Dissertations / Theses on the topic 'Topographie – Rome'
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Perrin-Macé, Françoise. "Recherche sur les arbres fondateurs exemplaires à Rome." Thesis, Paris, EPHE, 2015. http://www.theses.fr/2015EPHE4076/document.
Full textBefore the founding of Rome by Romulus, oak, fig tree and dogwood were part of various tree species growing on the territory of Rome. In the history of the origins of the city, the oak of Aeneas already presaged the destinies of Rome to whom the lupercal fig tree will give body, it was the dogwood which illustrated the creation and election of Rome. The tree, or rather the shrub, was a material sign for political, social and religious meanings of the acts of Romulus in his threefold role as provider of wealth by the gathering of heterogeneous people, warrior who was given a place surrounded by forests, a veritable territory centered on a city, Rome, and deified King. Three symbolic notions common to the three founding trees crosses : the notion of an origin of the territory and the people that was based on an ancient pre-Roman, Greek and/or Italic ; the idea that these legendary trees had been involved in acts of fundation and creation of a people ; finally the close relationship between a mythical Rome and that of historical times, according to the tripartite scheme established by G. Dumézil. The Tradition on the founding of Rome was not exempt from Greek influence but had appropriated this Greek ancestry to make a proper Roman history. The oak, which meant the end of Trojan Aeneas journey, the fig tree which, with the wolf, had helped to save Romulus and the dogwood, pushed at the top of the Palatine Hill, in the middle of Roma Quadrata, the three trees symbolized the place of the birth of Rome, a city that gave a town and a civilization to a grouping of diverse populations before scattered in the woods
Mahieu, Vincent. "Temps, espace et identités : recherches sur les coexistences religieuses dans la Rome tardo-antique (312-410)." Thesis, Paris Sciences et Lettres (ComUE), 2018. http://www.theses.fr/2018PSLEP029.
Full textThe fourth century AD is admittedly a major turning point in the history of Western Europe. The evolution of Christianity from the status of a marginal culture within a religious group to that of a cultural and normative pole within society constitutes an important transition specific to Late Antiquity. This transition from margin to norm started from the social frameworks of time and space, acting as strong identity markers. The great amount of evidence from the "Vrbs", its position as historical capital, as its recognized status as important city for the development of Christianity, make it a specific research framework. This study, which focuses on the sharing of time and space between the victory of the Milvius Bridge (312) and the sack of Alaric (410), reconstructs the organization of the times in the city and explores the mechanisms behind the development of the calendar structure of the Church within this urban space (part 1). On the basis of a catalogue that brings up to date the "LTVR(S)", this study rebuilds the polytheistic topography and scrutinizes the material inscription of the Christian cult on the Roman territory (part 2). On the basis of these cross-sectional analyses and case studies (part 3), it also attempts at understanding the modes of religious co-existence and interaction within a society. The results point towards a sense of continuity rather than breaking. This dissertation reveals a model that favours integration and conformation strategies to the Roman dynamics in the sharing of time and space. It argues in favour of a religious cohabitation mostly peaceful led by a common identity investment focused on the "Romanitas"
Fassbender, Andreas. "Untersuchungen zur Topographie von Grabstätten in Rom von der späten Republik bis in die Spätantike /." Köln : [s.n.], 2005. http://catalogue.bnf.fr/ark:/12148/cb400559455.
Full textFourmond, Catherine. "Recherches sur la topographie chrétienne des cités de l'Afrique antique (à l'exception de Carthage)." Paris 4, 2003. http://www.theses.fr/2003PA040148.
Full textIn order to understand the topography of Christian buildings within Towns of North Africa in Late Antiquity, we chose, on the basis of archeological informations, to point to practical and daily life of the Christian or Christian community. Since then, many questions came up : what process leads to the decision and how is the location chosen within the urban network ? Did the Christian community have the opportunity of such a choice ? What could be the practical implications of its devotional life ? Could the churches built in such locations be in harmony with Christian worship so as to contribute to its blooming ? and so on and so forth. Apparently churches did not change drastically the urban environment except in their very premices and even so in a quite neutral way. Thus, for example, if a church is built on a street, we can consider that it comes to alters the urban organisation. On the other hand, when it re-uses an old building such as a temple or thermae, neglected or inactive, we noticed that the implantation was taking place inside the building whereas most of the time the ouside appearance was left untouched : then the city's image was respected in its monumental components. According to a certain number of observations set out from this research, it finaly occurs to us that though christianism settled in the heart of urban daily life, for it does not mean necessarily a concern for ostentatious visibility or systematic search for an " architecture of power ". On the opposite it gives us the impression that Christian's presence is deeply rooted in daily life just as the other inhabitants of the city they fully belonged to
Prim, Joëlle. "Histoire de l'Aventin : Limites, fonctions urbaines et rôle symbolique d'un quartier romain (IIe siècle avant - 49 après J.-C.)." Paris 8, 2012. http://www.theses.fr/2012PA083465.
Full textThe Aventine, the southernmost hill of ancient Rome, played a particular role in the City’s history and the shaping of its urban space. Nevertheless, the only exhaustive study of the Aventine is still the monograph by Alfred Merlin published by the BEFAR in 1906, even though substantial progress has been made since then, both in the theoretical approach to the urban history of Rome and in the methods of analysing the available sources on the subject. Moreover, this corpus of sources has been considerably enriched, especially through the work accomplished over the last twenty years by the various archaeological departments in charge of excavating the hill. The combination of these facts justifies a new study of this urban space. However, the aim of this research is not to rewrite a complete history of the Aventine Hill. Focusing on the period from the 2nd century B. C. Until the inclusion of the hill within the Pomerium in 49 A. D. , this study offers a status report on current scientific thinking and the new documentation available on the subject. Also, and more importantly, it aims to refresh our way of viewing the specificities of this urban space by posing new questions. Identify the factors that define the boundaries of the Aventine, study its socio-urban characteristics and compare them with the plebeian image of the hill that developed during this period, and study the religious topography and some of the specific functions that took place in and around its shrines: these are the principal themes structuring this discontinuous history of the Aventine
Santi, Valentina de. "Topographie pittoresque : art et technique militaires dans la mise en oeuvre du « Plan-relief du Siège de Rome »." Paris, EHESS, 2016. http://www.theses.fr/2016EHES0107.
Full textThe tradition of plans-reliefs, an ancient practice of Fortifications Engineers, whose origin lie in the reign of Louis XIV, was revitalized at the turn of the eighteenth century. This moment is the starting point of our research which tackles in particular the second quarter of th nineteenth century by focusing on two main figures: Adolphe Leon Leymonnerye, topographer artist of the gallery, and Jean- Jacques Augustin Marie Leblanc, a topographe serving the Places Etrangeres du Genie and a member of the Geological Society of France Both are involved in the construction of the plan-relief du Siege de Rome (1849-1852), which constitutes the case study of our research. We question then the way by which plans-reliefs, a models, exceeding the geometric system, reveal a multiplicity of scales and a mixture of references, which reflect the complexity of approaches of the knowledge of the real. In particular, we will emphasize the continuity and the evolutions of the notion of picturesqu within the context of reflections on topographical maps language, of the emergence of geological knowledge and of the appropriation of space by the national history during th nineteenth century. Building on the heuristic role of the image within the analysis of historica geography as well as on the epistemological renewal of the history of cartography, our research lies in the axis of reflexions of the historical approach which proposes to question the method of observation and construction underlying visual devices and their role in the process of knowledge construction
Torrisi, Valentina. "La Casa di Livia al Palatino. Un nuovo studio topografico." Thesis, Sorbonne université, 2018. http://www.theses.fr/2018SORUL122.
Full textThis thesis show that there is cause to question the extension and the different construction phases of the House of Augustus and in particular, of a part of it, the House of Livia as recently Irene Iacopi and Giovanna Tedone published an important paper about the accuracy of dating of the construction phases in the Augustan palace. Currently I established four construction phases for the House of Livia, the first one can be dated around 70 B.C. because of the similarities between the type of its walls and the ones of Pompey’s theatre, built between 61 and 55 B.C. and also because of a tile’s stamp found in the substructure of the south-east complex, dated by Margareta Steinby around 79 B.C. Because of the underground remains I suppose the existence at the first floor, actually destroyed, of an oecus corinthius in the south-east side and a basilica in the north-west side of the building. The three more phases should have been linked to Augustus, who bought several houses on the Palatin hill in order to build a Hellenistic palace styled complex. La Rocca demonstrated that the decoration of the House of Livia started from 40 BC due to the presence of Cleopatra near Rome between 46 and 44 BC. The queen very probably was accompanied by artists working for her in the royal Alexandrian workshops. It is likely, therefore, that the Roman elite would have replicated the styles and tastes of Caesar and Cleopatra
Moreau, Hélène. "Entre deux rives-entre deux ponts : l'île Tibérine de la Rome antique : histoire, archéologie, urbanisme des origines au Vè siècle après J.C." Thesis, Lille 3, 2014. http://www.theses.fr/2014LIL30047/document.
Full textTiber Island, between Vrbs and Trastevere, is one of the topographical characteristic of the site ofRome. Its history and fame begun with the arrival of Asclepius, the Greek god of medicine brought fromEpidauros. No study went thoroughly back over the history and topography of this significant component ofroman scenery since the monograph written by M. Besnier in the early years of the 20th century. Nowadayscurrent developments in archeological research and new perspectives in roman topography throw new light onmany issues. This thesis aims to go back over the development, the town-planning but also the place the Tiberislet occupied in town. In this perspective, this is not just about grasping the island as a place but also as acomponent of roman landscape and urban development. Indeed Tiber island can only be apprehended at firstwithin its natural surroundings then its urban one. The island shows a high concentration of cults, which begunwith the advent of Aesculapius, who made it the “sacred island” thus permanently marking its topography.However, studying its planning and administration reveals it was real district too, with all the features as regardsarrangements and activities. At first on the fringe of the city, its integration to the city begun in the 2nd centuryBC until it was established as uicus Censori by the augustean reform. During the Imperial period, the island isalready seen as an old-settled part of the city, which will only know new changes with the banning ofpolytheistic cult
L’isola Tiberina, tra l’Vrbs e il Trastevere, costitui una delle particolarità topograficedel sito di Roma. La sua storia, ma supratutto la sua notorietà, comincia quando arriveEsculapio, il dio greco della medicina, importato da Epidauro. Dalla monografia di M.Besnier, pubblicata all’inizio del XX secolo, nessuna studia è tronata su questo soggetto inmodo approfondito. Ora, l’attualità della ricerca archeologica e le nuovi approci in topografiaromana getteno nuova luce su molte problematice. Duncque, questo lavoro propone diriesaminare l’evoluzione, gli insediamenti ma anche il ruolo dell’isola nella città. Inquest’ottica, non si considera solo l’isola in quanto luogo ma come elemento del paesaggio etdel urbanismo romani. Perché si posse capire l’isola Tiberina unicamente nel suo ambiante,innazi tutto naturale, poi urbano. L’isola si define soprattuto per la concentrazione di culti sulsuo territorio, iniziata dall’arrivo di Esculapio che l’insedia nel suo ruolo d’ « isola sacra » emarca definitavamente la sua topografia. Tuttavia, la studia del suo spazio et della suaamministrazione mostra che era anche un vero quartiere, di cui aveva tutti gli attributi inmateria di strutture ed attività. Inizialmente fuori dalla città, la sua intergrazione nelfunzionamento della città comincia dal II secolo a.C. fino alla riforma di Auguto che laistituisce uicus Censori. All’epoca imperiale, l’isola ostituisce già parte integrante della cittàda molto tempo, che conoscerà nuove trasformazioni col divieto del culto politeisti.Parole chiavi
Ribouillault, Denis. "Paysage et pouvoir : les décors topographiques à Rome et dans le Latium au XVIe siècle." Paris 1, 2006. http://www.theses.fr/2006PA010570.
Full textLocatelli, Lauriane. "La toponymie et l'ethnonymie de la Pisidie antique (XIIIe s.a.C. ; début IVe s.p.C.)." Thesis, Bourgogne Franche-Comté, 2017. http://www.theses.fr/2017UBFCC014.
Full textPisidia, a mountainous region in southwestern Asia Minor, is a real toponymic conservatory of Anatolian culture and languages. Our thesis deals with the toponymy and ethnonymy of Pisidia and the persistence of Anatolian languages in the toponymy of the region. Toponymy and ethnonymy reveal the territorial control of each settlement, whether it be Anatolian population or exogenous settlements (mainly Greek and Roman). Indeed, by choosing the language used to create the name of the place or the people, we learn more about the region. After having produced a catalog of toponyms and ethnonyms of the Pisidia classified by types and after having discussed their origin using linguistic arguments for each one, we study the Greek presence and the Roman colonies by considering the successive domination in regard to toponymy. Several themes were discussed : the question of the control of the region during the Hellenistic period, the Seleucid foundations, as well as the Roman colonies founded by Augustus. Then we focus on the identity of the Pisidians, studying the question of their origin and the topoi associated with them. The continuities and territorial cleavage of Pisidia are discussed before a toponymic panorama showing a linguistic classification and a semantic classification of toponyms based on the semantic repository (water, relief, vegetation, etc.). Most of the place names are descriptive and refer to elements of the landscape
HERNANDEZ, DAVID RAY. "STUDIES IN ROMAN REPUBLICAN TOPOGRAPHY: THE SERVIAN WALL AND THE PORTA TRIUMPHALIS." University of Cincinnati / OhioLINK, 2004. http://rave.ohiolink.edu/etdc/view?acc_num=ucin1077839141.
Full textKanekar, Aarati. "The geometry of love and the topography of fear : on translation and metamorphosis from poem to building." Diss., Georgia Institute of Technology, 2000. http://hdl.handle.net/1853/23286.
Full textKim, Yeonjoo 1977. "The role of topography in the emergence of African savannas." Thesis, Massachusetts Institute of Technology, 2003. http://hdl.handle.net/1721.1/44515.
Full textThesis (S.M.)--Massachusetts Institute of Technology, Dept. of Civil and Environmental Engineering, 2003.
The coexistence of trees and grasses in savannas are not well understood even though savannas occupy a wide area of West Africa. In this study, a hypothesis is proposed to investigate the question of how trees and grasses coexist in a region. The hypothesis suggests that the variation in elevation leads to the variation in soil moisture, which in turn can explain the coexistence of trees and grasses in savannas. To test this hypothesis, experimental simulations are performed using biospheric model, IBIS, and distributed hydrologic model, SHE. We, first, estimate the amount of rainfall required for trees and grasses under a certain atmospheric condition. Here, the variation of rainfall is prescribed to force a similar variation of soil moisture. A 30% decrease in rainfall is sufficient to simulate grasses at 9°N. A 100% increase in rainfall is sufficient to simulate trees at II°N. However, even with a five fold increase in rainfall, the model fails to simulate trees at 13°N. To study the influences of topography explicitly, a distributed hydrologic modeling is performed using SHE. The results suggest that the variation of the depth to water table induced by the varying elevation is highly correlated with the variation of soil moisture. Consequently, an asynchronous coupling of SHE and IBIS is designed to investigate the stated hypothesis. The coupling is performed by modifying IBIS to include the groundwater table as a boundary variable. The modified IBIS simulates both trees and grasses according to a different water table boundary condition in natural savannas of 11°N. The shallow water table of valleys allows the growth of trees, and the deep water table of hills allows the growth of grasses. The simulations in this study suggest that the variability of soil moisture resulting from the topographic variation can be a determinant of savanna ecosystems. Moreover, grasslands in 13°N cannot be changed into forests only by adjusting soil moisture. It suggests that the role of soil moisture can be significant to dictate the vegetation type only in a certain window characteristic of savanna climate.
by Yeonjoo Kim.
S.M.
McLauglin, Todd Robert. "The role of eph/ephrins in the development of retinotectal topography /." Diss., Connect to a 24 p. preview or request complete full text in PDF format. Access restricted to UC campuses, 2001. http://wwwlib.umi.com/cr/ucsd/fullcit?p3031944.
Full textSkopovi, Ivan 1976. "The role of background flow variations in stratified flows over topography." Thesis, Massachusetts Institute of Technology, 2006. http://hdl.handle.net/1721.1/35632.
Full textIncludes bibliographical references (leaves 89-91).
As the atmosphere and oceans feature density variations with depth, the flow of a density-stratified fluid over topography is central to various geophysical and meteorological applications and has been studied extensively. For reasons of convenience and mathematical tractability, the majority of theoretical treatments of stratified flow over a finite-amplitude obstacle assume idealized background flow conditions, namely constant free-stream velocity and either a homogeneous or two-layer buoyancy-frequency profile. In this work, a numerical model is developed that accounts for general variations in the buoyancy-frequency profile far upstream and the presence of unsteadiness in the free-stream velocity. The model employs a second-order projection method for solving the Euler equations for stratified flow over locally confined topography in a horizontally and vertically unbounded domain - the flow configuration most pertinent to atmospheric applications - combined with absorbing viscous layers at the upper and lateral boundaries of the computational domain. Using this model, a study is first made of the effect of variations in the buoyancy frequency on the generation of mountain gravity waves.
(cont.) Balloon measurements reveal that, apart from a sharp increase (roughly by a factor of 2) at the so-called tropopause, atmospheric buoyancy-frequency profiles often feature appreciable oscillations (typical wavelength 1-2 kni). It is found that such short-scale oscillatory variations can have a profound effect on mountain waves owing to a resonance mechanism that comes into play at certain wind speeds depending on the oscillation length scale. A simple linear model assuming small sinusoidal buoyancy-frequency oscillations suggests, and numerical simulations for more realistic flow conditions confirm, that the induced gravity-wave activity under resonant conditions is significantly increased above and upstream of the mountain, causing transient wave breaking (overturning), similarly to resonant flow of finite depth over topography. The effect of temporal variations in the free-stream velocity is then explored for a range of amplitudes and periods typical of those encountered in the field. The simulations reveal that transient disturbances resulting from such variations can be significant, particularly in the nonlinear regime, and steady states predicted on the assumption of uniform wind may not be attainable.
by Ivan Skopovi.
Ph.D.
Frost, Natalie Jane. "The role of topographic complexity in the structure and dynamics of rocky shore communities." Thesis, University of Southampton, 2001. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.342648.
Full textChoi, Octavio Seung. "The role of BDNF in the development of retinotectal topographic projections in the chick /." Diss., Connect to a 24 p. preview or request complete full text in PDF format. Access restricted to UC campuses, 2001. http://wwwlib.umi.com/cr/ucsd/fullcit?p3027043.
Full textMulryan, Michael James John. "The religious topography of late antique Rome (AD 313-440) : a case for a strategy." Thesis, University College London (University of London), 2008. http://discovery.ucl.ac.uk/1444463/.
Full textO'Hare, Peter. "The role of inner pore topography on osteoblast response in hydroxyapatite scaffolds." Thesis, University of Ulster, 2006. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.431548.
Full textKneafsey, Maria Anne. "The city boundary in Late Antique Rome." Thesis, University of Exeter, 2017. http://hdl.handle.net/10871/34000.
Full textIgneczi, Adam. "Greenland Ice Sheet hydrology and dynamics : the role of surface and basal topography." Thesis, University of Sheffield, 2018. http://etheses.whiterose.ac.uk/22746/.
Full textCessi, Paola. "On the role of topography and of boundary forcing in the ocean circulation." Thesis, Massachusetts Institute of Technology, 1987. http://hdl.handle.net/1721.1/55311.
Full textIncludes bibliographies.
by Paola Cessi.
Ph.D.
Booth, Adam, and Adam Booth. "The Role of Deep-Seated Landslides in Landscape Evolution: Quantitative Modeling and High-Resolution Topographic Analysis." Thesis, University of Oregon, 2012. http://hdl.handle.net/1794/12534.
Full textNettleton, Benjamin. "The role of vegetation-topographic interactions in a barrier island system: island migration in a changing climate." VCU Scholars Compass, 2018. https://scholarscompass.vcu.edu/etd/5572.
Full textPerea, Virginia Nicolas. "The role of weather and topography in the airborne dispersal of particulate matter in Kent." Thesis, University of Greenwich, 2011. http://gala.gre.ac.uk/7133/.
Full textKordinak, Jacqueline T. "Saint Peter's Needle: The Vatican Obelisk and Its Importance in Renaissance Rome." Ohio University / OhioLINK, 2013. http://rave.ohiolink.edu/etdc/view?acc_num=ohiou1375191561.
Full textFlexas, Sbert Maria del Mar. "Mesoscale variability of the northern current in the gulf of lions and the role of bottom topography." Doctoral thesis, Universitat Politècnica de Catalunya, 2003. http://hdl.handle.net/10803/6386.
Full textBaroclinic instability is viewed as a possible mechanism to explain the generation of the Northern Current meanders. The analytical model of Tang (1975) predicts the development of unstable waves of wavelength (> 60 km) and periods compatible with the 7.5 day band recorded with current meter devices. The higher frequency band of 3.5 days is out of the frequency range predicted by the classical baroclinic instability theory and it is discussed as a restriction of quasi-geostrophic theory.
Barotropic instability is studied using a laboratory model of a -westward' jet flowing over the lower half of the continental slope, which considers dynamic similarity with the Northern Current. The laboratory model is cross-validated with a corresponding numerical model. Jet instabilities of currents similar to the Northern Current (i.e. westward jets) occur at the edges of the jet, showing a clear meandering tendency over the mid-slope. Westward currents of Ro = 0.1 -- 0.2 develop instabilities of wavelengths (50 -- 75 km) similar to those observed from SST images, with periods (3.3 -- 3.8 days) compatible with the 3.5 days period band recorded with HFFE current meters.
The laboratory and numerical experiments have reproduced westward jets (as the Northern Current), but also eastward jets, in order to have a full approach to better understand the role of the bottom topography on barotropic instabilities. The slope current instabilities are successfully explained by the Marcus and Lee theory (1998) of jets on a beta plane. This theory is valid for westward flows with Ro > 0.1 and for eastward flows with Ro > 0.2 (jets of the so-called Regime II flows in this thesis), and it states that the instabilities of each shear layer of the barotropic jet take the appearance of a Kelvin-Helmholtz-like pattern, associated with a Rossby wave (of topographic origin in our case). According to this theory, the differences between eastward and westward jets rely on the disposition of the Rossby waves --at the centre of the current in eastward flows and at the edges of the jet in westward currents. Jets over a sloping bottom with small Rossby numbers (Ro < 0.1 for westward jets; Ro < 0.2 for eastward jets) show a flow pattern (the so-called Regime I in this thesis) that has common characteristics for eastward and westward flows. In these -small'-Ro flows, Kelvin-Helmholtz-like instabilities dominate, whereas Rossby waves are too weak to produce any major difference between jets flowing in eastward or westward direction. This occurs when the topographic influence, assumed proportional to the Ro number of the jet, is small.
The differences between eastward and westward slope currents observed in this work (and similar observations of jets on a beta-plane from previous works) are explained in this thesis by a simple scheme based on conservation of potential vorticity, considering there are two main components in balance: the shear-induced vorticity and the topographically induced vorticity. The signs of these two components are determined by the relative direction of the flow with respect to the inclination of the bottom topography. Once the critical Rossby number is overpassed so that the topographic effects are important (Ro > 0.1 for westward jets; Ro > 0.2 for eastward jets), conservation of potential vorticity tends to enhance vortices at the centre of eastward jets --eastward jets show meandering at the jet core. In westward jets, potential vorticity conservation is responsible of enhancing vortices at each edge of the jet. Thus, westward jets (as the Northern Current) are broad and meandering occurs at the jet edges.
In Ro > 0.1 westward flows (i.e. Regime II westward jets) a topographic Rossby wave appears over the shelf break. This result is likely observed because of the specific topography used in this work --a continental slope and a continental shelf separated by a shelf break, producing a strong change in ambient potential vorticity. Numerical simulations reveal that this Rossby wave is triggered by the slope current. This topographic Rossby wave is a robust pattern, since it is independent of the position of the current over the slope, the shape of the velocity shear profile of the jet, and the jet width. Although this type of wave could not be inferred from the HFFE field data, it could be a focus of study in further field experiments. It also needs further analytical consideration.
The general conclusion extracted from this thesis that tries to explain the mesoscale variability associated to the Northern Current is that both baroclinic and barotropic instability could explain part of the oceanic observations. As a consequence, mixed barotropic-baroclinic instability (which occurs at wavelengths which are between those corresponding to pure barotropic and pure baroclinic instability) is thought to play an important role on the observed mesoscale variability. The resulting wavelength would depend on the relative strength of both mechanisms.
Wright, Kierra D. "Chiral polymer surface-cell interaction: understanding the role of chirality & surface topography on polymer-cell interactions." DigitalCommons@Robert W. Woodruff Library, Atlanta University Center, 2012. http://digitalcommons.auctr.edu/dissertations/436.
Full textKim, Ah-Ram. "Experimental and theoretical investigation of the role of nanofibrous topography feature size on adhesion of Candida albicans." Thesis, Virginia Tech, 2015. http://hdl.handle.net/10919/73314.
Full textMaster of Science
Bumsted, Keely Maureen. "The role of opsin expression in the development of photoreceptor topography and synapses in the fetal primate retina /." Thesis, Connect to this title online; UW restricted, 1996. http://hdl.handle.net/1773/5679.
Full textLegg, Michael Antonio. "An Investigation of the Role of Silica Substrate Topography on the Tailing and Broadening of Basic Compounds in HPLC." Diss., The University of Arizona, 2007. http://hdl.handle.net/10150/193792.
Full textBisht, Gautam. "Satellite-based estimates of net radiation and modeling the role of topography and vegetation on inter-annual hydro-climatology." Thesis, Massachusetts Institute of Technology, 2010. http://hdl.handle.net/1721.1/60706.
Full textThis electronic version was submitted by the student author. The certified thesis is available in the Institute Archives and Special Collections.
Cataloged from student-submitted PDF version of thesis.
Includes bibliographical references (p. 229-260).
The Fourth Assessment Report of the Intergovernmental Panel on Climate Change acknowledged that the lack of relevant observations in various regions of the world is a crucial gap in understanding and modeling impacts of climate change related to hydrologic cycle. The Surface Radiation Budget (SRB) is an important component in the study of land surface processes. Existing SRB retrieval algorithms generally suffer from two major shortcomings: difficulty in dealing with cloudy sky conditions and reliance on study-site specific ancillary ground data. In this work, a framework of estimating net radiation from the MODerateresolution Imaging Spectroradiometer (MODIS) data is presented that is applicable under all-sky conditions, while solely relying on satellite data. The results from the proposed methodology are compared against several ground measurements within the United States for the entire 2006. Finally, monthly radiation maps for the Continental United States are produced. Modeling, similar to observations, is critical to the Earth Sciences and the second part of this work focuses on the impact of incorporating vegetation dynamics and topography in modeling hydro-climatology over large river basins. Land and atmosphere are coupled with each other through the exchange of heat, momentum and water at the boundary. This work involves coupling of a physically-based, fully distributed ecohydrology model with a numerical atmospheric model, using high performance computing. The ability of the ecohydrology model (in an offline mode) to accurately resolve hydro-climatic signatures and vegetation dynamics is first examined. The ecohydrology model is applied in a highly instrumented catchment, Walnut Gulch Experimental Watershed (WGEW) in Arizona, for a period of 11-years (1997-2007). The ecohydrology model is able to capture the behavior of several key hydrologic variables and vegetation dynamics within the WGEW. A series of three synthetic experiments are conducted with a coupled land-atmosphere model. The anomalies of various simulated quantities between the synthetic experiments are examined within the rainfall-soil moisture feedback hypothesis proposed by Elathir [1998]. The results from the experiments highlight the need to explicitly account for vegetation dynamics and topography within a numerical atmospheric model. The thesis concludes with a discussion of contributions, and future directions for this work.
by Gautam Bisht.
Ph.D.
Balcells, Eduardo. "I. Solubility and blend studies of nitrocellulose II. Relaxation properties of thin film coatings: the role of surface topography." Thesis, Virginia Polytechnic Institute and State University, 1988. http://hdl.handle.net/10919/80171.
Full textMaster of Science
Mukhatyar, Vivek. "Understanding the role topographical features play in stimulating the endogenous peripheral nerve regeneration across critically sized nerve gaps." Diss., Georgia Institute of Technology, 2011. http://hdl.handle.net/1853/45933.
Full textMartin, Samantha Leah. "The role of the Stoa in the topography of the ancient Athenian Agora : the Stoa Basileios, Stoa Poikile and Stoa of Zeus Eleutherios." Thesis, University of Cambridge, 2007. https://www.repository.cam.ac.uk/handle/1810/283829.
Full textHan, Guang. "The synergistic role of hierarchical macro- and mesoporous implant surface and microscopic view of enhanced osseointegration." Doctoral thesis, Stockholms universitet, Institutionen för material- och miljökemi (MMK), 2015. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-120584.
Full textAt the time of the doctoral defense, the following papers were unpublished and had a status as follows: Paper 3: In press. Paper 4: Manuscript.
Abdo, Amr. "Alexandria in antiquity: a topographical reconstruction." Doctoral thesis, Universitat Autònoma de Barcelona, 2019. http://hdl.handle.net/10803/670088.
Full textUna reconstrucción topográfica de Alejandría en la antigüedad es un intento de encontrar un camino en un laberinto arqueológico de evidencias fragmentarias (capít. II y III). A la luz de los recientes hallazgos, por lo tanto, se trata de un intento complementario a otros anteriores (Adriani 1934, 1966; Tkaczow 1993). El estudio actual, tiene en cuenta los últimos dos siglos de investigación sistemática sobre la topografía de la antigua ciudad, que tiene como objetivo: (i) un catálogo de yacimientos arqueológicos, desde la Expedición francesa (1798-9) hasta la actualidad; (ii) inferir la planta urbana y el paisaje de la ciudad en su fundación (siglo IV aC), y los subsiguientes cambios que tuvieron lugar hasta la conquista árabe de Egipto (VII dC). Por esta razón, se adopta una aproximación holística a la reconstrucción topográfica, donde la cultura material se estudia conjuntamente con el registro histórico (vol. I: texto). Vol. II de la tesis (imágenes; plantas de AutoCAD) sirven para mostrar los resultados.
A topographical reconstruction of Alexandria in antiquity is attempting to find a way through an archaeological labyrinth of fragmentary evidence. In the light of the recent discoveries, therefore, a new attempt becomes complementary to earlier ones (Adriani 1934, 1966; Tkaczow 1993). The current study, taking into account the last two centuries of systematic research into the topography of the ancient city, aims at: (i) cataloguing the archaeological sites, from the French Expedition (1798-99) to date; (ii) infer the urban plan and cityscape of the foundation (4th cent. BC), and the subsequent changes taking place to the Arab conquest of Egypt (7th cent. AD). To this end, a holistic approach to topographical reconstruction is adopted, where ‘material culture’ is studied in conjunction with the ‘historical record’ (vol. I: text). Vol. II of the thesis (plates; AutoCAD maps) serves to display the results.
Bell, Roslynne. "Power and Piety: Augustan Imagery and the Cult of the Magna Mater." Thesis, University of Canterbury. Classics and Linguistics, 2007. http://hdl.handle.net/10092/955.
Full text(5929451), Paul R. Acosta. "INTERACTIONS BETWEEN TOPOGRAPHY AND THE ATMOSPHERE:THE ROLE OF ASIAN TOPOGRAPHIES ON THE INDO-ASIAN MONSOON." 2019.
Find full textCrowther, Benjamin Miles. "Topographies of demonstration in the late Republican and Augustan Forum Romanum." Thesis, 2014. http://hdl.handle.net/2152/25786.
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Oakley, Carol. "Role of the cytoskeleton and substratum in cell topographic guidance." Thesis, 1995. http://hdl.handle.net/2429/6743.
Full text"Mesoscale variability of the northern current in the gulf of lions and the role of bottom topography." Universitat Politècnica de Catalunya, 2003. http://www.tesisenxarxa.net/TDX-1216103-124531/.
Full textNoriega, Sandra. "Role of scaffold topography and stimulation via ultrasound on the biosynthetic activity of chondrocytes seeded in 3D matrices." 2009. http://proquest.umi.com/pqdweb?did=1886658411&sid=2&Fmt=2&clientId=14215&RQT=309&VName=PQD.
Full textTitle from title screen (site viewed January 5, 2010). PDF text: xiv, 328 p. : ill. (some col.) ; 7.48 Mb. UMI publication number: AAT 3373081. Includes bibliographical references. Also available in microfilm and microfiche formats.
Yeh, Chun-Ming, and 葉峻銘. "The Role of Topography and Environmental Vertical Wind Shear in Forming the Convective Asymmetry in Typhoon Nanmadol (2011)." Thesis, 2014. http://ndltd.ncl.edu.tw/handle/4976qp.
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