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296,965 result(s) for "Raymond, A"
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Stories and the Promotion of Social Cognition
Engaging with fictional stories and the characters within them might help us better understand our real-world peers. Because stories are about characters and their interactions, understanding stories might help us to exercise our social cognitive abilities. Correlational studies with children and adults, experimental research, and neuropsychological investigations have all helped develop our understanding of how stories relate to social cognition. However, there remain a number of limitations to the current evidence, some puzzling results, and several unanswered questions that should inspire future research. This review traces multiple lines of evidence tying stories to social cognition and raises numerous critical questions for the field.
Large contribution to inland water CO2 and CH4 emissions from very small ponds
Very small ponds have been omitted from greenhouse gas budgets. Estimates of CO 2 and CH 4 emissions from 427 lakes and ponds show that very small ponds account for 15% of CO 2 and 40% of diffusive CH 4 emissions, but 8.6% of lake and pond area. Inland waters are an important component of the global carbon cycle. Although they contribute to greenhouse gas emissions 1 , 2 , 3 , 4 , 5 , estimates of carbon processing in these waters are uncertain. The global extent of very small ponds, with surface areas of less than 0.001 km 2 , is particularly difficult to map, resulting in their exclusion from greenhouse gas budget estimates. Here we combine estimates of the lake and pond global size distribution, gas exchange rates, and measurements of carbon dioxide and methane concentrations from 427 lakes and ponds ranging in surface area from 2.5 m 2 to 674 km 2 . We estimate that non-running inland waters release 0.583 Pg C yr −1 . Very small ponds comprise 8.6% of lakes and ponds by area globally, but account for 15.1% of CO 2 emissions and 40.6% of diffusive CH 4 emissions. In terms of CO 2 equivalence, the ratio of CO 2 to CH 4 flux increases with surface area, from about 1.5 in very small ponds to about 19 in large lakes. The high fluxes from very small ponds probably result from shallow waters, high sediment and edge to water volume ratios, and frequent mixing. These attributes increase CO 2 and CH 4 supersaturation in the water and limit efficient methane oxidation. We conclude that very small ponds represent an important inland water carbon flux.
Extending international human rights protections to vulnerable populations
\"This book inductively develops a new typology that identifies and evaluates three principal strategies that have been, and are being, used to extend international human rights protections to new categories of vulnerable populations. The book explicates the evolution and ongoing utility of the three strategies: categorical enlargement, conceptual expansion, and group-conscious universal application. The strategies are elucidated by case studies of nine distinct vulnerable populations: national minorities; those oppressed on the basis of caste; people with albinism; cross-cultural migrants; members of the African diaspora; Roma/Gypsies; persons affected by leprosy; older individuals; and lesbian, gay, bisexual, and transgender (LGBT) people. The book concludes by considering the utility of the three strategies for emerging vulnerable populations. It encourages discourse about the protection of vulnerable populations to move beyond a stale fixation on the texts of treaties and towards a more proactive normative framework that prioritizes the lived experiences of human beings. Extending International Human Rights Protections to Vulnerable Populations will be of key interest to students and scholars of international human rights, to social justice advocates, to human rights practitioners, and to those working with oppressed groups, human rights law, and international relations\"-- Provided by publisher.
Significant efflux of carbon dioxide from streams and rivers in the United States
Current estimates of carbon dioxide evasion from inland waters are based on incomplete spatial coverage. Streams and rivers in the United States release 97 Tg of carbon to the atmosphere each year, according to an analysis of chemical and morphological data. The evasion of carbon dioxide from inland waters was only recently included in assessments of the global carbon budget 1 , 2 , 3 . Present estimates of carbon dioxide release from global freshwater systems, including lakes and wetlands, range from 0.7 to 3.3 Pg C yr −1 (refs  1 , 4 , 5 , 6 , 7 ). However, these estimates are based on incomplete spatial coverage of carbon dioxide evasion, and an inadequate understanding of the factors controlling the efflux of carbon dioxide across large drainage networks 6 . Here, we estimate the amount of carbon degassed from streams and rivers in the United States using measurements of temperature, alkalinity and pH, together with high-resolution data on the morphology and surface area of these waterways. We show that streams and rivers in the US are supersaturated with carbon dioxide when compared with the atmosphere, emitting 97±32 Tg carbon each year. We further show that regionally, carbon dioxide evasion from streams and rivers is positively correlated with annual precipitation, which we attribute to climatic regulation of stream surface area, and the flushing of carbon dioxide from soils. Scaling our analysis from the US to temperate rivers between 25° N and 50° N, we estimate a release of around 0.5 Pg carbon to the atmosphere each year.
حياة بعد الحياة : تجارب الرجوع من العالم الآخر
كثير من العلماء كتبوا وبحثوا وناقشوا في موضوع حياة الإنسان على الأرض وحاولوا الربط بين عالم الإنسان على الأرض مع غيره من الكائنات الحية على الكواكب الأخرى وبقيت الكثير من الأسئلة حتى وقتنا الحاضر بلا أجوبة، يلقي مؤلف هذا الكتاب الضوء على بعض جوانب هذا الموضوع الذي ما زال موضوع نقاش. الكتاب مفيد وممتع لكافة القراء.
Hydrological and biogeochemical controls on watershed dissolved organic matter transport: pulse‐shunt concept
Hydrological precipitation and snowmelt events trigger large “pulse” releases of terrestrial dissolved organic matter (DOM) into drainage networks due to an increase in DOM concentration with discharge. Thus, low‐frequency large events, which are predicted to increase with climate change, are responsible for a significant percentage of annual terrestrial DOM input to drainage networks. These same events are accompanied by marked and rapid increases in headwater stream velocity; thus they also “shunt” a large proportion of the pulsed DOM to downstream, higher‐order rivers and aquatic ecosystems geographically removed from the DOM source of origin. Here we merge these ideas into the “pulse‐shunt concept” (PSC) to explain and quantify how infrequent, yet major hydrologic events may drive the timing, flux, geographical dispersion, and regional metabolism of terrestrial DOM. The PSC also helps reconcile long‐standing discrepancies in C cycling theory and provides a robust framework for better quantifying its highly dynamic role in the global C cycle. The PSC adds a critical temporal dimension to linear organic matter removal dynamics postulated by the river continuum concept. It also can be represented mathematically through a model that is based on stream scaling approaches suitable for quantifying the important role of streams and rivers in the global C cycle. Initial hypotheses generated by the PSC include: (1) Infrequent large storms and snowmelt events account for a large and underappreciated percentage of the terrestrial DOM flux to drainage networks at annual and decadal time scales and therefore event statistics are equally important to total discharge when determining terrestrial fluxes. (2) Episodic hydrologic events result in DOM bypassing headwater streams and being metabolized in large rivers and exported to coastal systems. We propose that the PSC provides a framework for watershed biogeochemical modeling and predictions and discuss implications to ecological processes.
The rise and fall of moral conflicts in the United States and Canada
\"In The Rise and Fall of Moral Conflicts in the United States and Canada, sociologist Mildred A. Schwartz and political scientist Raymond Tatalovich bring their disciplinary insights to the study of moral issues. Beginning with prohibition, Schwartz and Tatalovich trace the phases of its evolution from emergence, establishment, decline and resurgence, to resolution. Prohibition's life history generates a series of hypotheses about how passage through each of the phases affected subsequent developments and how these were shaped by the political institutions and social character of the United States and Canada. Using the history of prohibition in North America as a point of reference, the authors move on to address the anticipated progression and possible resolution of six contemporary moral issues: abortion, capital punishment, gun control, marijuana, pornography, and same-sex relations. Schwartz and Tatalovich build a new theoretical approach by drawing on scholarship on agenda-setting, mass media, social movements, and social problems. The Rise and Fall of Moral Conflicts provides new insights into how moral conflicts develop and interact with their social and political environment.\"-- Provided by publisher.
Rivers as the largest source of mercury to coastal oceans worldwide
Mercury is a potent neurotoxic substance and accounts for 250,000 intellectual disabilities annually. Worldwide, coastal fisheries contribute the majority of human exposure to mercury through fish consumption. Recent global mercury cycling and risk models attribute all the mercury loading to the ocean to atmospheric deposition. Nevertheless, new regional research has noted that the riverine mercury export to coastal oceans may also be significant to the oceanic burden of mercury. Here we construct an unprecedented high-spatial-resolution dataset estimating global river mercury and methylmercury exports. We find that rivers annually deliver 1,000 (minimum–maximum: 893–1,224) Mg mercury to coastal oceans, threefold greater than atmospheric deposition. Furthermore, high flow events, which are becoming more common with climate change, are responsible for a disproportionately large percentage of the export. Coastal oceans constitute 0.2% of the entire ocean volume but receive 27% of the external mercury input to the ocean. We estimate that the river mercury export could be responsible for a net annual export of 350 (interquartile range: 52–640) Mg mercury across the coastal–open-ocean boundary, although there is still high uncertainty around this estimate. Our results show that river export is the largest source of mercury to coastal oceans worldwide, and continued mercury risk modelling should incorporate the impact of rivers. Rivers transport about 1,000 Mg mercury annually to coastal oceans, which is threefold greater than the amount delivered by atmospheric deposition, according to a global analysis of mercury measurements in rivers.