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1
Caldiero, Alex. Various atmospheres: Poems and drawings. Salt Lake City: Signature Books, 1998.
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2
H, Wang A., und United States. National Aeronautics and Space Administration., Hrsg. Numerical modeling of coronal mass ejections based on various pre-event model atmospheres. [Washington, DC: National Aeronautics and Space Administration, 1994.
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3
H, Wang A., und United States. National Aeronautics and Space Administration., Hrsg. Numerical modeling of coronal mass ejections based on various pre-event model atmospheres. [Washington, DC: National Aeronautics and Space Administration, 1995.
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4
United States. National Aeronautics and Space Administration., Hrsg. [High resolution infrared absorption spectra of various trace gases present in the upper atmosphere of the earth. [Washington, DC: National Aeronautics and Space Administration, 1988.
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5
Banin, Amos. N₂O fluxes at the soil-atmosphere interface in various ecosystems, and the global N₂O budget: Final report. Los Altos, CA: Seti Institute, 1987.
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6
United States. National Aeronautics and Space Administration., Hrsg. N₂O fluxes at the soil-atmosphere interface in various ecosystems, and the global N₂O budget: Final report. Los Altos, CA: Seti Institute, 1987.
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7
Environmental Research Laboratories (U.S.) und Summer Science Institute (1993 : Boulder, Colo.), Hrsg. Weather II: Studies concerning the science of meteorology on various scales : a product of the 1993 Summer Science Institute with the National Oceanic and Atmospheric Administration (NOAA), Environmental Research Laboratories (ERL). [Boulder, Colo: The Laboratories, 1996.
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8
Environmental Research Laboratories (U.S.) und Summer Science Institute (1993 : Boulder, Colo.), Hrsg. Weather I: Studies concerning the science of meteorology on various scales : a product of the 1993 summer science institute with the National Oceanic and Atmospheric Administration (NOAA), Environmental Research Laboratories (ERL). [Boulder, Colo: The Laboratories, 1996.
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9
Mölder, Meelis. Parameterization of the interaction between the atmosphere and the land surface by means of roughness lengths: An experimental study over various surfaces. Uppsala: Sveriges lantbruksuniversitet, Institutionen för ekologi och miljövård, 1993.
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10
Holzhey, Christoph F. E., und Arnd Wedemeyer, Hrsg. Weathering. Berlin: ICI Berlin Press, 2020. http://dx.doi.org/10.37050/ci-17.
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Weathering is atmospheric, geological, temporal, transformative. It implies exposure to the elements and processes of wearing down, disintegration, or accrued patina. Weathering can also denote the ways in which subjects and objects resist and pass through storms and adversity. This volume contemplates weathering across many fields and disciplines; its contributions examine various surfaces, environments, scales, temporalities, and vulnerabilities. What does it mean to weather or withstand? Who or what is able to pass through safely? What is lost or gained in the process?
11
Merrill, Elizabeth, Hrsg. Creating Place in Early Modern European Architecture. NL Amsterdam: Amsterdam University Press, 2021. http://dx.doi.org/10.5117/9789463728027.
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The importance of place—as a unique spatial identity—has been recognized since antiquity. Ancient references to the ‘genius loci’, or spirit of place, evoked not only the location of a distinct atmosphere or environment, but also the protection of this location, and implicitly, its making and construction. This volume examines the concept of place as it relates to architectural production and building knowledge in early modern Europe (1400-1800). The places explored in the book’s ten essays take various forms, from an individual dwelling to a cohesive urban development to an extensive political territory. Within the scope of each study, the authors draw on primary source documents and original research to demonstrate the distinctive features of a given architectural place, and how these are related to a geographic location, social circumstances, and the contributions of individual practitioners. The essays underscore the distinct techniques, practices and organizational structures by which physical places were made in the early modern period.
12
Environmental Research Laboratories (U.S.) und Summer Science Institute (1993 : Boulder, Colo.), Hrsg. Weather I: Studies concerning the science of meteorology on various scales : a product of the 1993 summer science institute with the National Oceanic and Atmospheric Administration (NOAA), Environmental Research Laboratories (ERL). [Boulder, Colo: The Laboratories, 1996.
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13
Bindi, Marco, Giada Brandani, Alessandro Dessì, Camilla Dibari, Roberto Ferrise, Marco Moriondo und Giacomo Trombi, Hrsg. Impact of climate change on agricultural and natural ecosystems. Florence: Firenze University Press, 2009. http://dx.doi.org/10.36253/978-88-8453-921-2.
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This book illustrates the main results deriving from fourteen studies, dealing with the impact of climate change on different agricultural and natural ecosystems, carried out within the Impact of Climate change On agricultural and Natural Ecosystems (ICONE) project funded by the ALFA Programme of the European Commission. During this project, a common methodology on several Global Change-related matters was developed and shared among members of scientific communities coming from Latin America and Europe. In order to facilitate this interdisciplinary approach, specific mobility programmes, addressed to post-graduate, Master and PhD students, have been organized. The research, led by the research groups, was focused on the study of the impact of climate change on various environmental features (i.e. runoff in hydrological basins, soil erosion and moisture, forest canopy, sugarcane crop, land use, drought, precipitation, etc). Integrated and shared methodologies of atmospheric physics, remote sensing, eco-physiology and modelling have been applied.
14
Mihaylov, Vyacheslav, Elena Sotnikova und Nina Kalpina. Eco-friendly air protection systems for motor transport facilities. ru: INFRA-M Academic Publishing LLC., 2022. http://dx.doi.org/10.12737/1093106.
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The textbook considers the issue of assessing the heat and humidity state of air in the processes of its processing in various systems, provides requirements for air protection means, taking into account their environmental friendliness, shows ways of energy saving in cooling, heating and year-round air conditioning systems, as well as when protecting the atmosphere from harmful emissions. The way of energy saving with individual thermal protection of the operator by means of local cooling during air treatment in an irrigated intensified nozzle is shown and recommendations for reducing its material consumption are developed. The method and means of reducing the toxicity of emissions of tractor internal combustion engines during its operation in rooms of limited volume by water vapor humidification of the fuel-air mixture are demonstrated. The ways of noise reduction of air protection systems are shown.
Meets the requirements of the federal state educational standards of higher education of the latest generation.
It is intended for students studying in the specialties "Ground transport and technical means", "Operation of transport and technological machines and complexes", "Power engineering", "Ground transport and technological complexes", "Refrigeration, cryogenic equipment and life support systems", "Technosphere safety", "Ecology and nature management".
15
Calvert, Jack G., John J. Orlando, William R. Stockwell und Timothy J. Wallington. The Mechanisms of Reactions Influencing Atmospheric Ozone. Oxford University Press, 2015. http://dx.doi.org/10.1093/oso/9780190233020.001.0001.
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Ozone, an important trace component, is critical to life on Earth and to atmospheric chemistry. The presence of ozone profoundly impacts the physical structure of the atmosphere and meteorology. Ozone is also an important photolytic source for HO radicals, the driving force for most of the chemistry that occurs in the lower atmosphere, is essential to shielding biota, and is the only molecule in the atmosphere that provides protection from UV radiation in the 250-300 nm region. However, recent concerns regarding environmental issues have inspired a need for a greater understanding of ozone, and the effects that it has on the Earth's atmosphere. The Mechanisms of Reactions Influencing Atmospheric Ozone provides an overview of the chemical processes associated with the formation and loss of ozone in the atmosphere, meeting the need for a greater body of knowledge regarding atmospheric chemistry. Renowned atmospheric researcher Jack Calvert and his coauthors discuss the various chemical and physical properties of the earth's atmosphere, the ways in which ozone is formed and destroyed, and the mechanisms of various ozone chemical reactions in the different spheres of the atmosphere. The volume is rich with valuable knowledge and useful descriptions, and will appeal to environmental scientists and engineers alike. A thorough analysis of the processes related to tropospheric ozone, The Mechanisms of Reactions Influencing Atmospheric Ozone is an essential resource for those hoping to combat the continuing and future environmental problems, particularly issues that require a deeper understanding of atmospheric chemistry.
16
Fritsch, Andreas, Andreas Lischewski und Uwe Voigt, Hrsg. Comenius-Jahrbuch. Academia – ein Verlag in der Nomos Verlagsgesellschaft, 2021. http://dx.doi.org/10.5771/9783985720279.
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John Amos Comenius (1592-1670) is inspired by many sources and is connected to many developments after him. Thus he enters into manifold constellations à la Dieter Henrich: elements of a shared cognitive space in which creative impulses unfold. This volume explores such constellations in various directions from diverse perspectives: the biblical self-stylization of Comenius, sources and topicality of light as a metaphor, the philosophical importance of the image of God in Leibniz, Hume vs. cosmo-theology, organicist thought in Schelling and “atmospheres” in today’s schools.
17
Beerling, David. The Emerald Planet. Oxford University Press, 2007. http://dx.doi.org/10.1093/oso/9780192806024.001.0001.
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Global warming is contentious and difficult to measure, even among the majority of scientists who agree that it is taking place. Will temperatures rise by 2ºC or 8ºC over the next hundred years? Will sea levels rise by 2 or 30 feet? The only way that we can accurately answer questions like these is by looking into the distant past, for a comparison with the world long before the rise of mankind. We may currently believe that atmospheric shifts, like global warming, result from our impact on the planet, but the earth's atmosphere has been dramatically shifting since its creation. This book reveals the crucial role that plants have played in determining atmospheric change - and hence the conditions on the planet we know today. Along the way a number of fascinating puzzles arise: Why did plants evolve leaves? When and how did forests once grow on Antarctica? How did prehistoric insects manage to grow so large? The answers show the extraordinary amount plants can tell us about the history of the planet -- something that has often been overlooked amongst the preoccuputations with dinosaur bones and animal fossils. David Beerling's surprising conclusions are teased out from various lines of scientific enquiry, with evidence being brought to bear from fossil plants and animals, computer models of the atmosphere, and experimental studies. Intimately bound up with the narrative describing the dynamic evolution of climate and life through Earth's history, we find Victorian fossil hunters, intrepid polar explorers and pioneering chemists, alongside wallowing hippos, belching volcanoes, and restless landmasses.
18
Dunlop, Storm. 2. The circulation of the atmosphere. Oxford University Press, 2017. http://dx.doi.org/10.1093/actrade/9780199571314.003.0002.
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‘The circulation of the atmosphere’ outlines the general model of the movement of air around the Earth. There are three circulation cells either side of the equator: the Hadley cell (nearest to the equator) and the polar cell, driven by specific temperature and pressure gradients, and the Ferrel cell between them. It describes global pressure patterns and the Coriolis effect, which results in south-westerly trade winds in the northern hemisphere and north-westerly trade winds in the southern. Also described are the Intertropical Convergence Zone, the polar easterlies, the westerlies, and how air moves around high- and low-pressure regions. The action of the surface winds also produces the various ocean currents.
19
Jäntti, Saara, Kirsi Heimonen, Sari Kuuva, Karoliina Maanmieli und Anu Rissanen, Hrsg. Kokemuksia mielisairaalasta. Muistoihin kaivertuneet tilat. SKS Finnish Literature Society, 2022. http://dx.doi.org/10.21435/skst.1483.
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Experiences of Mental Hospitals. Spaces Engraved in Memories Finnish psychiatric practice has been heavily based on institutionalization, and mental hospitals have played important cultural and historical roles in Finland. Our multidisciplinary research focuses on the bodily, spatial, affective, and multisensory aspects of the memories of patients, relatives, staff, and their children. The memories were collected and archived in the Finnish Literature Society in 2014–2015. These 92 written pieces cover the period from the 1930s to the 2010s. They reflect significant changes in Finnish psychiatry and provide crucial insights into the various meanings of mental hospitals in people’s lives, and the social and cultural forces that shape attitudes to and ideas about mental health problems, psychiatric care, and service users today. Drawing on our backgrounds in history, artistic research, and visual, cultural and literary studies, we provide new ways of reading and interpreting the memories and experiences in psychiatry. The study discusses memory, mental hospitals as lived spaces, the history of Finnish psychiatry and the relation between the memories of the different groups of writers. The chapters approach memories from the perspectives of affects and atmospheres, violence and abuse, everyday life at the hospital in the 1930s, feelings of fear and safety in the memories of the children of the staff, and the historically and culturally contingent tensions between hospitals and homes.
20
Lippmann, Morton, und Richard B. Schlesinger. Dispersion of Contaminants. Oxford University Press, 2017. http://dx.doi.org/10.1093/med/9780190688622.003.0004.
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This chapter describes the pathways and dynamics of chemical contaminants within the various structural layers. In the atmosphere, the chemical contaminants are transferred by diffusion, turbulence, plume dispersion, long-range transport, and tropospheric-stratospheric interchange. They are transferred to the hydrosphere by surface deposition, rainout, and washout. They are transferred to the lithosphere by surface flow and penetration, and are transferred within the biosphere by food-chain concentration.
21
Clarke, Andrew. Global climate change and its ecological consequences. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780199551668.003.0016.
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The greenhouse effect is a simple consequence of an atmosphere containing gases that are transparent to visible light but which absorb infra-red radiation (radiatively active or greenhouse gases). The temperature of the lower troposphere is set by the radiation balance at the top of the atmosphere, and is determined predominantly by the CO2 concentration. Man has been adding radiatively active gases to the atmosphere since the Industrial Revolution, and this has led to an increase in the energy in the lower atmosphere, and thus a rise in its temperature. The bulk of the extra energy (~90%) has entered the ocean, which has also warmed significantly over the past century. The rate and extent of warming varies across the planet, depending on local circumstances. Palaeoecological studies have shown that changes in distribution have been a frequent response to climate change, though this requires somewhere for the organisms to move to. Many organisms have shifted their distribution in response to recent climate change. Many organisms have also shifted the timing of life-cycle events (phenology), with migration, breeding in animals, and germination, emergence, leafing and flowering in plants all occurring earlier in some (but not all) species. There are also changes in size, with some species becoming smaller as the climate warms.
22
Lippmann, Morton, und Richard B. Schlesinger. Characterization of Contaminants and Environments. Oxford University Press, 2017. http://dx.doi.org/10.1093/med/9780190688622.003.0002.
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This chapter describes the extensive scientific terminology needed to describe the various classes of chemical contaminants as they occur in environmental media (air, water, soil, etc.) and the structural aspects and dynamic mass and energy transfers within and among the atmosphere, hydrosphere, lithosphere, and biosphere. It also introduces: the characteristics of occupational environments; health effects attributable to occupational and environmental exposures; dose response relationships in populations; and how they are affected by anthropogenic (human activity caused) inputs and disruptions.
23
McClain, Michael E., Reynaldo Victoria und Jeffrey E. Richey, Hrsg. The Biogeochemistry of the Amazon Basin. Oxford University Press, 2001. http://dx.doi.org/10.1093/oso/9780195114317.001.0001.
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With a complex assemblage of largely intact ecosystems that support the earth's greatest diversity of life, the Amazon basin is a focal point of international scientific interest. And, as development and colonization schemes transform the landscape in increasing measure, scientists from around the world are directing attention to questions of regional and global significance. Some of these qustions are: What are the fluxes of greenhouse gases across the atmospheric interface of ecosystems? How mush carbon is stored in the biomass and soils of the basin? How are elements from the land transferred to the basin's surface waters? What is the sum of elements transferred from land to ocean, and what is its marine "fate"? This book of original chapters by experts in chemical and biological oceanography, tropical agronomy and biology, and the atmospheric sciences will address these and other important questions, with the aim of synthesizing the current knowledge of biochemical processes operating within and between the various ecosystems in the Amazon basin.
24
Omstedt, Anders. The Development of Climate Science of the Baltic Sea Region. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.654.
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Dramatic climate changes have occurred in the Baltic Sea region caused by changes in orbital movement in the earth–sun system and the melting of the Fennoscandian Ice Sheet. Added to these longer-term changes, changes have occurred at all timescales, caused mainly by variations in large-scale atmospheric pressure systems due to competition between the meandering midlatitude low-pressure systems and high-pressure systems. Here we follow the development of climate science of the Baltic Sea from when observations began in the 18th century to the early 21st century. The question of why the water level is sinking around the Baltic Sea coasts could not be answered until the ideas of postglacial uplift and the thermal history of the earth were better understood in the 19th century and periodic behavior in climate related time series attracted scientific interest. Herring and sardine fishing successes and failures have led to investigations of fishery and climate change and to the realization that fisheries themselves have strongly negative effects on the marine environment, calling for international assessment efforts. Scientists later introduced the concept of regime shifts when interpreting their data, attributing these to various causes. The increasing amount of anoxic deep water in the Baltic Sea and eutrophication have prompted debate about what is natural and what is anthropogenic, and the scientific outcome of these debates now forms the basis of international management efforts to reduce nutrient leakage from land. The observed increase in atmospheric CO2 and its effects on global warming have focused the climate debate on trends and generated a series of international and regional assessments and research programs that have greatly improved our understanding of climate and environmental changes, bolstering the efforts of earth system science, in which both climate and environmental factors are analyzed together.Major achievements of past centuries have included developing and organizing regular observation and monitoring programs. The free availability of data sets has supported the development of more accurate forcing functions for Baltic Sea models and made it possible to better understand and model the Baltic Sea–North Sea system, including the development of coupled land–sea–atmosphere models. Most indirect and direct observations of the climate find great variability and stochastic behavior, so conclusions based on short time series are problematic, leading to qualifications about periodicity, trends, and regime shifts. Starting in the 1980s, systematic research into climate change has considerably improved our understanding of regional warming and multiple threats to the Baltic Sea. Several aspects of regional climate and environmental changes and how they interact are, however, unknown and merit future research.
25
Ellam, Rob. 8. Scratching the surface with cosmogenic isotopes. Oxford University Press, 2016. http://dx.doi.org/10.1093/actrade/9780198723622.003.0008.
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‘Scratching the surface with cosmogenic isotopes’ explains spallation—when a high energy cosmic ray particle removes several nucleons from an atom. Spallation produces 10Be from 16O in the atmosphere and rock surfaces, while spallation of silicon produces another cosmogenic isotope, 26Al. Cosmogenic isotope production is about four times greater at the poles than at the equator and is also greater at higher altitudes. To calculate a cosmogenic isotope exposure age, the latitude and altitude at which the sample was exposed needs to be known. Using ‘exposure’ and ‘burial’ methodologies, cosmogenic isotopes can be used to address various scientific problems such as recreating the seismic histories of tectonically active areas.
26
Canfield, Donald Eugene. Oxygen. Princeton University Press, 2017. http://dx.doi.org/10.23943/princeton/9780691145020.001.0001.
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The air we breathe is 21 percent oxygen, an amount higher than on any other known world. While we may take our air for granted, Earth was not always an oxygenated planet. How did it become this way? This book covers this vast history, emphasizing its relationship to the evolution of life and the evolving chemistry of the Earth. The book guides readers through the various lines of scientific evidence, considers some of the wrong turns and dead ends along the way, and highlights the scientists and researchers who have made key discoveries in the field. Showing how Earth's atmosphere developed over time, the book takes readers on a remarkable journey through the history of the oxygenation of our planet.
27
Lurcock, Pontus, und Fabio Florindo. Antarctic Climate History and Global Climate Changes. Oxford University Press, 2017. http://dx.doi.org/10.1093/oxfordhb/9780190676889.013.18.
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Antarctic climate changes have been reconstructed from ice and sediment cores and numerical models (which also predict future changes). Major ice sheets first appeared 34 million years ago (Ma) and fluctuated throughout the Oligocene, with an overall cooling trend. Ice volume more than doubled at the Oligocene-Miocene boundary. Fluctuating Miocene temperatures peaked at 17–14 Ma, followed by dramatic cooling. Cooling continued through the Pliocene and Pleistocene, with another major glacial expansion at 3–2 Ma. Several interacting drivers control Antarctic climate. On timescales of 10,000–100,000 years, insolation varies with orbital cycles, causing periodic climate variations. Opening of Southern Ocean gateways produced a circumpolar current that thermally isolated Antarctica. Declining atmospheric CO2 triggered Cenozoic glaciation. Antarctic glaciations affect global climate by lowering sea level, intensifying atmospheric circulation, and increasing planetary albedo. Ice sheets interact with ocean water, forming water masses that play a key role in global ocean circulation.
28
Lurcock, Pontus, und Fabio Florindo. Antarctic Climate History and Global Climate Changes. Oxford University Press, 2017. http://dx.doi.org/10.1093/oxfordhb/9780190699420.013.18.
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Antarctic climate changes have been reconstructed from ice and sediment cores and numerical models (which also predict future changes). Major ice sheets first appeared 34 million years ago (Ma) and fluctuated throughout the Oligocene, with an overall cooling trend. Ice volume more than doubled at the Oligocene-Miocene boundary. Fluctuating Miocene temperatures peaked at 17–14 Ma, followed by dramatic cooling. Cooling continued through the Pliocene and Pleistocene, with another major glacial expansion at 3–2 Ma. Several interacting drivers control Antarctic climate. On timescales of 10,000–100,000 years, insolation varies with orbital cycles, causing periodic climate variations. Opening of Southern Ocean gateways produced a circumpolar current that thermally isolated Antarctica. Declining atmospheric CO2 triggered Cenozoic glaciation. Antarctic glaciations affect global climate by lowering sea level, intensifying atmospheric circulation, and increasing planetary albedo. Ice sheets interact with ocean water, forming water masses that play a key role in global ocean circulation.
29
Dunlop, Storm. 9. Worldwide effects and forecasting. Oxford University Press, 2017. http://dx.doi.org/10.1093/actrade/9780199571314.003.0009.
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Observing the weather for purposes of forecasting is a worldwide enterprise. Routine measurements are made by national agencies in every country of the globe. These observations and their distribution are handled by international agreement and the World Meteorological Organization, a specialized agency of the United Nations. It has become obvious that events in one part of the world may have a great effect on weather experienced in distant regions. ‘Worldwide effects and forecasting’ considers these long-distance relationships between various atmospheric conditions—teleconnections—the most famous being El Niño. It also looks at the potential solar influence on Earth’s weather, as well as how chaos theory is used in ensemble forecasting.
30
Trencsényi, Balázs, Michal Kopeček, Luka Lisjak Gabrijelčič, Maria Falina, Mónika Baár und Maciej Janowski. A New State for “New Men”. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198737155.003.0006.
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Growing disappointment with party politics in the 1920s gave rise to discourses extolling the state as the principal actor of societal change. A common denominator of the various versions of etatism and technocratism in the region was a strong “anti-political” ideological reflex. In the 1930s, this was coupled with a discourse of a preventive strike, defending dictatorial policies as measures to hinder radical left- and right-wing movements from taking power. In turn, East Central European fascism emerged in the post-First World War atmosphere of insecurity and polarization. This was reinforced by the collapse of parliamentary democracy in the 1930s and the reconfiguration of the geopolitical framework of the region due to the rise of fascist Italy and Nazi Germany. The ensuing fascist projects offered a particularly violent ideological mixture, preventing any empathy toward ethnic and social groups targeted for persecution.
31
Wilsey, Brian J. Response of Grasslands to Global Change. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198744511.003.0007.
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Global change factors are ecologically-relevant variables that are changing, and that have global impacts. In grasslands, changes in the atmosphere, biological invasions, N deposition, and land-use change are global change factors. Photosynthesis increases under elevated CO2 and C3 plant species respond more strongly than C4 species to CO2 enrichment. Leaf N contents are typically lower under elevated CO2, especially in C3 species, and this is expected to have a negative effect on large grazing mammals. Temperature increases are expected to have significant effects on phenology. Most grasslands are being impacted by biological invasions to various degrees. Communities dominated by exotics are considered to be “novel systems” because they contain species from a variety of regions that do not have an evolutionary history of interaction. Among the most noxious grassland invaders is the red imported fire ant Solonopsis invicta, which lowers ant diversity and negatively affects prey species.
32
Merrill, Elizabeth M., Hrsg. Creating Place in Early Modern European Architecture. Amsterdam University Press, 2021. http://dx.doi.org/10.1017/9789048550814.
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The importance of place 'as a unique spatial identity' has been recognized since antiquity. Ancient references to the 'genius loci', or spirit of place, evoked not only the location of a distinct atmosphere or environment, but also the protection of this location, and implicitly, its making and construction. This volume examines the concept of place as it relates to architectural production and building knowledge in early modern Europe (1400-1800). The places explored in the book's ten essays take various forms, from an individual dwelling to a cohesive urban development to an extensive political territory. Within the scope of each study, the authors draw on primary source documents and original research to demonstrate the distinctive features of a given architectural place, and how these are related to a geographic location, social circumstances, and the contributions of individual practitioners. The essays underscore the distinct techniques, practices and organizational structures by which physical places were made in the early modern period.
33
Jacobsen, Dean, und Olivier Dangles. The high altitude environment. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780198736868.003.0001.
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Chapter 1 gives a brief overview of the climatic and terrestrial environment in which high altitude waters are embedded. This context is necessary to understand the prevailing environmental conditions in the aquatic systems. The chapter begins by defining high altitude, alpine, and mountain, and provides an overview of the distribution of the world’s main high altitude regions. The overall picture of the climatic setting is drawn, from the inevitable consequences of high altitude (low temperature, low atmospheric pressure, and high solar radiation) to the highly region-specific patterns in precipitation and wind. The various ways that highland regions are formed, their temporal evolution, and climatic changes are treated in a section on the palaeo-environmental perspective. Finally, general patterns in high altitude (alpine) vegetation zones and treelines on different continents are synthesized, as well as major soil-forming processes in the catchments surrounding aquatic systems.
34
12th International School-Seminar “Satellite Methods and Systems for Earth Exploration”. IKI, 2024. http://dx.doi.org/10.21046/2070-7401-12tarusa2024.
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The 12th International School-Seminar “Satellite Methods and Systems for Earth Exploration” took place in the town of Tarusa, at the Intercosmos representative office of Space Research Institute of the Russian Academy of Sciences on March 21–25, 2024. The main topics were devoted to various aspects of satellite methods of atmospheric and water objects studies. Six sessions were held, during which 6 lectures were delivered and 14 reports were made, and a master class called “Neural Networks in Earth Remote Sensing Tasks” was conducted. Researchers, postgraduates and students from 14 scientific organizations and higher educational institutions took part in the School-Conference. For the first time students from the People’s Republic of China attended the School-Seminar. Information about the program of the School-Seminar, including links to the presentations and the collection of materials, can be found at http://d33.infospace.ru/d33_conf/tarusa2024.html
35
Billing, Gert D., Hrsg. The Quantum Classical Theory. Oxford University Press, 2003. http://dx.doi.org/10.1093/oso/9780195146196.001.0001.
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Over a period of fifty years, the quantum-classical or semi-classical theories have been among the most popular for calculations of rates and cross sections for many dynamical processes: energy transfer, chemical reactions, photodissociation, surface dynamics, reactions in clusters and solutions, etc. These processes are important in the simulation of kinetics of processes in plasma chemistry, chemical reactors, chemical or gas lasers, atmospheric and interstellar chemistry, as well as various industrial processes. This book gives an overview of quantum-classical methods that are currently used for a theoretical description of these molecular processes. It gives the theoretical background for the derivation of the theories from first principles. Enough details are provided to allow numerical implementation of the methods. The book gives the necessary background for understanding the approximations behind the methods and the working schemes for treating energy transfer processes from diatomic to polyatomic molecules, reactions at surfaces, non-adiabatic processes, and chemical reactions.
36
Rosenzweig, Cynthia, und Daniel Hillel. Climate Variability and the Global Harvest. Oxford University Press, 2008. http://dx.doi.org/10.1093/oso/9780195137637.001.0001.
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The Earth's climate is constantly changing. Some of the changes are progressive, while others fluctuate at various time scales. The El Niño-la Niña cycle is one such fluctuation that recurs every few years and has far-reaching impacts. It generally appears at least once per decade, but this may vary with our changing climate. The exact frequency, sequence, duration and intensity of El Niño's manifestations, as well as its effects and geographic distributions, are highly variable. The El Niño-la Niña cycle is particularly challenging to study due to its many interlinked phenomena that occur in various locations around the globe. These worldwide teleconnections are precisely what makes studying El Niño-la Niña so important. Cynthia Rosenzweig and Daniel Hillel describe the current efforts to develop and apply a global-to-regional approach to climate-risk management. They explain how atmospheric and social scientists are cooperating with agricultural practitioners in various regions around the world to determine how farmers may benefit most from new climate predictions. Specifically, the emerging ability to predict the El Niño-Southern Oscillation (ENSO) cycle offers the potential to transform agricultural planning worldwide. Biophysical scientists are only now beginning to recognize the large-scale, globally distributed impacts of ENSO on the probabilities of seasonal precipitation and temperature regimes. Meanwhile, social scientists have been researching how to disseminate forecasts more effectively within rural communities. Consequently, as the quality of climatic predictions have improved, the dissemination and presentation of forecasts have become more effective as well. This book explores the growing understanding of the interconnectedness of climate predictions and productive agriculture for sustainable development, as well as methods and models used to study this relationship.
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Lavoisier, Antoine Laurent. Essays, on the Effects Produced by Various Processes on Atmospheric Air; with a Particular View to an Investigation of the Constitution of the Acids. by M. Lavoisier, ... Translated from the French, by Thomas Henry,. Creative Media Partners, LLC, 2018.
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Netzer, Falko P., und Claudine Noguera. Oxide Thin Films and Nanostructures. Oxford University Press, 2021. http://dx.doi.org/10.1093/oso/9780198834618.001.0001.
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Nanostructured oxide materials ultra-thin films, nanoparticles and other nanometer-scale objects play prominent roles in many aspects of our every-day life, in nature and in technological applications, among which is the all-oxide electronics of tomorrow. Due to their reduced dimensions and dimensionality, they strongly interact with their environment gaseous atmosphere, water or support. Their novel physical and chemical properties are the subject of this book from both a fundamental and an applied perspective. It reviews and illustrates the various methodologies for their growth, fabrication, experimental and theoretical characterization. The role of key parameters such as film thickness, nanoparticle size and support interactions in driving their fundamental properties is underlined. At the ultimate thickness limit, two-dimensional oxide materials are generated, whose functionalities and potential applications are described. The emerging field of cation mixing is mentioned, which opens new avenues for engineering many oxide properties, as witnessed by natural oxide nanomaterials such as clay minerals, which, beyond their role at the Earth surface, are now widely used in a whole range of human activities. Oxide nanomaterials are involved in many interdisciplinary fields of advanced nanotechnologies: catalysis, photocatalysis, solar energy materials, fuel cells, corrosion protection, and biotechnological applications are amongst the areas where they are making an impact; prototypical examples are outlined. A cautious glimpse into future developments of scientific activity is finally ventured to round off the treatise.
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Johansen, Bruce E. Global Warming 101. Greenwood Publishing Group, Inc., 2008. http://dx.doi.org/10.5040/9798400657900.
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The accelerating pace of global warming is provoking anxiety that the Earth is reaching an ominous threshold, a point of no return. Within a decade or two, various feedbacks may take greenhouse warming past any human ability to contain or reverse it. Carbon-dioxide levels in the atmosphere are rising rapidly, fed by increasing fossil-fuel use world-wide, melting permafrost, slash-and-burn agriculture in Indonesia and Brazil, increasing wildfires, as well as rapid industrialization using dirty coal in China and India. Global warming may well become the most urgent problem the world faces during the 21st Century . Natural variations are no longer the major contribution (or forcing) in Earth's climate. Human contributions became the major factor about 1950. This book has been prepared as a reference for high-school students, but it also will be useful for anyone who wants a compact, plain-spoken basic guide to the science of global warming. Global Warming 101 begins with an examination of basic issues, followed by important controversies in the field. The book then describes scientific issues related to melting ice, rising seas, and effects on plants and animals, as well as human health. Global Warming 101 concludes with consideration of possible solutions. Global Warming 101 combines a survey of the science of global warming with reporting from around the world, from sinking Pacific islands and thawing Arctic permafrost, which indicate that significant global warming already has begun.
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Suthers, Iain, David Rissik und Anthony Richardson, Hrsg. Plankton. CSIRO Publishing, 2019. http://dx.doi.org/10.1071/9781486308804.
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Healthy waterways and oceans are essential for our increasingly urbanised world. Yet monitoring water quality in aquatic environments is a challenge, as it varies from hour to hour due to stormwater and currents. Being at the base of the aquatic food web and present in huge numbers, plankton are strongly influenced by changes in environment and provide an indication of water quality integrated over days and weeks. Plankton are the aquatic version of a canary in a coal mine. They are also vital for our existence, providing not only food for fish, seabirds, seals and sharks, but producing oxygen, cycling nutrients, processing pollutants, and removing carbon dioxide from our atmosphere.
This Second Edition of Plankton is a fully updated introduction to the biology, ecology and identification of plankton and their use in monitoring water quality. It includes expanded, illustrated descriptions of all major groups of freshwater, coastal and marine phytoplankton and zooplankton and a new chapter on teaching science using plankton. Best practice methods for plankton sampling and monitoring programs are presented using case studies, along with explanations of how to analyse and interpret sampling data.
Plankton is an invaluable reference for teachers and students, environmental managers, ecologists, estuary and catchment management committees, and coastal engineers.
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Zeitlin, Vladimir. Geophysical Fluid Dynamics. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198804338.001.0001.
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The book explains the key notions and fundamental processes in the dynamics of the fluid envelopes of the Earth (transposable to other planets), and methods of their analysis, from the unifying viewpoint of rotating shallow-water model (RSW). The model, in its one- or two-layer versions, plays a distinguished role in geophysical fluid dynamics, having been used for around a century for conceptual understanding of various phenomena, for elaboration of approaches and methods, to be applied later in more complete models, for development and testing of numerical codes and schemes of data assimilations, and many other purposes. Principles of modelling of large-scale atmospheric and oceanic flows, and corresponding approximations, are explained and it is shown how single- and multi-layer versions of RSW arise from the primitive equations by vertical averaging, and how further time-averaging produces celebrated quasi-geostrophic reductions of the model. Key concepts of geophysical fluid dynamics are exposed and interpreted in RSW terms, and fundamentals of vortex and wave dynamics are explained in Part 1 of the book, which is supplied with exercises and can be used as a textbook. Solutions of the problems are available at Editorial Office by request. In-depth treatment of dynamical processes, with special accent on the primordial process of geostrophic adjustment, on instabilities in geophysical flows, vortex and wave turbulence and on nonlinear wave interactions follows in Part 2. Recently arisen new approaches in, and applications of RSW, including moist-convective processes constitute Part 3.
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Busuioc, Aristita, und Alexandru Dumitrescu. Empirical-Statistical Downscaling: Nonlinear Statistical Downscaling. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.770.
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This is an advance summary of a forthcoming article in the Oxford Research Encyclopedia of Climate Science. Please check back later for the full article.The concept of statistical downscaling or empirical-statistical downscaling became a distinct and important scientific approach in climate science in recent decades, when the climate change issue and assessment of climate change impact on various social and natural systems have become international challenges. Global climate models are the best tools for estimating future climate conditions. Even if improvements can be made in state-of-the art global climate models, in terms of spatial resolution and their performance in simulation of climate characteristics, they are still skillful only in reproducing large-scale feature of climate variability, such as global mean temperature or various circulation patterns (e.g., the North Atlantic Oscillation). However, these models are not able to provide reliable information on local climate characteristics (mean temperature, total precipitation), especially on extreme weather and climate events. The main reason for this failure is the influence of local geographical features on the local climate, as well as other factors related to surrounding large-scale conditions, the influence of which cannot be correctly taken into consideration by the current dynamical global models.Impact models, such as hydrological and crop models, need high resolution information on various climate parameters on the scale of a river basin or a farm, scales that are not available from the usual global climate models. Downscaling techniques produce regional climate information on finer scale, from global climate change scenarios, based on the assumption that there is a systematic link between the large-scale and local climate. Two types of downscaling approaches are known: a) dynamical downscaling is based on regional climate models nested in a global climate model; and b) statistical downscaling is based on developing statistical relationships between large-scale atmospheric variables (predictors), available from global climate models, and observed local-scale variables of interest (predictands).Various types of empirical-statistical downscaling approaches can be placed approximately in linear and nonlinear groupings. The empirical-statistical downscaling techniques focus more on details related to the nonlinear models—their validation, strengths, and weaknesses—in comparison to linear models or the mixed models combining the linear and nonlinear approaches. Stochastic models can be applied to daily and sub-daily precipitation in Romania, with a comparison to dynamical downscaling. Conditional stochastic models are generally specific for daily or sub-daily precipitation as predictand.A complex validation of the nonlinear statistical downscaling models, selection of the large-scale predictors, model ability to reproduce historical trends, extreme events, and the uncertainty related to future downscaled changes are important issues. A better estimation of the uncertainty related to downscaled climate change projections can be achieved by using ensembles of more global climate models as drivers, including their ability to simulate the input in downscaling models. Comparison between future statistical downscaled climate signals and those derived from dynamical downscaling driven by the same global model, including a complex validation of the regional climate models, gives a measure of the reliability of downscaled regional climate changes.
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Lilja, Sven. Climate, History, and Social Change in Sweden and the Baltic Sea Area From About 1700. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.633.
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The growing concern about global warming has turned focus in Sweden and other Baltic countries toward the connection between history and climate. Important steps have been taken in the scientific reconstruction of climatic parables. Historic climate data have been published and analyzed, and various proxy data have been used to reconstruct historic climate curves. The results have revealed an ongoing regional warming from the late 17th to the early 21st century. The development was not continuous, however, but went on in a sequence of warmer and colder phases.Within the fields of history and socially oriented climate research, the industrial revolution has often been seen as a watershed between an older and a younger climate regime. The breakthrough of the industrial society was a major social change with the power to influence climate. Before this turning point, man and society were climate dependent. Weather and short-term climate fluctuations had major impacts on agrarian culture. When the crops failed several years in sequence, starvation and excess mortality followed. As late as 1867–1869, northern Sweden and Finland were struck by starvation due to massive crop failures.Although economic activities in the agricultural sector had climatic effects before the industrial society, when industrialization took off in Sweden in the 1880s it brought an end to the large-scale starvations, but also the start of an economic development that began to affect the atmosphere in a new and broader way. The industrial society, with its population growth and urbanization, created climate effects. Originally, however, the industrial outlets were not seen as problems. In the 18th century, it was thought that agricultural cultivation could improve the climate, and several decades after the industrial take-off there still was no environmental discourse in the Swedish debate. On the contrary, many leading debaters and politicians saw the tall chimneys, cars, and airplanes as hopeful signs in the sky. It was not until the late 1960s that the international environmental discourse reached Sweden. The modern climate debate started to make its imprints as late as the 1990s.During the last two decades, the Swedish temperature curve has unambiguously turned upwards. Thus, parallel to the international debate, the climate issue has entered the political agenda in Sweden and the other Nordic countries. The latest development has created a broad political consensus in favor of ambitious climate goals, and the people have gradually started to adapt their consumption and lifestyles to the new prerequisites.Although historic climate research in Sweden has had a remarkable expansion in the last decades, it still leans too much on its climate change leg. The clear connection between the climate fluctuations during the last 300 years and the major social changes that took place in these centuries needs to be further studied.
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Pomer, Janice. Elementary Dance Education. Human Kinetics, 2023. http://dx.doi.org/10.5040/9781718227408.
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Children love to observe, explore, learn, and create. Elementary Dance Education helps them do all four. And it does so in a unique way, shaping its movement activities around nature themes. In fact, all of the learning experiences are based on different aspects of nature, as the text intertwines children’s innate curiosity and observation skills with the processes of scientific inquiry and artistic creation. Elementary Dance Education helps teachers develop the instructional skills they need to incorporate dance into their curricula, providing over 70 movement activities and exercises for students in grades K-6. The activities, which stimulate children’s minds and bodies through the process of collaborative dance creation, include variations for younger and older students. Ideas are offered for partner or small-group explorations, making the activities more inclusive and appropriate for each age group. Another unique feature of this book is the original music accompanying it. Teachers have access to 90 minutes of dynamic sounds, rhythmic percussion, captivating electro-acoustic compositions, and gentle atmospheric selections, delivered through HKPropel, to accompany the learning experiences. The compositions support students’ movement explorations, conveying a range of images and emotions and inspiring a variety of responses. In addition, Elementary Dance Education offers the following: Discussion questions for each exercise, prompting in-class discussion and student exploration; the questions come with sample answers or ideas to encourage student responses and spur a fruitful discussion75 photos and several diagrams to illustrate positions and poses and stimulate ideas for the movement exercisesJournal prompts, tailored for older and younger children, to give students the opportunity to respond and reflect on the learning experiencesVideo links (provided in HKPropel) to help illustrate concepts and exercises, offer examples, or encourage students to watch for something specific in an activity The book’s first chapter introduces the basic elements of dance; the remaining seven chapters offer movement exercises in various areas of nature: plants, animals, water, earth, sky, people, and other wonders. This book is a rich and easy-to-implement resource not only for elementary dance educators and physical educators but for classroom teachers as well. The exercises in this book use a template for movement discovery in which students will observe, explore, create, and share. This template “can be applied to all areas of the curriculum,” says author Janice Pomer. “It’s an invaluable tool for student engagement, satisfying children’s capacity to watch, wonder, move, interact, discover, and share.” Elementary Dance Education will promote children’s creativity and curiosity, engage and challenge their minds and bodies, and help them learn to appreciate and support each other as they work together exploring, creating, and sharing their ideas and insights about the natural world through dance. Note: A code for accessing HKPropel is included with all new print books.
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Stamenkoviç, Marko, Hrsg. Resistance. 2. Aufl. punctum books, 2021. http://dx.doi.org/10.53288/0384.1.00.
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esistance features a selection of overtly non-conformist positions in the contemporary visual art scene of Albania vis-à-vis the most recent social, political, and economic turmoils in the Western Balkans – a region marked by the dark side of political governances that have remained “democratic” in their outward appearance (especially toward the European Union), while dramatically leaning toward autocratic regimes in the eyes of their own citizens. Regardless of their citizens’ primary interests, and despite some positive signals surfacing in the international media, almost every attempt to establish lasting conditions for democratic governance in the Western Balkans has been shrouded in the veil of profit-driven political scandals, personal greed for more and more power over the people’s rights, and the extinction of public property in pursuit of social elite’s corporate and private interests. Additionally, and more specifically related to Tirana, artists and citizens have, over the years, been involved in various types of revolt, expressing their disagreements with the ongoing destruction of public property in the name of “modernization and development”: a movement led by local political powers through financially and strategically motivated processes of architectural cannibalism – not only at the expense of erasing Albanian cultural heritage or long-term residents’ habitats, but also at the expense of taking human lives under the pretext of “urbanization.” The most obvious instance of this economy of destruction was the complex of buildings linked to the National Theater of Albania in downtown Tirana that has served as a symbolic and material place of citizens’ resistance: for more than two years, together with local artists, they have been opposing the government’s plans to demolish the old complex in order to build a new one – until this finally happened in Spring 2020, in the midst of the ongoing COVID19 pandemic. Rooted in the atmosphere of the National Theater Protests in Tirana, RESISTANCE was conceived in Summer 2019 by ZETA Center for Contemporary Art as the International Artists-in-Residence Program, in cooperation with three partner organizations from Kosovo, Serbia and North Macedonia (Stacion – Center for Contemporary Art in Prishtina; Ilija & Mangelos Foundation in Novi Sad; and Faculty of Things That Can’t Be Learned in Bitola) and supported by Swiss Cultural Fund in Albania, a project of the Swiss Agency for Development and Cooperation. Gradually, the project expanded into an exhibition (Heterotopias of Resistance, curated by Blerta Hoçia and featuring works by Lori Lako, Fatlum Doçi, Edona Kryeziu, Nina Galiç, Darko Vukiç, Nikola Slavevski, and Natasha Nedelkova) and a series of interviews and panel discussions (with contributions by Lindita Komani, Edmond Budina, Ervin Goci, Ergin Zaloshnja, Pleurad Xhafa, Gentian Shkurti, Stefano Romano, Luçjan Bedeni, HAVEIT, Leonard Qylafi, Jonida Gashi, and Fatmira Nikolli). The results of both have been collected and presented in the format of a publication that, besides serving as an indispensable reading material concerning visual arts and politics in contemporary Albania, especially to those abroad, functions by itself as a form of resistance against contagious cultural policies in weak post-socialist “democracies” in Southeastern Europe.