221-240 of 317 Results


Performance Bonding for Environmental Protection  

Olli-Pekka Kuusela

Performance bonds are a widely used enforcement and assurance mechanism in extractive activities and large-scale projects that are associated with clearly defined environmental liabilities. They are especially effective and useful in conditions where the judgment-proof problem is a pervasive challenge. Bonds provide an assurance for the regulator that funds are available to complete the decommissioning activities and the termination of operations under contingencies where the operator fails to follow the contractual obligations or becomes insolvent. Applications of bonding are found in oil and gas drilling, surface mining, renewable energy projects, and timber concessions. However, real bonding systems are not without issues and limitations. Defining a sufficiently high enough bond has been especially challenging in conditions with limited information about costs and environmental risks and where smaller operators may not be able to secure access to required funds or financial services for posting the bond. The use of surety companies, bond pools, and blanket bonds provides a solution to these problems, albeit not without issues of their own. Furthermore, to keep up with the technological developments in extractive industries and with the inescapable uncertainties related to reclamation costs and environmental damages, the regulator should continually review and update bonding instruments based on new available information. Regulatory rules and statistical models that have been developed to adjust the required bonds, based on observable risk factors, provide some encouraging examples for how to design more responsive and effective bonding systems.


Pesticides and Human Health  

Pierluigi Cocco

The fight against agricultural and household pests accompanies the history of humanity, and a total ban on the use of pesticides seems unlikely to happen in the foreseeable future. Currently, about 100,000 different chemicals, inorganic and organic, are currently in the market, grouped according to their function as insecticides, herbicides, fungicides, fumigants, rodenticides, fertilizers, growth regulators, etc. against specific pests, such as snails or human parasites, or their chemical structure—organochlorines, organophosphates, pyrethroids, carbamates, dithiocarbamates, organotin compounds, phthalimides, phenoxy acids, heterocyclic azole compounds, coumarins, etc. Runoff from agricultural land and rain precipitation and dry deposition from the atmosphere can extend exposure to the general environment through the transport of pesticides to streams and ground-water. Also, the prolonged bio-persistence of organochlorines generates their accumulation in the food chain, and their atmospheric drift toward remote geographical areas is mentioned as the cause of elevated fat contents in Arctic mammals. Current regulation in the developed world and the phasing out of more toxic pesticides have greatly reduced the frequency of acute intoxications, although less stringent regulations in the developing world contribute to a complex pattern of exposure circumstances worldwide. Nonetheless, evidence is growing about long-term health effects following high-level, long-lasting exposure to specific pesticides, including asthma and other allergic diseases, immunotoxicity, endocrine disruption, cancer, and central and peripheral nervous system effects. Major reasons for uncertainty in interpreting epidemiological findings of pesticide effects include the complex pattern of overlapping exposure due to multiple treatments applied to different crops and their frequent changes over time to overcome pest resistance. Further research will have to address specific agrochemicals with well-characterized exposure patterns.


Philosophy of the Anthropocene  

Sébastien Dutreuil and Pierre Charbonnier

The Anthropocene was proposed in 2000 as the name of a new geological epoch, succeeding to the Holocene, and marked by the influence of humanity as a biological species on its geological environment. It has resonated differently in three major epistemological domains, where the configurations of the debate has varied. For Earth system science, within which the term emerged, the Anthropocene was a keyword encompassing and stimulating large research programs which stimulated original and new scientific investigations and synthesis. The term had a more specific and evidential meaning for the geological community, which seized it after 2008. Documenting empirically the Anthropocene meant different things for these two scientific communities: tracking down every single impact humanity has on the environment on which humanity depends upon to survive for the former; analyzing how this influence can be documented in Earth’s strata for the latter. These two different epistemological regimes are intertwined with two different normative registers. Earth system science assumed from the very start a normative position: international experts elaborate normative concepts and produce scientific synthesis meant to define the conceptual space, quantitatively delimited, within which political decisions related to global environmental issues ought to be taken. By contrast, geologists were more cautious, and for some, reluctant, to engage in normative issues; but political issues unavoidably emerged when the starting date was discussed. This politicization of the debate was accompanied by human and social sciences, seizing up the debate at the same time as geologists and lay public did, toward the end of the 2000s.


Planning for Resilient and Sustainable Coastal Shorelands and Communities in the Face of Global Climate Change  

Richard K. Norton

Coastal shorelands and communities are among the most beautiful, vital, remunerative, popular, inequitable, and hazardous of places to live, work, and play. Because of the varied and intensive uses of them combined with climate-related impacts to them, they increasingly experience threats from coastal hazards, suffer ecological degradation, and engender contentious conflicts. Although some coastal shorelands are publicly owned, many are privately owned. Coastal states and communities confront many challenges as they plan for and manage the use of privately owned coastal shorelands. Coastal shorelands encompass the near-shore beaches, dunes, wetlands, and other transitional areas within dynamic coastal zones, whether developed or natural. Sustainability suggests the ability of natural and social coastal systems to persist, whereas resilience speaks to the sustainability of those systems when subject to substantial disruptions such as flooding from extreme storms. In addition to promoting sustainable and resilient coastal shorelands in general, advocates also call for redressing the heightened risks and other inequities experienced by historically marginalized communities. Most of the challenges prompting calls for enhanced coastal resilience, sustainability, and equity are not unique to coastal settings, but coastal communities especially need to attend to them given the heightened risks and development pressures they face. Broadly, they include increasingly frequent and fierce storms, floods, drought, fires, and heatwaves. Coastal communities also face unique challenges, including accelerating rates of shoreline recession and increasing near-shore flooding. Further complicating these natural dynamics are complex and poorly adapted property right, public interest, and related legal/administrative institutional arrangements shaping both private and public expectations in coastal settings. Community planning, if well executed, offers the promise of facilitating and advancing the kinds of nuanced and adaptive resiliency and sustainability goals needed everywhere, especially in coastal settings. Toward that end, researchers and advocates promote a range of planning principles, such as recognizing that coastal economies are nested within and dependent upon coastal ecosystems; promoting culturally aware, place-based, and infrastructure-efficient development policies; adopting no- to low-regrets climate adaptation policies; and encouraging ongoing learning and adaptative management. They similarly promote a variety of planning methods to support those policies, such as land suitability, infrastructure capacity, hazard vulnerability, and social vulnerability analyses, best engaged through scenario-based planning given climate-related uncertainties. Coastal communities experiencing aggressive shoreline recession face difficult choices as well—such as whether to armor receding shores or withdraw—most of which will require acknowledging and working through unavoidable trade-offs. Finally, providing knowledge about natural coastal dynamics and management systems is necessary but not by itself sufficient. Also needed are enhanced local capacity to conduct the analyses required to identify policies and programs that will effectively and equitably advance coastal sustainability and the firm commitment of local residents and officials to adopt those policies—challenges that are daunting but not insurmountable.


Politics of Local Community Engagement in Transboundary Water Negotiations  

Isabela Espindola and Pilar Villar

The sharing of transboundary water resources, whether surface or groundwater, is a significant challenge, both in theory and practice. Countries in situations of sharing these natural resources are predisposed to interact with each other. These interactions, here called transboundary water interactions, are characterized by the coexistence of cooperation and conflict, which can arise at different governance levels. However, negotiations around transboundary water resources primarily occur between diplomats and high government members from riparian countries and river basin organization (RBO) managers. Transboundary water negotiations are usually considered high-level political discussions, given the complexity and scale of the water challenges. Consequently, decision-making processes incorporate only a limited number of participants, who make decisions capable of impacting the entire population that depend on the shared waters. Over the last 20 years, there has been a need for greater transparency and a participatory process in transboundary water negotiations, especially for local community engagement and collaboration in these processes. Many of the negotiation processes around transboundary water resources need the participation of municipalities and local populations, concomitant with the involvement of RBOs, to carry out decisions to manage transboundary waters in an integrated manner. There are several reasons for this demand, including negotiation effectiveness, contestation prevention, data sharing, ensuring continuing participation and collaboration, and promoting public awareness related to water resources. Discussing social participation, particularly in the management of transboundary water resources, requires attention to the historical context and its constraints. Considering the enormous challenge, the experiences of local community engagement in transboundary water negotiations in South America, especially from the Guarani Aquifer and the La Plata Basin, are good examples for improving this discussion around transboundary water interactions and local community engagement. The La Plata Basin is the second-largest transboundary basin in the continent, shared by Argentina, Bolivia, Brazil, Uruguay, and Paraguay, while the Guarani Aquifer is one of the largest reservoirs of freshwater worldwide, shared by Argentina, Brazil, Paraguay, and Uruguay. Even with both having cooperation agreements in place between the riparian states, there are still great difficulties with regard to the participation of local communities in transboundary water negotiations.


Exploring the Politics of Institutional Fragmentation in Transboundary River Basins  

Christian Bréthaut and Laura Turley

Institutional fragmentation has been less addressed by research when considering the specific context of transboundary river basins, settings that are often characterized by multiple regulatory frameworks as well as by a great range of uses and users of the river that intervene at different institutional levels. Considering that such contexts represent fertile ground for reinforced use rivalries and exacerbated power relations, it is key to focus on the very nature and results of such institutional fragmentation; in other words, it is necessary to explore the politics of institutional fragmentation in transboundary rivers. Three main bodies of literature are suggested as insightful perspectives to provide enhanced understanding of such contexts: (a) institutional fit literature: challenges of fits between institutions and ecosystems, (b) legal pluralism: interplay and co-existence of different normative orders, (c) polycentric governance: coordination modalities between different and independent decision-making centers.


Politics of Water Flows: Water Supply, Sanitation, and Drainage  

Tatiana Acevedo Guerrero

Since the late 20th century, water and sanitation management has been deeply influenced by ideas from economics, specifically by the doctrine of neoliberalism. The resulting set of policy trends are usually referred to as market environmentalism, which in broad terms encourages specific types of water reforms aiming to employ markets as allocation mechanisms, establish private-property rights and full-cost pricing, reduce (or remove) subsidies, and promote private sector management to reduce government interference and avoid the politicization of water and sanitation management. Market environmentalism sees water as a resource that should be efficiently managed through economic reforms. Instead of seeing water as an external resource to be managed, alternative approaches like political ecology see water as a socio-nature. This means that water is studied as a historical-geographical process in which society and nature are inseparable, mutually produced, and transformable. Political ecological analyses understand processes of environmental change as deeply interrelated to socioeconomic dynamics. They also emphasize the impact of environmental dynamics on social relations and take seriously the question of how the physical properties of water may be sources of unpredictability, unruliness, and resistance from human intentions. As an alternative to the hydrologic cycle, political ecology proposes the concept of hydrosocial cycle, which emphasizes that water is deeply political and social. An analysis of the politics of water flows, drawing from political ecology explores the different relationships and histories reflected in access to (and exclusion from) water supply, sanitation, and drainage. It portrays how power inequalities are at the heart of differentiated levels of access to infrastructure.


Pollen, Allergens, and Human Health  

Rachel N. McInnes

Allergenic pollen is produced by the flowers of a number of trees, grasses, and weeds found throughout the world. Human exposure to such pollen grains can exacerbate pollen-related asthma and allergenic conditions such as allergic rhinitis (hay fever). While allergenic pollen comes from three main groups of plants—certain trees, grasses, and weeds—many people are sensitive to pollen from one or a few taxa only. Weather, climate, and environmental conditions have a significant impact on the levels and varieties of pollen grains present in the air. These allergenic conditions significantly reduce the quality of life of affected individuals and have been shown to have a major economic impact. Pollen production depends on both the current meteorological conditions (including day length, temperature, irradiation, precipitation, and wind speed/direction), and the water availability and other environmental and meteorological conditions experienced in the previous year. The climate affects the types of vegetation and taxa that can grow in a particular location through availability of different habitats. Land-use or land management is also crucial, and so this field of study has implications for vegetation management practices and policy. Given the influential effects of weather and climate on pollen, and the significant health impacts globally, the total effect of any future environmental and climatic changes on aeroallergen production and spread will be significant. The overall impact of climate change on pollen production and spread remains highly uncertain, and there is a need for further understanding of pollen-related health impact information. There are a number of ways air quality interacts with the impact of pollen. Further understanding of the risks of co-exposure to both pollen and air pollutants is needed to better inform public health policy. Furthermore, thunderstorms have been linked to asthma epidemics, especially during the grass pollen seasons. It is thought that allergenic pollen plays a role in this “thunderstorm asthma.” To reduce the exposure to, or impact from, pollen grains in the air, a number of adaptation and mitigation options may be adopted. Many of these would need to be done either through policy changes, or at a local or regional level, although some can be done by individuals to minimize their exposure to pollen they are sensitive to. Improved aeroallergen forecast models could be developed to provide detailed taxon-specific, localized information to the public. One challenge will be combining the many different sources of aeroallergen data that are likely to become available in future into numerical forecast systems. Examples of these potential inputs are automated observations of aeroallergens, real-time phenological observations and remote sensing of vegetation, social sensing, DNA analysis of specific aeroallergens, and data from symptom trackers or personal monitors. All of these have the potential to improve the forecasts and information available to the public.


Pollution in Terrestrial and Aquatic Sediment  

Rodney Stevens

This is an advance summary of a forthcoming article in the Oxford Research Encyclopedia of Environmental Science. Please check back later for the full article. Pollution problems in aquatic sediments and on land can be quite varied—from the widespread contamination of a coastal bay receiving untreated urban or industrial discharge to the local leakage from underground petroleum tanks or pipelines. Such problems are related to the range of sediment and soil in which they occur. Sediments and soil particles can be carriers, receptors, and sources for contaminants. The effectiveness of these roles is largely related to their adsorptive capacity and is governed mainly by particle size, mineralogy, and organic matter as well as site-specific geochemical conditions. Sustainable use of land and marine areas requires a source-to-sink system perspective in order to prescribe remedial actions. Measures can focus on preventing release from the source, spreading along selective pathways, stabilization, and isolation to protect the receptor. Therefore, many traditional scientific goals, such as provenance (sediment source) identification, the interpretation of sediment transport modes and directions, and post-depositional (diagenetic) changes, are applicable and complementary tools to increase predictability between sampled sites. The carrier function of aquatic sediments is emphasized when contaminates are transported to the site of accumulation. Ground pollution in terrestrial settings, on the other hand, is often due to more local sources. Nevertheless, retention and ecological exposure is dependent on the particle-solute interactions. The stratigraphic architecture of ground environments can also decisively influence the spread of contaminants, contrasting with the largely two-dimensional redistribution of eroded aquatic sediments. Diffuse pollution sources, including agriculture, urban, transportation, and industrial sources, contribute significantly to overall environmental stress. Quantitative modeling of contaminant fluxes is increasingly possible with database availability, but relative risk ranking is still a necessary simplification in many decision-support evaluations due to the complexity of sediment and ground environments.


Potential Impacts of Deep-Sea Mining on Ecosystems  

Rahul Sharma

Deep-sea mining pertains to underwater minerals such as polymetallic nodules, ferromanganese crusts, and hydrothermal sulfides that are considered as alternative sources for metals such as Cu, Ni, Co, Pb, Zn, Cd, Mn, Fe, and rare earths that could be exploited in the future by developing suitable technologies. Many of these deposits occur in international waters in which several “contractors” have staked claims over large tracts of the seafloor under the United Nations Law of the Sea, whereas attempts are also being made to develop the deposits within the Exclusive Economic Zone of some countries. However, several concerns have emerged over potential impacts of mining these deposits, leading to regulations being framed as well as measures being devised for conserving the marine ecosystems. The likely sources of environmental impact of deep-sea mining include those from the mining ship where handling of ore, machinery, oil will take place; the lift mechanism that would transfer the minerals from the sea bottom to the surface through the entire water column; as well as the mining machine that would actually scrape the seafloor for minerals. This article describes the likely impacts that could be caused due to mining of three different types of deep-sea minerals, viz. polymetallic nodules, hydrothermal sulfides and ferromanganese crusts. It further shows the estimation of impacts in terms of mining area, volume and weight of associated substrates; and goes on to suggest mitigation measures to minimize the potential impacts of deep-sea mining. Finally, the national and international environmental regulations for deep-sea mining have been discussed.


Prehistoric Agriculture in China: Food Globalization in Prehistory  

Giedrė Motuzaitė Matuzevičiūtė and Xinyi Liu

It is commonly recognised that farming activities initiated independently in different parts of the world between approximately 12,000 and 8,000 years ago. Two of such agricultural centres is situated in modern-day China, where systems based on the cultivation of plants and animal husbandry has developed. Recent investigations have shown that between 5000 and 1500 cal. bce, the Eurasian and African landmass underpinned a continental-scale process of food “globalisation of staple crops. In the narrative of food domestication and global food dispersal processes, China has played a particularly important role, contributing key staple food domesticates such as rice, broomcorn, and foxtail millet. The millets dispersed from China across Eurasia during the Bronze Age, becoming an essential food for many ancient communities. In counterpoise, southwest Asian crops, such as wheat or barley, found new habitats among the ancient populations of China, dramatically changing the course of its development. The processes of plant domestication and prehistoric agriculture in China have been a topic of extensive research, review, and discussion by many scholars around the world, and there is a great deal of literature on these topics. One of the consequences of these discoveries concerning the origins of agriculture in China has been to undermine the notion of a single centre of origin for civilisation, agriculture, and urbanism, which was a popular and widespread narrative in the past. It has become clear that agricultural centres of development in China were concurrent with, rather than after, the Fertile Crescent.


Prehistoric and Traditional Agriculture in Lowland Mesoamerica  

Clarissa Cagnato

Mesoamerica is one of the world’s primary centers of domestication where agriculture arose independently. Paleoethnobotany (or archaeobotany), along with archaeology, epigraphy, and ethnohistorical and ethnobotanical data, provide increasingly important insights into the ancient agriculture of Lowland Mesoamerica (below 1000 m above sea level). Moreover, new advances in the analysis of microbotanical remains in the form of pollen, phytoliths, and starch-grain analysis and chemical analysis of organic residues have further contributed to our understanding of ancient plant use in this region. Prehistoric and traditional agriculture in the lowlands of Mesoamerica—notably the Maya lowlands, the Gulf Coast, and the Pacific Coast of southern Chiapas (Mexico) and Guatemala—from the Archaic (ca. 8000/7000–2000 bc) through the Preclassic/Formative (2000 bc–ad 250) and into the Classic (ad 250–900) period, are covered. During the late Archaic, these lowland regions were inhabited by people who took full advantage of the rich natural biodiversity but also grew domesticates before becoming fully sedentary. Through time, they developed diverse management strategies to produce food, from the forest management system (which includes swidden agriculture), to larger scale land modifications such as terraces, and continued to rely on semidomesticated and wild plant resources. Although lowland populations came to eventually rely on maize as a staple, other resources such as root crops and fruit trees were also cultivated, encouraged, and consumed. The need for additional research that includes systematic collection of paleoethnobotanical data, along with other lines of evidence, will be key to continue refining the understanding of ancient subsistence systems and how these changed through time and across lowland Mesoamerica.


Pros and Cons of GMO Crop Farming  

Rene Van Acker, M. Motior Rahman, and S. Zahra H. Cici

The global area sown to genetically modified (GM) varieties of leading commercial crops (soybean, maize, canola, and cotton) has expanded over 100-fold over two decades. Thirty countries are producing GM crops and just five countries (United States, Brazil, Argentina, Canada, and India) account for almost 90% of the GM production. Only four crops account for 99% of worldwide GM crop area. Almost 100% of GM crops on the market are genetically engineered with herbicide tolerance (HT), and insect resistance (IR) traits. Approximately 70% of cultivated GM crops are HT, and GM HT crops have been credited with facilitating no-tillage and conservation tillage practices that conserve soil moisture and control soil erosion, and that also support carbon sequestration and reduced greenhouse gas emissions. Crop production and productivity increased significantly during the era of the adoption of GM crops; some of this increase can be attributed to GM technology and the yield protection traits that it has made possible even if the GM traits implemented to-date are not yield traits per se. GM crops have also been credited with helping to improve farm incomes and reduce pesticide use. Practical concerns around GM crops include the rise of insect pests and weeds that are resistant to pesticides. Other concerns around GM crops include broad seed variety access for farmers and rising seed costs as well as increased dependency on multinational seed companies. Citizens in many countries and especially in European countries are opposed to GM crops and have voiced concerns about possible impacts on human and environmental health. Nonetheless, proponents of GM crops argue that they are needed to enhance worldwide food production. The novelty of the technology and its potential to bring almost any trait into crops mean that there needs to remain dedicated diligence on the part of regulators to ensure that no GM crops are deregulated that may in fact pose risks to human health or the environment. The same will be true for the next wave of new breeding technologies, which include gene editing technologies.


Quaternary Science  

Kenneth Addison

This is an advance summary of a forthcoming article in the Oxford Research Encyclopedia of Environmental Science. Please check back later for the full article. The Quaternary period of Earth history, which commenced ca. 2.6 Ma ago, is noted for a series of dramatic shifts in global climate between long, cool (“icehouse”) and short, temperate (“greenhouse”) stages. This also coincides with the extinction of later Australopithecine hominins and evolution of modern Homo sapiens. Wide recognition of a fourth, Quaternary, order of geologic time emerged in Europe between ca. 1760–1830 and became closely identified with the concept of an ice age. This most recent episode in Earth history is also the best preserved in stratigraphic and landscape records. Indeed, much of its character and processes continue in present time, which prompted early geologists’ recognition of the concept of uniformitarianism—the present is the key to the past. Quaternary time was quickly divided into a dominant Pleistocene (“most recent”) epoch, characterized by cyclical growth and decay of major continental ice sheets and peripheral permafrost. Disappearance of most of these ice sheets, except in Antarctica and Greenland today, ushered in the Holocene (“wholly modern”) epoch, once thought to terminate the Ice Age but now seen as the current interglacial or temperate stage, commencing ca. 11.7 ka ago. Covering 30–50% of Earth’s land surface at their maxima, ice sheets and permafrost squeezed remaining biomes into a narrower circum-equatorial zone, where research indicated the former occurrence of pluvial and desiccation events. Early efforts to correlate them with mid-high latitude glacials and interglacials revealed the complex and often asynchronous Pleistocene record. Nineteenth-century recognition of just four glaciations reflected a reliance on geomorphology and short terrestrial stratigraphic records, concentrated in northern hemisphere mid- and high-latitudes, until the 1970s. Correlation of δ16-18 O isotope signals from seafloor sediments (from ocean drilling programs after the 1960s) with polar ice core signals from the 1980s onward has revolutionized our understanding of the Quaternary, facilitating a sophisticated, time-constrained record of events and environmental reconstructions from regional to global scales. Records from oceans and ice sheets, some spanning 105–106 years, are augmented by similar long records from loess, lake sediments, and speleothems (cave sediments). Their collective value is enhanced by innovative analytical and dating tools. Over 100 Marine Isotope Stages (MIS) are now recognized in the Quaternary, with dramatic climate shifts at decadal and centennial timescales—with the magnitude of 22 MIS in the past 900,000 years considered to reflect significant ice sheet accumulation and decay. Each cycle between temperate and cool conditions (odd- and even-numbered MIS respectively) is time-asymmetric, with progressive cooling over 80,000 to 100,000 years, followed by an abrupt termination then rapid return to temperate conditions for a few thousand years. The search for causes of Quaternary climate and environmental change embraces all strands of Earth System Science. Strong correlation between orbital forcing and major climate changes (summarized as the Milankovitch mechanism) is displacing earlier emphasis on radiative (direct solar) forcing, but uncertainty remains over how the orbital signal is amplified or modulated. Tectonic forcing (ocean-continent distributions, tectonic uplift, and volcanic outgassing), atmosphere-biogeochemical and greenhouse gas exchange, ocean-land surface albedo and deep- and surface-ocean circulation are all contenders and important agents in their own right. Modern understanding of Quaternary environments and processes feeds an exponential growth of multidisciplinary research, numerical modeling, and applications. Climate modeling exploits mutual benefits to science and society of “hindcasting,” using paleoclimate data to aid understanding of the past and increasing confidence in modeling forecasts. Pursuit of more detailed and sophisticated understanding of ocean-atmosphere-cryosphere-biosphere interaction proceeds apace. The Quaternary is also the stage on which human evolution plays. And the essential distinction between natural climate variability and human forcing is now recognized as designating, in present time, a potential new Anthropocene epoch. Quaternary past and present are major keys to its future.


Radiation and the Environment  

E. Jerry Jessee

The “Atomic Age” has long been recognized as a signal moment in modern history. In popular memory, images of mushroom clouds from atmospheric nuclear weapons tests recall a period when militaries and highly secretive atomic energy agencies poisoned the global environment and threatened human health. Historical scholarship has painted a more complicated picture of this era by showing how nuclear technologies and radioactive releases transformed the environment sciences and helped set the stage for the scientific construction of the very idea of the “global environment.” Radioactivity presented scientists with a double-edged sword almost as soon as scientists explained how certain unstable chemical elements emit energic particles and rays in the process of radioactive decay at the turn of the 20th century. Throughout the 1920s and 1930s, scientists hailed radioactivity as a transformative discovery that promised to transform atomic theory and biomedicine by using radioisotopes—radioactive versions of stable chemical elements—which were used to tag and trace physiological processes in living systems. At the same time, the perils of overexposure to radioactivity were becoming more apparent as researchers and industrial workers laboring in new radium-laced luminescent paint industries began suffering from radiation-induced illnesses. The advent of a second “Atomic Age” in wake of the bombing of Japan was characterized by increased access to radiotracer technologies for science and widespread anxiety about the health effects of radioactive fallout in the environment. Powerful new atomic agencies and military institutions created new research opportunities for scientists to study the atmospheric, oceanic, and ecological pathways through which bomb test radiation could make their way to human bodies. Although these studies were driven by concerns about health effects, the presence of energy-emitting radioactivity in the environment also meant that researchers could utilize it as a tracer to visualize basic environmental processes. Throughout the 1950s and early 1960s, as a result, ecologists pioneered the use of radiotracers to investigate energy flows and the metabolism of ecosystem units. Oceanographers similarly used bomb blast radiation to trace the physical processes in oceans and the uptake of radioactivity in aquatic food chains. Meteorologists meanwhile tracked bomb debris as high as the stratosphere to predict fallout patterns and trace large-scale atmospheric phenomenon. By the early 1960s, these studies documented how radioactive fallout produced by distant nuclear tests spread across the globe and infiltrated the entire planet’s air, water, biosphere, and human bodies. In 1963, the major nuclear powers agreed to end above-ground nuclear testing with the Limited Test Ban Treaty, the first international treaty to recognize a global environmental hazard of planetary proportions. Throughout the 1960s and into the 1980s, research on the global effects of nuclear weapons continued to shape global environmental thinking and concern as debates about nuclear winter directed professional and public attention toward humanity’s ability to alter the climate.


Recreation Use Values for Water-Based Recreation  

John Loomis and Lucas Bair

Outdoor recreation is an important and growing activity worldwide. Water-based outdoor recreation is a subset that includes various activities such as fishing, boating, and swimming. While a large portion of water-based recreation is either free or provided at administratively set minimal entrance fees, these activities still involve significant economic value in aggregate. Because many water-based recreation activities do not have market prices, economists have developed nonmarket valuation methods to estimate the full scope of economic values to participants associated with these activities. Estimates of the economic value of water-based recreation are important in water resource management. While water resource infrastructure investment decisions typically include the economic value of recreation, periodic evaluation of infrastructure operations after construction may not. Re-evaluation of operations is particularly important if rapid changes in future conditions such as drought or changes in recreational demand occur. Because developing original site-based estimates of economic value requires significant effort, it is important to understand the general economic value of specific water-based recreational activities and methods used to transfer benefit estimates from existing studies to other sites.


Renewable Energy for Human Sustainability  

Peter J. Schubert

Renewable energy was used exclusively by the first humans and is likely to be the predominant source for future humans. Between these times the use of extracted resources such as coal, oil, and natural gas has created an explosion of population and affluence, but also of pollution and dependency. This article explores the advent of energy sources in a broad social context including economics, finance, and policy. The means of producing renewable energy are described in an accessible way, highlighting the broad range of considerations in their development, deployment, and ability to scale to address the entirety of human enterprises.



Carl Folke

Resilience thinking in relation to the environment has emerged as a lens of inquiry that serves a platform for interdisciplinary dialogue and collaboration. Resilience is about cultivating the capacity to sustain development in the face of expected and surprising change and diverse pathways of development and potential thresholds between them. The evolution of resilience thinking is coupled to social-ecological systems and a truly intertwined human-environment planet. Resilience as persistence, adaptability and, transformability of complex adaptive social-ecological systems is the focus, clarifying the dynamic and forward-looking nature of the concept. Resilience thinking emphasizes that social-ecological systems, from the individual, to community, to society as a whole, are embedded in the biosphere. The biosphere connection is an essential observation if sustainability is to be taken seriously. In the continuous advancement of resilience thinking there are efforts aimed at capturing resilience of social-ecological systems and finding ways for people and institutions to govern social-ecological dynamics for improved human well-being, at the local, across levels and scales, to the global. Consequently, in resilience thinking, development issues for human well-being, for people and planet, are framed in a context of understanding and governing complex social-ecological dynamics for sustainability as part of a dynamic biosphere.


Rethinking Conflict over Water  

Scott M. Moore

It has long been accepted that non-renewable natural resources like oil and gas are often the subject of conflict between both nation-states and social groups. But since the end of the Cold War, the idea that renewable resources like water and timber might also be a cause of conflict has steadily gained credence. This is particularly true in the case of water: in the early 1990s, a senior World Bank official famously predicted that “the wars of the next century will be fought over water,” while two years ago Indian strategist Brahma Chellaney made a splash in North America by claiming that water would be “Asia’s New Battleground.” But it has not quite turned out that way. The world has, so far, avoided inter-state conflict over water in the 21st century, but it has witnessed many localized conflicts, some involving considerable violence. As population growth, economic development, and climate change place growing strains on the world’s fresh water supplies, the relationship between resource scarcity, institutions, and conflict has become a topic of vocal debate among social and environmental scientists. The idea that water scarcity leads to conflict is rooted in three common assertions. The first of these arguments is that, around the world, once-plentiful renewable resources like fresh water, timber, and even soils are under increasing pressure, and are therefore likely to stoke conflict among increasing numbers of people who seek to utilize dwindling supplies. A second, and often corollary, argument holds that water’s unique value to human life and well-being—namely that there are no substitutes for water, as there are for most other critical natural resources—makes it uniquely conductive to conflict. Finally, a third presumption behind the water wars hypothesis stems from the fact that many water bodies, and nearly all large river basins, are shared between multiple countries. When an upstream country can harm its downstream neighbor by diverting or controlling flows of water, the argument goes, conflict is likely to ensue. But each of these assertions depends on making assumptions about how people react to water scarcity, the means they have at their disposal to adapt to it, and the circumstances under which they are apt to cooperate rather than to engage in conflict. Untangling these complex relationships promises a more refined understanding of whether and how water scarcity might lead to conflict in the 21st century—and how cooperation can be encouraged instead.


Rethinking Hydropower: The Economics and Politics of Privately Owned Hydropower in the United States  

Lynne Y. Lewis

2019 marked the 20th anniversary of the removal of the Edwards Dam in Augusta, Maine (USA). Edwards Dam was the first federally licensed hydropower dam to be denied relicensing, and the dam was removed for the purpose of restoring the 10 anadromous fish species that use the Kennebec River. Since that time, numerous other small dams have been removed in the United States. The relicensing process considers benefit-cost analysis, yet remains fundamentally flawed in the consideration of the benefits of dam removals and fish passage. Successful dam removals rely (mostly) on local efforts and outside analysis.