Bücher: „MELTING CHARGE“

1

Kotter, John P. Our iceberg is melting. [Seattle, Wash.]: J. Kotter and H. Rathgeber, 2005.

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2

ill, Bersani Shennen, Hrsg. The glaciers are melting! Mt. Pleasant, SC: Sylvan Dell Pub., 2011.

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3

Melting point: New Zealand and the climate change crisis. North Shore, N.Z: Penguin Books/Penguin Group, 2008.

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4

Holger, Rathgeber, Hrsg. Bing shan zai rong hua: Our lceberg is melting. Hefei: An'hui ren min chu ban she, 2006.

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5

The melting edge: Alaska at the frontier of climate change. Anchorage, AK: Alaska Geographic Association, 2011.

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6

Kotter, John, Holger Rathgeber und Spenser Johnson. Our Iceberg Is Melting: Changing and Succeeding Under Any Conditions. New York: St. Martin's Press, 2006.

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7

Carey, Mark. In the shadow of melting glaciers: Climate change and Andean society. Oxford: Oxford University Press, 2010.

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8

Carey, Mark. In the shadow of melting glaciers: Climate change and Andean society. New York: Oxford University Press, 2010.

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9

In the shadow of melting glaciers: Climate change and Andean society. New York: Oxford University Press, 2010.

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10

Polar bear, why is your world melting? Morton Grove, Ill: Albert Whitman & Co., 2008.

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11

Struzik, Edward. The big thaw: Travels in the melting north. Mississauga, ON: John Wiley & Sons Canada, 2009.

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12

The big thaw: Travels in the melting north. Mississauga, ON: John Wiley & Sons Canada, 2009.

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13

Holger, Rathgeber, Hrsg. Our iceberg is melting: Changing and succeeding under any conditions. New York: St. Martin's Press, 2006.

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14

Eurotherm, Seminar (30th 1992 Orsay France). Heat transfer in phase-change processes: Melting and solidification : Eurotherm Seminar 30 proceedings : October 22-23, 1992, Orsay, France. [France?]: s.n., 1992.

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15

National Heat Transfer Conference (29th 1993 Atlanta, Ga.). Heat transfer in melting, solidification, and crystal growth, 1993: Presented at the 29th National Heat Transfer Conference, Atlanta, Georgia, August 8-11, 1993. New York: American Society of Mechanical Engineers, 1993.

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16

American Society of Mechanical Engineers. Winter Meeting. Fundamentals of Phase Change: Freezing, Melting, and Sublimation--1992 : presented at the Winter Annual Meeting of the American Society of Mechanical Engineers, Anaheim, California, November 8-13, 1992. New York, N.Y: American Society of Mechanical Engineers, 1992.

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17

Our Iceberg Is Melting. PAN MACMILLAN U.K, 2017.

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18

Below Freezing: Elegy for the Melting Planet. University of New Mexico Press, 2018.

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19

Brave New Arctic: The Untold Story of the Melting North. Princeton University Press, 2020.

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20

Brave new Arctic: The untold story of the melting North. Princeton University Press, 2018.

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21

Serreze, Mark C. Brave New Arctic: The Untold Story of the Melting North. Princeton University Press, 2018.

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22

Fundamentals of Phase Change: Freezing, Melting, & Sublimation - 1992 (Htd). American Society of Mechanical Engineers, 1992.

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23

Johnson, Elizabeth Lominska, und Graham E. Johnson. A Chinese Melting Pot. Hong Kong University Press, 2019. http://dx.doi.org/10.5790/hongkong/9789888455898.001.0001.

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A Chinese Melting Pot: Original People and Immigrants in Hong Kong’s First ‘New Town’ traces the transformation of Tsuen Wan from a poor and marginal district of agricultural villages, culturally distinctive in that all were Hakka. Like others present in the New Territories in 1898, they enjoyed special privileges under British colonialism as ‘original inhabitants’. This study is focused, in part, on one of their villages: its history, lineages, relationships among and through women, and their songs and laments. In the aftermath of the Japanese occupation and revolution in China, the town, with its daily coastal market, rapidly grew into a major industrial area and assumed an intense, if chaotic, urban form. Its industries attracted enormous numbers of immigrants from China, who created a large variety of voluntary associations to ease their adaptation to the new environment, while the original inhabitants, as property owners, benefited financially from the immigrants’ need for housing, and politically from continuing government support. In the 1980s, changes in economic policies in China led to Tsuen Wan’s present post-industrial form. The original inhabitants remain as a small fragment of the population, their villages intact, although re-sited away from the town centre as part of greatly increased government intervention in creating a planned ‘new town’. Their language and traditions are disappearing as they, like the immigrants, are absorbed into the wider Hong Kong lifestyle.

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24

Kotter, John. Our Iceberg Is Melting: Changing and Succeeding Under Any Conditions. Macmillan Audio, 2006.

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25

Our Iceberg Is Melting: Changing and Succeeding Under Any Conditions. Penguin Random House, 2016.

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26

Jacobsen, Dean, und Olivier Dangles. High altitude waters in the face of climate change. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780198736868.003.0008.

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Chapter 8 focuses on the effects of warming and changes in precipitation patterns on aquatic life at high altitude. Located near the edge of their climatic limits, in regions where the rate of warming is generally amplified compared with lowlands, high altitude aquatic systems present a high sensitivity to climate change. Changes in mountain climate create a number of indirect effects on aquatic life through the control of hydrological systems and processes, particularly those associated with the cryosphere (e.g. permafrost and ice melting) and the soil–vegetation interface (e.g. treeline expansion). The chapter then presents the three basic options faced by all aquatic organisms as their environmental conditions alter as a result of climate change: adapt, migrate, or perish. At an ecosystem level, small changes in physical, chemical, or biological characteristics can be amplified into major shifts in limnological properties.

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27

Xu, Jianchu, und International Centre for Integrated Mountain Development, Hrsg. The melting Himalayas: Regional challenges and local impacts of climate change on mountain ecosystems and livelihoods. Kathmandu: International Centre for Integrated Mountain Development, 2007.

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28

Kister, Chad. Arctic Melting: How Climate Change Is Destroying One of the World's Largest Wilderness Areas. Common Courage Press, 2008.

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29

Kister, Chad. Arctic Melting: How Climate Change Is Destroying One of the World's Largest Wilderness Areas. Common Courage Press, 2008.

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30

Arctic Melting: How Global Warming Is Destroying One Of The World's Largest Wilderness Areas. Common Courage Press, 2005.

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31

Arctic Melting: How Global Warming Is Destroying One Of The World's Largest Wilderness Areas. Common Courage Press, 2006.

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32

Effect of microgravity on material undergoing melting and freezing: The TES experiment. [Washington, DC]: National Aeronautics and Space Administration, 1995.

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33

Bayazitoglu, Y. Fundamentals of Phase Change: Freezing, Melting, and Sublimation (Proceedings of the Asme Heat Transfer Division). Amer Society of Mechanical, 1990.

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34

Melting away: A ten-year journey through our endangered polar regions. 2015.

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35

Lau, William K. M. Impacts of Aerosols on Climate and Weather in the Hindu-Kush-Himalayas-Gangetic Region. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.590.

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Situated at the southern edge of the Tibetan Plateau (TP), the Hindu-Kush-Himalayas-Gangetic (HKHG) region is under the clear and present danger of climate change. Flash-flood, landslide, and debris flow caused by extreme precipitation, as well as rapidly melting glaciers, threaten the water resources and livelihood of more than 1.2 billion people living in the region. Rapid industrialization and increased populations in recent decades have resulted in severe atmospheric and environmental pollution in the region. Because of its unique topography and dense population, the HKHG is not only a major source of pollution aerosol emissions, but also a major receptor of large quantities of natural dust aerosols transported from the deserts of West Asia and the Middle East during the premonsoon and early monsoon season (April–June). The dust aerosols, combined with local emissions of light-absorbing aerosols, that is, black carbon (BC), organic carbon (OC), and mineral dust, can (a) provide additional powerful heating to the atmosphere and (b) allow more sunlight to penetrate the snow layer by darkening the snow surface. Both effects will lead to accelerated melting of snowpack and glaciers in the HKHG region, amplifying the greenhouse warming effect. In addition, these light-absorbing aerosols can interact with monsoon winds and precipitation, affecting extreme precipitation events in the HKHG, as well as weather variability and climate change over the TP and the greater Asian monsoon region.

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36

DeAugustinas, M., und A. Kiely. Periocular Infections. Oxford University Press, 2016. http://dx.doi.org/10.1093/med/9780199976805.003.0015.

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Periocular Infections occur when there is inflammation of the conjunctiva. Uncomplicated viral infections can usually be managed with careful hand hygiene and lubrication of the eye with artificial tears. More severe infections are notable for purulent discharge, membrane formation, and scarring, and can lead to corneal change. For suspected bacterial conjunctivitis, empiric therapy begins with broad spectrum antibiotic eye drops or ointment, which are supplemented with oral antibiotics in cases associated with pharyngitis and in children with H. influenzae infection. For gonococcal conjunctivitis, systemic ceftriaxone is recommended for both adults and children (including neonates) due to the increasing prevalence of penicillin-resistant N. gonorrhoeae. If the cornea is not involved and the patient is extremely reliable, next day referral to an ophthalmologist in addition to management with IM ceftriaxone is sufficient. Otherwise, admission for IV therapy is advised. Copious, repeated irrigation is also advised to remove inflammatory mediators and debris that can contribute to corneal melting.

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37

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.

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38

Liu, Xiaodong, und Libin Yan. Elevation-Dependent Climate Change in the Tibetan Plateau. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.593.

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As a unique and high gigantic plateau, the Tibetan Plateau (TP) is sensitive and vulnerable to global climate change, and its climate change tendencies and the corresponding impact on regional ecosystems and water resources can provide an early alarm for global and mid-latitude climate changes. Growing evidence suggests that the TP has experienced more significant warming than its surrounding areas during past decades, especially at elevations higher than 4 km. Greater warming at higher elevations than at lower elevations has been reported in several major mountainous regions on earth, and this interesting phenomenon is known as elevation-dependent climate change, or elevation-dependent warming (EDW).At the beginning of the 21st century, Chinese scholars first noticed that the TP had experienced significant warming since the mid-1950s, especially in winter, and that the latest warming period in the TP occurred earlier than enhanced global warming since the 1970s. The Chinese also first reported that the warming rates increased with the elevation in the TP and its neighborhood, and the TP was one of the most sensitive areas to global climate change. Later, additional studies, using more and longer observations from meteorological stations and satellites, shed light on the detailed characteristics of EDW in terms of mean, minimum, and maximum temperatures and in different seasons. For example, it was found that the daily minimum temperature showed the most evident EDW in comparison to the mean and daily maximum temperatures, and EDW is more significant in winter than in other seasons. The mean daily minimum and maximum temperatures also maintained increasing trends in the context of EDW. Despite a global warming hiatus since the turn of the 21st century, the TP exhibited persistent warming from 2001 to 2012.Although EDW has been demonstrated by more and more observations and modeling studies, the underlying mechanisms for EDW are not entirely clear owing to sparse, discontinuous, and insufficient observations of climate change processes. Based on limited observations and model simulations, several factors and their combinations have been proposed to be responsible for EDW, including the snow-albedo feedback, cloud-radiation effects, water vapor and radiative fluxes, and aerosols forcing. At present, however, various explanations of the mechanisms for EDW are mainly derived from model-based research, lacking more solid observational evidence. Therefore, to comprehensively understand the mechanisms of EDW, a more extensive and multiple-perspective climate monitoring system is urgently needed in the areas of the TP with high elevations and complex terrains.High-elevation climate change may have resulted in a series of environmental consequences, such as vegetation changes, permafrost melting, and glacier shrinkage, in mountainous areas. In particular, the glacial retreat could alter the headwater environments on the TP and the hydrometeorological characteristics of several major rivers in Asia, threatening the water supply for the people living in the adjacent countries. Taking into account the climate-model projections that the warming trend will continue over the TP in the coming decades, this region’s climate change and the relevant environmental consequences should be of great concern to both scientists and the general public.

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39

McElroy, Michael B. Energy and Climate. Oxford University Press, 2016. http://dx.doi.org/10.1093/oso/9780190490331.001.0001.

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The climate of our planet is changing at a rate unprecedented in recent human history. The energy absorbed from the sun exceeds what is returned to space. The planet as a whole is gaining energy. The heat content of the ocean is increasing; the surface and atmosphere are warming; mid-latitude glaciers are melting; sea level is rising. The Arctic Ocean is losing its ice cover. None of these assertions are based on theory but on hard scientific fact. Given the science-heavy nature of climate change, debates and discussions have not played as big a role in the public sphere as they should, and instead are relegated to often misinformed political discussions and inaccessible scientific conferences. Michael B. McElroy, an eminent Harvard scholar of environmental studies, combines both his research chops and pedagogical expertise to present a book that will appeal to the lay reader but still be grounded in scientific fact. In Energy and Climate: Vision for the Future, McElroy provides a broad and comprehensive introduction to the issue of energy and climate change intended to be accessible for the general reader. The book includes chapters on energy basics, a discussion of the contemporary energy systems of the US and China, and two chapters that engage the debate regarding climate change. The perspective is global but with a specific focus on the US and China recognizing the critical role these countries must play in addressing the challenge of global climate change. The book concludes with a discussion of initiatives now underway to at least reduce the rate of increase of greenhouse gas emissions, together with a vision for a low carbon energy future that could in principle minimize the long-term impact of energy systems on global climate.

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40

Yıldız, Bayazıtoğlu, Kroeger Peter G, American Society of Mechanical Engineers. Winter Meeting und American Society of Mechanical Engineers. Heat Transfer Division., Hrsg. Fundamentals of phase change: Freezing, melting, and sublimation : presented at the Winter Annual Meeting of the American Society of Mechanical Engineers, Dallas, Texas, November 25-30, 1990. New York, N.Y: American Society of Mechanical Engineers, 1990.

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41

Bridges, John C. Evolution of the Martian Crust. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190647926.013.18.

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This is an advance summary of a forthcoming article in the Oxford Encyclopedia of Planetary Science. Please check back later for the full article.Mars, which has a tenth of the mass of Earth, has cooled as a single lithospheric plate. Current topography gravity maps and magnetic maps do not show signs of the plate tectonics processes that have shaped the Earth’s surface. Instead, Mars has been shaped by the effects of meteorite bombardment, igneous activity, and sedimentary—including aqueous—processes. Mars also contains enormous igneous centers—Tharsis and Elysium, with other shield volcanoes in the ancient highlands. In fact, the planet has been volcanically active for nearly all of its 4.5 Gyr history, and crater counts in the Northern Lowlands suggest that may have extended to within the last tens of millions of years. Our knowledge of the composition of the igneous rocks on Mars is informed by over 100 Martian meteorites and the results from landers and orbiters. These show dominantly tholeiitic basaltic compositions derived by melting of a relatively K, Fe-rich mantle compared to that of the Earth. However, recent meteorite and lander results reveal considerable diversity, including more silica-rich and alkaline igneous activity. These show the importance of a range of processes including crystal fractionation, partial melting, and possibly mantle metasomatism and crustal contamination of magmas. The figures and plots of compositional data from meteorites and landers show the range of compositions with comparisons to other planetary basalts (Earth, Moon, Venus). A notable feature of Martian igneous rocks is the apparent absence of amphibole. This is one of the clues that the Martian mantle had a very low water content when compared to that of Earth.The Martian crust, however, has undergone hydrothermal alteration, with impact as an important heat source. This is shown by SNC analyses of secondary minerals and Near Infra-Red analyses from orbit. The associated water may be endogenous.Our view of the Martian crust has changed since Viking landers touched down on the planet in 1976: from one almost entirely dominated by basaltic flows to one where much of the ancient highlands, particularly in ancient craters, is covered by km deep sedimentary deposits that record changing environmental conditions from ancient to recent Mars. The composition of these sediments—including, notably, the MSL Curiosity Rover results—reveal an ancient Mars where physical weathering of basaltic and fractionated igneous source material has dominated over extensive chemical weathering.

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42

Vuorinen, Ilppo. Post-Glacial Baltic Sea Ecosystems. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.675.

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Post-glacial aquatic ecosystems in Eurasia and North America, such as the Baltic Sea, evolved in the freshwater, brackish, and marine environments that fringed the melting glaciers. Warming of the climate initiated sea level and land rise and subsequent changes in aquatic ecosystems. Seminal ideas on ancient developing ecosystems were based on findings in Swedish large lakes of species that had arrived there from adjacent glacial freshwater or marine environments and established populations which have survived up to the present day. An ecosystem of the first freshwater stage, the Baltic Ice Lake initially consisted of ice-associated biota. Subsequent aquatic environments, the Yoldia Sea, the Ancylus Lake, the Litorina Sea, and the Mya Sea, are all named after mollusc trace fossils. These often convey information on the geologic period in question and indicate some physical and chemical characteristics of their environment. The ecosystems of various Baltic Sea stages are regulated primarily by temperature and freshwater runoff (which affects directly and indirectly both salinity and nutrient concentrations). Key ecological environmental factors, such as temperature, salinity, and nutrient levels, not only change seasonally but are also subject to long-term changes (due to astronomical factors) and shorter disturbances, for example, a warm period that essentially formed the Yoldia Sea, and more recently the “Little Ice Age” (which terminated the Viking settlement in Iceland).There is no direct way to study the post-Holocene Baltic Sea stages, but findings in geological samples of ecological keystone species (which may form a physical environment for other species to dwell in and/or largely determine the function of an ecosystem) can indicate ancient large-scale ecosystem features and changes. Such changes have included, for example, development of an initially turbid glacial meltwater to clearer water with increasing primary production (enhanced also by warmer temperatures), eventually leading to self-shading and other consequences of anthropogenic eutrophication (nutrient-rich conditions). Furthermore, the development in the last century from oligotrophic (nutrient-poor) to eutrophic conditions also included shifts between the grazing chain (which include large predators, e.g., piscivorous fish, mammals, and birds at the top of the food chain) and the microbial loop (filtering top predators such as jellyfish). Another large-scale change has been a succession from low (freshwater glacier lake) biodiversity to increased (brackish and marine) biodiversity. The present-day Baltic Sea ecosystem is a direct descendant of the more marine Litorina Sea, which marks the beginning of the transition from a primeval ecosystem to one regulated by humans. The recent Baltic Sea is characterized by high concentrations of pollutants and nutrients, a shift from perennial to annual macrophytes (and more rapid nutrient cycling), and an increasing rate of invasion by non-native species. Thus, an increasing pace of anthropogenic ecological change has been a prominent trend in the Baltic Sea ecosystem since the Ancylus Lake.Future development is in the first place dependent on regional factors, such as salinity, which is regulated by sea and land level changes and the climate, and runoff, which controls both salinity and the leaching of nutrients to the sea. However, uncertainties abound, for example the future development of the Gulf Stream and its associated westerly winds, which support the sub-boreal ecosystems, both terrestrial and aquatic, in the Baltic Sea area. Thus, extensive sophisticated, cross-disciplinary modeling is needed to foresee whether the Baltic Sea will develop toward a freshwater or marine ecosystem, set in a sub-boreal, boreal, or arctic climate.

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43

Orvell, Miles. Empire of Ruins. Oxford University Press, 2021. http://dx.doi.org/10.1093/oso/9780190491604.001.0001.

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Empire of Ruins explores the meaning of ruins in American culture, from the mid-nineteenth century to the twenty-first century, arguing that photographs have been the chief means by which the significance of ruins has been created in American culture. The book traces a historical argument that begins in the nineteenth century, when Americans yearned for the ruins of Europe, then moves to the discovery of Native American ruins in the Southwest. Later chapters explore the visualization of inner city ruins, abandoned factories, and shopping malls, and the “creative destruction” of buildings in order to make way for bigger ones. In addition, it analyzes the imagery of the 9/11 World Trade Center disaster; the ruins of the industrial landscape through mining operations; the ruins created by natural disasters like Hurricanes Katrina and Sandy; and the ruins produced by climate change, including the melting of the ice caps. Empire of Ruins considers, in conclusion, the way the picturing of ruins has served to mark revolutionary moments in political culture, symbolizing the choices societies must make. Empire of Ruins focuses mainly on photography, but it encompasses painting, literature, and popular films as well, in order to provide a larger picture of the cultural meaning of ruins. At the same time, it examines the powerful aesthetic attraction of ruin imagery in photographs and films, showing how the Destructive Sublime, a new category of experience, evokes contrary responses in viewers.

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Bücher zum Thema „MELTING CHARGE“

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