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Catherine Peters discusses how writers such as the Cuban poet Juan Francisco Manzano reworked the Romantic trope of the revolutionary “common wind” to forge kinship networks among forcibly displaced peoples. In formulating this argument, Peters shifts the conventional focus on the French Revolution as the hub of radical Romantic thought to the Haitian Revolution, where “fraternité” refers not to an abstract ideal but a very real desire to reconstitute those family relations disrupted by the institution of slavery.
As some of the most intensively devoted football fans in Germany, ultras coordinate crowd atmosphere in the arena to support their respective clubs on the field while actively positioning themselves against sport’s governing bodies, whom they see as corrupted by the strategies used to transform professional football from a game into a capitalist industry. Focusing on travel and transportation as a key feature of hardcore fandom, I examine the relationship between ultras’ activities in transit to games and their congregation in public spaces (on the streets, on trains, at rest stops, in stadia), in which quotidian ambience is often hijacked and repurposed as an estranged form of public address. I focus on the dynamic ways that ultras move through space as a means of charting the stages in which fan scenes become crowds, and crowds are mobilized as a means of protesting against the alienating dynamics of modern football, the contrasting stylistics of which result in divergent outsider interpretations and reactions from the state, the German Football Association (DFB), the media, and onlookers confronted by ultras’ public transgressions. Through the fan scene’s ability to coordinate movement and heighten bodily capacity, varied expressions of antisocial behavior become a means of harnessing fans’ own disaffection in a way that reclaims public space as it conjures a heightened emotive environment.
Life as we know it requires the presence of liquid water and the availability of nutrients, which are mainly based on the elements C, H, N, O, P and S (CHNOPS) and trace metal micronutrients. We aim to understand the presence of these nutrients within atmospheres that show the presence of water cloud condensates, potentially allowing the existence of aerial biospheres. In this paper, we introduce a framework of nutrient availability levels based on the presence of water condensates and the chemical state of the CHNOPS elements. These nutrient availability levels are applied to a set of atmospheric models based on different planetary surface compositions resulting in a range of atmospheric compositions. The atmospheric model is a bottom-to-top equilibrium chemistry atmospheric model which includes the atmosphere–crust interaction and the element depletion due to the formation of clouds. While the reduced forms of CNS are present at the water cloud base for most atmospheric compositions, P and metals are lacking. This indicates the potential bio-availability of CNS, while P and metals are limiting factors for aerial biospheres.
Observations of radiocarbon (14C) in Earth’s atmosphere and other carbon reservoirs are important to quantify exchanges of CO2 between reservoirs. The amount of 14C is commonly reported in the so-called Delta notation, i.e., Δ14C, the decay- and fractionation-corrected departure of the ratio of 14C to total C from that ratio in an absolute international standard; this Delta notation permits direct comparison of 14C/C ratios in the several reservoirs. However, as Δ14C of atmospheric CO2, Δ14CO2 is based on the ratio of 14CO2 to total atmospheric CO2, its value can and does change not just because of change in the amount of atmospheric14CO2 but also because of change in the amount of total atmospheric CO2, complicating ascription of change in Δ14CO2 to change in one or the other quantity. Here we suggest that presentation of atmospheric 14CO2 amount as mole fraction relative to dry air (moles of 14CO2 per moles of dry air in Earth’s atmosphere), or as moles or molecules of 14CO2 in Earth’s atmosphere, all readily calculated from Δ14CO2 and the amount of atmospheric CO2 (with slight dependence on δ13CO2), complements presentation only as Δ14CO2, and can provide valuable insight into the evolving budget and distribution of atmospheric 14CO2.
Utopia is nominally a ‘nowhere’ that is also, as Thomas More tells us, a ‘good’ place. Although there are competing cognate notions, the Greek description looms large in most accounts of utopia. The details of this ideal are so specified that utopic literature consists in a catalogue (and critique) of specifications. This essay draws attention to the fragrance attributed to Lucian’s ‘Isles of the Blest’ together with Ivan Illich’s attention to ‘atmosphere’ and to the aura and the nose along with Nietzsche’s emphasis on the sense of smell. Utopic suspicion is discussed as parallels are drawn with pragmatic critiques of utopia as inherently totalitarian along with the ‘good life’ in political theory and the programmatic default of techno-utopic fantasy. In the historical context of ‘conspiracy’ and the politics of living and breathing together in community, I conclude with Illich on pax and breath.
The Mediterranean boat crossing highlights vulnerability and risk along migrants’ unauthorized journeys. This chapter attends to migrants’ experiences of taking a boat from Libya to Europe. The chapter enlivens affective and meteorological dimensions of the crossing to show how they configure mobilities and peoples’ futures. It provides a unique insight into unauthorized migration and its intersections with affect and atmospheres.
The 1890s have a special significance in the literary history of the Anthropocene, and the fin de siècle has traditionally been understood as a moment when artifice triumphed over nature. Reexamining the period today, we can instead see how literature and art of the 1890s reckons with the idea of an indeterminate nature without design, purpose, or end – a nature profoundly shaped by human forces and yet beyond human reckoning and control. The concentrated finitude of the era, as framed in literary and historical study, actually reflects the period’s own grasp of the finitudes and vicissitudes of the natural world. This chapter aims to tease out the environmental and ecological inheritance of the decadent 1890s while simultaneously teasing apart the complex conceptual contestation among rival assaults on the category of the “natural” in the 1890s, assaults that can be roughly grouped around Oscar Wilde’s 1895 denaturalizing of heterosexuality and Svante Arrhenius’s 1896 denaturalizing of the atmosphere in his landmark essay “On the Influence of Carbonic Acid in the Air upon the Temperature of the Ground.”
An overview of optical scattering in the atmosphere includes the sizes and concentration of scatterers, the mathematical formalism of scattering, and definitions of the lidar scattering and extinction coefficients. The Rayleigh, Mie, and geometric scattering regimes are defined by the scattering parameter, and implications of Rayleigh scattering on lidar measurements are elucidated for both signals and background. Molecules store energy in translational, rotational, and vibrational motions, and atoms store energy in electronic excitations. These energy storage mechanisms cause the lidar observables of Doppler shifts, molecular and Raman spectra, and atomic spectra, which, along with Rayleigh scattering, enable lidar measurements of temperatures and winds; water vapor and trace gas concentrations; and aerosol extinction coefficients at altitudes from the surface up to the mesosphere and lower thermosphere. The lidar techniques that exploit all these phenomena operate over a range of wavelengths from the long wave infrared to the ultraviolet and the reasons for the differing wavelengths of the various techniques are explained with a graphic that summarizes the chapter.
A brief overview and description of the atmospheric lidar measurement technique is followed by the structure of the atmosphere in terms of the troposphere, stratosphere, and mesosphere, as it is usually presented in atmospheric science and meteorology. The atmosphere is then described in terms of lidar observables at all altitudes, including water vapor; trace gases; clouds; several other kinds of particulate matter; and metal atoms, as well as density, temperature, and winds. Examples of lidar measurements include tropospheric and stratospheric ozone, greenhouse gases, other pollutants, tropospheric and stratospheric aerosols, polar stratospheric clouds, and atoms of sodium, potassium, calcium, and iron in the mesosphere. Finally, the structure and contents of the book are described, and suggestions for further reading are given.
Explore the spectrum of lidar engineering in this one-of-a-kind introduction. For the first time, this multidisciplinary resource covers all the scientific and engineering aspects of atmospheric lidar – including atmospheric science, spectroscopy, lasers and eye safety, classical optics and electro-optics, electrical and mechanical engineering, and software algorithms – in a single comprehensive and authoritative book. Discover up-to-date material not included in any other book, including simple treatments of the lidar crossover range and depolarization in lidar signals, an improved explanation of lidar data inversion algorithms, digital signal processing applications in lidar, and statistical limitations of lidar signal-to-noise ratios. This is an ideal standalone text for students seeking a thorough grounding in lidar, whether through a taught course or self-study.
In 1972, James Lovelock and Lynn Margulis began collaborating on the Gaia hypothesis. They suggested that over geological time, life on Earth has had a major role in both producing and regulating its own environment. Gaia is now an ecological and environmental worldview underpinning vital scientific and cultural debates over environmental issues. Their ideas have transformed the Earth and life sciences, as well as contemporary conceptions of nature. Their correspondence describes these crucial developments from the inside, showing how their partnership proved decisive for the development of the Gaia hypothesis. Clarke and Dutreuil provide historical background and explain the concepts and references introduced throughout the Lovelock-Margulis correspondence, while highlighting the major landmarks of their collaboration within the sequence of almost 300 letters written between 1970 and 2007. This book will be of interest to researchers in ecology, history of science, environmental history and climate change, and cultural science studies.
This chapter reviews how literary and literal atmospheres have cut across each other in complex transactions of meaning and practice over the past 400 years. It traces how atmosphere was first literalised in early modern science, in a process that identified air as a new object of empirical knowledge while also awarding a new meaning of empirical objectivity to literalness. It then shows how this scientifically literal atmosphere was taken up in an expanded set of metaphoric and figurative uses from around 1800, in which such formulations as ‘political atmosphere’ and ‘poetic atmosphere’ breathed new life into traditional understandings of air that had moved fluidly between the spiritual and the empirical. The large-scale cultural re-metaphoricisation of air in this period formed the platform for the emergence of literary atmosphere as a specific practice of double troping, in which aerial figures were reflexively marked as at once figurative and literal. That marking proved integral to the emergence of both modernist poetry and the modern novel. But the discursive divisions and oppositions that underwrote it are brought under unprecedented pressure by climate change, which therefore requires new methods for the writing and reading of literary atmospheres.
This is our quick jog through climate science, intended to ground future climate discussions in a solid factual context. We review: the earth’s energy budget via the Trenberth diagram; the role of greenhouse gases, the Keeling Curve, and global warming potential; atmospheric structure and the environmental lapse rate; global atmospheric and oceanic circulations; paleoclimatology over both the last million and the last 1,500 years; and the role of oceans and ice.
Direct atmospheric 14CO2 measurements began in New Zealand in 1954, initially to improve 14C as a dating tool, but quickly evolving into a method for understanding the carbon cycle. These early 14CO2 measurements immediately demonstrated the existence of an “Atom Bomb Effect,” as well as an “Industrial Effect.” These two gigantic tracer experiments have been utilized via 14CO2 measurements over the years to produce a wealth of knowledge in multiple research fields including atmospheric carbon cycle research, oceanography, soil science, and aging of post-bomb materials.
The major contribution of Oliver Williamson, who was a 2009 Nobel Prize co-Laureate in economics, consists of proposing a heuristic analysis of governance structures, namely, the firm, the market, and what he will later call the ‘hybrid forms’. This cardinal issue in organizational economics has made it possible to propose rigorous arbitration tools for the famous ‘make or buy’ decisions in modern market economies based on asset specificity and quasi-rents. However, Williamson's work goes far beyond these contributions alone. His contribution is based on a multidisciplinary theoretical background in building the science of organization. This is the important but sometimes neglected aspect of Williamson's work that I wish to highlight in this paper in memory of Williamson in regard to three major pieces on atmosphere (and informal organization), private ordering, and industrial pluralism. In doing so, I also propose reconsidering the different stages of Williamson's evolving science of organization from recent neo-institutional works.
This is the first study of Renaissance architecture as an immersive, multisensory experience that combines historical analysis with the evidence of first-hand accounts. Questioning the universalizing claims of contemporary architectural phenomenologists, David Karmon emphasizes the infinite variety of meanings produced through human interactions with the built environment. His book draws upon the close study of literary and visual sources to prove that early modern audiences paid sustained attention to the multisensory experience of the buildings and cities in which they lived. Through reconstructing the Renaissance understanding of the senses, we can better gauge how constant interaction with the built environment shaped daily practices and contributed to new forms of understanding. Architecture and the Senses in the Italian Renaissance offers a stimulating new approach to the study of Renaissance architecture and urbanism as a kind of 'experiential trigger' that shaped ways of both thinking and being in the world.
The Anthropocene tasks literary critics and historians with rethinking literature through the lens of a civilizational catastrophe not yet fully realized but well-modeled and forecast in the IPCC reports, which describe a future planet drastically altered by greenhouse gas emissions. The hidden angle of literature is that it has always subtended a long arc from a mostly stable climate regime to the chaotic one that awaits above 400-plus ppm. Within literary texts we may find clues to explain how, in the face of a planetary emergency, we persist in our frustrating denialism (and find, too, perhaps some remedies for it). The American Renaissance is an important locus for such rereadings. This essay takes an indirect line through the central figures associated with the period (Emerson, Thoreau, Whitman, and Hawthorne), adding Dickinson, Poe, Fuller, and Susan Fenimore Cooper. The remarks on these authors’ “climate-imaginary” are mostly observational, sometimes notional, and admittedly provisional. Uncovering the climatic unconscious of the American Renaissance can only be understood as a literary version of paleoclimatology, with all the attendant gaps and uncertainties.
Paleosols formed in direct contact with the Earth's atmosphere, so they can record the composition of the atmosphere through weathering processes and products. Herein we critically review a variety of different approaches for reconstructing atmospheric O2 and CO2 over the past three billion years. Paleosols indicate relatively low CO2 over that time, requiring additional greenhouse forcing to overcome the 'faint young Sun' paradox in the Archean and Mesoproterozoic, as well as low O2 levels until the Neoproterozoic. Emerging techniques will revise the history of Earth's atmosphere further and may provide a window into atmospheric evolution on other planets.
Craftsmanship, making and do-it-ocracy are prominent elements of the so-called new world of work. In this chapter, we describe the ‘experience of making’ in two makerspaces, one located in France and the other in the United States. In particular, we focus on three concepts – silence, atmosphere and togetherness – in order to flesh out, or make visible, the specificities of Do-It-Yourself (DIY) and Do-It-Together (DIT) processes in makerspaces. We mobilise Merleau-Ponty’s work and an aesthetic perspective on time and place to delve into the experience of making. This leads us to propose the concept of New Collaborative Experiences (NCE), which we define as new modes of feeling and expressing the self and the world in a context that requires a collective production and coordination, as a way of illuminating our two ethnographic accounts.