1,592 research outputs found

    The British art show 8, Norwich: transformative experiences fade away

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    Classification of Generalized Multiresolution Analyses

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    We discuss how generalized multiresolution analyses (GMRAs), both classical and those defined on abstract Hilbert spaces, can be classified by their multiplicity functions mm and matrix-valued filter functions HH. Given a natural number valued function mm and a system of functions encoded in a matrix HH satisfying certain conditions, a construction procedure is described that produces an abstract GMRA with multiplicity function mm and filter system HH. An equivalence relation on GMRAs is defined and described in terms of their associated pairs (m,H)(m,H). This classification system is applied to classical examples in L2(Rd)L^2 (\mathbb R^d) as well as to previously studied abstract examples.Comment: 18 pages including bibliograp

    Drumming Up an Audience: When Spectacle Becomes Failure

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    Funding streams designed to enable wider participation with contemporary visual art often fail to meet their objectives. Faced with the need to show increased engagement in return for public funding, fear of failure has led many organisations to turn to what we describe as the ‘art-spectacle’: public artworks developed as a means of demonstrating public participation. What is the nature of the engagement when large crowds encounter an art-spectacle? When art-spectacles appropriate an existing cultural form and rebrand it as ‘art’, by what criteria can it be judged a success or failure? Our discussion centres on The History Train, an event that formed part of British Art Show 8 in Norwich in 2016. As it received funding to engage new audiences, we assess The History Train against the criteria by which the funding was awarded. We also look at the degree to which it met Debord’s (1983) logic of spectacle and the necessity of visibility over experience

    Submergence and uplift associated with the giant 1833 Sumatran subduction earthquake: Evidence from coral microatolls

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    The giant Sumatran subduction earthquake of 1833 appears as a large emergence event in fossil coral microatolls on the reefs of Sumatra's outer-arc ridge. Stratigraphic analysis of these and living microatolls nearby allow us to estimate that 1833 emergence increased trenchward from about 1 to 2 m. This pattern and magnitude of uplift are consistent with about 13 m of slip on the subduction interface and suggest a magnitude (M_w) of 8.8–9.2 for the earthquake. The fossil microatolls also record rapid submergence in the decades prior to the earthquake, with rates increasing trenchward from 5 to 11 mm/yr. Living microatolls show similar rates and a similar pattern. The fossil microatolls also record at least two less extensive emergence events in the decades prior to 1833. These observations show that coral microatolls can be useful paleoseismic and paleogeodetic instruments in convergent tectonic environments
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