6,461 research outputs found

    Minimum entropy restoration using FPGAs and high-level techniques

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    One of the greatest perceived barriers to the widespread use of FPGAs in image processing is the difficulty for application specialists of developing algorithms on reconfigurable hardware. Minimum entropy deconvolution (MED) techniques have been shown to be effective in the restoration of star-field images. This paper reports on an attempt to implement a MED algorithm using simulated annealing, first on a microprocessor, then on an FPGA. The FPGA implementation uses DIME-C, a C-to-gates compiler, coupled with a low-level core library to simplify the design task. Analysis of the C code and output from the DIME-C compiler guided the code optimisation. The paper reports on the design effort that this entailed and the resultant performance improvements

    Restoration of star-field images using high-level languages and core libraries

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    Research into the use of FPGAs in Image Processing began in earnest at the beginning of the 1990s. Since then, many thousands of publications have pointed to the computational capabilities of FPGAs. During this time, FPGAs have seen the application space to which they are applicable grow in tandem with their logic densities. When investigating a particular application, researchers compare FPGAs with alternative technologies such as Digital Signal Processors (DSPs), Application-Specific Integrated Cir-cuits (ASICs), microprocessors and vector processors. The metrics for comparison depend on the needs of the application, and include such measurements as: raw performance, power consumption, unit cost, board footprint, non-recurring engineering cost, design time and design cost. The key metrics for a par-ticular application may also include ratios of these metrics, e.g. power/performance, or performance/unit cost. The work detailed in this paper compares a 90nm-process commodity microprocessor with a plat-form based around a 90nm-process FPGA, focussing on design time and raw performance. The application chosen for implementation was a minimum entropy restoration of star-field images (see [1] for an introduction), with simulated annealing used to converge towards the globally-optimum solution. This application was not chosen in the belief that it would particularly suit one technology over another, but was instead selected as being representative of a computationally intense image-processing application

    The Influence of Whaler William Scoresby, Jr. on the Arctic Observations of Sir James Lamont

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    Scottish adventurer James Lamont led hunting expeditions to Svalbard (1858 and 1859) and to Svalbard and Novaya Zemlya (1869 to 1871), voyages chronicled in his two publications, Seasons with the Sea-horses (1861) and Yachting in the Arctic Seas (1876). These works were modeled on the English whaler William Scoresby, Jr.’s An Account of the Arctic Regions, with a History and Description of the Northern Whale-Fishery, Vol. 1, written in 1820. Scoresby’s book, as well as a correspondence with evolutionary theorist, Charles Darwin, inspired Lamont to pursue science during an Arctic hunt. Lamont’s scientific endeavours included geographical surveys, the collection of geological specimens, and basic experiments in physical oceanography. However, most importantly, Lamont provided the first account of Arctic wildlife in the context of natural selection. Lamont’s legacy as an Arctic explorer linked the early sea-hunters like Scoresby to a later generation of Victorian hunter-explorers, such as Benjamin Leigh Smith, who followed Lamont’s lead and journeyed northward to hunt and conduct scientifically grounded explorations.James Lamont, aventurier Ă©cossais, a menĂ© des expĂ©ditions de chasse au Svalbard (en 1858 et en 1859) ainsi qu’au Svalbard et Ă  Novaya Zemlya (de 1869 Ă  1871). Il a racontĂ© ses expĂ©ditions dans ses deux publications, Seasons with the Sea-horses (1861) et Yachting in the Arctic Seas (1876). Ces oeuvres prenaient modĂšle sur celle de William Scoresby, fils, chasseur de baleines anglais qui a publiĂ© An Account of the Arctic Regions, with a History and Description of the Northern Whale-Fishery, Vol. 1, en 1820. L’oeuvre de William Scoresby de mĂȘme que la correspondance avec Charles Darwin, thĂ©oricien Ă©volutionnaire, a inspirĂ© James Lamont Ă  explorer l’aspect scientifique d’une de ses expĂ©ditions de chasse dans l’Arctique. À cette occasion, il a fait des levĂ©s gĂ©ographiques, prĂ©levĂ© des Ă©chantillons gĂ©ologiques et rĂ©alisĂ© des expĂ©riences rudimentaires en ocĂ©anographie physique. Mais qui plus est, James Lamont a fait les premiers rĂ©cits sur la faune arctique dans le contexte de la sĂ©lection naturelle. Le travail effectuĂ© par James Lamont en tant qu’explorateur de l’Arctique a permis de faire le pont entre les premiers chasseurs de baleines comme William Scoresby et une gĂ©nĂ©ration plus tardive d’explorateurs-chasseurs victoriens, comme Benjamin Leigh Smith, qui a suivi les traces de Lamont vers le nord pour chasser et faire des explorations Ă  caractĂšre scientifique

    A Study of Marine Terrace Formation Along the California Central Coast

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    Marine terrace formation is in many instances attributed to wave action, and shore platforms are often called “wave-cut”. However, alternative models for marine terrace formation suggest that other types of physical and chemical weathering have a more central role in the formation of marine terraces than is widely acknowledged. Roering and Retallack (2012) concluded that the roles of subaerial physical and chemical weathering are significant, and played a major role in the formation of the terraces. In this study, weathering of beach cliffs and shore platforms associated with marine terraces at eight sites in two different locations along the central California Coast is assessed, and results are compared to those of Roering and Retallack. Findings for rock hardness along the profile of modern shore platform and cliff face are similar to the results from the Roering and Retallack study: the Schmidt rock hardness of cliff faces within the bottom 1.5 meters above the modern shoreline angle are significantly lower than the rock hardness of the shore platform. Oxidation color of shore platforms, assessed using a Munsell color and described in Munsell color notation, is consistently within the Gley 1 range in both study areas. Beach cliff oxidation color varied from Gley to colors indicating oxidation. Oxidation on beach cliffs was more prevalent within the upper half meter of the part of the beach cliff that was sampled, and oxidation within fractures and cracks was also apparent in some cliff faces
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