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1
Mellen, R. H. Global model for sound absorption in sea water. Newport, R.I: Naval Underwater Systems Center, 1987.
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3
Global and regional climate interaction: The Caspian Sea experience. Dordrecht: Kluwer Academic, 1994.
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4
United States. Congress. Senate. Committee on Energy and Natural Resources. Sea level rise: Hearing before the Committee on Energy and Natural Resources, United States Senate, One Hundred Twelfth Congress, second session, to receive testimony on the impacts of sea level rise on domestic energy and water infrastructure, April 19, 2012. Washington: U.S. G.P.O., 2012.
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5
International Meeting "Cities on Water". (1st 1989 Venice, Italy). Impact of sea level rise on cities and regions: Proceedings of the First International Meeting "Cities on Water", Venice, December 11-13, 1989. Venice: Marsilio Editori, 1991.
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6
Wahyudi, S. Imam. Polder system development model for handling of sea water level rising caused by global warming: Research report first year, overseas research collaboration and international publication. Semarang]: Universitas Islam Sultan Agung, 2010.
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7
Wahyudi, S. Imam. Polder system development model for handling of sea water level rising caused by global warming: Research report first year, overseas research collaboration and international publication. Semarang]: Universitas Islam Sultan Agung, 2010.
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8
Lurcock, Pontus, and 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.
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Lurcock, Pontus, and 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.
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The World Market for Common Salt, Rock Salt, Sea Salt, Sea Water, and Pure Sodium Chloride: A 2004 Global Trade Perspective. Icon Group International, Inc., 2005.
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11
Parker, Philip M. The World Market for Common Salt, Rock Salt, Sea Salt, Sea Water, and Pure Sodium Chloride: A 2007 Global Trade Perspective. ICON Group International, Inc., 2006.
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12
Joseph, Rhea W., Tran An Van, and Jet Propulsion Laboratory (U.S.), eds. Joint Global Ocean Flux Study, Hawaii Ocean Time-Series, HOT-3: R/V Moana Wave, January 6-10, 1989. Pasadena, Calif: National Aeronautics and Space Administration, Jet Propulsion Laboratory, California Institute of Technology, 1990.
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13
Ranganathan, Surabhi. The Law of the Sea and Natural Resources. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198825210.003.0008.
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Ranganathan’s chapter observes that the construction of the oceans as a global commons has changed over time. Once asserted as an arena of freedoms, the oceans are now enclosed in large part within national and international jurisdictions. However, sovereign rights are accompanied by community obligations. The deep seabed and its mineral resources, in particular, are designated the common heritage of mankind. The chapter traces the evolution of this concept. Following a roughly chronological approach, it situates legal developments in political and economic context. Noting that the concept does not conform to a broad narrative of progress—a high-water mark reached in the 1980s was followed by a period of recession—the chapter evaluates whether the current framework offers an appropriate expression. It supplies the tools for a fine-grained analysis of the degree to which international law realizes this particular community obligation in principle and in practice.
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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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Räisänen, Jouni. Future Climate Change in the Baltic Sea Region and Environmental Impacts. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.634.
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The warming of the global climate is expected to continue in the 21st century, although the magnitude of change depends on future anthropogenic greenhouse gas emissions and the sensitivity of climate to them. The regional characteristics and impacts of future climate change in the Baltic Sea countries have been explored since at least the 1990s. Later research has supported many findings from the early studies, but advances in understanding and improved modeling tools have made the picture gradually more comprehensive and more detailed. Nevertheless, many uncertainties still remain.In the Baltic Sea region, warming is likely to exceed its global average, particularly in winter and in the northern parts of the area. The warming will be accompanied by a general increase in winter precipitation, but in summer, precipitation may either increase or decrease, with a larger chance of drying in the southern than in the northern parts of the region. Despite the increase in winter precipitation, the amount of snow is generally expected to decrease, as a smaller fraction of the precipitation falls as snow and midwinter snowmelt episodes become more common. Changes in windiness are very uncertain, although most projections suggest a slight increase in average wind speed over the Baltic Sea. Climatic extremes are also projected to change, but some of the changes will differ from the corresponding change in mean climate. For example, the lowest winter temperatures are expected to warm even more than the winter mean temperature, and short-term summer precipitation extremes are likely to become more severe, even in the areas where the mean summer precipitation does not increase.The projected atmospheric changes will be accompanied by an increase in Baltic Sea water temperature, reduced ice cover, and, according to most studies, reduced salinity due to increased precipitation and river runoff. The seasonal cycle of runoff will be modified by changes in precipitation and earlier snowmelt. Global-scale sea level rise also will affect the Baltic Sea, but will be counteracted by glacial isostatic adjustment. According to most projections, in the northern parts of the Baltic Sea, the latter will still dominate, leading to a continued, although decelerated, decrease in relative sea level. The changes in the physical environment and climate will have a number of environmental impacts on, for example, atmospheric chemistry, freshwater and marine biogeochemistry, ecosystems, and coastal erosion. However, future environmental change in the region will be affected by several interrelated factors. Climate change is only one of them, and in many cases its effects may be exceeded by other anthropogenic changes.
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Petersen-Perlman, Jacob D., Julie E. Watson, and Aaron T. Wolf. Transboundary Unbound. Edited by Ken Conca and Erika Weinthal. Oxford University Press, 2017. http://dx.doi.org/10.1093/oxfordhb/9780199335084.013.19.
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This chapter calls for a new examination of the water conflict‒cooperation dialogue, beyond the traditional areas of water allocation and utilization. It calls for dialogue to incorporate two critical dimensions: (1) variability linked to climate change and the water-food-energy-environment nexus when framing parameters of water-related conflict; and (2) “unbounding” of analysis beyond political and geographical borders to include internal, regional, and global conflict and cooperation. It discusses three basins as case studies: the Nile, the Mekong, and the Aral Sea. It discusses how water conflicts are not bound to political or natural borders, or to disputes explicitly over water. Rather, it explores how resources intrinsically tied to water decisions may prompt conflict; yet, water may be a leverage point for peace, as well. It concludes by identifying relevant water-conflict transformation strategies that may be applied to use water as a nexus for peace-building.
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Evans, David J. A. Glaciation: A Very Short Introduction. Oxford University Press, 2018. http://dx.doi.org/10.1093/actrade/9780198745853.001.0001.
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Vast, majestic, and often stunningly beautiful, glaciers lock up some 10 per cent of the world’s fresh water. These great bodies of ice play an important part in the Earth system, carving landscapes and influencing climate on regional and hemispheric scales, as well as having a significant impact on global sea level. Glaciation: A Very Short Introduction offers an overview of glaciers and ice sheets as systems, considering the role of geomorphology and sedimentology in studying them, and their impacts on our planet in terms of erosional and depositional processes. Looking at our glaciers today, and their ongoing processes, it considers the extent to which we can use this knowledge in reconstructing and interpreting ancient glacial landscapes.
18
Shue, Henry. Basic Rights. Princeton University Press, 2020. http://dx.doi.org/10.23943/princeton/9780691202280.001.0001.
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Since its original publication, this book has proven increasingly influential to those working in political philosophy, human rights, global justice, and the ethics of international relations and foreign policy, particularly in debates regarding foreign policy's role in alleviating global poverty. The book asks: Which human rights ought to be the first honored and the last sacrificed? It argues that subsistence rights, along with security rights and liberty rights, serve as the ground of all other human rights. This classic work, now available in a thoroughly updated fortieth-anniversary edition, includes a substantial new chapter examining how the accelerating transformation of our climate progressively undermines the bases of subsistence like sufficient water, affordable food, and housing safe from forest-fires and sea-level rise. Climate change threatens basic rights.
19
James, Harrison. 6 Marine Environmental Threats from Shipping. Oxford University Press, 2017. http://dx.doi.org/10.1093/law/9780198707325.003.0006.
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The prevention of pollution from ships as a topic is largely addressed at the global level through the International Maritime Organization (IMO). Chapter 6 analyses the main treaties in this field, including the International Convention on the Prevention of Pollution from Ships (MARPOL Convention), the International Convention on the Safety of Life at Sea (SOLAS Convention), the International Convention on Ballast Water Management, and the International Convention on Anti-Fouling Substances. The analysis addresses both the types of rules employed in the IMO treaties and the processes through which the rules are amended and updated over time. The standards prescribed by these treaties are not only relevant to their Parties but also have a wider influence through the operation of rules of reference contained in United Nations Convention on the Law of the Sea (UNCLOS). The chapter also takes into account the emergence of broader concerns relating to the impact of shipping on marine biodiversity, such as noise pollution and ship strikes and the challenges in the implementation and enforcement of international shipping standards.
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Koyagi, Mikiya. Iran in Motion. Stanford University Press, 2021. http://dx.doi.org/10.11126/stanford/9781503613133.001.0001.
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Completed in 1938, the Trans-Iranian Railway connected Tehran to Iran's two major bodies of water: the Caspian Sea in the north and the Persian Gulf in the south. Iran's first national railway, it produced and disrupted various kinds of movement—voluntary and forced, intended and unintended, on different scales and in different directions—among Iranian diplomats, tribesmen, migrant laborers, technocrats, railway workers, tourists and pilgrims, as well as European imperial officials alike. Iran in Motion tells the hitherto unexplored stories of these individuals as they experienced new levels of mobility. Drawing on newspapers, industry publications, travelogues, and memoirs, as well as American, British, Danish, and Iranian archival materials, Mikiya Koyagi traces contested imaginations and practices of mobility from the conception of a trans-Iranian railway project during the nineteenth-century global transport revolution to its early years of operation on the eve of Iran's oil nationalization movement in the 1950s. Weaving together various individual experiences, this book considers how the infrastructural megaproject reoriented the flows of people and goods. In so doing, the railway project simultaneously brought the provinces closer to Tehran and pulled them away from it, thereby constantly reshaping local, national, and transnational experiences of space among mobile individuals.
21
Cook, Kerry H. Climate Change Scenarios and African Climate Change. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.545.
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Accurate projections of climate change under increasing atmospheric greenhouse gas levels are needed to evaluate the environmental cost of anthropogenic emissions, and to guide mitigation efforts. These projections are nowhere more important than Africa, with its high dependence on rain-fed agriculture and, in many regions, limited resources for adaptation. Climate models provide our best method for climate prediction but there are uncertainties in projections, especially on regional space scale. In Africa, limitations of observational networks add to this uncertainty since a crucial step in improving model projections is comparisons with observations. Exceeding uncertainties associated with climate model simulation are uncertainties due to projections of future emissions of CO2 and other greenhouse gases. Humanity’s choices in emissions pathways will have profound effects on climate, especially after the mid-century.The African Sahel is a transition zone characterized by strong meridional precipitation and temperature gradients. Over West Africa, the Sahel marks the northernmost extent of the West African monsoon system. The region’s climate is known to be sensitive to sea surface temperatures, both regional and global, as well as to land surface conditions. Increasing atmospheric greenhouse gases are already causing amplified warming over the Sahara Desert and, consequently, increased rainfall in parts of the Sahel. Climate model projections indicate that much of this increased rainfall will be delivered in the form of more intense storm systems.The complicated and highly regional precipitation regimes of East Africa present a challenge for climate modeling. Within roughly 5º of latitude of the equator, rainfall is delivered in two seasons—the long rains in the spring, and the short rains in the fall. Regional climate model projections suggest that the long rains will weaken under greenhouse gas forcing, and the short rains season will extend farther into the winter months. Observations indicate that the long rains are already weakening.Changes in seasonal rainfall over parts of subtropical southern Africa are observed, with repercussions and challenges for agriculture and water availability. Some elements of these observed changes are captured in model simulations of greenhouse gas-induced climate change, especially an early demise of the rainy season. The projected changes are quite regional, however, and more high-resolution study is needed. In addition, there has been very limited study of climate change in the Congo Basin and across northern Africa. Continued efforts to understand and predict climate using higher-resolution simulation must be sustained to better understand observed and projected changes in the physical processes that support African precipitation systems as well as the teleconnections that communicate remote forcings into the continent.