947 resultados para gee analyses


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La version intégrale de cette thèse est disponible uniquement pour consultation individuelle à la Bibliothèque de l'Université de Montréal (www.bib.umontreal.ca/MU).

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Avec la sécularisation, la laïcité et la diversité croissantes de la société québécoise, la place de la religion en général et du catholicisme en particulier se sont vues remises en question. Cette situation a d’ailleurs mené à la mise en place de deux commissions : l’une sur la place de la religion à l’école (1999) et l’autre sur les pratiques d’accommodements reliées aux différences culturelles (2008). Ces deux commissions auront fourni énormément d’informations sur les rapports qu’entretiennent encore les Québécois avec le catholicisme. Cette recherche a donc pour but de faire le point sur certains aspects du catholicisme au Québec à partir d’une perspective reposant principalement sur des instruments heuristiques issus des écrits signés « Jacques Derrida ». Pour ce faire, nous nous appuierons sur les travaux du Groupe de travail sur la religion à l’école, de la consultation générale sur la place de la religion à l’école et de la commission de consultation sur les pratiques d’accommodement reliées aux différences culturelles. Nous posons comme hypothèse que de manière générale, les Québécois entretiennent avec le catholicisme, des rapports « archivaux », c’est-à-dire conditionnés par des perceptions de ce dernier informées par son passé, plutôt que par son présent. De plus, ces perceptions du catholicisme, probablement développées dans le sillage de la Révolution tranquille et peut-être même un peu avant, nourriraient l’existence de « spectres » qui viendraient hanter les rapports des Québécois à tout ce qui touche le religieux et la diversité culturelle. En ce sens, il s’agit d’une dimension essentielle de ce que nous appellerions la « postmodernité » religieuse québécoise. Pour illustrer ce propos, nous mènerons une analyse de contenu documentaire. Premièrement, nous procéderons à l’analyse thématique de centaines de documents (rapports de recherche, rapports officiels, mémoires) déposés lors de ces débats. Le logiciel QDA Miner permettra d’effectuer une analyse documentaire en identifiant les passages thématiques reliés à la recherche. Nous procéderons ensuite à une analyse plus fine de ces extraits sélectionnés à partir de perspectives philosophiques provenant principalement du philosophe Jacques Derrida.

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Medipix2 (MPX) sont des détecteurs semi-conducteurs au silicium montés sur 256x256 pixels. Chaque pixel a une aire de 55x55μm2. L’aire active d’un détecteur MPX est d’environ 2 cm2. Avec deux modes de détection, un seuil et un temps d’exposition ajustables, leur utilisation peut être optimisée pour une analyse spécifique. Seize de ces détecteurs sont présentement installés dans l’expérience ATLAS (A Toroidal LHC ApparatuS) au CERN (Organisation Européenne pour la Recherche Nucléaire). Ils mesurent en temps réel le champ de radiation dû aux collisions proton-proton, au point d’interaction IP1 (Point d’Interaction 1) du LHC (Grand Collisionneur d’Hadrons). Ces mesures ont divers buts comme par exemple la mesure du champ de neutrons dans la caverne d’ATLAS. Le réseau de détecteurs MPX est complètement indépendant du détecteur ATLAS. Le groupe ATLAS-Montréal s’est intéressé à l’analyse des données récoltées par ces détecteurs pour calculer une valeur de la luminosité du LHC au point de collision des faisceaux, autour duquel est construit le détecteur ATLAS. Cette valeur est déterminée indépendamment de la luminosité mesurée par les divers sous-détecteurs d’ATLAS dédiés spécifiquement à la mesure de la luminosité. Avec l’augmentation de la luminosité du LHC les détecteurs MPX les plus proches du point d’interaction détectent un grand nombre de particules dont les traces sont impossibles à distinguer sur les images ("frames") obtenues, à cause de leur recouvrement. Les paramètres de mesure de certains de ces détecteurs ont été optimisés pour des mesures de luminosité. Une méthode d’analyse des données permet de filtrer les pixels bruyants et de convertir les données des images, qui correspondent à des temps d’exposition propres aux détecteurs MPX, en valeur de luminosité pour chaque LumiBlock. Un LumiBlock est un intervalle de temps de mesure propre au détecteur ATLAS. On a validé les mesures de luminosité premièrement en comparant les résultats obtenus par différents détecteurs MPX, et ensuite en comparant les valeurs de luminosité relevées à celles obtenues par les sous-détecteurs d’ATLAS dédiés spécifiquement à la mesure de la luminosité.

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Travail dirigé présenté à la Faculté des arts et sciences en vue de l'obtention du grade de Maîtrise en criminologie, option criminalistique et information.

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Cette thèse a été réalisée, entre autres, grâce à une subvention reçue du Fonds de recherche du Québec – Société et culture et de son partenaire le ministère de l’Éducation, du Loisir et du Sport (MELS) Les analyses contenues dans cette thèse ont été réalisées au Centre interuniversitaire québécois de statistiques sociales (CIQSS), membre du Réseau canadien des centres de données de recherche (RCCDR). Les activités du CIQSS sont rendues possibles grâce à l’appui financier du CRSHC, des IRSC, de la FCI, de Statistique Canada, du FRQSC ainsi que de l’ensemble des universités québécoises qui participent à leur financement. Les idées exprimées dans ce texte sont celles des auteurs et non celles des partenaires financiers.

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A problem in the archaeometric classification of Catalan Renaissance pottery is the fact, that the clay supply of the pottery workshops was centrally organized by guilds, and therefore usually all potters of a single production centre produced chemically similar ceramics. However, analysing the glazes of the ware usually a large number of inclusions in the glaze is found, which reveal technological differences between single workshops. These inclusions have been used by the potters in order to opacify the transparent glaze and to achieve a white background for further decoration. In order to distinguish different technological preparation procedures of the single workshops, at a Scanning Electron Microscope the chemical composition of those inclusions as well as their size in the two-dimensional cut is recorded. Based on the latter, a frequency distribution of the apparent diameters is estimated for each sample and type of inclusion. Following an approach by S.D. Wicksell (1925), it is principally possible to transform the distributions of the apparent 2D-diameters back to those of the true three-dimensional bodies. The applicability of this approach and its practical problems are examined using different ways of kernel density estimation and Monte-Carlo tests of the methodology. Finally, it is tested in how far the obtained frequency distributions can be used to classify the pottery

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The Canadian Migration Monitoring Network (CMMN) consists of standardized observation and migration count stations located largely along Canada’s southern border. A major purpose of CMMN is to detect population trends of migratory passerines that breed primarily in the boreal forest and are otherwise poorly monitored by the North American Breeding Bird Survey (BBS). A primary limitation of this approach to monitoring is that it is currently not clear which geographic regions of the boreal forest are represented by the trends generated for each bird species at each station or group of stations. Such information on “catchment areas” for CMMN will greatly enhance their value in contributing to understanding causes of population trends, as well as facilitating joint trend analysis for stations with similar catchments. It is now well established that naturally occurring concentrations of deuterium in feathers grown in North America can provide information on their approximate geographic origins, especially latitude. We used stable hydrogen isotope analyses of feathers (δ²Hf) from 15 species intercepted at 22 CMMN stations to assign approximate origins to populations moving through stations or groups of stations. We further constrained the potential catchment areas using prior information on potential longitudinal origins based upon bird migration trajectories predicted from band recovery data and known breeding distributions. We detected several cases of differences in catchment area of species passing through sites, and between seasons within species. We discuss the importance of our findings, and future directions for using this approach to assist conservation of migratory birds at continental scales.

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Reanalysis data obtained from data assimilation are increasingly used for diagnostic studies of the general circulation of the atmosphere, for the validation of modelling experiments and for estimating energy and water fluxes between the Earth surface and the atmosphere. Because fluxes are not specifically observed, but determined by the data assimilation system, they are not only influenced by the utilized observations but also by model physics and dynamics and by the assimilation method. In order to better understand the relative importance of humidity observations for the determination of the hydrological cycle, in this paper we describe an assimilation experiment using the ERA40 reanalysis system where all humidity data have been excluded from the observational data base. The surprising result is that the model, driven by the time evolution of wind, temperature and surface pressure, is able to almost completely reconstitute the large-scale hydrological cycle of the control assimilation without the use of any humidity data. In addition, analysis of the individual weather systems in the extratropics and tropics using an objective feature tracking analysis indicates that the humidity data have very little impact on these systems. We include a discussion of these results and possible consequences for the way moisture information is assimilated, as well as the potential consequences for the design of observing systems for climate monitoring. It is further suggested, with support from a simple assimilation study with another model, that model physics and dynamics play a decisive role for the hydrological cycle, stressing the need to better understand these aspects of model parametrization. .

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Tropical cyclones have been investigated in a T159 version of the MPI ECHAM5 climate model using a novel technique to diagnose the evolution of the 3-dimensional vorticity structure of tropical cyclones, including their full life cycle from weak initial vortex to their possible extra-tropical transition. Results have been compared with reanalyses (ERA40 and JRA25) and observed tropical storms during the period 1978-1999 for the Northern Hemisphere. There is no indication of any trend in the number or intensity of tropical storms during this period in ECHAM5 or in re-analyses but there are distinct inter-annual variations. The storms simulated by ECHAM5 are realistic both in space and time, but the model and even more so the re-analyses, underestimate the intensities of the most intense storms (in terms of their maximum wind speeds). There is an indication of a response to ENSO with a smaller number of Atlantic storms during El Niño in agreement with previous studies. The global divergence circulation responds to El Niño by setting up a large-scale convergence flow, with the center over the central Pacific with enhanced subsidence over the tropical Atlantic. At the same time there is an increase in the vertical wind shear in the region of the tropical Atlantic where tropical storms normally develop. There is a good correspondence between the model and ERA40 except that the divergence circulation is somewhat stronger in the model. The model underestimates storms in the Atlantic but tends to overestimate them in the Western Pacific and in the North Indian Ocean. It is suggested that the overestimation of storms in the Pacific by the model is related to an overly strong response to the tropical Pacific SST anomalies. The overestimation in 2 the North Indian Ocean is likely to be due to an over prediction in the intensity of monsoon depressions, which are then classified as intense tropical storms. Nevertheless, overall results are encouraging and will further contribute to increased confidence in simulating intense tropical storms with high-resolution climate models.

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[1] Temperature and ozone observations from the Microwave Limb Sounder (MLS) on the EOS Aura satellite are used to study equatorial wave activity in the autumn of 2005. In contrast to previous observations for the same season in other years, the temperature anomalies in the middle and lower tropical stratosphere are found to be characterized by a strong wave-like eastward progression with zonal wave number equal to 3. Extended empirical orthogonal function (EOF) analysis reveals that the wave 3 components detected in the temperature anomalies correspond to a slow Kelvin wave with a period of 8 days and a phase speed of 19 m/s. Fluctuations associated with this Kelvin wave mode are also apparent in ozone profiles. Moreover, as expected by linear theory, the ozone fluctuations observed in the lower stratosphere are in phase with the temperature perturbations, and peak around 20–30 hPa where the mean ozone mixing ratios have the steepest vertical gradient. A search for other Kelvin wave modes has also been made using both the MLS observations and the analyses from one experiment where MLS ozone profiles are assimilated into the European Centre for Medium-Range Weather Forecasts (ECMWF) data assimilation system via a 6-hourly 3D var scheme. Our results show that the characteristics of the wave activity detected in the ECMWF temperature and ozone analyses are in good agreement with MLS data.

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Predicting metal bioaccumulation and toxicity in soil organisms is complicated by site-specific biotic and abiotic parameters. In this study we exploited tissue fractionation and digestion techniques, combined with X-ray absorption spectroscopy (XAS), to investigate the whole-body and subcellular distributions, ligand affinities, and coordination chemistry of accumulated Pb and Zn in field populations of the epigeic earthworm Lumbricus rubellus inhabiting three contrasting metalliferous and two unpolluted soils. Our main findings were (i) earthworms were resident in soils with concentrations of Pb and Zn ranging from 1200 to 27 000 mg kg(-1) and 200 to 34 000 mg kg(-1), respectively; (ii) Pb and Zn primarily accumulated in the posterior alimentary canal in nonsoluble subcellular fractions of earthworms; (iii) site-specific differences in the tissue and subcellular partitioning profiles of populations were observed, with earthworms from a calcareous site partitioning proportionally more Pb to their anterior body segments and Zn to the chloragosome-rich subcellular fraction than their acidic-soil inhabiting counterparts; (iv) XAS indicated that the interpopulation differences in metal partitioning between organs were not accompanied by qualitative differences in ligand-binding speciation, because crystalline phosphate-containing pyromorphite was a predominant chemical species in the whole-worm tissues of all mine soil residents. Differences in metal (Pb, Zn) partitioning at both organ and cellular levels displayed by field populations with protracted histories of metal exposures may reflect their innate ecophysiological responses to essential edaphic variables, such as Ca2+ status. These observations are highly significant in the challenging exercise of interpreting holistic biomarker data delivered by "omic" technologies.

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Silchester is the site of a major late Iron Age and Roman town (Calleva Atrebatum), situated in northern Hampshire (England (UK)) and occupied between the late first century BC and the fifth or sixth century AD. Extensive evidence of the nature of the buildings and the plan of the town was obtained from excavations undertaken between 1890 and 1909. The purpose of this study was to use soil geochemical analyses to reinforce the archaeological evidence particularly with reference to potential metal working at the site. Soil analysis has been used previously to distinguish different functions or land use activity over a site and to aid identification and interpretation of settlement features (Entwistle et al., 2000). Samples were taken from two areas of the excavation on a 1-metre grid. Firstly from an area of some 500 square metres from contexts of late first/early second century AD date throughout the entirety of a large 'town house' (House 1) from which there was prima facie evidence of metalworking.