78,312 research outputs found
Edward Harris Kemp Papers
Correspondence of Dr. Neill Barlett and others, and biographical information on Dr. Edward Harris Kemp, alumnus of Wake Forest College (Class of 1928) and a prominent psychologist
Letter. Late cretaceous seasonal ocean variability from the arctic
The modern Arctic Ocean is regarded as barometer of global change and amplifier of global warming1 and therefore records of past Arctic change are of a premium for palaeoclimate reconstruction. Little is known of the state of the Arctic Ocean in the greenhouse period of the late Cretaceous, yet records from such times may yield important clues to its future behaviour given current global warming trends. Here we present the first seasonally resolved sedimentary record from the Cretaceous from the Alpha Ridge of the Arctic Ocean. This “paleo-sediment trap” provides new insights into the workings of the Cretaceous marine biological carbon pump. Seasonal primary production was dominated by diatom algae but was not related to upwelling as previously hypothesised. Rather, production occurred within a stratified water column, involving specially adapted species in blooms resembling those of the modern North Pacific Subtropical Gyre, or those indicated for the Mediterranean sapropels. With increased CO2 levels and warming currently driving increased stratification in the global ocean, this style of production that is adapted to stratification may become more widespread. Our evidence for seasonal diatom production and flux testify to an ice-free summer, but thin accumulations of terrigenous sediment within the diatom ooze are consistent with the presence of intermittent sea ice in the winter, supporting a wide body of evidence for low temperatures in the Late Cretaceous Arctic Ocean, rather than recent suggestions of a 15 °C mean annual temperature at this time
The Benefits of Being Economics Professor A (and not Z)
Alphabetic name ordering on multi-authored academic papers, which is the convention in the economics discipline and various other disciplines, is to the advantage of people whose last name initials are placed early in the alphabet. As it turns out, Professor A, who has been a first author more often than Professor Z, will have published more articles and experienced afaster growth rate over the course of her career as a result of reputation and visibility. Moreover, authors know that name ordering matters and indeed take ordering seriously: Several characteristics of an author group composition determine the decision to deviate from the default alphabetic name order to a significant extent.performance measurement, incentives, economists, name ordering
Body, mind, spirit, voice : Helen Kemp and the development of the children's choir movement
The purpose of this research was to document the contributions of Helen Kemp to the development of the children's choir movement. As a result of her professional contributions, Kemp became an internationally recognized specialist in the area of children's choirs and the child's voice. A brief overview of the children's choir movement in the United States is included to provide a context from which Helen Kemp's role in the children's choir movement can be more clearly understood. Helen Kemp (1918-)received vocal and church music training at Westminster Choir College. As a result of early experiences as a vocalist, children's choir director, and mother, Kemp developed an interest in child vocal development and children's choirs. After moving to Oklahoma with her husband in 1949, Kemp established many of her children's choir philosophies and techniques while serving as children's choir director at First Presbyterian Church in Oklahoma City
Final word on Jersey Dutch
In this article, William Z. Shetter compares and contrasts the dialects that developed between different Dutch colonies in the New World. He explores in-depth the nuances of Jersey Dutch, and provides theories to explain how Dutch and colonial languages blended. The article is reprinted from American Speech, December 1958, Volum XXXIII, No. 4
Teaching wellbeing science
This project describes an innovative optional wellbeing science module being offered at Swansea University, focusing on individual, collective and planetary wellbeing. The information provided here relate to supporting information and preprints of two papers published in the Teaching of Psychology journal including:
Kemp, A. H., and Fisher, Z. (2021). Application of Single-Case Research Designs in Undergraduate Student Reports: An Example From Wellbeing Science. Teaching of Psychology. https://doi.org/10.1177/00986283211029929
Kemp, A. H., Mead, J. & Fisher, Z. (2022). Improving Student Wellbeing: Evidence from a Mixed Effects Design and Comparison to Normative Data. Teaching of Psychology. https://doi.org/10.1177/0098628322111242
A Preregistered, Quasi-Experimental, Mixed Effects Analysis on the Impacts of a Third-Wave Positive Psychology Course for Undergraduate Students
This project has been created to make data available for preprint titled: "Reimagining Student Wellbeing: A Preregistered, Quasi-Experimental, Mixed Effects Analysis on the Impacts of a Third-Wave Positive Psychology Course for Undergraduate Students".
Our study was preregistered (see associated component) and builds on prior published work (Kemp, Mead & Fisher, 2022). The reference for our earlier study is:
Kemp, A. H., Mead, J., & Fisher, Z. (2022). Improving Student Wellbeing: Evidence From a Mixed Effects Design and Comparison to Normative Data. Teaching of Psychology, 51(4), 389-395. https://doi.org/10.1177/00986283221112428 (Original work published 2024
Migration of the Antarctic Polar Front through the mid-Pleistocene transition: evidence and climatic implications
The Antarctic Polar Front is an important biogeochemical divider in the Southern Ocean. Laminated diatom mat deposits record episodes of massive flux of the diatom Thalassiothrix antarctica beneath the Antarctic Polar Front and provide a marker for tracking the migration of the Front through time. Ocean Drilling Program Sites 1091, 1093 and 1094 are the only deep piston cored record hitherto sampled from the sediments of the circumpolar biogenic opal belt. Mapping of diatom mat deposits between these sites indicates a glacial-interglacial front migration of up to 6 degrees of latitude in the early / mid Pleistocene. The mid Pleistocene transition marks a stepwise minimum 7 degree northward migration of the locus of the Polar Front sustained for about 450 kyr until an abrupt southward return to a locus similar to its modern position and further south than any mid-Pleistocene locus. This interval from a “900 ka event” that saw major cooling of the oceans and a ?13C minimum through to the 424 ka Mid-Brunhes Event at Termination V is also seemingly characterised by 1) sustained decreased carbonate in the subtropical south Atlantic, 2) reduced strength of Antarctic deep meridional circulation, 3) lower interglacial temperatures and lower interglacial atmospheric CO2 levels (by some 30 per mil) than those of the last 400 kyr, evidencing less complete deglaciation. This evidence is consistent with a prolonged period lasting 450 kyr of only partial ventilation of the deep ocean during interglacials and suggests that the mechanisms highlighted by recent hypotheses linking mid-latitude atmospheric conditions to the extent of deep ocean ventilation and carbon sequestration over glacial-interglacial cycles are likely in operation during the longer time scale characteristic of the Mid-Pleistocene Transition. The cooling that initiated the “900 ka event” may have been driven by minima in insolation amplitude related to eccentricity modulation of precession that also affected low latitude climates as marked by threshold changes in the African monsoon system. The major thresholds in earth system behaviour through the Mid-Pleistocene Transition were likely governed by an interplay of the 100 kyr and 400 kyr eccentricity modulation of precession
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