the early winter period (November to early December) over Canadian region are called Canadian warmings. There is strong interaction between stratosphere and troposphere during SSW period over high and low latitudes regions. The thesis consists of 7 chapters

Characteristics of oscillation in surface layer and above over Cochin

The oscillations in the Atmospheric Boundary Layer (ABL) are important because the transport mechanism from the surface to the upper atmosphere is governed by the ABL characteristics. The study was carried out using wind and temperature data observed at surface, 925 hPa and 850 hPa levels over Cochin and the different frequencies embedded in the boundary layer parameters are identified by employing wavelet technique. Surface boundary layer characteristics over the monsoon region are closely linked to the upper layer monsoon features. In this perception it is important to study the various oscillations in the surface boundary layer and the layer above. It is found that the wind and temperature at different levels show oscillations in Quasi Biweekly Mode (QBM) and Intra Seasonal Oscillation (ISO) bands as observed in a typical monsoon system. Amplitude of the oscillation varies with height. The amplitude of the QBM periodicity is more in the surface levels but in the upper levels the amplitude of the ISO periodicity is more than that of the QBM. From this, it is obvious that the controlling mechanism of QBM band is surface parameters such as surface friction and that for ISO band is associated with the active-break cycles of monsoon system

Assessment of Convective Activity Using Stability Indices as Inferred from Radiosonde and MODIS Data

The combined use of both radiosonde data and three-dimensional satellite derived data over ocean and land is useful for a better understanding of atmospheric thermodynamics. Here, an attempt is made to study the ther-modynamic structure of convective atmosphere during pre-monsoon season over southwest peninsular India utilizing satellite derived data and radiosonde data. The stability indices were computed for the selected stations over southwest peninsular India viz: Thiruvananthapuram and Cochin, using the radiosonde data for five pre- monsoon seasons. The stability indices studied for the region are Showalter Index (SI), K Index (KI), Lifted In-dex (LI), Total Totals Index (TTI), Humidity Index (HI), Deep Convective Index (DCI) and thermodynamic pa-rameters such as Convective Available Potential Energy (CAPE) and Convective Inhibition Energy (CINE). The traditional Showalter Index has been modified to incorporate the thermodynamics over tropical region. MODIS data over South Peninsular India is also used for the study. When there is a convective system over south penin-sular India, the value of LI over the region is less than −4. On the other hand, the region where LI is more than 2 is comparatively stable without any convection. Similarly, when KI values are in the range 35 to 40, there is a possibility for convection. The threshold value for TTI is found to be between 50 and 55. Further, we found that prior to convection, dry bulb temperature at 1000, 850, 700 and 500 hPa is minimum and the dew point tem-perature is a maximum, which leads to increase in relative humidity. The total column water vapor is maximum in the convective region and minimum in the stable region. The threshold values for the different stability indices are found to be agreeing with that reported in literature.

Meteorological aspects of an abnormal cooling event over Iran in April 2009

During the period from 12 to 15 April, 2009 nearly the entire Iran, apart from the southern border, experienced an advective cooling event. While winter freezing concerns are typical, the nature of this freezing event was unusual with respect to its date of occurrence and accompanying synoptic meteorological situation. To analyze the freezing event, the relevant meteorological data at multiple levels of the atmosphere were examined from the NCEP/ NCAR reanalysis dataset. The results showed that a polar vortex was responsible for the freezing event over the country extending southward extraordinarily in such a way that its ridge influenced most parts of Iran. This was recognized as an abnormal extension of a polar vortex in the recent years. The sea-level pressure fields indicated that a ridge of large-scale anticyclone centered over Black Sea extended southward and prevailed over most parts of Iran. This resulted in the formation of a severe cold air advection from high latitudes (Polar region) over Iran. During the study period, moisture pumping was observed from the Arabian Sea and Persian Gulf. The winds at 1000 hPa level blew with a magnitude of 10 m s-1 toward south in the region of convergence (between -2 9 10-6 s-1 and -12 9 10-6 s-1). The vertical profilesof temperature and humidity also indicated that the ICE structural icing occurred at multiple levels of the atmosphere, i.e, from 800 hPa through 400 hPa levels. In addition to the carburetor (or induction), icing occurred between 900 and 700 hPa levels in the selected radiosonde stations during the study period. In addition, the HYSPLIT backward trajectory model outputs were in quite good agreement with the observed synoptic features

Large-Size AlGaN/GaN HEMT Large-Signal Electrothermal Characterization and Modeling for Wireless Digital Communications

The rapid growth in high data rate communication systems has introduced new high spectral efficient modulation techniques and standards such as LTE-A (long term evolution-advanced) for 4G (4th generation) systems. These techniques have provided a broader bandwidth but introduced high peak-to-average power ratio (PAR) problem at the high power amplifier (HPA) level of the communication system base transceiver station (BTS). To avoid spectral spreading due to high PAR, stringent requirement on linearity is needed which brings the HPA to operate at large back-off power at the expense of power efficiency. Consequently, high power devices are fundamental in HPAs for high linearity and efficiency. Recent development in wide bandgap power devices, in particular AlGaN/GaN HEMT, has offered higher power level with superior linearity-efficiency trade-off in microwaves communication. For cost-effective HPA design to production cycle, rigorous computer aided design (CAD) AlGaN/GaN HEMT models are essential to reflect real response with increasing power level and channel temperature. Therefore, large-size AlGaN/GaN HEMT large-signal electrothermal modeling procedure is proposed. The HEMT structure analysis, characterization, data processing, model extraction and model implementation phases have been covered in this thesis including trapping and self-heating dispersion accounting for nonlinear drain current collapse. The small-signal model is extracted using the 22-element modeling procedure developed in our department. The intrinsic large-signal model is deeply investigated in conjunction with linearity prediction. The accuracy of the nonlinear drain current has been enhanced through several issues such as trapping and self-heating characterization. Also, the HEMT structure thermal profile has been investigated and corresponding thermal resistance has been extracted through thermal simulation and chuck-controlled temperature pulsed I(V) and static DC measurements. Higher-order equivalent thermal model is extracted and implemented in the HEMT large-signal model to accurately estimate instantaneous channel temperature. Moreover, trapping and self-heating transients has been characterized through transient measurements. The obtained time constants are represented by equivalent sub-circuits and integrated in the nonlinear drain current implementation to account for complex communication signals dynamic prediction. The obtained verification of this table-based large-size large-signal electrothermal model implementation has illustrated high accuracy in terms of output power, gain, efficiency and nonlinearity prediction with respect to standard large-signal test signals.

La Geografia política en Vidal de la Blanche: la France de l'Est

En 1979 Y. Lacoste a publié dans la revue "Hérodote" un article surprenant intitulé "A bas Vidal ... Viva Vidal" qui exhumait la dernière œuvre de Vidal de la Blache: La france de I'Est (Loraine-Alsace) (1917). Dans cet article, Lacoste faisait l'éloge de certains aspects économiques, sociaux et surtout géopolitiques, non traités dans le traditionnel modèle vidalien. Nous tenterons d'approfondir dans cet essai l'une des questions qu'a induite l'article de Lacoste, a savoir la place qu'occupe la Géographie Politique dans l'école vidalienne. Les différents travaux et actions des disciples de Vidal ont fait preuve d’un grand intérêt pour la Géographie Politique en abandonnant provisoirement le schéma descriptif prope à la géographie régionale française. À la fin de la première guerre mondiale, le problème frontalier de l'Alsace-Loraine devient l'axe central de La France de I'Est; On a fait ressortir les éléments géopolitiques de cette œuvre a fin de démontrer que l'aspect géopolitique de l'école vidalienne est méconnu

Relación costo beneficio de plaquetas estándar versus plaquetas por aféresis en el Banco de Sangre de la Clínica Colsanitas

Se realizó un estudio costo beneficio para el tratamiento de trombocitopenias en pacientes con discrasias sanguíneas, comparando dos hemoderivados sanguíneos: las plaquetas estándar y plaquetas por aféresis. El estudio se realizó en el Banco de Sangre de la Clínica Colsanitas S.A, con información obtenida sobre pacientes que fueron transfundidos con dichos componentes durante los años 2009 al 2010. Ambos hemoderivados presentaron un nivel de respuesta terapéutica adecuado; se evidenció que los pacientes transfundidos con plaquetas por aféresis, requirieron ser transfundidos menos veces a comparación del grupo transfundido con plaquetas estándar, representando una ventaja respecto a la exposición antigénica de hemoderivados transfundidos, a la necesidad de requerir transfusiones próximas y en el costo del tratamiento para la Entidad hospitalaria. Surge la necesidad de continuar con estudios prospectivos en los Servicios Transfusionales y Bancos de Sangre, como la determinación por inmuno-genética de la aloinmunización HLA, desarrollo HPA, frente a la exposición antigénica que permita evidenciar el desenlace clínico, gestionar los riesgos inherentes a la transfusión y promover la producción de determinado hemoderivado.

Desconocimiento de la propiedad colectiva en Colombia: a la luz del Sistema Interamericano de Derechos Humanos

La jurisprudencia de la Corte Interamericana de Derechos Humanos de los últimos años, ha establecido una serie de criterios y medidas que configurarían un catálogo de disposiciones que deben emprender los Estados para garantizar la real protección del derecho de propiedad de las comunidades indígenas y tribales. Dichas medidas deben ser implementadas en los procesos de formalización y titularización de las tierras ancestrales ocupadas, en la delimitación y demarcación del terreno, en la restitución de porciones de tierra pérdida, en la estipulación de criterios para el otorgamiento de tierras alternativas; y en los estudios que tiendan a establecer políticas públicas para la satisfacción de las necesidades de las comunidades relativas a la producción y posesión de la tierra como mecanismo idóneo para el mantenimiento de condiciones de vida digna. La regulación colombiana para las tierras de las comunidades indígenas y las comunidades afrocolombianas presenta aspectos divergentes: las primeras poseen una reglamentación destinada a la ampliación, reestructuración y saneamiento de los resguardos indígenas, y las segundas están regidas bajo un estatuto general de la propiedad colectiva y adjudicación de baldíos. En los dos sistemas, los procedimientos son complejos, tardíos, confusos, requieren de sofisticados prerrequisitos, y ante todo su estructura está basada bajo criterios de una sociedad no indígena y no tribal. Adicionalmente, el compendio normativo en materia de titulación, delimitación y demarcación de tierras de comunidades afrocolombianas antes enunciado, presenta diversas lagunas normativas que se acentúan con la carencia de actualización de dicha regulación a las condiciones actuales si se tiene en cuenta que no ha existido modificación a la misma en los últimos 19 años, y que hacen necesario aplicar analógicamente las disposiciones del Código Civil en materia de propiedad individual a efectos de dar respuesta a los supuestos de hecho no contemplados.

Efecto del estrés ocasionado por las pruebas académicas sobre los niveles de cortisol y prolactina en un grupo de estudiantes de Medicina

Introducción: La relación entre el sistema inmune y el estrés ha sido motivo de debate en los últimos años. Los cambios neurohormonales generan variaciones en la respuesta inmunológica, con cambios importantes en los niveles de citoquinas lo que causa a su vez, en algunos casos, depresión de la respuesta citotóxica debida a la disminución de la población de células asesinas naturales (NK) (1). El estrés académico constituye un buen modelo para estudiar los cambios asociados en la secreción de algunas hormonas del eje Hipotalámico- Pituitario-Adrenocortical -HPA- (2, 3). Materiales y métodos: En el presente estudio se evaluó el comportamiento de las hormonascortisol y prolactina, así como su incidencia en la respuesta adaptativa a Herpes Simple tipo I, en una población de estudio constituída por 26 estudiantes de la Facultad de Medicina, con edades comprendidas entre 14 y 27 años, con mayor frecuencia de género masculino (80.8%). Se realizó un estudio de intervención longitudinal en tres momentos, donde se midieron los niveles de cortisol, prolactina y anticuerpos contra Herpes Simple tipo I. Así mismo, se realizó una medición 15 días antes de la exposición al estresor, durante la aplicación del estresor (semana de exámenes trimestrales), y quince días después de la exposición al estresor Todas las muestras fueron tomadas entre las 8:00 a.m. y las 10:00 a.m. Resultados y discusión: Se encontraron diferencias significativas (p < 0.001) en los valores promedio de prolactina, pues hubo una tendencia secular al aumento en los tres momentos evaluados. Para el cortisol, los cambios estuvieron cerca de mostrar diferencias significativas (p = 0.098), con un aumento en el momento del estresor y una disminución después del estresor. También hubo diferencias significativas (p = 0.043) en los niveles de anticuerpos para Herpes Simple tipo I, con una tendencia secular al aumento en los tres momentos evaluados. La respuesta adaptativa a Herpes Simple tipo I aumentó notoriamente como resultado de los cambios en la concentración de prolactina, la que, a su vez, aumentó de manera significativa después de la exposición al estresor. Aunque los niveles de cortisol no aumentan significativamente durante la semana del estresor, podrían ser suficientes para mantener niveles basales de prolactina, sin que haya un aumento de la respuesta adaptativa. Se podría inferir que el cortisol regula la síntesis de prolactina, pues en los resultados se observa que, a medida que disminuye la concentración de cortisol, los niveles de prolactina aumentan significativamente.

Orientación profesional y situación socio-económica en Argentina. 'Career guidance and socio-economic situation in Argentina'.

Resumen tomado de la publicación. Con el apoyo económico del departamento MIDE de la UNED

A new perspective on Southern hemisphere storm-tracks.

A detailed view of Southern Hemisphere storm tracks is obtained based on the application of filtered variance and modern feature-tracking techniques to a wide range of 45-yr European Centre for Medium-Range Weather Forecasts (ECMWF) Re-Analysis (ERA-40) data. It has been checked that the conclusions drawn in this study are valid even if data from only the satellite era are used. The emphasis of the paper is on the winter season, but results for the four seasons are also discussed. Both upper- and lower-tropospheric fields are used. The tracking analysis focuses on systems that last longer than 2 days and are mobile (move more than 1000 km). Many of the results support previous ideas about the storm tracks, but some new insights are also obtained. In the summer there is a rather circular, strong, deep high-latitude storm track. In winter the high-latitude storm track is more asymmetric with a spiral from the Atlantic and Indian Oceans in toward Antarctica and a subtropical jet–related lower-latitude storm track over the Pacific, again tending to spiral poleward. At all times of the year, maximum storm activity in the higher-latitude storm track is in the Atlantic and Indian Ocean regions. In the winter upper troposphere, the relative importance of, and interplay between, the subtropical and subpolar storm tracks is discussed. The genesis, lysis, and growth rate of lower-tropospheric winter cyclones together lead to a vivid picture of their behavior that is summarized as a set of overlapping plates, each composed of cyclone life cycles. Systems in each plate appear to feed the genesis in the next plate through downstream development in the upper-troposphere spiral storm track. In the lee of the Andes in South America, there is cyclogenesis associated with the subtropical jet and also, poleward of this, cyclogenesis largely associated with system decay on the upslope and regeneration on the downslope. The genesis and lysis of cyclones and anticyclones have a definite spatial relationship with each other and with the Andes. At 500 hPa, their relative longitudinal positions are consistent with vortex-stretching ideas for simple flow over a large-scale mountain. Cyclonic systems near Antarctica have generally spiraled in from lower latitudes. However, cyclogenesis associated with mobile cyclones occurs around the Antarctic coast with an interesting genesis maximum over the sea ice near 150°E. The South Pacific storm track emerges clearly from the tracking as a coherent deep feature spiraling from Australia to southern South America. A feature of the summer season is the genesis of eastward-moving cyclonic systems near the tropic of Capricorn off Brazil, in the central Pacific and, to a lesser extent, off Madagascar, followed by movement along the southwest flanks of the subtropical anticyclones and contribution to the “convergence zone” cloud bands seen in these regions.

A note on atmospheric predictability

Using the method of Lorenz (1982), we have estimated the predictability of a recent version of the European Center for Medium-Range Weather Forecasting (ECMWF) model using two different estimates of the initial error corresponding to 6- and 24-hr forecast errors, respectively. For a 6-hr forecast error of the extratropical 500-hPa geopotential height field, a potential increase in forecast skill by more than 3 d is suggested, indicating a further increase in predictability by another 1.5 d compared to the use of a 24-hr forecast error. This is due to a smaller initial error and to an initial error reduction resulting in a smaller averaged growth rate for the whole 7-d forecast. A similar assessment for the tropics using the wind vector fields at 850 and 250 hPa suggests a huge potential improvement with a 7-d forecast providing the same skill as a 1-d forecast now. A contributing factor to the increase in the estimate of predictability is the apparent slow increase of error during the early part of the forecast.

Global observations and forecast skill

The impact of selected observing systems on forecast skill is explored using the European Centre for Medium-Range Weather Forecasts (ECMWF) 40-yr reanalysis (ERA-40) system. Analyses have been produced for a surface-based observing system typical of the period prior to 1945/1950, a terrestrial-based observing system typical of the period 1950-1979 and a satellite-based observing system consisting of surface pressure and satellite observations. Global prediction experiments have been undertaken using these analyses as initial states, and which are available every 6 h, for the boreal winters of 1990/1991 and 2000/2001 and the summer of 2000, using a more recent version of the ECMWF model. The results show that for 500-hPa geopotential height, as a representative field, the terrestrial system in the Northern Hemisphere extratropics is only slightly inferior to the control system, which makes use of all observations for the analysis, and is also more accurate than the satellite system. There are indications that the skill of the terrestrial system worsens slightly and the satellite system improves somewhat between 1990/1991 and 2000/2001. The forecast skill in the Southern Hemisphere is dominated by the satellite information and this dominance is larger in the latter period. The overall skill is only slightly worse than that of the Northern Hemisphere. In the tropics (20 degrees S-20 degrees N), using the wind at 850 and 250 hPa as representative fields, the information content in the terrestrial and satellite systems is almost equal and complementary. The surface-based system has very limited skill restricted to the lower troposphere of the Northern Hemisphere. Predictability calculations show a potential for a further increase in predictive skill of 1-2 d in the extratropics of both hemispheres, but a potential for a major improvement of many days in the tropics. As well as the Eulerian perspective of predictability, the storm tracks have been calculated from all experiments and validated for the extratropics to provide a Lagrangian perspective.

The predictability of extratropical storm tracks and the sensitivity of their prediction to the observing system

A new method for assessing forecast skill and predictability that involves the identification and tracking of extratropical cyclones has been developed and implemented to obtain detailed information about the prediction of cyclones that cannot be obtained from more conventional analysis methodologies. The cyclones were identified and tracked along the forecast trajectories, and statistics were generated to determine the rate at which the position and intensity of the forecasted storms diverge from the analyzed tracks as a function of forecast lead time. The results show a higher level of skill in predicting the position of extratropical cyclones than the intensity. They also show that there is potential to improve the skill in predicting the position by 1 - 1.5 days and the intensity by 2 - 3 days, via improvements to the forecast model. Further analysis shows that forecasted storms move at a slower speed than analyzed storms on average and that there is a larger error in the predicted amplitudes of intense storms than the weaker storms. The results also show that some storms can be predicted up to 3 days before they are identified as an 850-hPa vorticity center in the analyses. In general, the results show a higher level of skill in the Northern Hemisphere (NH) than the Southern Hemisphere (SH); however, the rapid growth of NH winter storms is not very well predicted. The impact that observations of different types have on the prediction of the extratropical cyclones has also been explored, using forecasts integrated from analyses that were constructed from reduced observing systems. A terrestrial, satellite, and surface-based system were investigated and the results showed that the predictive skill of the terrestrial system was superior to the satellite system in the NH. Further analysis showed that the satellite system was not very good at predicting the growth of the storms. In the SH the terrestrial system has significantly less skill than the satellite system, highlighting the dominance of satellite observations in this hemisphere. The surface system has very poor predictive skill in both hemispheres.