Technical Report Background Reading Guidance and Links

Handout which contains a set of links to a variety of background resources associated with the topics for a technical report coursework. Resources are clustered into three overview areas, but contain links which be used to address each of the six questions scenarios.

Data Protection Act links to film, slides, quesions; overview notes

Published on Jun 7, 2012 by icocomms This ICO training video helps answer questions about the Data Protection Act, its impact on the working environment and how to handle and protect people's information. (Produced by Central Office of Information, Crown Copyright 2006)

Making Links: An Introduction to Hypertext

Introduction to hypertext, looking at its roots in information science, scholarly communication and experimental literature.

Sustaining Success Links and Readings

Links to video's (wip)

Sustaining Success Submitted Tasks Summary Links

link to the documents which describe each of the tasks, one of which students may choose to submit

FY14-15 Links

Useful/relevant sites

FY-RTS 3 Videos 1 of 3 (six links)

Watch, discuss, reflect CONTENT: Six videos introducing ideas about learning and reflection

Technical report template, links to additonal writing resources

A set of support material to be used when preparing a technical report. Includes report template, and links to other supporting materials specific to the University. Finally link to 2015 COMP1205 technical report assignment specification and allocations http://www.edshare.soton.ac.uk/14582/

Technical report specification, 2015 allocations, mark scheme, links

Specification for technical report, allocations (2015) mark scheme. Also contains a links to supporting materials including Harvard referencing. A template for a technical report is found at http://www.edshare.soton.ac.uk/14581

A proposal of categorization for analysing inductive reasoning. 'Una propuesta de categorización para analizar el razonamiento inductivo'.

Investigación original con el título: 'Razonamiento inductivo puesto de manifiesto por alumnos de Secundaria' de María Consuelo Cañadas Santiago, publicada en 2002 por la Universidad de Granada

Water vapor variability in the tropics and its links to dynamics and precipitation

The distribution and variability of water vapor and its links with radiative cooling and latent heating via precipitation are crucial to understanding feedbacks and processes operating within the climate system. Column-integrated water vapor (CWV) and additional variables from the European Centre for Medium-Range Weather Forecasts (ECMWF) 40-year reanalysis (ERA40) are utilized to quantify the spatial and temporal variability in tropical water vapor over the period 1979–2001. The moisture variability is partitioned between dynamical and thermodynamic influences and compared with variations in precipitation provided by the Climate Prediction Center Merged Analysis of Precipitation (CMAP) and the Global Precipitation Climatology Project (GPCP). The spatial distribution of CWV is strongly determined by thermodynamic constraints. Spatial variability in CWV is dominated by changes in the large-scale dynamics, in particular associated with the El Niño–Southern Oscillation (ENSO). Trends in CWV are also dominated by dynamics rather than thermodynamics over the period considered. However, increases in CWV associated with changes in temperature are significant over the equatorial east Pacific when analyzing interannual variability and over the north and northwest Pacific when analyzing trends. Significant positive trends in CWV tend to predominate over the oceans while negative trends in CWV are found over equatorial Africa and Brazil. Links between changes in CWV and vertical motion fields are identified over these regions and also the equatorial Atlantic. However, trends in precipitation are generally incoherent and show little association with the CWV trends. This may in part reflect the inadequacies of the precipitation data sets and reanalysis products when analyzing decadal variability. Though the dynamic component of CWV is a major factor in determining precipitation variability in the tropics, in some regions/seasons the thermodynamic component cancels its effect on precipitation variability.