998 resultados para Leckingfield Manor House, Yorkshire, England.


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Mode of access: Internet.

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Self-adaptation is emerging as an increasingly important capability for many applications, particularly those deployed in dynamically changing environments, such as ecosystem monitoring and disaster management. One key challenge posed by Dynamically Adaptive Systems (DASs) is the need to handle changes to the requirements and corresponding behavior of a DAS in response to varying environmental conditions. Berry et al. previously identified four levels of RE that should be performed for a DAS. In this paper, we propose the Levels of RE for Modeling that reify the original levels to describe RE modeling work done by DAS developers. Specifically, we identify four types of developers: the system developer, the adaptation scenario developer, the adaptation infrastructure developer, and the DAS research community. Each level corresponds to the work of a different type of developer to construct goal model(s) specifying their requirements. We then leverage the Levels of RE for Modeling to propose two complementary processes for performing RE for a DAS. We describe our experiences with applying this approach to GridStix, an adaptive flood warning system, deployed to monitor the River Ribble in Yorkshire, England.

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Este trabajo es el resultado de un detallado estudio acerca del modo como la justicia e institución inquisitorial consiguieron penetrar en los espacios propios de la jurisdicción señorial de Monarquía Hispánica durante el siglo XVII. Para realizar este análisis se ha tomado como objeto de estudio el ducado y la villa de Pastrana, situados en la Alcarria. Los protagonistas de esta compleja problemática estudiada fueron los grupos de portugueses que se asentaron en el territorio de este señorío y en su villa principal a lo largo de los siglos XVI y XVII, los cuales participaron en su vida social, económica y política de manera muy intensa. Su papel en la dinamización y organización interna de este espacio señorial fue notable. La acusación de judaísmo contra algunos de estos portugueses y el procesamiento inquisitorial al que fueron sometidos nos permite ver algunos aspectos fundamentales de esta interesante cuestión.

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At various times during the Quaternary, north-eastern England was a zone of confluence between dynamic ice lobes sourced from the Pennines, northern Scotland, the Cheviots, and Scandinavia. The region thus has some of the most complex exposures of Middle to Late Pleistocene sediments in Britain, with both interglacial and glacial sediments deposited in terrestrial and marine settings. We investigated sedimentary sequences exposed on the coastline of County Durham at Warren House Gill, and present a new model of British and Fennoscandian Ice Sheet interaction in the North Sea Basin during the Middle Pleistocene. The stratigraphy at Warren House Gill consists of a lower diamicton and upper estuarine sediments, both part of the Warren House Formation. They are separated from the overlying Weichselian Blackhall and Horden tills by a substantial unconformity. The lower diamicton of the Warren House Formation is re-interpreted here as an MIS 8 to 12 glaciomarine deposit containing ice-rafted lithics from north-eastern Scotland and the northeast North Sea, and is renamed the ‘Ash Gill Member’. It is dated by lithological comparison to the Easington Raised Beach, Middle Pleistocene Amino Acid Racemisation values, and indirectly by optically stimulated luminescence. The overlying shallow subaqueous sediments were deposited in an estuarine environment by suspension settling and bottom current activity. They are named the ‘Whitesides Member’, and form the uppermost member of the Warren House Formation. During glaciation, ice-rafted material was deposited in a marine embayment. There is no evidence of a grounded, onshore Scandinavian ice sheet in County Durham during MIS 6, which has long been held as the accepted stratigraphy. This has major implications for the currently accepted British Quaternary Stratigraphy. Combined with recent work on the Middle Pleistocene North Sea Drift from Norfolk, which is now suggested to have been deposited by a Scottish ice sheet, the presence of a Scandinavian ice sheet in eastern England at any time during the Quaternary is becoming increasingly doubtful.

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Illustrated t.-p.

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"Although the life of Walter Spencer-Stanhope occupies a large proportion of the present volumes, it is not the object of these pages to present one particular biography. They aim rather to be a record of certain facts and anecdotes gleaned from the papers of that old Yorkshire house of which he become owner."--Pref.

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"The reports to which this index is now attached form four volumes ... The present Digest forms a fifth volume and completes the set." - Pref.