Studies of internal gravity waves in the earth's upper atmosphere are of considerable interest. These waves play a very important role in the dynamics of the mesosphere and lower thermosphere (ML T) region where they can transfer large amounts of energy and momentum from the lower atmosphere via wave saturation and dissipation. In particular, small-scale short-period (50ms"1) . Another unusual characteristic of "frontal events" is an apparent reversal in contrast of the wave structures as imaged in the hydroxyl (OH) emission (peak altitude- 87 km) when compared with the oxygen (OJ) "green line" (557.7 nm) emission (peak altitude -96 km) that can sometimes occur. In one isolated case, observed from Haleakala, Hawaii, the bright wave crests in the OH emission appeared to propagated through a dark structureless sky, whereas in the OI emission the same waves appeared to propagate into a bright sky, leaving an apparently depleted emission in its wake. Recent theoretical studies based on noble measurements have shown that frontal events may be due to a "bore-like" intrusion that raises the OJ (557. 7 nm) layer by a few km and at the same time depresses the OH layer by a similar amount. However, studies of fronts and bores in the ML T region are exceptionally rare. I have discovered and analyzed 16 frontal events from image data recorded at Bear Lake Observatory, Utah ( 41.6°N, 111.6°W), over the past four years. I have investigated some of their properties such as their horizontal wavelengths, horizontal phase speeds, observed periods, and their directions of motion. In addition, I have made comparative measurements of their relative intensities in the OH and OI emissions. These studies provide the first "extensive" data set on such events detailing their morphology and dynamics and should provide important information necessary for a deeper understanding of their occurrence frequency and properties.

La hausse des températures et les modifications du régime des précipitations affectent les écosystèmes particulièrement fragiles des régions arctiques et subarctiques et ont des conséquences socio-économiques pour les populations locales. La perception et l'évaluation des opportunités et des risques qui y sont associés, dépendent des moyens de subsistance, des normes, des valeurs et des représentations du monde des individus qui y sont confrontés.La perception du climat est culturellement et socialement construite. Cette perception varie dans le temps et dans l'espace et, parfois même, diffère parmi différents groupes sociaux en fonction des valeurs et des modes de représentation du monde. Pour toutes ces raisons, nous avons non seulement étudié certains phénomènes météorologiques mais aussi intégré le cadre culturel, politique et historique dans lesquels ils s'inscrivent. Nous avons analysé l'environnement et le climat – et par extension, les événements météorologiques à forts impacts – comme des objets socio-culturels afin de mieux comprendre à la fois leurs impacts mais aussi leurs perceptions par les habitants. Ce travail se situe à la croisée de ces chemins, en confrontant l'observation, et donc les changements, et la perception qu'en ont différents acteurs, en considérant deux régions distinctes, les mers nordiques et la République de Touva.Dans une première partie, nous avons analysés l'impact des Polar Lows, d'intenses cyclones de méso-échelle qui se développent sur les mers libres de glace de l'Arctique pendant l'hiver, sur les régions côtières du nord de la Norvège. Ces systèmes sont associés à des vents de surface forts avec bien souvent des rafales qui peuvent être très violentes (Heinemann et Claud, 1997). Les conditions en mer lors du passage d'un PL peuvent s'avérer dangereuses avec des fortes vagues, des précipitations neigeuses brutales et du blizzard. Ces événements météorologiques extrêmes représentent un véritable risque pour les activités maritimes et côtières de la région, notamment pour le transport maritime, la pêche et les plateformes pétrolières et gazières offshore. En effet, les nouvelles zones libres de glace offrent de multiples opportunités économiques dans ces régions, en particulier en mer de Barents. Or dans le même temps, le recul de la banquise élargit mécaniquement les régions de formation des PLs.Dans une seconde partie, nous avons regardé les impacts du changement climatique et des événements météorologiques sévères en République de Touva. La République de Touva se localise entre 49°5 et 53°5 N en latitude, 88°5 et le 99°E en longitude, c'est par conséquent une région subarctique très méridionale. Le climat y est extrêmement continental et les précipitations ont tendance à être faibles en raison de la faible teneur en humidité dans l'air froid. La plupart du territoire est caractérisé par une végétation forestière de taïga ou de steppe semi-aride. Au cours du XXème siècle, la région a connu des changements socio-économiques majeurs, parfois brutaux, avec notamment le passage d'une société communiste à l'économie planifiée à une économie de marché au début des années 1990. Malgré ces récents bouleversements, les pasteurs nomades (chevaux, vaches, yaks, moutons, chameaux) en Touva occidentale et les chasseurs-cueilleurs éleveurs de rennes en Touva orientale, vivent toujours en étroite relation avec l’environnement naturel. Les populations autochtones de Touva, confrontées à un changement rapide de la société et à des changements globaux causés par certaines politiques régionales et nationales contemporaines, avec notamment l’expansion de l'industrie minière et par le développement de mégaprojets (complexe hydroéléctrique, construction d'une voie chemin de fer), offrent des points de vue variés, en fonction de leurs modes de vie, sur les changements environnementaux qu'ils observent et leurs impacts sur leurs activités quotidiennes. / The perception of the climate is culturally and socially constructed. For this reason, we have studied some weather events integrating the cultural, political and historical contexts in which they occur.In a first part, we analyzed the impact of Polar Lows, intense mesocyclones that develop over ice-free Arctic seas during winter time, on coastal regions of Norway. The passage of PL can provoke dangerous sea conditions with strong waves, sudden snowfall and blizzard. This phenomenon may represent a risk to maritime and coastal activities in the region, particularly for shipping, fishing and oil and gas offshore platforms.In a second part we studied the impacts of climate change and severe weather events in the Republic of Tuva. Tuva is a very southern subarctic region. Its climate is extremely continental and precipitation tend to be low due to the low moisture content in the cold air. During the twentieth century, the region has experienced major socio-economic changes, sometimes brutal, including the transition from a communist and planned economy to a market economy in the early 1990. Despite these recent changes, pastoralists in western Tuva (horses, cows, yaks, sheep, camels) and reindeer herders in eastern Tuva, still live in close contact with the natural environment. Indigenous peoples of Tuva are facing global changes caused by certain contemporary regional and national policies, including the expansion of the mining industry and the development of mega projects. They offer different points of view, describing environmental changes and their impact on their daily activities.

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Mass mortality events (MMEs) are die-offs that result in increased carrion biomass and sometimes the impairment of functional roles. Concurrently, several vulture species are declining. Carrion is a basal resource in ecosystems and its recycling by vultures is considered an ecosystem service. However, the consequences of simultaneously increasing carrion loads and declining vulture populations are unknown. I developed a theoretical framework predicting that, with increasing carrion biomass, carrion food web diversity would increase horizontally and vertically, respectively increasing and decreasing carrion recycling efficiency. Using a manipulative experiment, I investigated the role of bottom-up and top-down forces affecting plant communities during an MME. I selected 5 sites to establish 6 treatments crossing different levels of carrion addition and nutrient addition, and control with vertebrate scavenger and herbivore access. I transplanted six cherrybark oak (Quercus pagoda) seedlings to each plot, protecting half of them from herbivory. Carrion biomass shifted dominance of plant functional groups to favor annual plants, an effect reduced by scavenger access. Herbivore access affected plant community response to carrion and limited growth and survival of transplanted seedlings regardless of treatment. Nutrient addition did not affect plant communities, growth, and survival suggesting that MME effects on plants are likely mediated primarily by top-down forces. To determine if behavioral plasticity of vultures affects carrion recycling efficiency, I monitored turkey (Cathartes aura) and black (Coragyps atratus) vulture behavior. Both species increased group size, but only black vultures increased individuals feeding per group and activity overlap between species increased with increasing carrion biomass. As a result, estimated carrion consumption by vultures increased with carrion biomass suggesting behavioral plasticity may alleviate some of the effects of vulture declines on carrion recycling. Finally, vultures compete with invertebrate scavengers so declining vultures may release their populations to compensate for the loss. However, in one of my experiments, variation in vulture visitation was negatively correlated with the abundance of blowflies parasitized by Entomophthora sp. Our observations may suggest that vultures were more likely mediating carrion decomposition affecting parasitism, which may limit blowflies from compensating for declining vultures.

Adaptation to climate change requires a careful evaluation of the infrastructure performance under extreme events in a changing climate. Earthen levees are critical infrastructure systems, which play a vital role to the country’s safety, environment, and economic security. The main objective of this study is to quantitatively assess the integrity of earthen levees subject to extreme precipitation and flooding under a changing climate. A multi-disciplinary modeling framework is developed and applied to two earthen levees, Elkhorn and Sherman Island levees, in California. Patterns of extreme precipitation and flooding are obtained for the study areas under current and future climate. A nonstationary framework is employed, which accounts for climate change-induced changes in statistics of future extreme precipitation. The precipitation and flooding data are then applied as hydraulic loads in a set of fully coupled stresslow finite element simulations to determine the factory of safety (FOS) and probability of failure (Pf) of the levees for different scenarios. The Pf values are used to develop fragility curves, which can provide valuable tools for risk assessments. The modeling framework is used to study three distinct yet interrelated problems. The first problem assesses the performance of the Elkhorn levee using historical and projected future precipitation patterns. The results show that Pf increases 3%-12% under the projected extreme precipitation compared to the baseline scenario. The second problem involves quantifying the effects of changes in future streamflow on the fragility behavior of the Elkhorn levee considering multiple modes of failure. For the cases examined, incorporating future floods leads to up to 23% reduction in FOS and 95% increase in Pf. The third problem assesses the fragility behavior of the Sherman Island levee under compound flooding (induced by coastal, fluvial and pluvial processes), an overlooked aspect in the majority of the existing flood hazard analyses. Results show that considering compound flooding leads to 22% and 30% reductions in FOS for 2- and 50-year recurrence intervals, respectively. Using the projected future pluvial flooding increases Pf by 13%. Findings of this research suggest that risk assessments based on historical records can significantly underestimate the levee’s Pf in a changing climate.

The current study examined the relationships between Major Depressive Disorder, negative life events, perceived parenting style, perceived family environment and Disruptive Behavior Disorders, specifically Conduct Disorder, Oppositional Defiant Disorder, and Attention-Deficit/Hyperactivity Disorder, in adolescent participants, (N = 381). Results indicated that those factors, with the exception of authoritarian parenting, correlated positively with symptoms consistent with Disruptive Behavior Disorders. In addition, the overall effect of those factors predicted symptoms consistent with Disruptive Behavior Disorders more strongly than each risk factor in isolation. In conclusion, results indicated that negative life events and symptoms consistent with Major Depressive Disorder mediated the effects of perceived parenting and perceived family environment on symptoms consistent with Disruptive Behavior Disorders.

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