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acase@tulane.edu / The current study examined the impact of a professional development training in trauma-informed approaches on teacher attitudes. The current study had two main purposes: first, to determine whether two components of attitudes, perception of the problem and self-efficacy, became more trauma-informed among teachers following a professional development training; and second, to investigate whether that change in attitudes was linked to initial levels of familiarity with trauma-informed approaches and/or years of experience. Teachers from 6 schools that are part of the New Orleans Trauma-Informed Schools Learning Collaborative participated in the study (N = 163; 68.7% female, 58.9% White). Teachers filled out demographic information and completed the ARTIC scale (Baker, Brown, Wilcox, Overstreet & Arora, 2015) both before and after training. A paired-samples t-test revealed that perception of a problem and self-efficacy among teachers did become significantly more aligned with trauma-informed approaches following the training. However, contrary to the hypothesis, familiarity and years of experience did not moderate perception of a problem or self-efficacy. Regardless, these results have important implications for the trauma-informed schools movement as they show that PD trainings can positively impact teacher attitudes, potentially increasing teacher motivation to carry out trauma-informed practices in the classroom. / 1 / Juliana Vanderburg

The dynamics of the polar mesosphere and lower thermosphere ( MLT ) is investigated using MF radars at Davis ( 69 ° S, 78 ° E ), Syowa ( 69 ° S, 40 ° E ) and Rothera ( 68 ° S, 68 ° W ) in the Antarctic, and Poker Flat ( 65 ° N, 147 ° W ) and Andenes ( 69 ° N, 16 ° E ) in the Arctic. Mean winds and gravity waves are investigated on a climatological scale and also during sudden stratospheric warmings. Mean wind climatologies in the MLT show differences that are often hemispheric in nature. For example, summer peaks in westward and equatorward winds occur earlier ( closer to the solstice ) in the Antarctic than in the Arctic. The greater symmetry around the solstice of phenomena such as these indicates that radiative effects may play a greater role in controlling the state of the Antarctic MLT than in the Arctic, where dynamical effects might be more important. Gravity wave observations are consistent with this theory, suggesting more wave drag may occur in the Arctic MLT. The equatorward jet persists for about 2 weeks later in summer in the Arctic than in the Antarctic, as do satellite observations of polar mesospheric clouds ( PMCs ) ( a temperature dependent phenomenon ). It is proposed that the meridional winds can be used as a proxy for gravity wave driving and consequent adiabatic cooling in the MLT. VHF radar observations of polar mesospheric summer echoes ( PMSEs ) at Davis, and the satellite PMC observations, both occur at a similar time to the equatorward jet. Seasonal variations in gravity wave activity are generally a combination of annual ( with winter maxima and summer minima ) and semi - annual ( with maxima near the solstices and minima near the equinoxes ) components. The winter maxima and spring / summer minima both occur about 3 weeks later in the Antarctic than in the Arctic, with the difference in magnitude between these extrema being about 90 % larger in the Antarctic. The available MF radar data include six major sudden stratospheric warmings in the northern hemisphere, and the unprecedented southern event which occurred during 2002 splitting the Antarctic ozone hole apart. Three of the six northern events are relatively weak and could almost be classed as minor warmings, while the larger three are similar in strength and duration to the southern event. Gravity wave activity reduces dramatically at Davis during the southern event, but not at Syowa ( possibly due to differences in critical level filtering ). The influence of major warmings on mesospheric gravity wave strength and polarisation varies significantly between locations, and individual events. Zonal wind reversals associated with the large major warmings are all weaker and occur earlier in the mesosphere than in the stratosphere. Another hemispherically common response is zonal wave - 1 planetary wave signatures in the mesospheric meridional winds ( i.e., a flow over the pole ). The planetary wave signatures have 14 - day periodicity and are westward propagating leading up to the southern event. The zonal winds are weaker than average during the 2002 southern winter, and also during the transition to the summer circulation. This is not seen for the large northern major warmings. There appears to be both hemispheric similarities and differences in polar middle atmosphere dynamics during stratospheric warmings, and also on a climatological scale. / Thesis (Ph.D.)--School of Chemistry and Physics, 2005.

The dynamics of the polar mesosphere and lower thermosphere ( MLT ) is investigated using MF radars at Davis ( 69 ° S, 78 ° E ), Syowa ( 69 ° S, 40 ° E ) and Rothera ( 68 ° S, 68 ° W ) in the Antarctic, and Poker Flat ( 65 ° N, 147 ° W ) and Andenes ( 69 ° N, 16 ° E ) in the Arctic. Mean winds and gravity waves are investigated on a climatological scale and also during sudden stratospheric warmings. Mean wind climatologies in the MLT show differences that are often hemispheric in nature. For example, summer peaks in westward and equatorward winds occur earlier ( closer to the solstice ) in the Antarctic than in the Arctic. The greater symmetry around the solstice of phenomena such as these indicates that radiative effects may play a greater role in controlling the state of the Antarctic MLT than in the Arctic, where dynamical effects might be more important. Gravity wave observations are consistent with this theory, suggesting more wave drag may occur in the Arctic MLT. The equatorward jet persists for about 2 weeks later in summer in the Arctic than in the Antarctic, as do satellite observations of polar mesospheric clouds ( PMCs ) ( a temperature dependent phenomenon ). It is proposed that the meridional winds can be used as a proxy for gravity wave driving and consequent adiabatic cooling in the MLT. VHF radar observations of polar mesospheric summer echoes ( PMSEs ) at Davis, and the satellite PMC observations, both occur at a similar time to the equatorward jet. Seasonal variations in gravity wave activity are generally a combination of annual ( with winter maxima and summer minima ) and semi - annual ( with maxima near the solstices and minima near the equinoxes ) components. The winter maxima and spring / summer minima both occur about 3 weeks later in the Antarctic than in the Arctic, with the difference in magnitude between these extrema being about 90 % larger in the Antarctic. The available MF radar data include six major sudden stratospheric warmings in the northern hemisphere, and the unprecedented southern event which occurred during 2002 splitting the Antarctic ozone hole apart. Three of the six northern events are relatively weak and could almost be classed as minor warmings, while the larger three are similar in strength and duration to the southern event. Gravity wave activity reduces dramatically at Davis during the southern event, but not at Syowa ( possibly due to differences in critical level filtering ). The influence of major warmings on mesospheric gravity wave strength and polarisation varies significantly between locations, and individual events. Zonal wind reversals associated with the large major warmings are all weaker and occur earlier in the mesosphere than in the stratosphere. Another hemispherically common response is zonal wave - 1 planetary wave signatures in the mesospheric meridional winds ( i.e., a flow over the pole ). The planetary wave signatures have 14 - day periodicity and are westward propagating leading up to the southern event. The zonal winds are weaker than average during the 2002 southern winter, and also during the transition to the summer circulation. This is not seen for the large northern major warmings. There appears to be both hemispheric similarities and differences in polar middle atmosphere dynamics during stratospheric warmings, and also on a climatological scale. / Thesis (Ph.D.)--School of Chemistry and Physics, 2005.

Le Paléogène est une période de perturbations importantes du système climatique terrestre, marquée notamment par des optima climatiques reconnus à la fois en environnement continental et marin. Dans le contexte de réchauffement climatique actuel, l’étude et la compréhension de cette période de fortes fluctuations climatiques et de transition entre un climat de type « greenhouse » et « icehouse » est un enjeu capital. Par ailleurs, de nombreuses études ont été menées sur les basses et moyennes latitudes, alors que peu de travaux se focalisent sur les hautes latitudes. Dans cette étude, des successions deltaïques d’âge Paléocène-Eocène sont utilisées pour étudier la réponse du système Arctique à des évènements globaux, les optima climatiques du Paléogène (PETM, ETM2, EECO et l’évènement Azolla) et tenter de répondre à ces questions : le bassin a-t-il eu une réponse spécifique aux stimuli climatiques globaux? Existe-t-il des mécanismes de couplage/découplage de la dynamique du bassin Arctique de celle de l’océan global ? Cette étude est basée sur des analyses multiproxies : la minéralogie de la roche totale et de la fraction argileuse, la pyrolyse Rock Eval, la palynologie, les palynofaciès et les isotopes stables du carbone organique. Les résultats suggèrent des épisodes de réchauffement permettant l’installation de la mangrove dans le Bassin Arctique dans un contexte climatique déjà chaud. Dans les Territoires du Nord-Ouest, les résultats minéralogiques suggèrent l’existence de fluctuations locales des sources détritiques contrôlées par la tectonique et/ou l’eustatisme et qui peuvent se superposer à l’enregistrement climatique. / The Palaeogene is a period of major climate system disturbances, especially marked by climatic optima recognized in both continental and marine environments. In the context of current global warming, the study and understanding of this period of strong climate fluctuations and transition between a greenhouse and an icehouse world is a major issue. Numerous studies have been conducted on low and mid latitudes, while only few studies focus on high latitudes. In this study, Paleocene-Eocene deltaic successions are used to study the response of the Arctic system to global events, the Paleogene climatic optima (PETM, ETM2, EECO and the Azolla event) and attempt to respond to these questions: did the basin have a specific response to global climate stimuli? Are there coupling / decoupling mechanisms between the dynamics of the Arctic basin and the global ocean? This study is based on multiproxies analysis: bulk and clay mineralogy, Rock Eval pyrolysis, palynology, palynofacies and stable isotopes of organic carbon. The results suggest warming episodes allowing the installation of mangroves in the Arctic Basin in an already warm climate. In the Northwestern Territories, mineralogical results suggest local fluctuations in detritic sources controlled by tectonics and / or eustatism and may overlap with the climate record.

<p> The prime objective is to define and characterize the various coastal environments in the Canadian Arctic Archipelago. The research, Hhich utilizes both secondary source information and actual field observations, takes into account coastal morphology, beach profile, sediment types, sea ice conditions, tidal range, depth of the frost table and wave energy. From a total of twelve coastal divisions based on the criteria of coastal morphology, tidal conditions and length of open water season, five have been chosen as t he basic coastal environ ments of the Arctic Archipelago. They are as follows: the Arctic Coastal Plain, the Ice Shelf, the Fiord environment, the High Straight coastal environment, and the Ridge and Valley coastal environment. Field observations within the last three environments provided additional evidence for the divisions and observations on the beach and nearshore characteristics at five selected locations. </p> / Thesis / Master of Science (MSc)

The Sub artic regions are becoming increasingly important due to the effects of climate change. In northern Sweden, thawing of permafrost has led to significant increases in annual minimum flows in several catchments. This has led to studies of groundwater flow, responses to precipitation and runoff, and subsurface connectivity of springs on slopes. However, there remains a limited understanding of the interplay between surface flow and subsurface flow in the hillslopes of subarctic region. There is a need to better understand the flow pathways and connectivity of groundwater flows within the slopes. This study aims to analyze the interactions between surface flow and subsurface flow on an Sub artic mountainside. Utilizing tracer experiments and a hydrological model, the complex dynamics governing water movement within this intricate system have been studied.  Tracer experiments affirmed the hydraulic connection between hillslope and spring. The spring's response to tracer injection hinted at dominant preferential flow paths within the regolith layer's base. Nonetheless, only 40% mass recovery raised queries about factors affecting the flow in the hillslope. Thus, in this project, a model was developed using Advanced Terrestrial Simulator (ATS) to examine the dominant flow processes and evaluate the influence of various hydrogeology parameters and fluid flow properties on tracer movement. The results highlight the dominance of subsurface flows occurring close to the surface. The parameter sensitivity analysis conducted in the study showed that roughness coefficient and permeability significantly influenced specific pathways and directions that water, and tracers took as they moved through the hillslope's subsurface layers and regolith.  However, the model has limitations, such as neglecting the lateral variations of the subsurface material, seasonal freeze-thaw processes and the simplified representation of the slope and catchment. The results of this study show the need for utilizing more field-based methodologies and further refinement of the modeling approach to improve our understanding of hydrologic processes in high latitude areas.

Dans le contexte des changements climatiques, les écosystèmes marins arctiques sont confrontés à des modifications environnementales accélérés, dont les conséquences sur les communautés biotiques sont encore débattues. La diminution du couvert de glace, l’augmentation de la turbidité et des apports d’eau douce vont affecter les producteurs primaires arctiques, avec des effets en cascade sur un processus-clé de ces écosystèmes : la relation trophique entre producteurs primaires et consommateurs benthiques (à laquelle se réfère généralement l’expression « couplage pélagos-benthos »). L’étude directe de ces interactions complexes n’est pas aisée dans ces milieux. Le modèle biologique des bivalves filtreurs peut permettre de contourner ces problèmes en remplissant une fonction d’ « intermédiaire » pour la compréhension de ces processus écologiques. Parmi les avantages de ce modèle d’étude, il y a tout d’abord le fait que ces organismes enregistrent au sein de leur coquille, dans les couches de biocarbonates, certaines dynamiques de leurs environnements. Les informations contenues dans ces « bioarchives » sont interprétées grâce aux méthodes de la sclérochronologie et de la sclérochimie et concernent une fenêtre temporelle correspondante à la vie des individus (de quelques années à plus que 500 ans). Un autre avantage de ce modèle biologique est que, s’agissant d’organismes qui sont des consommateurs primaires, l’étude de leur régime alimentaire peut apporter des éléments sur la relation trophique avec les producteurs primaires. Avec les méthodes de l’écologie trophique, en particulier les acides gras et les isotopes stables, l’étude des tissus permet d’obtenir des informations sur les sources assimilées à l’échelle de quelques semaines/mois. L’objectif de cette thèse est de tester le potentiel des bivalves Astarte moerchi (complexe borealis) comme modèle biologique pour l’étude des écosystèmes marins arctiques. Pour ce faire, une approche couplée est utilisée combinant l’analyse de la coquille par les méthodes de la sclérochronologie et de la sclérochimie (ratios élémentaires) et l’analyse des tissus par les méthodes de l’écologie trophique (acides gras, isotopes stable du carbone et de l’azote, isotopes du carbone sur acides gras individuels). Deux populations actuelles d’Astarte moerchi ont été étudiées dans deux fjords présentant des caractéristiques environnementales contrastées : le Young Sound au Nord-Est du Groenland (considéré comme fjord « arctique ») et le Kongsfjorden à l’Ouest de l’Archipel du Svalbard (considéré comme site « sub-arctique »). L’étude des tissus d’A. moerchi a permis de mettre en évidence la plasticité trophique de cette espèce, avec des différences dans les sources d’alimentation de deux populations liées aux dynamiques locales de production primaire. L’étude de la coquille d’A. moerchi a permis de : a) corroborer l’hypothèse de la formation annuelle des stries de croissance, confirmant la longévité de cette espèce pouvant atteindre 150 ans ; b) montrer l’intérêt potentiel de l’étude des ratios élémentaires dans les biocarbonates et en particulier du ratio Barium sur Calcium (Ba/Ca), qui pourrait être relié aux efflorescences phytoplanctoniques et c) montrer que les conditions environnementales contrastées du site arctique et sub-arctique se traduisent dans des patrons de croissance coquillère différents. Des perspectives pour l’utilisation ultérieure de ce modèle en écologie sont discutées. Pour conclure, une réflexion épistémologique est amorcée sur la spécificité du modèle biologique d’étude des bivalves filtreurs. En opposition à une notion plus classique d’ « organisme modèle » utilisée en biologie expérimentale, nous proposons que les bivalves filtreurs (à l’instar d’autres « bioarchives » comme les arbres, des coraux et des algues corallines) appartiennent à une catégorie de modèles biologiques qu’on pourrait qualifier « in situ » et qui semble être spécifique à la discipline écologique. / In the context of climate change, Arctic marine ecosystems are affected by rapid environmental modifications, whose effects on biotic communities are still debated. The sea-ice decline and the increase in freshwater inputs and turbidity are likely to impact Arctic primary producers, with cascade effects on a key-process in those ecosystems: the trophic relationship between primary producers and benthic consumers (generally referred as “pelagic-benthic coupling”). The direct study of such complex interaction is not straightforward in the Arctic. The biological model of filter-feeding bivalves offers the possibility to get around these problems, allowing to study those ecological processes indirectly. Among the advantages of this model, there is first of all the fact that these organisms record in their shell, in the carbonate layers, some dynamics of their environments. The information recorded in such “bioarchives” are interpreted through the methods of sclerochronology and sclerochemistry and relate to a time window corresponding to the organism lifespan (from some years to more than 500 years). Given that these organisms are primary consumers, another advantage of this biological model is that the study of their diet can provide information about the trophic relationship with primary producers. With the methods of trophic ecology, especially fatty acids and stable isotopes, the study of the tissues allows the investigation of sources assimilated at a timescale of weeks/months.The main objective of this thesis is to test the potential of bivalves Astarte moerchi (borealis complex) as a biological model for the study of marine Arctic ecosystems. A coupled approach is used to combine shell analysis by the methods of sclerochronology and sclerochemistry (elemental ratios) and tissue analysis by the methods of trophic ecology (fatty acids, carbon and nitrogen stable isotopes, compound-specific carbon stable isotopes on individual fatty acids). Two living A. moerchi populations have been studied in two fjords presenting contrasted environmental conditions: Young Sound in North-East Greenland (considered as “Arctic” site) and Kongsfjorden in the West coast of the Svalbard Archipelago (considered as a “sub-Arctic” site). The study of the tissues of A. moerchi allowed to show the trophic plasticity of this species, with differences in food sources of the two populations linked to local primary production dynamics. The analysis of the shell of A. moerchi allowed to: a) corroborate the hypothesis of annual growth lines formation, thus confirming the longevity of this species that can attain 150 years; b) show the potential interest of the analysis of elemental ratios and particularly the ratio between Barium and Calcium (Ba/Ca), which could be relied to phytoplanktonic blooms and c) show that contrasted environmental conditions in the Arctic and sub-Arctic sites result in different shell growth patterns. Some perspectives for the further use of this model study in ecology are discussed. To conclude, an epistemological reflection is sketched about the specificity of the biological model study of filter-feeding bivalves. In contrast to the classical notion of “model organism” used in experimental biology, we suggest that filter-feeding bivalves (as well as other “bioarchives” like trees, corals and coralline algae) belong to a category of biological models that could be named “in situ” and seems specific to the ecological discipline.

Social robots are becoming more and more common in our everyday lives. In the field of conversational robotics, the development goes towards socially engaging robots with humanlike conversation. This project looked into one of the technical aspects when recognizing speech, videlicet speech activity detection (SAD). The presented solution uses a convolutional neural network (CNN) based system to detect speech in a forward azimuth area. The project used a dataset from FestVox, called CMU Artic and was complimented by adding recorded noises. A library called Pyroomacoustics were used to simulate a real world setup to create a robust system. A simplified version was built, this model only detected speech activity and a accuracy of 95%was reached. The finished model resulted in an accuracy of 93%.It was compared with similar project, a voice activity detection(VAD) algorithm WebRTC with beamforming, as no previous published solutions to our project was found. Our solution proved to be higher in accuracy in both cases, compared to the accuracy WebRTC achieved on our dataset. / Sociala robotar blir vanligare och vanligare i våra vardagliga liv. Inom konversationsrobotik går utvecklingen mot socialt engagerande robotar som kan ha mänskliga konversationer. Detta projekt tittar på en av de tekniska aspekterna vid taligenkänning, nämligen talaktivitets detektion. Den presenterade lösningen använder ett convolutional neuralt nätverks(CNN) baserat system för att detektera tal i ett framåtriktat azimut område. Projektet använde sig av ett dataset från FestVox, kallat CMU Artic och kompletterades genom att lägga till ett antal inspelade störningsljud. Ett bibliotek som heter Pyroomacoustics användes för att simulera en verklig miljö för att skapa ett robust system. En förenklad modell konstruerades som endast detekterade talaktivitet och en noggrannhet på 95% uppnåddes. Den färdiga maskinen resulterade i en noggrannhet på 93%. Det jämfördes med liknande projekt, en röstaktivitetsdetekterings (VAD) algoritm WebRTC med strålformning, eftersom inga tidigare publicerade lösningar för vårt projekt hittades. Det visade sig att våra lösningar hade högre noggrannhet än den WebRTC uppnådde på vårt dataset. / Kandidatexjobb i elektroteknik 2020, KTH, Stockholm