3,931 research outputs found
Evaluation as adventure: taking that risk
No full textHelen Simons traces the values that underpin her preferred methodology of case study and democratic evaluation to the central values she gained from the land of her birth. She looks back to consider what early experiences may have influenced her deep commitment to these values and how they impacted on her professional world as a teacher, a psychologist, and an evaluator. Her interview transcript which was a stimulus for this article is here: http://onlinelibrary.wiley.com/wol1/doi/10.1002/ev.20302/suppinfo. Read only. This should not be used in any form without explicit permission from the author.</p
Parental engagement in learning
No full textRobert Simons examines whether levels of parental engagement can be improved by increasing the capacity of schools and principals for local decision making
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A probabilistic assessment of sea level variations within the Last Interglacial stage
No full textThe Last Interglacial (LIG) stage (ca. 130–115 ka) provides a relatively recent example of a world with both poles characterized by greater-than- Holocene temperatures similar to those expected later in this century under a range of greenhouse gas emission scenarios. Previous analyses inferred that LIG mean global sea level (GSL) peaked 6–9 m higher than today (Kopp et al. 2009; Dutton & Lambeck 2012). Here, we extend our earlier work to perform a probabilistic assessment of sea level variability within the LIG highstand. Using the terminology for probability employed in the Intergovernmental Panel on Climate Change (IPCC) assessment reports, we find it extremely likely (95% probability) that the paleo-sea level record allows resolution of at least two intra-LIG sea level peaks and likely (67% probability) that the magnitude of low-to-high swings exceeded 4 m. Moreover, it is likely that there was a period during the LIG in which GSL rose at a 1000-year average rate exceeding 3 m/ky, but unlikely (33% probability) that the rate exceeded 7 m/ky and extremely unlikely (5% probability) that it exceeded 11 m/ky. These rate estimates can provide insight into rates of Greenland and/or Antarctic melt under climate conditions partially analogous to those expected in the twenty- first century.This is the authors’ preprint version of the manuscript: 23 January 2013. Originally submitted 18 September 2012. Accepted for publication in Geophysical Journal International, published by Oxford University Press.Peer reviewe
Analysis of watersheds and river systems: short course
No full textShort course: Analysis of Watersheds and River Systems, Session I and II, held on May 28-June 1, 1979 and June 4-June 8, 1979 at Colorado State University, Fort Collins, Colorado.Speakers: Dr. E. V. Richardson, Dr. David Duttweiller, Mr. Lee Mulkey, Dr. Stanley A. Schumm, Dr. Daryl B. Simons, Dr. Ross Carder.Includes bibliographical references.This short course is designed for individuals dealing with the analysis of watersheds and rivers. Practical applications concerning physical processes will be emphasized.Chapter 1. General introduction / Daryl B. Simons and Ruh-Ming Li -- Chapter 2. Introduction to watershed and river analysis / Daryl B. Simons and Ruh-Ming Li -- Chapter 3. Physical processes governing response of watersheds and rivers / Daryl B. Simons, Timothy J. Ward and Ruh-Ming Li -- Chapter 4. Sediment transport / H. W. Shen -- Chapter 5. Alluvial bed roughness / H. W. Shen -- Chapter 6. Overview of flood routing methods / Ruh-Ming Li and V. Miguel Ponce -- Chapter 7. Water routing and yield from watersheds, Part I and II / Ruh-Ming Li, Daryl B. Simons, and Kenneth G. Eggert -- Chapter 8. Water routing in rivers / Yung-Hai Chen -- Chapter 9. Stage discharge relations / Robert K. Simons, Ruh-Ming Li, and Daryl B. Simons -- Chapter 10. Watershed sediment yield / Ruh-Ming Li, Daryl B. Simons, and Timothy J. Ward -- Chapter 11. Unsteady sediment routing models in rivers / Yung-Hai Chen and Daryl B. Simons -- Chapter 12. Known discharge sediment routing / Glenn O. Brown and Ruh-Ming Li -- Chapter 13. Landslide potential delineation / Timothy J. Ward, Ruh-Ming Li, and Daryl B. Simons -- Chapter 14. Application of Kalman filtering in watershed and river analysis / Nguyen Duong -- Chapter 15. Handheld calculator programs for analysis / Kenneth G. Eggert, Ruh-Ming Li, and Daryl B. Simons -- Chapter 16. Overview of case studies and data management / Daryl B. Simons, Ruh-Ming Li, and Nguyen Duong -- Chapter 17. Canal and channel design and river response analysis / Daryl B. Simons, Ruh-Ming Li, and Yung-Hai Chen -- Chapter 18. Degradation and aggradation analysis / Ruh-Ming Li and Daryl B. Simons -- Chapter 19. Watershed best management analysis / Ruh-Ming Li, Timothy J. Ward, and Daryl B. Simons -- Chapter 20. Large river basin analysis: Yazoo River Sedimentation Study / Daryl B. Simons and Ruh-Ming Li
Two-loop Sudakov form factor in ABJM
No full textThis article is distributed under the terms of the Creative Commons Attribution License (CC-BY 4.0), which permits any use, distribution and reproduction in any medium, provided the original author(s) and source are credited
Trasmissible Spongiform Encephalopathies
No full textProtein folding and misfolding, relevance to disease and function / Massimi Stefani --
Alzheimer's disease / Charlotte E. Teunissen and Tischa M. van der Cammen --
Improving Cholinergic Transmission --
Cholinergic transmission and acetylcholine release enhancers / Pierre Francotte, Pascal de Tullio and Bernard Pirotte --
AChE and its inhibition / Jure Stojan --
AChE inhibitors and their clinical assessment / Pierre Francotte, Pascal de Tullio and Bernard Pirotte --
Reduction in plaque formation / Christian Czech, Helmut Jacobsen and Celine Adessi --
Non-steroidal anti-inflammatory drugs (NSAIDs) / Bruno P. Imbimbo and Francesca Speroni --
3-hydroxy-3-methyl-glutaryl-coenzyme reductase inhibitors / Dario Cattaneo --
A' polymerization reduction / Harry LeVine III and Corrine E. Augelli-Szafran --
Carbonic anhydrase activators as potential anti-Alzheimer's disease agents / Claudiu T. Supuran and Andrea Scozzafava --
Detection and reduction of neurofibrillary lesions / Jeff Kuret --
Protein misfolding in Alzheimer disease : pathogenic or protective? / Rudy J. Castellani ... [et al.] --
Enhancement of brain retinoic acid levels / Ann B. Goodman ... [et al.] --
Parkinson's disease : what is it? what causes it? and how can it be cured? / Tom Foltynie, Andrew W. Michell and Roger A. Barker --
Restoring dopamine levels / Nuno Palma .. [et al.] --
Huntington's disease / Claire-Anne Gutekunst and Fran Norflus --
Amyotrophic lateral sclerosis (motor neuron disease) / Teresa Sanelli ... [et al.] --
Transmissible spongiform encephalopathies (TSEs) / Michael D. Geschwind and Giuseppe Legname --
Overview / H. John Smith, Claire Simons and Robert D.E. Sewell
Probabilistic assessment of sea level during the last interglacial stage
No full textWith polar temperatures ∼3–5 °C warmer than today, the last interglacial stage (∼125 kyr ago) serves as a partial analogue for 1–2 °C global warming scenarios. Geological records from several sites indicate that local sea levels during the last interglacial were higher than today, but because local sea levels differ from global sea level, accurately reconstructing past global sea level requires an integrated analysis of globally distributed data sets. Here we present an extensive compilation of local sea level indicators and a statistical approach for estimating global sea level, local sea levels, ice sheet volumes and their associated uncertainties. We find a 95% probability that global sea level peaked at least 6.6 m higher than today during the last interglacial; it is likely (67% probability) to have exceeded 8.0 m but is unlikely (33% probability) to have exceeded 9.4 m. When global sea level was close to its current level (≥-10 m), the millennial average rate of global sea level rise is very likely to have exceeded 5.6 m kyr-1 but is unlikely to have exceeded 9.2 m kyr-1. Our analysis extends previous last interglacial sea level studies by integrating literature observations within a probabilistic framework that accounts for the physics of sea level change. The results highlight the long-term vulnerability of ice sheets to even relatively low levels of sustained global warming.This is a post-print version of an article published in Nature. The published version is available at http://www.nature.com/nature/journal/v462/n7275/full/nature08686.htmlPeer reviewe
Music education for the 21st century: epistemology and ontology as bases for student aesthetic education
No full textWe seek to understand why persons develop their musical preferences by identifying with a particular cultural group and social background. This identification is greatly shaped by experience in their environment. Resources employed for this identification are mostly different from those employed in schools to foster academic knowledge. We argue that there needs to be renewed attention to the epistemological and ontological bases of education to examine how we can most effectively educate for the 21st Century in a relativistic and globalized world. Our focus is on music education but with the entire curriculum near at hand, together seeking to bring about a better intellectual, sociological, and aesthetic process of education. Our interest in music stems from a perceived necessity that persons trained in the arts will have special answers to the challenges of this so-called postmodern world. We offer: (1) elements of epistemology, discussing how education and music education have traditionally been focused on propositional rather than interpretive knowledge; (2) a particular perspective on ontology, making evident the ways that individuals construct meanings, interacting with their cultural environment in the shaping of social identity; and (3) the need, today more than ever, for a music curriculum fostering aesthetic experiences that develop interpretive understanding of reality and personal self. Characteristics of postmodernism in cultural studies will be employed throughout the paper
Consideration of risk in hydraulic design of bank protection using Reno matresses and riprap
No full textThis report discusses channel stabilization design by erosion protection measures considering risk analysis. Although many different erosion protection measures have been used, this report only considers rip-rap and wire enclosed rock (in mattresses) which are two of the most widely used methods of erosion protection. The purpose of erosion protection and channel stabilization is, of course, to maintain a channel and its banks and/or bed in a relatively fixed location to protect property, structures or other development from erosion related damage. Because rivers are quite dynamic and development continues along rivers and other types of channels, the need for erosion protection and bank stabilization will continue. Chapter II discusses briefly the dynamic nature of rivers and the need for erosion protection and channel stabilization. Various types of engineering analysis are required in developing an erosion protection design. These include hydrology, hydraulics, geomorphic, erosion and sediment transport. Where ship or barge traffic is of concern, ship-generated waves and other related impacts should also be accounted for. Chapter III discusses the data and analysis required for designing erosion protection and channel stabilization projects. This is by no means a comprehensive discussion of these topics but is meant to serve as an introduction and guide to the subject. The reader is encouraged to refer to the references given on these topics for further information. Chapter IV discusses common failure modes of erosion protection projects. There are a number of distinct and independent causes of failure. Each one alone can be sufficient to induce failure or they may, in some cases, act in concert to induce failure. A fairly comprehensive list of potential modes of failure is included ranging from the obvious to the more obscure and often overlooked. Flowing water causes forces or stresses to act on the bed and banks of a river. These are the forces that cause erosion and attempt to damage any erosion protection. They basically include shear, lift and drag forces acting on each individual particle on the bed and banks. The beginning portion of Chapter V analyzes the hydrodynamic forces due to flowing water acting on erosion protection works. Then based on the most important or frequent modes of failure and an evaluation of the forces acting on rip-rap or wire enclosed rock, methods to evaluate the probability of failure for each of the selected modes were developed. The remqinder of Chapter V covers this topic. The methods presented can be used either directly in a design application or as a tool in evaluating an existing design. Chapter VI outlines these methodologies in step by step format and then gives an example to follow for each procedure. Because the individual modes of failure can be treated independently, the total probability of failure is obtained by summing the individual probabilities. If the probability of failure thus obtained is too high for the given event, redesign is required. The next chapter (Chapter VII) is called "Risk Analysis." This type of an analysis actually is an economic optimization procedure but it has been previously called risk analysis in the literature. Risk analysis consists basically of designing a structure or whatever in order to minimize overall costs. These overall costs include both the initial construction costs as well as long term maintenance and repair costs. It is based on the logic that one may design something that can withstand the forces of a 1,000 year flood but the initial cost and therefore the total cost would be unreasonably high. One may also design a project to withstand the forces of a two year event which would have a very low initial cost but again the overall cost would be very high because of the frequency of maintenance and/or repair and replacement costs. The purpose of risk analysis is to find the minimum overall cost by varying the hydrologic return period of a project and associated designs and their costs in order to minimize the overall project cost. The design is selected that then gives this minimum cost or at least is in the range where costs are near the minimum. Chapter VIII contains the summary and conclusions. References and an appendix of terminology follows the final chapter
Robert Barnwell to John Kean, September 3, 1792
No full textRobert Barnwell in Charleston, SC wrote to John Kean, unaddressed. Barnwell gave Kean permission to vote in his place for any election of the director for Bank of the United States. People included: Benjamin Villepontoux, Benjamin Simons, Stephen Elliot Planter.https://digitalcommons.kean.edu/lhc_1790s/1176/thumbnail.jp
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