BDNF impairs recovery of synaptic transmission after hypoxia even with blockage of adenosine A2A receptors

Trabalho Final do Curso de Mestrado Integrado em Medicina, Faculdade de Medicina, Universidade de Lisboa, 2014

A matemática e as tic no processo de ensino e aprendizagem : o geogebra no ensino de funções e gráficos de uma função

Dissertação de mestrado, Educação (Área de especialidade em Educação e Tecnologias Digitais), Universidade de Lisboa, Instituto de Educação, 2016

Cyclical dimensions of labour mobility after EU enlargement. Bruegel Working Paper 2009/03, May 2009

At a time of symmetric global slowdown, migration cannot contribute as much to absorbing economic shocks as it could if the shock were asymmetric. • Early evidence suggests that the crisis has led to a drop in immigration and even net return migration from some countries. This has helped the adjustment of former EU15 host countries and has exacerbated adjustment in former source countries in the new member states. In the short run, the stock of new member-state migrants in the EU15 will fall owing to diminished job opportunities for migrants. • Changes in the unemployment rate in the host country are found to impact migration more than that of changes in the unemployment rate in the source country. In part, this can be explained by the disproportionate risk of migrants losing their jobs in the downturn. • In the longer run, the crisis is set to increase migration from the new member states compared to what would have been the case without the crisis. This is because the crisis has undermined the economic growth model of those new member states that relied heavily on external financing to fuel their growth.

Die Europäische Union und das Rahmenübereinkommen zum Schutz nationaler Minderheiten: ignorieren, parallell “umsetzen“ oder gar beitreten? = The European Union and the Framework Convention for the Protection of National Minorities: ignore, "implement" or even join? EDAP Paper 04/2014

This paper looks at the Council of Europe Framework Convention for the Protection of National Minorities (FCNM) through the lense of European Union law. It does so by posing four major questions: does the fact that 24 of 28 Member States of the EU ratified the FCNM have any legal implications for the European Union itself? Secondly, turning to the national level, does it make a difference for the implementation of the FCNM whether or not a state that has ratified the FCNM is also a member to the European Union? Thirdly, returning to the European Union itself, can and should the EU accede to the FCNM? Or are there, finally, any means beside ratification that would allow the European Union to implement the objectives and obligations as enshrined in the FCNM? These four questions are analysed in detail before the paper concludes on the potential role of the European Union in managing diversity and protecting (persons belonging to) minorities.

Don’t complicate it even further: Macroeconomic Conditionality as a Substitute for new Structural Reform Contracts. European Policy Brief No. 15, May 2013

The idea of introducing contracts between Member States and the EU on structural reforms has its merits, it also has several disadvantages. Most notably, the contracts risk rendering European economic governance even more complex and cumbersome. It is therefore sensible to first try to integrate the structural reform contracts into one of the foreseen economic governance instruments. This Policy Brief argues that macroeconomic conditionality can serve this purpose. With some minor reforms, it could even become a full-fledged substitute for structural reform contracts – without suffering some of latter’s disadvantages.

MRTAB: Stata module to compute one- and two-way tables/graphs of multiple responses

mrtab tabulates multiple responses which are held as a set of indicator variables or as a set of polytomous response variables.

Datasets for the graphs of the paper (Fig. 2 to Fig. 7)

Investigating the relationship between factors (climate change, atmospheric CO2 concentrations enrichment, and vegetation structure) and hydrological processes is important for understanding and predicting the interaction between the hydrosphere and biosphere. The Integrated Biosphere Simulator (IBIS) was used to evaluate the effects of climate change, rising CO2, and vegetation structure on hydrological processes in China at the end of the 21st century. Seven simulations were implemented using the assemblage of the IPCC climate and CO2 concentration scenarios, SRES A2 and SRES B1. Analysis results suggest that (1) climate change will have increasing effects on runoff evapotranspiration (ET), transpiration (T), and transpiration ratio (transpiration/evapotranspiration, T/E) in most hydrological regions of China except in the southernmost regions; (2) elevated CO2 concentrations will have increasing effects on runoff at the national scale, but at the hydrological region scale, the physiology effects induced by elevated CO2 concentration will depend on the vegetation types, climate conditions, and geographical background information with noticeable decreasing effects shown in the arid Inland region of China; (3) leaf area index (LAI) compensation effect and stomatal closure effect are the dominant factors on runoff in the arid Inland region and southern moist hydrological regions, respectively; (4) the magnitudes of climate change (especially the changing precipitation pattern) effects on the water cycle are much larger than those of the elevated CO2 concentration effects; however, increasing CO2 concentration will be one of the most important modifiers to the water cycle; (5) the water resource condition will be improved in northern China but depressed in southernmost China under the IPCC climate change scenarios, SRES A2 and SRES B1.

Raw data of SCADCP (self-contained Acoustic Doppler Current Profiler) from three moorings in the Eastern Weddell Sea, 2005-2008

The success of any efforts to determine the effects of climate change on marine ecosystems depends on understanding in the first instance the natural variations, which contemporarily occur on the interannual and shorter time scales. Here we present results on the environmental controls of zooplankton distribution patterns and behaviour in the eastern Weddell Sea, Southern Ocean. Zooplankton abundance and vertical migration are derived from the mean volume backscattering strength (MVBS) and the vertical velocity measured by moored acoustic Doppler current profilers (ADCPs), which were deployed simultaneously at 64°S, 66.5°S and 69°S along the Greenwich Meridian from February, 2005, until March, 2008. While these time series span a period of full three years they resolve hourly changes. A highly persistent behavioural pattern found at all three mooring locations is the synchronous diel vertical migration (DVM) of two distinct groups of zooplankton that migrate between a deep residence depth during daytime and a shallow depth during nighttime. The DVM was closely coupled to the astronomical daylight cycles. However, while the DVM was symmetric around local noon, the annual modulation of the DVM was clearly asymmetric around winter solstice or summer solstice, respectively, at all three mooring sites. DVM at our observation sites persisted throughout winter, even at the highest latitude exposed to the polar night. Since the magnitude as well as the relative rate of change of illumination is minimal at this time, we propose that the ultimate causes of DVM separated from the light-mediated proximal cue that coordinates it. In all three years, a marked change in the migration behaviour occurred in late spring (late October/early November), when DVM ceased. The complete suspension of DVM after early November is possibly caused by the combination of two factors: (1) increased availability of food in the surface mixed layer provided by the phytoplankton spring bloom, and (2) vanishing diurnal enhancement of the threat from visually oriented predators when the illumination is quasi-continuous during the polar and subpolar summer. Zooplankton abundance in the water column, estimated as the mean MVBS in the depth range 50-300 m, was highest end of summer and lowest mid to end winter on the average annual cycle. However, zooplankton abundance varied several-fold between years and between locations. Based on satellite and in situ data of chlorophyll and sea ice as well as on hydrographic measurements, the interannual and spatial variations of zooplankton mean abundance can be explained by differences in the magnitude of the phytoplankton spring bloom, which develops during the seasonal sea ice retreat. Whereas the vernal ice melt appears necessary to stimulate the blooming of phytoplankton, it is not the determinator of the blooms magnitude, its areal extent and duration. A possible explanation for the limitation of the phytoplankton bloom in some years is top-down control. We hypothesise that the phytoplankton spring development can be curbed by grazing when the zooplankton had attained high abundance by growth during the preceding summer.