A functional analysis of change propagation

A thorough understanding of change propagation is fundamental to effective change management during product redesign. A new model of change propagation, as a result of the interaction of form and function is presented and used to develop an analysis method that determines how change is likely to propagate. The analysis produces a Design Structure Matrix, which clearly illustrates change propagation paths and highlights connections that could otherwise be ignored. This provides the user with an in-depth knowledge of product connectivity, which has the potential to support the design process and reduce the product's susceptibility to future change

Dual-frequency GPS survey for validation of a regional DTM and for the generation of local DTM data for sea-level rise modelling in an estuarine salt marsh

Global average temperatures have risen by an average of 0.07°C per decade over the last 100 years, with a warming trend of 0.13°C per decade over the last 50 years. Temperatures are predicted to rise by 2°C - 4.4°C by 2100 leading to global average sealevel rise (SLR) of 2 – 6mm per year (20 – 60cms in total) up to 2100 (IPCC 2007) with impacts for protected coastal habitats in Ireland. Estuaries are predominantly sedimentary environments, and are characterised by shallow coastal slope gradients, making them sensitive to even modest changes in sea-level. The Shannon estuary is the largest river estuary in Ireland and is designated as a Special Area of Conservation (SAC) under the EU Habitats Directive (EU 1992) providing protection for listed habitats within it, including estuarine salt marsh. Trends in Shannon estuary tidal data from 1877 – 2004 suggest an average upward SLR trend of 4 - 5mm/yr over this period. A simple linear extension of this historical trend would imply that local SLR will be in the region of 40 - 45cm by 2100. However, this may underestimate actual SLR for the estuary by 2100, since it takes no account of predicted climate-driven global SLR acceleration (IPCC 2007) up to 2100

Modeling the effect of predicted sea-level rise on coastal conservation habitats using GIS

Global average temperatures have in creased by about 0.6°C (± 0.2°C) during the 20th century, and are project ed to increase by 1.4 - 5.8°C by 2100 (IPCC, 2001a). The relationship between atmospheric warming and sea-level rise (SLR) is well understood, and this change is predicted to lead to SLR of up to 1m by 2100, cr eating consequences for coastal communities and environments worldwide (IPCC, 2001b)

How sensitive is tropospheric oxidation to anthropogenic emissions?

We use a global chemistry transport model to explore how changes in anthropogenic emissions alter ozone production and tropospheric oxidizing capacity over decadal (1990–2010) and centennial timescales (1900–2100). We find that the spatial extent of O3 production and loss in the troposphere changes very little despite large projected increases in precursor emissions. While tropospheric OH shows a long-term decrease of only 20% between 1900 and 2100, there are widespread changes in distribution which alter regional oxidation capacity substantially. We show that the remote marine boundary layer remains an important net sink of O3, as greater production related to increased continental NO x emissions is outweighed by greater O3 destruction. The critical NO x level required to support net O3 production doubles between 1900 and 2100, from 28 to 55 pptv on average, preventing any large-scale shift in production regime

Towards the assignment for the 41S04 ^1S_0 meson nonet

The strong decays of the $\pi(2070)$, $\eta(2010)$, $\eta(2100)$, $\eta(2190)$, and $\eta(2225)$ as the $4 ^1S_0$ quark-antiquark states are investigated in the framework of the $^3P_0$ meson decay model. It is found that the $\pi(2070)$, $\eta(2100)$, and $\eta(2225)$ appear to be the convincing $4 ^1S_0$ $q\bar{q}$ states while the assignment of the $\eta(2010)$ and $\eta(2190)$ as the $4 ^1S_0$ isoscalar states is not favored by their widths. In the presence of the $\pi(2070)$, $\eta(2100)$, and $\eta(2225)$ being the members of the $4 ^1S_0$ meson nonet, the $4 ^1S_0$ kaon is phenomenologically determined to has a mass of about 2153 MeV. The width of this unobserved kaon is expected to be about 197 MeV in the $^3P_0$ decay model.Comment: 15 pages, 5 figures, version accepted for publication in Physical Review

Information Management: A Consolidation of Operations, Analysis and Strategy

The book provides an exposition on the discipline of information management. It is organised into four parts. The first of these deals with factors that shape the meaning of information management - the professional associations that have formed; the science of information; and corporate approaches to consideration of information as an enterprise resource. The following three parts explain how information management is undertaken in three domains: operational, analytical and administrative. The operational domain details techniques that are concerned with processing information about information - the organising structures, finding aids, classification and retrieval systems, that make their respective information systems useable. The analytical domain is concerned with determining enterprise and user information requirements; undertaking requirements analysis; information audits; and evaluation of information operations. The administrative domain is concerned with the strategic approach – fostering effective utilisation of information and knowledge resources using a planning framework that aligns information services with that of an enterprise’s objectives and resourcing, and works effectively within constraints imposed by the broader regulatory and business environment

Disaggregate Inter-Urban Mode Choice Models: A review of British Evidence with special Reference to Cross Elasticities.

The research reported in this paper forms part of EPSRC project GRK52522 entitled 'National Multi-Modal Travel Forecasts'. The principal aim of this project is to develop a set of national and regional travel demand forecasts by land-based modes. These demand models for car, bus and rail will be based on a hierarchy of techniques and hence there are several strands to this research. One aspect of the research involves the review of aggregate models, based on collective travel behaviour, and the evidence that they yield on own and cross elasticities. Whilst such models provide a wealth of information on own elasticities, and are particularly well suited to the analysis of the effects of exogenous factors on travel demand, they tend to make little allowance for competitive effects and hence provide little evidence regarding cross-elasticities. Furthermore, their nature is such that there can be only limited segmentation of the elasticities by relevant travel and socio-economic factors. Another aspect of the study is reviewing the evidence that is provided by disaggregate models where, in contrast to the aggregate models, the unit of observation is the individual decision maker. Since such models examine competition between modes, they are particularly useful in providing evidence on cross-elasticities. A further aspect of the work will be the actual estimation of relevant demand models and elasticities for a range of circumstances and by a variety of means. The final stage prior to application of the models is to draw all the evidence together in a consistent manner, drawing upon the strengths of different approaches and the various insights that they provide