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1
Surface modes in physics. Berlin: Wiley-VCH, 2001.
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2
Sernelius, B. Surface modes in physics. Berlin: Wiley-VCH, 2001.
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3
Al-Jibouri, Khalid Ibrahim G. Electromagnetic linear surface guided modes and plasmon couplers. Salford: University of Salford, 1991.
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4
Grama, Nicolae, Cornelia Grama, and Ioan Zamfirescu. Riemann surface approach to natural modes: Exotic resonant states. Hauppauge, N.Y: Nova Science Publishers, 2011.
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5
Lawrence, Richard T. Experimental inquires into collective sea state modes in deep water surface gravity waves. Monterey, Calif: Naval Postgraduate School, 1992.
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6
Choudhari, Meelan. Long-wavelength asymptotics of unstable crossflow modes, including the effect of surface curvature. Hampton, Va: Langley Research Center, 1994.
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7
Kang, Jinsheng. Influences of surface quality on the rolling contact fatique behaviour of ceramics: An investigation into the relationship between the finishing process, surface quality and failure modes of advanced Si3N4 rolling elements. Poole: Bournemouth University, 2001.
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8
Sernelius, Bo E. Surface Modes in Physics. Wiley & Sons, Incorporated, John, 2011.
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9
Sernelius, Bo E. Surface Modes in Physics. Wiley-VCH Verlag GmbH, 2005.
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10
Chen, Lin, Fei Gao, Wei E. I. Sha, and Zhi Ning Chen, eds. Recent Progress in Surface Electromagnetic Modes. Frontiers Media SA, 2021. http://dx.doi.org/10.3389/978-2-88966-984-4.
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11
Center, Langley Research, ed. Long-wavelength asymptotics of unstable crossflow modes, including the effect of surface curvature. Hampton, Va: National Aeronautics and Space Administration, Langley Research Center, 1994.
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12
Center, Langley Research, ed. Long-wavelength asymptotics of unstable crossflow modes, including the effect of surface curvature. Hampton, Va: National Aeronautics and Space Administration, Langley Research Center, 1994.
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13
Long-wavelength asymptotics of unstable crossflow modes, including the effect of surface curvature. Hampton, Va: National Aeronautics and Space Administration, Langley Research Center, 1994.
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14
Center, Langley Research, ed. Evaluation of Ti-6A1-4V surface treatments for use with a polyphenylquinoxaline adhesive. Hampton, Va: National Aeronautics and Space Administration, Langley Research Center, 1986.
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15
Gariglio, S., M. S. Scheurer, J. Schmalian, A. M. R. V. L. Monteiro, S. Goswami, and A. D. Caviglia. Surface and Interface Superconductivity. Edited by A. V. Narlikar. Oxford University Press, 2017. http://dx.doi.org/10.1093/oxfordhb/9780198738169.013.7.
Повний текст джерелаАнотація:
This article focuses on surface and interface superconductivity, a pivotal area of mesoscopic superconductivity. It discusses theoretical ideas regarding superconductivity in the 2D limit; pairing symmetry in systems with broken inversion symmetry and in the presence of Rashba spin–orbit interaction; and coupling of substrate phonon modes to layer electronic states to induce or enhance the superconducting condensate. It also reviews the experimental ongoing efforts to fabricate, characterize, and measure these systems, with particular emphasis on oxide materials. Superconductivity in two dimensions, in ultra-thin metals on Si(111), and at the LaAlO3/SrTiO3 interface is examined. The article concludes with an analysis of theoretical propositions aimed at realizing and testing novel superconducting states occurring at the surfaces and interfaces.
16
Zeitlin, Vladimir. Instabilities in Cylindrical Geometry: Vortices and Laboratory Flows. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198804338.003.0011.
Повний текст джерелаАнотація:
Vortex solutions in cyclo-geostrophic equilibrium are described and their geostrophic and ageostrophic barotropic and baroclinic instabilities are studied along the lines of Chapter 10. Special attention is paid to centrifugal instability which, as the inertial instability of jets, is due to modes trapped in the anticyclonic shear in the vortex, and has asymmetric counterparts. Saturation of this instability is shown to exhibit some specific patterns. Instabilities of intense hurricane-like vortices are analysed and shown to be sensitive to fine details of the vortex profile. Nonlinear saturation of such instabilities exhibits typical secondary meso-vortex structures, and leads to intensification of the vortex. Special attention is paid to instabilities in laboratory flows in rotating cylindrical channels. Classification of these instabilities is given, and their nature, in terms of resonances between different wave modes, is established. Rigid-lid and free-surface configuration with topography are considered and compared with experiments.
17
Read, Nick D. Fungal cell structure and organization. Edited by Christopher C. Kibbler, Richard Barton, Neil A. R. Gow, Susan Howell, Donna M. MacCallum, and Rohini J. Manuel. Oxford University Press, 2017. http://dx.doi.org/10.1093/med/9780198755388.003.0004.
Повний текст джерелаАнотація:
Human pathogenic fungi produce three basic ‘cell’ types: hyphae, yeast cells, and spores. The organization and subcellular structure of these different cell types and their modes of growth and formation are reviewed. Growth and form is the consequence of how new cell surface is formed. This is generated by the delivery of vesicles to the surface which provides new membrane and the enzymes for cell wall synthesis. To generate these various cell types, the pathway of vesicle secretion to the surface has to be carefully regulated. These vesicles have to be transported through the cell by the cytoskeleton, and in filamentous cells these vesicles accumulate at a supply centre called the Spitzenkörper before docking and fusion with the hyphal apex. Ultimately, membrane is also endocytosed and recycled behind actively expanding regions of the fungal surface. These various processes are described and particular emphasis is given to the structural and organizational features of fungal cells that play roles in their pathogenesis and virulence.
18
Onuf, Nicholas Greenwood. Transitional Figures: Edmund Husserl, Emile Durkheim, the Fabian Society. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780190879808.003.0010.
Повний текст джерелаАнотація:
Discussion of modernism tends to be confined to specific modes of expression—architecture, art, literature, music, photography. Generalizing nonetheless, modernism works by breaking the surface and working through layers. There is no empty space; there are only ensembles of relations, stable or shifting, linked by purpose. Form follows function; complexity induces functional differentiation. A distinctively modernist philosophy must dig beneath, or get inside, the questions: what is it possible to think, and ask? What is doing the work called thinking? Husserl’s phenomenology is the one philosophical program of its time directed to these questions and their implications for social existence. Durkheim expressly developed a functionalist perspective for social theory. Looking below the surface, he found social complexity subject to the differentiation of ever more specialized institutions performing more specialized tasks. Closely affiliated with London modernists, the Fabian Society began the task of assessing global administration in just these terms.
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Vaez-Zadeh, Sadegh. Vector Control. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198742968.003.0003.
Повний текст джерелаАнотація:
The chapter begins with a description of the scalar control of PMS motors. The fundamentals of PMS motor vector control (VC) are then presented with an eye on the analogy with DC motor operating principles. The VC of surface-mounted permanent magnet pole motors and interior permanent magnet (IPM) motors are presented in various reference frames. Current and voltage operating limits are incorporated into the control systems. Flux control modes of operation of PMS motors together with the corresponding control means in different reference frames are also presented in detail, as a particular feature of this book. These include maximum torque per ampere (MTPA) control, maximum torque per voltage control, and unity power factor control. Finally, loss minimization control by offline and online strategies is elaborated after presenting the method of motors loss reduction and the PMS motor loss modeling.
20
Krishnamurti, T. N., H. S. Bedi, and V. M. Hardiker. An Introduction to Global Spectral Modeling. Oxford University Press, 1998. http://dx.doi.org/10.1093/oso/9780195094732.001.0001.
Повний текст джерелаАнотація:
This book is an indispensable guide to the methods used by nearly all major weather forecast centers in the United States, England, Japan, India, France, and Australia. Designed for senior-level undergraduates and first-year graduate students, the book provides an introduction to global spectral modeling. It begins with an introduction to elementary finite-difference methods and moves on towards the gradual description of sophisticated dynamical and physical models in spherical coordinates. Topics include computational aspects of the spectral transform method, the planetary boundary layer physics, the physics of precipitation processes in large-scale models, the radiative transfer including effects of diagnostic clouds and diurnal cycle, the surface energy balance over land and ocean, and the treatment of mountains. The discussion of model initialization includes the treatment of normal modes and physical processes, and the concluding chapter covers the spectral energetics as a diagnostic tool for model evaluation.
21
El Refaie, Elisabeth. Visual Metaphor and Embodiment in Graphic Illness Narratives. Oxford University Press, 2019. http://dx.doi.org/10.1093/oso/9780190678173.001.0001.
Повний текст джерелаАнотація:
This study uses the analysis of visual metaphor in 35 graphic illness narratives—book-length stories about disease in the comics medium—in order to re-examine embodiment in traditional Conceptual Metaphor Theory (CMT) and propose the more nuanced notion of “dynamic embodiment.” Building on recent strands of research within CMT, and drawing on relevant concepts and findings from other disciplines, including psychology, phenomenology, social semiotics, and media theory, the book develops the argument that the experience of one’s own body is constantly adjusting to changes in one’s individual state of health, sociocultural practices, and the activities in which one is engaged at any given moment, including the modes and media that are being used to communicate. This leads to a more fluid and variable relationship between physicality and metaphor use than many CMT scholars assume. For example, representing the experience of cancer through the graphic illness narrative genre draws attention to the unfathomable processes going on beneath the body’s visible surface, particularly now that digital imaging technologies play such a central role in the diagnosis and treatment of the disease. This may lead to a reversal of conventional conceptualizations of knowing and understanding in terms of seeing, so that vision itself becomes the target of metaphorical representations. A novel classification system of visual metaphor, based on a three-way distinction between pictorial, spatial, and stylistic metaphors, is also proposed.
22
Simpson, Gerry. The Sentimental Life of International Law. Oxford University Press, 2021. http://dx.doi.org/10.1093/oso/9780192849793.001.0001.
Повний текст джерелаАнотація:
The Sentimental Life of International Law is about our age-old longing for a decent international society and the ways of seeing, being and speaking that might help us consummate that longing. This book treats international law as an experience, a language and an aspiration. It is the culmination of a decade of thinking about the practice of international lawyering (in classrooms, at conferences, in treaty negotiation) and the modes of thinking and being that naturalise that practice. In particular, it asks both how we might engage in a professional practice that has become, to adapt a title of Janet Malcolm’s, not just impossible but also difficult; and whether we might be disabled by the governing idioms of international lawyering and, then, importantly, re-enabled, by speaking different sorts of international law or by speaking international law in different sorts of ways. It tries to answer that question by making the effort to discern or, better still, to bring to the surface international law’s hidden literary prose or its redemptive enclaves, and it does so in a series of chapters on international law’s bathetic underpinnings, its friendly relations, the neurotic foundations of its underlying social order, its screened-off comic dispositions, its anti-method, and the life-worlds of its practitioners, and then, finally in a chapter in which international law is re-envisioned through the practice of gardening. All of this done in the hope of offering a contribution to the project of making international law, again, a compelling language for our times.
23
Kazemi, Farshid. A Girl Walks Home Alone at Night. Liverpool University Press, 2021. http://dx.doi.org/10.3828/liverpool/9781800859203.001.0001.
Повний текст джерелаАнотація:
A Girl Walks Home Alone at Night analyses the eponymous film within three theoretical coordinates: vampire cinema, psychoanalytic (film) theory and German Idealism. The book situates the film in the history of the vampire genre through the spectral vampire in early German expressionist cinema (Murnau’s Nosferatu, 1922) and theorizes it as part of a transnational movement in Iranian films that represents ‘the uncanny’ between the two modes of ‘the weird and the eerie,’ theorized by Mark Fisher. The film is situated in relation to the history of Iranian horror films, as well as the female vampire’s evocation of the figure of the Nightmare in Iranian myth-folklore, and the cinematic vampire’s relation to Islamicate occult sciences. The book provides an intervention in second-wave psychoanalytic film theory (Joan Copjec, Slavoj Žižek) through a Lacanian reading of the film that analyzes the female vampire as ‘the return of the repressed’ of feminine sexuality, and as the Lacanian (traumatic) Real in female sexuality for the Shi’ite clerical order in Iran. The romantic love story at the heart of the film is theorized through ideas of central figures in German Idealism, such as Hegel and Schelling. The book establishes a relation between the female vampire and the spectral vampire by linking German Idealism and its deployment of metaphors such as phantasmagoria in early magic lantern projections. The book’s central theoretical intervention is an enactment of Freudo-Lacanian psychoanalytic theory and Hegelian dialectics that brings out what is hidden on the surface of the film’s textual unconscious.
24
Hameed, Saji N. The Indian Ocean Dipole. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.619.
Повний текст джерелаАнотація:
Discovered at the very end of the 20th century, the Indian Ocean Dipole (IOD) is a mode of natural climate variability that arises out of coupled ocean–atmosphere interaction in the Indian Ocean. It is associated with some of the largest changes of ocean–atmosphere state over the equatorial Indian Ocean on interannual time scales. IOD variability is prominent during the boreal summer and fall seasons, with its maximum intensity developing at the end of the boreal-fall season. Between the peaks of its negative and positive phases, IOD manifests a markedly zonal see-saw in anomalous sea surface temperature (SST) and rainfall—leading, in its positive phase, to a pronounced cooling of the eastern equatorial Indian Ocean, and a moderate warming of the western and central equatorial Indian Ocean; this is accompanied by deficit rainfall over the eastern Indian Ocean and surplus rainfall over the western Indian Ocean. Changes in midtropospheric heating accompanying the rainfall anomalies drive wind anomalies that anomalously lift the thermocline in the equatorial eastern Indian Ocean and anomalously deepen them in the central Indian Ocean. The thermocline anomalies further modulate coastal and open-ocean upwelling, thereby influencing biological productivity and fish catches across the Indian Ocean. The hydrometeorological anomalies that accompany IOD exacerbate forest fires in Indonesia and Australia and bring floods and infectious diseases to equatorial East Africa. The coupled ocean–atmosphere instability that is responsible for generating and sustaining IOD develops on a mean state that is strongly modulated by the seasonal cycle of the Austral-Asian monsoon; this setting gives the IOD its unique character and dynamics, including a strong phase-lock to the seasonal cycle. While IOD operates independently of the El Niño and Southern Oscillation (ENSO), the proximity between the Indian and Pacific Oceans, and the existence of oceanic and atmospheric pathways, facilitate mutual interactions between these tropical climate modes.
25
Goswami, B. N., and Soumi Chakravorty. Dynamics of the Indian Summer Monsoon Climate. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.613.
Повний текст джерелаАнотація:
Lifeline for about one-sixth of the world’s population in the subcontinent, the Indian summer monsoon (ISM) is an integral part of the annual cycle of the winds (reversal of winds with seasons), coupled with a strong annual cycle of precipitation (wet summer and dry winter). For over a century, high socioeconomic impacts of ISM rainfall (ISMR) in the region have driven scientists to attempt to predict the year-to-year variations of ISM rainfall. A remarkably stable phenomenon, making its appearance every year without fail, the ISM climate exhibits a rather small year-to-year variation (the standard deviation of the seasonal mean being 10% of the long-term mean), but it has proven to be an extremely challenging system to predict. Even the most skillful, sophisticated models are barely useful with skill significantly below the potential limit on predictability. Understanding what drives the mean ISM climate and its variability on different timescales is, therefore, critical to advancing skills in predicting the monsoon. A conceptual ISM model helps explain what maintains not only the mean ISM but also its variability on interannual and longer timescales.The annual ISM precipitation cycle can be described as a manifestation of the seasonal migration of the intertropical convergence zone (ITCZ) or the zonally oriented cloud (rain) band characterized by a sudden “onset.” The other important feature of ISM is the deep overturning meridional (regional Hadley circulation) that is associated with it, driven primarily by the latent heat release associated with the ISM (ITCZ) precipitation. The dynamics of the monsoon climate, therefore, is an extension of the dynamics of the ITCZ. The classical land–sea surface temperature gradient model of ISM may explain the seasonal reversal of the surface winds, but it fails to explain the onset and the deep vertical structure of the ISM circulation. While the surface temperature over land cools after the onset, reversing the north–south surface temperature gradient and making it inadequate to sustain the monsoon after onset, it is the tropospheric temperature gradient that becomes positive at the time of onset and remains strongly positive thereafter, maintaining the monsoon. The change in sign of the tropospheric temperature (TT) gradient is dynamically responsible for a symmetric instability, leading to the onset and subsequent northward progression of the ITCZ. The unified ISM model in terms of the TT gradient provides a platform to understand the drivers of ISM variability by identifying processes that affect TT in the north and the south and influence the gradient.The predictability of the seasonal mean ISM is limited by interactions of the annual cycle and higher frequency monsoon variability within the season. The monsoon intraseasonal oscillation (MISO) has a seminal role in influencing the seasonal mean and its interannual variability. While ISM climate on long timescales (e.g., multimillennium) largely follows the solar forcing, on shorter timescales the ISM variability is governed by the internal dynamics arising from ocean–atmosphere–land interactions, regional as well as remote, together with teleconnections with other climate modes. Also important is the role of anthropogenic forcing, such as the greenhouse gases and aerosols versus the natural multidecadal variability in the context of the recent six-decade long decreasing trend of ISM rainfall.
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Ross, Stephen J. Invisible Terrain. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780198798385.001.0001.
Повний текст джерелаАнотація:
In his debut collection, Some Trees (1956), John Ashbery poses a question that resonates across his oeuvre and much modern art: “How could he explain to them his prayer / that nature, not art, might usurp the canvas?” When Ashbery asks this strange question, he joins a host of transatlantic avant-gardists—from the Dadaists to the 1960s neo-avant-gardists and beyond—who have dreamed the paradoxical dream of turning art into nature. Invisible Terrain examines Ashbery’s poetic mediation of this fantasy, reading his work alongside an array of practitioners, from Wordsworth to Warhol, as an exemplary case study of avant-garde transvaluation of Western nature aesthetics. Ashbery takes his coordinates from a constellation of British, American, and continental European poetic and visual art practices—from romantic nature poet John Clare’s presentational immediacy to the French “New Realism” movement’s “direct appropriation of the real” in the early 1960s—that share an emphasis on somehow transforming the material of art into a “second nature.” Nature, as Ashbery and his company understand it, is a vanguard horizon, a metaphor for art, that which lies beyond “art as we know it.” The fact that the artist can never realize this aesthetic fiction—which overturns what we generally mean by “art” and “nature”—makes it all the more powerful as a tool for staking out the limits of art. In chronicling Ashbery’s articulation of “a completely new kind of realism,” Invisible Terrain tells the larger story of nature’s transformation into a resolutely unnatural aesthetic resource in twentieth-century art and literature. But in documenting Ashbery’s eventual turn against this avant-garde tradition—most conspicuously in his archive of campy, intentionally “bad” nature poems—the project also registers queer resistance to the normative concept of nature itself as a governing conceit for art. The story begins in the late 1940s with the Abstract Expressionist valorization of process, surface, and immediacy—summed up by Jackson Pollock’s famous quip, “I am Nature”—that so influenced Ashbery’s early quest for transparent, anti-mimetic modes of composition. It ends with “Breezeway,” a poem about Hurricane Sandy and climate change. Along the way, Invisible Terrain documents Ashbery’s strategic literalization of the stream-of-consciousness metaphor, his pastoral dispersal of the lyric subject during the politically fraught Vietnam era, and his investment in “bad” nature poetry.
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Nash, David. Changes in Precipitation Over Southern Africa During Recent Centuries. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.539.
Повний текст джерелаАнотація:
Precipitation levels in southern Africa exhibit a marked east–west gradient and are characterized by strong seasonality and high interannual variability. Much of the mainland south of 15°S exhibits a semiarid to dry subhumid climate. More than 66 percent of rainfall in the extreme southwest of the subcontinent occurs between April and September. Rainfall in this region—termed the winter rainfall zone (WRZ)—is most commonly associated with the passage of midlatitude frontal systems embedded in the austral westerlies. In contrast, more than 66 percent of mean annual precipitation over much of the remainder of the subcontinent falls between October and March. Climates in this summer rainfall zone (SRZ) are dictated by the seasonal interplay between subtropical high-pressure systems and the migration of easterly flows associated with the Intertropical Convergence Zone. Fluctuations in both SRZ and WRZ rainfall are linked to the variability of sea-surface temperatures in the oceans surrounding southern Africa and are modulated by the interplay of large-scale modes of climate variability, including the El Niño-Southern Oscillation (ENSO), Southern Indian Ocean Dipole, and Southern Annular Mode.Ideas about long-term rainfall variability in southern Africa have shifted over time. During the early to mid-19th century, the prevailing narrative was that the climate was progressively desiccating. By the late 19th to early 20th century, when gauged precipitation data became more readily available, debate shifted toward the identification of cyclical rainfall variation. The integration of gauge data, evidence from historical documents, and information from natural proxies such as tree rings during the late 20th and early 21st centuries, has allowed the nature of precipitation variability since ~1800 to be more fully explored.Drought episodes affecting large areas of the SRZ occurred during the first decade of the 19th century, in the early and late 1820s, late 1850s–mid-1860s, mid-late 1870s, earlymid-1880s, and mid-late 1890s. Of these episodes, the drought during the early 1860s was the most severe of the 19th century, with those of the 1820s and 1890s the most protracted. Many of these droughts correspond with more extreme ENSO warm phases.Widespread wetter conditions are less easily identified. The year 1816 appears to have been relatively wet across the Kalahari and other areas of south central Africa. Other wetter episodes were centered on the late 1830s–early 1840s, 1855, 1870, and 1890. In the WRZ, drier conditions occurred during the first decade of the 19th century, for much of the mid-late 1830s through to the mid-1840s, during the late 1850s and early 1860s, and in the early-mid-1880s and mid-late 1890s. As for the SRZ, markedly wetter years are less easily identified, although the periods around 1815, the early 1830s, mid-1840s, mid-late 1870s, and early 1890s saw enhanced rainfall. Reconstructed rainfall anomalies for the SRZ suggest that, on average, the region was significantly wetter during the 19th century than the 20th and that there appears to have been a drying trend during the 20th century that has continued into the early 21st. In the WRZ, average annual rainfall levels appear to have been relatively consistent between the 19th and 20th centuries, although rainfall variability increased during the 20th century compared to the 19th.