422 research outputs found

    Notre article de synthèse: Que nous a appris la comète de Halley?

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    Comet Halley is already back in the outer solar system, forgotten by most of us. But the cometary specialists are still busy with the wealth of data gathered during a few months of frantic activity, peaking with the spacecraft fly-bys. The author summarizes here some of the new results which have been obtained up to now about P/Halley

    Sporadic imprinting defects in Prader-Willi-Syndrome and Angelman-Syndrome - implications for imprint-switch models, genetic counseling, and prenatal diagnosis

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    Karin Buiting, Bärbel Dittrich, Stephanie Groß, Christina Lich, Claudia Färber, Tina Buchholz, Ellie Smith, André Reis, Joachim Bürger, Markus M. Nöthen, Ulli Barth-Witte, Bart Janssen, Dvorah Abeliovich, Israela Lerer, Ans M.W. van den Ouweland, Dicky J.J. Halley, Connie Schrander-Stumpel, Hubert Smeets, Peter Meinecke, Sue Malcolm, Anne Gardner, Marc Lalande, Robert D. Nicholls, Kathie Friend, Astrid Schulze, Gert Matthijs, Hannaleena Kokkonen, Pascale Hilbert, Lionel Van Maldergem, Guillermo Glover, Pablo Carbonell, Patrick Willems, Gabriele Gillessen-Kaesbach, Bernhard Horsthemk

    On the use of satellite observations to fill gaps in the Halley station total ozone record

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    Measurements by the Dobson ozone spectrophotometer at the British Antarctic Survey's (BAS) Halley research station form a record of Antarctic total column ozone that dates back to 1956. Due to its location, length, and completeness, the record has been, and continues to be, uniquely important for studies of long-term changes in Antarctic ozone. However, a crack in the ice shelf on which it resides forced the station to abruptly close in February of 2017, leading to a gap of two ozone hole seasons in its historic record. We develop and test a method for filling in the record of Halley total ozone by combining and adjusting overpass data from a range of different satellite instruments. Comparisons to the Dobson suggest that our method reproduces monthly ground-based total ozone values with an average difference of 1.1 ± 6.2 DU for the satellites used to fill in the 2017–2018 gap. We show that our approach more closely reproduces the Dobson measurements than simply using the raw satellite average or data from a single satellite instrument. The method also provides a check on the consistency of the provisional data from the automated Dobson used at Halley after 2018 with earlier manual Dobson data and suggests that there were likely inconsistencies between the two. The filled Halley dataset provides further support that the Antarctic ozone hole is healing, not only during September but also in January

    Color gradients in the coma of P/Halley

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    Some important information relevant to the understanding of the gas/dust dynamics near the surface of a comet nucleus concerns knowledge of the grain composition and scattering properties as well as the particle size distribution of dust in the coma. Ground based measurements of light scattered from the dust comae can provide some information about the physical grain properties, in particular about the mean optically dominant grain size. Optical spectra of continua of nine comets presented by Jewitt and Meech, 1986, show that all of the scattered light is reddened with respect to the Sun. There is significant scatter in the amount of reddening seen for different comets. In the near IF regions, the reddening decreases until near 2 to 3 micrometers where the reflectivity is nearly neutral. It is of particular interest to see if there are any observable changes in the grain size distribution during outburst. Although no coma colar changes were observed during the Nov. 1985 outbursts, a color gradient within the coma has been observed in Halley. Radial color gradients in J, H, and K images of Halley as reported by Campins have not been observed by the author

    Convergence regions for the Chebyshev–Halley family

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    In this paper we study the dynamical behavior of the Chebyshev–Halley methods on the family of degree n polynomials . We prove that, despite increasing the degree, it is still possible to draw the parameter space by using the orbit of a single critical point. For the methods having as an attracting fixed point, we show how the basins of attraction of the roots become smaller as the value of n grows. We also demonstrate that, although the convergence order of the Chebyshev–Halley family is 3, there is a member of order 4 for each value of n. In the case of quadratic polynomials, we bound the set of parameters which correspond to iterative methods with stable behaviour other than the basins of attraction of the roots

    Methods and results for estimating the hydraulic characteristics of the subsurface materials in the Harney Basin, Oregon

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    Gerald H. Grondin, Darrick E. Boschmann, Halley J. Schibel, Benjamin P. Scandella.Title from PDF cover (viewed on December 20, 2021).This archived document is maintained by the State Library of Oregon as part of the Oregon Documents Depository Program. It is for informational purposes and may not be suitable for legal purposes.Includes bibliographical references (pages 56-63).Mode of access: Internet from the Oregon Government Publications Collection.Text in English

    A chart of the ocean between South America and Africa with the tracks of Dr. Edmund Halley in 1700 and Monsr. Lozier Bouvet in 1738 [cartographic material] /

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    Map of the South Atlantic Ocean flanked by South America on the left and Africa on the right. The map features the time-dated sea-tracks of 18th century explorers Edmund Halley in command of HM Pink Paramore and later Lozier Bouvet in command of the Eagle and the Mary.; Imprint on map: Published according to Act of Parliament, April 1769.; Prime meridian: Greenwich.; From: A collection of voyages chiefly in the South Atlantick Ocean / Alexander Dalrymble. London : Printed for the author; sold by J. Nourse, 1775.; Also available in an electronic version via the Internet at: http://nla.gov.au/nla.map-rm461

    Release and uptake of lysosomal enzymes : studied in cultured cells

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    The purpose of the experimental work described in this thesiswas to investigate some aspects of the release and uptake of lysosomal enzymes. The experiments involved the use of normal human and animal fibroblasts and some other cell types such as hepatocytes and hepatoma cells as sources of hydrolytic enzymes, and fibroblasts from patients with lysosomal storage diseases associated with a single lysosomal enzyme deficiency and with "1-cell" disease as recipient cells. In a number of studies co-cultivation of normal and mutant cells was applied. as a means to study the release and uptake of lysosomal enzymes at physiological concentrations. We have also studied some characteristics of released lysosomal enzyme activities in· normal and mutant cell cultures in comparison with the corresponding intracellular activities. Finally, we have used somatic cell hybridization to investigate the genetic background of the metabolic abnormalities in some of the human mutant cells. Our studies have provided information on the normal transport of lysosomal enzymes within the cell and between cells. Furthermore, we hope that more knowledge about recognition and uptake of lysosomal enzymes by deficient cells from patients with lysosomal storage diseases will have future implications for enzyme therapy

    Halley's Method as the First Member of an Infinite Family of Cubic Order Rootfinding Methods

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    For each natural number m ≥ 3, we give a rootfinding method Hm, with cubic order of convergence for simple roots. However, for quadratic polynomials the order of convergence of Hm is m. Each Hm depends on the input, the corresponding function value, as well as the first two derivatives. We shall refer to this family as Halley Family, since H3 is the well-known method of Halley. For all m ≥ 4, the asymptotic error constant of Hm is the same constant. Each Hm is described in terms of determinants that are computable recursively. The Halley Family and their derivative-free variants offer alternatives to the traditional rootfinding methods, such as secant, Newton, and Muller methods, as well as Halley’s method itself.Technical report DCS-TR-37
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