1,721,197 research outputs found

    Going Beyond Counting First Authors in Author Co-citation Analysis

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    The present study examines one of the fundamental aspects of author co-citation analysis (ACA) - the way co-citation counts are defined. Co-citation counting provides the data on which all subsequent statistical analyses and mappings are based, and we compare ACA results based on two different types of co-citation counting - the traditional type that only counts the first one among a cited work's authors on the one hand and a non-traditional type that takes into account the first 5 authors of a cited work on the other hand. Results indicate that the picture produced through this non-traditional author co-citation counting contains more coherent author groups and is therefore considerably clearer. However, this picture represents fewer specialties in the research field being studied than that produced through the traditional first-author co-citation counting when the same number of top-ranked authors is selected and analyzed. Reasons for these effects are discussed

    Variations on the Author

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    “Variations on the Author” discusses two of Eduardo Coutinho’s recent films (Um Dia na Vida, from 2010, and Últimas Conversas, posthumously released in 2015) and their contribution to the general question of documentary authorship. The director’s filmography is characterized by a consistent yet self-effacing form of authorial self-inscription: Coutinho often features as an interviewer that rather than express opinions propels discourses; an interviewer that is good at listening. This mode of self-inscription characterizes him as an author who is not expressive but who is nonetheless markedly present on the screen. In Um Dia na Vida, however, Coutinho is completely absent form the image, while Últimas Conversas, on the contrary, includes a confessional prologue that moves the director from the margins to the center of his films. This article examines the ways in which these works stand out in the filmography of a director who offers new insights into the notion of cinematic authorship

    Appropriate Similarity Measures for Author Cocitation Analysis

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    We provide a number of new insights into the methodological discussion about author cocitation analysis. We first argue that the use of the Pearson correlation for measuring the similarity between authors’ cocitation profiles is not very satisfactory. We then discuss what kind of similarity measures may be used as an alternative to the Pearson correlation. We consider three similarity measures in particular. One is the well-known cosine. The other two similarity measures have not been used before in the bibliometric literature. Finally, we show by means of an example that our findings have a high practical relevance.information science;Pearson correlation;cosine;similarity measure;author cocitation analysis

    Dispelling the Myths Behind First-author Citation Counts

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    We conducted a full-scale evaluative citation analysis study of scholars in the XML research field to explore just how different from each other author rankings resulting from different citation counting methods actually are, and to demonstrate the capability of emerging data and tools on the Web in supporting more realistic citation counting methods. Our results contest some common arguments for the continued use of first-author citation counts in the evaluation of scholars, such as high correlations between author rankings by first-author citation counts and other citation counting methods, and high costs of using more realistic citation counting methods that are not well-supported by the ISI databases. It is argued that increasingly available digital full text research papers make it possible for citation analysis studies to go beyond what the ISI databases have directly supported and to employ more sophisticated methods

    Author Index

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    koamabayili/VECTRON-author-checklist: VECTRON author checklist

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    We have done our best to complete the author checklist relating to the use of animals in the hut study. Note that the objective for the hut study was to evaluate the IRS treatment applications for residual efficacy against Anopheles mosquitoes, including the local An. coluzzii mosquito population. Cows were only used to attract mosquitoes into the huts and no tests were carried out directly on the cows. The author checklist is intended for use with studies where experiments are carried out on animals, which is why we have had such difficulty in completing this for the hut study, as many of the questions do not relate to how the cows were used

    The cycling of sulfur dioxide in the marine boundary layer

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    The atmospheric cycling of sulfur dioxide (SO\sb2) is examined through the use of field measurements and photochemical modeling. A question exists as to whether or not SO\sb2 is a major product of dimethylsulfide (DMS) oxidation and subsequently important in the formation of new particles and cloud condensation nuclei (CCN). The relative magnitudes of the different sources and sinks of SO\sb2 in the remote marine boundary layer are looked at using field measurements of SO\sb2, DMS, and hydrogen sulfide (H\sb2S) and a time dependent photochemical box model of an air mass in the marine boundary layer.A new automated technique for measuring SO\sb2 was developed. It enables continuous real-time measurement of SO\sb2 using HPLC/Fluorescence at parts-per-trillion levels. Atmospheric and seawater DMS and atmospheric H\sb2S were also measured during these cruises in order to define the biogenic sources of SO\sb2.The observed SO\sb2 levels in the marine boundary layer are much lower than those predicted by current photochemical models using the measured DMS concentrations. Also, current models predict that SO\sb2 should have a pronounced diel cycle that is anticorrelated to that of DMS, however there is no observable diel cycle in the SO\sb2 data. Using a time-dependent photochemical box model and a model of the aqueous phase sea-salt aerosol chemistry, we examine the role of heterogeneous loss to sea-salt aerosols as a potentially important but previously unaccounted for sink for SO\sb2 in the marine boundary layer. Our results indicate that this is a large sink for SO\sb2 in this region.</p

    A study of methanesulfonic acid in ice cores

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    Methanesulfonic acid (MSA), an oxidation product of DMS, is used as a biogenic sulfur tracer in deposited snow layers to better understand the relative importance of various sulfur inputs (biogenic, volcanic and anthropogenic sulfur) to both polar regions in the past.The ice cores and snowpit samples were collected from the 20D site (Greenland) and the Dominion Range site (Antarctica). A suppressed ion chromatographic method was used to measure MSA in snow and ice. The mean concentration of MSA in the 20D ice core is 3.30 ppb (σ\sigma = 2.38 ppb, n = 1134). The MSA concentrations have decreased since 1900. The ratios of MSA/total S(VI) in the 20D ice core ranged from 15% before 1900 to 5% after 1900. These results suggest a non-biogenic sulfate source to the Greenland ice sheet at the present time. Based on the assumption that the pre-industrial ratios reflect the biogenic sulfur component in the sulfur burden, we estimate that, at the present time, approximately 80% of sulfur input to Greenland is contributed to non-biogenic sulfur.Seasonal variations of MSA in ice are observed in many but not all years. The seasonality in the 20D ice core is consistent with aerosol MSA data from high latitude stations which confirms that ice records that atmospheric changes. Complications of meterological conditions are believed to be responsible for the lack of seasonality of MSA in ice.The mean concentrations of MSA in the Dominion Range snowpit and ice core are 2.76 ppb (σ\sigma = 2.36, n = 199) and 0.94 ppb (σ\sigma = 0.56, n = 258), respectively. The mean MSA/total S(VI) ratio is below 1% at the Dominion Range site. These data confirm that the MSA fraction in the high plateau is considerably lower than in coastal Antarctica and in the low- and the high-latitude marine boundary layer. Possible causes include volcanic sulfate input, long range transport of low-latitude biogenic sulfur, and additional stratospheric sulfate input.In summary, all of the above suggest that transport related sulfur source changes may primarily control the atmospheric chemistry, and consequently the ice chemistry, in both polar regions.</p
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