Driven by the surging need for seamless connectivity, research in the wireless communication area has dramatically evolved over the years to meet the increasing demand for data rate and seamless coverage. Such evolvement concurs with a notable increase in data traffic and the widespread of data-hungry devices, thereby inflicting stringent requirements on terrestrial networks. Despite the tremendous advances achieved through the past generations of wireless systems, almost half of the world's population remains unconnected, leading to an accentuated digital divide problem. Therefore, this work invigorates a new connectivity solution that integrates aerial and terrestrial communications with a high-altitude platform station (HAPS) to promote a sustainable connectivity landscape. The connectivity solution adopted in this thesis specifically integrates terrestrial base stations with hot-air balloons under the framework of a cloud-enabled HAPS via a data-sharing fronthauling strategy. The aerial (hot-air balloons) and terrestrial base stations, grouped into disjoint clusters, coordinate their mutual transmission to serve aerial (i.e., drones) and terrestrial users. This work studies the downlink communication from the cloud-enabled HAPS to the aerial and terrestrial users under practical system considerations, namely the limited transmit power and the limited-capacity fronthaul link, per-base station. To this end, the first part of the thesis devises a specific optimization problem that maximizes the network sum-rate while accounting for system design constraints to determine the user association strategy, i.e., user to terrestrial clusters or user to air clusters, and the associated beamforming vectors. The second part of the thesis, then, designs a different resource allocations optimization problem that accounts for the fairness among the users, thus adopting a proportionally fair scheduling scheme to assign users on frequency tones to maximize the log of the long-term average rate. On this account, the work solves a handful of non-convex intricate optimization problems using techniques from optimization theory, namely, fractional programming and $\ell_0$-norm approximation. The work consequently outlines the gains realized by providing on-demand coverage in crowded and unserved areas. Moreover, the thesis illustrates the benefits of coordinating the operations of aerial and terrestrial base stations for interference management, load-balancing, and fairness measures.

Adaptation to chronic hypoxia induces endogenous cardioprotection and increases the heart resistance to ischemia/reperfusion injury. The heart mitochondria, which produce reactive oxygen species (ROS) in addition to ATP, play an important role in these processes. During ischemia/reperfusion, ROS are produced in excessive amounts and damage the cells. However, in lower concentrations, ROS are involved in the signalling pathway of cardioprotection induced by adaptation to chronic hypoxia. In the heart, two mitochondrial subpopulations have been observed, subsarcolemmal mitochondria (SSM) and intermyofibrillar mitochondria (IMFM), which differ in cell localization as well as in morphological and biochemical properties. The aim of this work was to introduce the method of SSM and IMFM isolation in our laboratory and to analyse their antioxidative capacity after adaptation to chronic hypoxia. Adult male Wistar rats were kept either under normoxic conditions or exposed to intermittent high-altitude hypoxia (IHA; 7000 m, 5 days a week/8 hours a day, totally 25 exposures). Mitochondrial subpopulations were isolated from heart left ventricle and their functionality was verified by measuring oxygen consumption and enzyme activities. The IMFM had higher oxygen consumption in comparison with SSM and activities...

Les particules d'aérosol sont importantes en raison de leurs impacts directs et indirects sur le climat. Dans la couche limite (CL), ces particules ont une durée de vie relativement courte en raison de leur élimination fréquente par dépôt humide. En revanche, lorsque les aérosols sont transportés dans la troposphère libre (TL), leur durée de vie dans l'atmosphère augmente de manière significative, ce qui les rend représentatifs de vastes zones spatiales. Dans le cadre de ces travaux de thèse, nous avons utilisé une combinaison de mesures in situ effectuées à la station PUY (Puy de Dôme, 45 ° 46 'N, 2 ° 57'E, 1465 m d'altitude), ainsi que des profils LIDAR obtenus depuis Clermont-Ferrand pour identifier les conditions de TL et caractériser davantage les propriétés physiques et chimiques des aérosols dans cette zone de l'atmosphère peu documentée. Dans un premier temps, une combinaison de quatre critères a été utilisée pour déterminer le positionnement de la station PUY en TL ou en CL. Les résultats montrent que la station est située en CL avec des fréquences allant de 50% en hiver à 97% en été. Cette classification a ensuite été utilisée pour évaluer, sur un an de mesures, les différences qui existent entre la TL et la CL en termes de caractéristiques physique (distribution en taille) et chimique (fraction non réfractaire) de l’aérosol, et vis-à-vis des concentrations en carbone suie (BC). Sur la base de cette ségrégation, nous avons observé pour la plupart des saisons que les concentrations en particules des modes Aitken et accumulation ainsi que la concentration en BC sont plus élevées dans la CL que dans la TL. Cette observation est cohérente avec le fait que la majorité des sources d’aérosol sont situées dans la CL. Au contraire, des concentrations plus élevées en particules dans les modes Aitken et accumulation (notamment organiques) et en BC sont observées en TL au printemps. Ces aérosols organiques ont été identifiés comme étant âgés / moins âgés ; ils coïncident avec la présence de fortes concentrations en sulfate et en BC et sont probablement originaires de processus de combustion de biomasse, à la suite desquels ils sont directement injectés en TL sous l’effet d’une convection thermique intense. Aucune différence significative entre les concentrations de CL et de TL n'a été observée pour les particules du mode nucléation, et ce quelle que soit la saison, ce qui suggère une source supplémentaire continue de particules du mode nucléation dans la TL en hiver et en automne. Les concentrations en particules du mode grossier sont en revanche plus élevées dans la TL que dans la CL pour toutes les saisons, et en particulier en été. Cela indique un transport longue distance efficace des grosses particules dans la TL depuis des sources lointaines (marines et désertiques), probablement favorisé par les vitesses de vent accrues dans la TL par rapport à la CL. Nous avons ensuite calculé les rétro-trajectoires des masses d'air que nous avons combinées aux estimations de hauteur de couche limite du modèle ECMWF ERA-Interim pour estimer le temps passé par les masses d’air dans la TL depuis leur dernier contact avec la CL, et pour évaluer l'impact de ce paramètre sur les propriétés des aérosols. Nous avons observé que même après 75 heures sans aucun contact avec la CL, les aérosols de la TL conservent les propriétés spécifiques du type de masse d'air auquel ils appartiennent. Ce manuscrit présente également une étude des mesures simultanées au PUY et à une station urbaine à basse altitude, AtmoAura. Les résultats montrent que lorsque le PUY est en TL, les concentrations des PM1 (particules de diamètre inférieur à 1 µm) sont plus faibles au PUY qu’à AtmoAura, ce qui confirme notre classification. Lorsque le PUY est en CL, la composition en aérosol est similaire pour les deux sites, ce qui a permis de quantifier la contribution de la pollution urbaine locale issue de la ville de Clermont-Ferrand. / Aerosol particles are important due to their direct and indirect impacts on climate. Within the planetary boundary layer (BL), these particles have a relatively short lifetime due to their frequent removal process by wet deposition. When aerosols are transported into the free troposphere (FT), their atmospheric lifetime increases significantly, making them representative of large spatial areas. In this work, we use a combination of in situ measurements performed at the high altitude PUY (Puy de Dôme, 45°46’ N, 2°57’E, 1465 m asl) station, together with LIDAR profiles at Clermont-Ferrand for characterizing FT conditions, and further characterize the physical and chemical properties of aerosol in this poorly documented area of the atmosphere. First, a combination of four criteria was used to identify whether the PUY station lies within the FT or within the BL. Results show that the PUY station is located in BL with frequencies ranging from 50% during the winter, up to 97% during the summer. Then, the classification is applied to a year-long dataset of particle size distribution and NR-PM1 data’s to study the differences in particle physical and chemical characteristics and BC concentrations between the FT and the BL. Based on this segregation, we observed higher concentrations in the BL compared to FT for BC, Aitken and accumulation mode particle concentrations for most seasons, as expected from larger sources originating from the surface. However, BC, Aitken mode, accumulation mode and organic aerosols concentrations were higher in the FT compared to BL during spring. These organic aerosols were identified as aged/less aged, and were correlated with sulphate and BC and we suspect that the higher concentrations of particles observed in the FT compared to BL during spring originate from direct injection of BB aerosols in the FT through strong heat convection. No significant difference between the BL and the FT concentrations was observed for the nucleation mode particles for all seasons, suggesting a continuous additional source of nucleation mode particles in the FT during winter and autumn. Coarse mode particle concentrations were found higher in the FT than in the BL for all seasons and especially during summer. This indicates an efficient long-range transport of large particles in the FT from distant sources (marine and desert) due to higher wind speeds in the FT compared to BL. For FT air masses, we used 204-h air mass back-trajectories combined with boundary layer height estimations from ECMWF ERA-Interim to assess the time they spent in the FT since their last contact with the BL and to evaluate the impact of this parameter on the aerosol properties. We observed that even after 75 h without any contact with the BL, FT aerosols preserve specific properties of their air mass type. This manuscript is also presenting a study of simultaneous measurements at PUY and an urban low altitude station AtmoAura. Results show that when the PUY is influenced by FT air masses, the PM1 species are lower at the PUY compared to AtmoAura confirming our classification. When the PUY is predicted to lay within the BL, the aerosol composition was similar among the two sites for several species, which allowed for a quantification of the local urban pollution contribution for the species enhanced within the city of Clermont-Ferrand.

Pygmy tarsiers (Tarsius pumilus) of Central Sulawesi, Indonesia are the only species of tarsier known to live exclusively at high altitudes. This study was the first to locate and observe multiple groups of this elusive primate. This research tested the hypothesis that variation in pygmy tarsier behavior and morphology correlates with measurable ecological differences that occur along an altitudinal gradient. As a response to decreased resources at higher altitudes and the associated effects on foraging competition and energy intake, pygmy tarsiers were predicted to exhibit lower population density, smaller group sizes, larger home ranges, and reduced sexually selected traits compared to lowland tarsiers. Six groups containing a total of 22 individuals were observed. Pygmy tarsiers were only found between 2000 and 2300 m, indicating allopatric separation from lowland tarsiers. As expected, the observed pygmy tarsiers lived at a lower density than lowland tarsier species, in association with decreased resources at higher altitudes. The estimated population density of pygmy tarsiers was 92 individuals per 100 ha, with 25 groups per 100 ha. However, contrary to expectation, home range sizes were not significantly larger than lowland tarsier home ranges, and average NPL was smaller than those of lowland tarsiers. The average home range size for the observed pygmy tarsiers was 2.0 ha, and the average nightly path length (NPL) was 365.36 m. Pygmy tarsiers exhibited a nonrandom, clumped distribution near forest edges. While insect abundance and biomass were found to decrease as altitude increased, insect abundance and biomass was higher along anthropogenic edges. Thus, tarsiers within the study area may mitigate the decreased availability of insects at high altitudes by remaining close to forest edges, which in turn may be related to smaller than expected home range sizes. Further, estimates of pygmy tarsier abundance may be inflated because of increased insect abundance along anthropogenic edges. Contrary to the prediction for smaller group sizes as a response to feeding competition, the observed pygmy tarsiers lived in relatively large groups with multiple adult males. However, in support of the prediction for energetic constraints on body proportions, the observed pygmy tarsiers did not exhibit sexually selected traits. The pygmy tarsiers exhibited low sexual dimorphism and small relative testes mass, a trend opposite from lowland tarsier species, which may indicate a constraint on the development of those traits. Considered together, these results suggest that the observed pygmy tarsiers have adapted to life in an environment with limited resources. Future studies should explore the possible contributing effects of seasonality and topography.

Les sources d’émissions de polluants organiques persistants (POP) dans l’atmosphère sont relativement bien connues. Une fois dans ce compartiment sous formes gazeuse et/ou particulaire, ces composés sont transportés à plus ou moins longue distance puis éliminés en fonction des conditions météorologiques par dépôts secs (aérosols) ou humides (pluie et neige). L’impact des POP est planétaire, tous les milieux de l’environnement sont touchés et les milieux aquatiques de montagne ne sont pas épargnés. Plusieurs études ont rapportées la présence de Polychlorobiphényles (PCB) et d’Hydrocarbures Aromatiques Polycycliques (HAP) sur des lacs d’altitude européens où l’atmosphère est l’unique source de pollution. A ce jour, très peu d’études ont été menées en milieux de montagne pour comprendre et identifier les mécanismes de transfert à l’interface entre l’air et l’eau. Ces travaux de thèse sont ainsi focalisés sur les échanges de POP à l’interface air-eau en milieu aquatique de montagne. Dans le but de définir le rôle de l’atmosphère sur ces milieux et de calculer des flux de POP, deux systèmes hydriques distincts ont été étudiés : un lac d’altitude (Lac de la Muzelle, Oisans) et une rivière alpine (Arc, vallée de la Maurienne). Deux familles de POP ont été ciblées pour leurs différentes propriétés physico-chimiques : les HAP et les PCB. Pour l’étude de ces milieux de montagne parfois difficile d’accès, une stratégie d’échantillonnage passive a été choisie. Les systèmes d’échantillonnage employé ont été améliorés, développés au laboratoire ou utilisés tel quel pour échantillonner distinctement toutes les formes de POP dans l’air (gaz, particules, dépôts secs et humides) et dans l’eau (phase dissoute et particulaire). Une comparaison des systèmes d’échantillonneurs atmosphériques passifs a été réalisée pour définir le plus fiable et représentatif. Ces études de transferts air-eau ont été conduites sur le lac d’altitude pendant deux périodes estivales (2014 et 2015) et un suivi de deux ans a été réalisé (2014 à 2016) sur la rivière alpine.Le rôle de l’atmosphère en période estivale a pu être ainsi défini sur le lac d’altitude et des flux d’échanges de polluants à l’interface ont pu être calculés. La rivière alpine étant un système hydrique dynamique plus complexe pour l’étude des transferts air-eau et la quantification de flux, un suivi spatio-temporel de la contamination a tout d’abord été réalisé le long de la rivière et une première approche de calcul de flux de polluants à l’interface a été appliquée. / Atmospheric sources of persistent organic pollutants (POPs) are relatively well known. Once in this compartment under both gas and particulate forms, these compounds are carried on more or less long range. Then, pollutants are eliminated by dry (aerosol) or wet (rain, snow) depositions according to meteorological conditions. The global planetary distribution of POPs affects all environments and mountain aquatic environments are not spared. Several studies on European high altitude mountain lakes have reported the presence of Polychlorinated Biphenyls (PCBs) and Polycyclic Aromatic Hydrocarbons (PAHs). In these remote areas, the atmospheric compartment is the unique source of pollution. Few studies were conducted in order to understand and identify transfer mechanisms at the air-water interface in mountain. So, this thesis focused on POP exchanges at the air-water interface. In order to characterize atmospheric influence on aquatic compartment and calculate pollutant fluxes, two separate water systems were studied: a high altitude lake (Muzelle lake, Oisans) and an alpine river (Arc, Maurienne valley). Two POP families were targeted for their different physicochemical properties: PAHs and PCBs.In these mountain environments with limited access and energy, passive sampling strategy was chosen. Samplers were improved, developed in the lab or used to distinctly collect all POP forms in the air (gas, particulate, dry and wet depositions) and water (dissolved, particulate). A comparison of different atmospheric passive samplers was conducted to define the most reliable and representative. The air-water transfer studies were realized on the high altitude lake over two summer periods (2014 and 2015) and over a two years monitoring (2014 to 2016) in the alpine river. So, the atmospheric role on the alpine lake in summer was defined and air-water flux exchanges were calculated. As the alpine river is a more complex water system for the air-water transfers study and quantification, in a first time a space-time contamination monitoring was conducted along the river and a first approach was applied to calculate pollutant fluxes at the interface.

In the archaeological literature, mountains are often portrayed as the boundaries between inhabited spaces. Yet occupying high elevations may have been an adaptive choice for ancient peoples, as rapidly changing elevations also offer variation in climate and resources over a relatively small area. So what happens, instead, if we put mountain landscapes at the center of our analyses of prehistoric seasonal rounds and ecological adaptation? This Ph.D. argues that, in order to understand any landscape that includes mountains, from the Alps to the Andes, one must include the ecology and archaeology of the highest elevations. Specifically, I base my findings on new fieldwork and lithic collections from the Absaroka and Beartooth Mountains in the Greater Yellowstone Ecosystem (GYE) of the Rocky Mountains, which was a vital crossroads of prehistoric cultures for more than 11,000 years. I include five interlocking analyses. First, I consider the impacts of anthropogenic climate change on high elevation cultural resources, focusing on the diminishing resiliency of ancient high elevation ice patches and the loss of the organic artifacts and paleobiological materials they contain. Second, I create a dichotomous key for chronologically typing projectile points, suggesting a methodological improvement for typological dating in the GYE and for surface archaeology more broadly. Third, I use obsidian source data to consider whether mountain people were a single, unified group or were represented by a variety of peoples with different zones of land tenure. Fourth, I consider high elevation occupation in both mountain ranges as part of the seasonal round, using indices of diversity in tool types and raw material to study how the duration of those occupations changed through time. And, finally, I test the common contention that ancient people primarily used mountains as refugia from extreme climatic pressure at lower elevations. Ultimately, I find that, in both mountain ranges, increased high elevation activity is most highly correlated with increased population, not with hot, dry climatic conditions. In other words, the mountains were more than simply refugia for plains or basin people to occupy when pressured by climatic hardship. In addition, between the Absarokas and the Beartooths the evidence suggests two different patterns of occupation, not a monolithic pan-mountain adaptation. These results demonstrate the potential contributions of surface archaeology to our understanding of prehistory, and have important implications for the way we think about mountain landscapes as peopled spaces in relation to adjacent lower-elevation areas.

Wireless operation, near-field or far-field, is a core functionality of any mobile or autonomous system. These systems are battery operated or most often utilize energy scavenging as a means of power generation. Limited access to power, expected long and uninterrupted operation, and constrained physical parameters (e.g. weight and size), which limit overall power harvesting capabilities, are factors that outline the importance for innovative low-power approaches and designs in advanced low-power wireless applications. Low-power approaches become especially important for the wireless transceiver, the block in charge of wireless/remote functionality of the system, as this block is usually the most power hungry component in an integrated system-on-chip (SoC). Three such advanced applications with stringent power requirements are examined including space-based exploratory remote sensing probes and their associated radiation effects, millimeter-wave phased-array radar for high-altitude tactical and geological imaging, and implantable biomedical devices (IMDs), leading to the proposal and implementation of low-power wireless solutions for these applications in SiGe BiCMOS and CMOS and platforms.

Ce travail a été consacré à l’étude non invasive de la circulation pulmonaire normale par mise en œuvre de l’échocardiographie Doppler. <p>En intégrant les mesures obtenues dans une approche physiopathologique, et en exploitant les nouvelles possibilités d’échocardiographes portables, techniquement performants, nous avons analysé les effets d’un inhibiteur de la phosphodiestérase-5 et d’une prostacycline, pour tenter d’en identifier d’éventuels effets introtropes intrinsèques, nous avons exploré le concept de réserve vasculaire pulmonaire comme facteur limitant de l’aptitude aérobie et indice potentiel d’une atteinte vasculaire pulmonaire précoce, et obtenu des résultats préliminaires permettant d’identifier une hypertension artérielle pulmonaire (HTAP) latente. Nos principaux résultats peuvent être résumés comme suit :<p>1. Chez le sujet sain, en normoxie ou dans un modèle expérimental d’HTAP induite par l’inhalation d’un mélange gazeux hypoxique, le sildenafil per os ou l’epoprostenol par voie intraveineuse, à des doses utilisées en clinique pour le traitement de l’HTAP, améliorent les indices de la fonction ventriculaire droite en proportion de leurs effets vasodilatatoires pulmonaires, sans effets inotropes intrinsèques détectables.<p>2. La consommation d’oxygène maximale du sujet sain augmente en raison directe de son volume capillaire pulmonaire (calculé à partir de sa capacité de diffusion pour l’oxyde nitrique et le monoxyde de carbone) et en raison inverse de sa résistance vasculaire pulmonaire, non seulement en altitude, mais aussi au niveau de la mer. Ce résultat suggère qu’une plus grande réserve vasculaire pulmonaire est propice aux efforts aérobiques intenses, probablement par moindre postcharge ventriculaire droite.<p>3. Des mesures réalisées chez un petit nombre de sujets suggèrent que la distensibilité vasculaire pulmonaire, calculée à partir d’une relation débit-pression vasculaire pulmonaire, est typiquement réduite chez des porteurs asymptomatiques de la mutation BMPR2, qui est actuellement le facteur de risque le plus élevé connu de l’HTAP. La mutation BMPR2 pourrait aussi être associée à une réactivité vasculaire pulmonaire accrue à l’hypoxie. <p>Nos résultats suggèrent indirectement que l’échocardiographie Doppler, de repos ou de stress, pourrait être davantage développée dans la mise au point de patients à risque d’HTAP./<p><p>Novel advances in echocardiography offer the opportunity to reliably characterize pulmonary circulation in terms of pressure-flow relationship, and to better understand the coupling of right ventricular (RV) function with normal and abnormal pulmonary hemodynamics. Moreover, when combined with the measurement of pulmonary capillary blood volume, this renewed methodological approach may help to understand the concept of pulmonary vascular reserve as a limiting factor of exercise capacity and potential sensitive marker of early vascular disease.<p><p>In the present work we used a model of hypoxic pulmonary vasoconstriction to analyse the effects of two targeted therapies of pulmonary arterial hypertension (PAH) on the RV function. We showed that the beneficial effects of these drugs are mainly driven by a decrease in RV afterload and not an enhanced myocardial inotropic state. Whether this is transposable to abnormal RV-arterial coupling in PAH patients remains to be investigated.<p><p>Echocardiography may be useful to explore the pulmonary vascular reserve as an important limiting factor of exercise capacity. We showed that a higher pulmonary vascular reserve, defined by a decreased PVR and increased lung diffusing capacity, allows for an improved aerobic exercise capacity (as assessed by a higher peak oxygen consumption), at a lower ventilatory cost, at sea level and at high altitude. <p><p>Stress echocardiography may detect an abnormal pulmonary vasoreactivity. We showed that asymptomatic relatives of patients suffering from idiopathic pulmonary arterial hypertension, and who carry a bone morphogenetic protein receptor type 2 mutation (BMPR2) present with a decreased pulmonary vascular distensibility and an enhanced pulmonary vasoreactivity to hypoxia, which are identifiable by echocardiography examination. However, the predictive value of these findings is not known. <p><p>Thus echocardiography may represent, in experienced and dedicated hands, a noninvasive, safe, widely available, applicable at the bed-side as well as in extreme environment (e.g. high altitudes), less expensive alternative for the evaluation of the pulmonary circulation, either by the interrogation of pressure-flow relationship (stress echocardiography), by the investigation of the right ventricle global and regional function in relation to its afterload (standard and Tissue Doppler Imaging), or by a combined approach with the measurement of lung diffusing capacity (DLNO / DLCO) to assess the pulmonary vascular reserve.<p><p>The present data are encouraging for further development and implementation of echocardiography for the detection, but also the diagnosis and follow-up of patients with pulmonary hypertension.<p><p> / Doctorat en Sciences médicales / info:eu-repo/semantics/nonPublished

Tato práce se zabývá problematikou zavedení a provozu nadzvukových business jetů. V dnešní době se v civilní letecké přepravě, po ukončení provozu Concordu, žádná nadzvuková letadla nevyskytují. V dnešní době existuje mnoho projektů a organizací, které se zabývají znovuzavedením nadzvukových letounů do civilního letectví a soustředí se převážně na business jety. Hlavní otázkou je, zda je vůbec vhodné, či rozumné se k tomu typu dopravy znovu vracet. Existuje hodně problémů, které toto komplikují. Tyto letouny způsobují příliš velký hluk, mají obrovskou spotřebu paliva a musí řešit nadměrné emise, létají ve vysokých výškách ve kterých může docházet k problémům s přetlakováním kabiny, navigací, radioaktivním zářením apod. Navíc zákaz supersonických letů nad pevninou letové cesty omezuje a prodlužuje. Současně vznikající projekty navíc nedosahují tak velkého doletu jako klasické moderní bussjety, což způsobuje, že se nadzvukové business jety se na delších tratích stávají neefektivní. I přes tyto problémy, je víceméně jisté, že k zavedení nadzvukových business jetů dojde během následujících 10 - 15 let, i kdyby to měla být jen otázka jisté prestiže velmi bohatých lidí.