531 resultados para Stagnation


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Desde el surgimiento de las doctrinas económicas sobre el crecimiento endógeno, se ha determinado que la inversión extranjera es un factor que contribuye al crecimiento económico, ya que facilita la transferencia de tecnología y conocimientos en técnicas de producción, de mercadeo y de gestión en mercado extranjeras donde la competencia permite la existencia de incrementos en la productividad de los factores. Hacia el año 2000 la política de IED en Colombia, contemplaba unas políticas de gobierno centradas en la paz, reformas estructurales y promoción a las exportaciones. Dadas estas condiciones, los retos concernientes a aumentar la inversión extranjera eran bastante exigentes al momento de iniciar el periodo de gobierno de Álvaro Uribe Vélez (2002 – 2010), razón por la cual el objetivo de esta investigación es analizar los resultados al finalizar los dos periodos consecutivos de mandato del Presidente Uribe. Durante su gobierno, el Presidente Uribe Vélez, logró que la inversión extranjera directa alcanzara un notable incremento en sectores específicos como el minero y el petrolero, acompañando el proceso de crecimiento económico, sin embargo, este crecimiento no figura generalizado y contrariamente los índices de desempleo se incrementaron y las utilidades generadas se convierten en remesas al exterior conllevando baja reinversión en el país y estancamiento de otros sectores. Centraré la investigación en las situaciones inicial y final del periodo presidencial, en los aspectos concernientes a los niveles de inversión captados en Colombia, los sectores más favorecidos con dicha inversión, el origen de los recursos y la relación que estos flujos han tenido en los resultados de indicadores de crecimiento económico, productividad, competitividad, empleo y reinversión de utilidades.

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El lobby o cabildeo es una de las tácticas más utilizadas por los grupos de presión para lograr sus objetivos. Este mecanismo se refiere a la presión ejercida sobre un ente gubernamental con el fin de promover intereses particulares

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O trabalho cooperativo nas comunidades escolares apresenta inúmeras vantagens ao nível do desenvolvimento dos alunos, dos professores e da própria escola. No entanto, continuam a existir várias lacunas neste tipo de actividades e, especificando Portugal, existem muitos trabalhos de tipo diagnóstico, que não chegam para implantar cultura de cooperação. Quando falamos da implementação da cooperação nas escolas, temos de atender, obrigatoriamente, à cultura de escola vivenciada nas mesmas e à liderança, pois influenciam a cooperação. Este trabalho tem como finalidade verificar até que ponto existe trabalho cooperativo entre professores e perceber como se desenvolve a cultura de cooperação entre professores nos diferentes grupos de área disciplinar duma mesma escola. Para verificar este objectivo, participaram 13 responsáveis dos diferentes grupos de Áreas Disciplinares de uma escola secundária da zona do Estoril. Estes foram inquiridos através da aplicação de um questionário adaptado, daquele que foi validado e utilizado por Bolam et al (2005), e através de uma entrevista semi-estruturada, para análise da percepção que os mesmos têm sobre a cooperação e a cultura vivenciada dentro dos seus Grupos de Área Disciplinar. No geral, verificou-se que, relativamente à cooperação e à cultura cooperativa de grupo, os Departamentos de Área Curricular não diferem significativamente entre si, não existindo um grande sentido de cooperação. De acordo com as percepções dos inquiridos, verificou-se que existe uma fraca participação dos professores em acções cooperativas focalizadas no desenvolvimento profissional docente e focalizadas no desenvolvimento da cultura cooperativa ou através das precárias condições ou práticas extrínsecas a este desenvolvimento. Analisando a globalidade das mudanças verificadas nos últimos dois anos, constatou-se que os Grupos de Área Disciplinar estão a viver um momento de estagnação na maioria das questões inquiridas. Averiguou-se, também, que a não/fraca liderança por parte dos responsáveis de grupo de área disciplinar, resulta numa fraca participação dos professores em questões cooperativas. Através deste estudo, pode-se concluir que existe uma fraca cooperação entre os professores do mesmo Grupo de Área Disciplinar desta escola. Conclui-se também que a escola atravessa um momento de estagnação, não existindo um real desenvolvimento da cultura cooperativa na escola.

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The present essay’s central argument or hypothesis is, consequently, that the mechanisms accelerating a wealth concentrating and exclusionary economy centred on the benefit and overprotection of big business—with a corresponding plundering of resources that are vital for life—generated forms of loss and regression in the right to healthcare and the dismantling of institutional protections. These are all expressed in indicators from 1990-2005, which point not only to the deterioration of healthcare programs and services but also to the undermining of the general conditions of life (social reproduction) and, in contrast to the reports and predictions of the era’s governments, a stagnation or deterioration in health indicators, especially for those most sensitive to the crisis. The present study’s argument is linked together across distinct chapters. First, we undertake the necessary clarification of the categories central to the understanding of a complex issue; clarifying the concept of health itself and its determinants, emphasizing the necessity of taking on an integral understanding as a fundamental prerequisite to unravelling what documents and reports from this era either leave unsaid or distort. Based on that analysis, we will explain the harmful effects of global economic acceleration, the monopolization and pillaging of strategic healthcare goods; not only those which directly place obstacles on the access to health services, but also those like the destructuration of small economies, linked to the impoverishment and worsening of living modes. Thinking epidemiologically, we intend to show signs of the deterioration of broad collectivities’ ways of life as a result of the mechanisms of acceleration and pillage. We will then collect disparate evidence of the deterioration of human health and ecosystems to, finally, establish the most urgent conclusions about this unfortunate period of our social and medical history.

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In most EU member states, the business services industry has booked no productivity growth during the last two decades. The industry’s performance in the other member states was weaker than that of its US counterparts. Exploring what may be causing this productivity stagnation, this policy brief reports that weak competition has contributed to the continuing malaise in European business services. The study analyzed the persistence (over time) of firm-level inefficiencies. The evidence further suggests that competition between small firms and large firms in business services is weak. Markets for business services work best in countries with flexible regulation on employment change and with low regulatory costs for firms that start up or close down a business. Countries that are more open to foreign competition perform better in terms of competitive selection and productivity. The policy simulations in this paper show that greater import openness strengthens competition in business services markets. The largest positive impact comes from lower regulatory barriers for growing and shrinking firms. More particularly, competitive selection would be fostered by a reduction of administrative and regulatory costs related to labour contracts, bankruptcy and start-up requirements. A key element of the European Commission’s Europe-2020 strategy is the Single European Market for Services. Business services form one of the largest industries in Europe – and given its productivity stagnation, it deserves to be a priority target of the Europe-2020 strategy. Improving the way the business services market functions may have large positive knock-on effects for the EU economy.

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The influence of a large meridional submarine ridge on the decay of Agulhas rings is investigated with a 1 and 2-layer setup of the isopycnic primitive-equation ocean model MICOM. In the single-layer case we show that the SSH decay of the ring is primarily governed by bottom friction and secondly by the radiation of Rossby waves. When a topographic ridge is present, the effect of the ridge on SSH decay and loss of tracer from the ring is negligible. However, the barotropic ring cannot pass the ridge due to energy and vorticity constraints. In the case of a two-layer ring the initial SSH decay is governed by a mixed barotropic–baroclinic instability of the ring. Again, radiation of barotropic Rossby waves is present. When the ring passes the topographic ridge, it shows a small but significant stagnation of SSH decay, agreeing with satellite altimetry observations. This is found to be due to a reduction of the growth rate of the m = 2 instability, to conversions of kinetic energy to the upper layer, and to a decrease in Rossby-wave radiation. The energy transfer is related to the fact that coherent structures in the lower layer cannot pass the steep ridge due to energy constraints. Furthermore, the loss of tracer from the ring through filamentation is less than for a ring moving over a flat bottom, related to a decrease in propagation speed of the ring. We conclude that ridges like the Walvis Ridge tend to stabilize a multi-layer ring and reduce its decay.

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This article assesses the extent to which sampling variation affects findings about Malmquist productivity change derived using data envelopment analysis (DEA), in the first stage by calculating productivity indices and in the second stage by investigating the farm-specific change in productivity. Confidence intervals for Malmquist indices are constructed using Simar and Wilson's (1999) bootstrapping procedure. The main contribution of this article is to account in the second stage for the information in the second stage provided by the first-stage bootstrap. The DEA SEs of the Malmquist indices given by bootstrapping are employed in an innovative heteroscedastic panel regression, using a maximum likelihood procedure. The application is to a sample of 250 Polish farms over the period 1996 to 2000. The confidence intervals' results suggest that the second half of 1990s for Polish farms was characterized not so much by productivity regress but rather by stagnation. As for the determinants of farm productivity change, we find that the integration of the DEA SEs in the second-stage regression is significant in explaining a proportion of the variance in the error term. Although our heteroscedastic regression results differ with those from the standard OLS, in terms of significance and sign, they are consistent with theory and previous research.

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A numerical study of fluid mechanics and heat transfer in a scraped surface heat exchanger with non-Newtonian power law fluids is undertaken. Numerical results are generated for 2D steady-state conditions using finite element methods. The effect of blade design and material properties, and especially the independent effects of shear thinning and heat thinning on the flow and heat transfer, are studied. The results show that the gaps at the root of the blades, where the blades are connected to the inner cylinder, remove the stagnation points, reduce the net force on the blades and shift the location of the central stagnation point. The shear thinning property of the fluid reduces the local viscous dissipation close to the singularity corners, i.e. near the tip of the blades, and as a result the local fluid temperature is regulated. The heat thinning effect is greatest for Newtonian fluids where the viscous dissipation and the local temperature are highest at the tip of the blades. Where comparison is possible, very good agreement is found between the numerical results and the available data. Aspects of scraped surface heat exchanger design are assessed in the light of the results. (C) 2003 Elsevier Ltd. All rights reserved.

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This is a study of singular solutions of the problem of traveling gravity water waves on flows with vorticity. We show that, for a certain class of vorticity functions, a sequence of regular waves converges to an extreme wave with stagnation points at its crests. We also show that, for any vorticity function, the profile of an extreme wave must have either a corner of 120° or a horizontal tangent at any stagnation point about which it is supposed symmetric. Moreover, the profile necessarily has a corner of 120° if the vorticity is nonnegative near the free surface.

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This paper studies periodic traveling gravity waves at the free surface of water in a flow of constant vorticity over a flat bed. Using conformal mappings the free-boundary problem is transformed into a quasilinear pseudodifferential equation for a periodic function of one variable. The new formulation leads to a regularity result and, by use of bifurcation theory, to the existence of waves of small amplitude even in the presence of stagnation points in the flow.

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We study stagnation points of two-dimensional steady gravity free-surface water waves with vorticity. We obtain for example that, in the case where the free surface is an injective curve, the asymptotics at any stagnation point is given either by the “Stokes corner flow” where the free surface has a corner of 120°, or the free surface ends in a horizontal cusp, or the free surface is horizontally flat at the stagnation point. The cusp case is a new feature in the case with vorticity, and it is not possible in the absence of vorticity. In a second main result we exclude horizontally flat singularities in the case that the vorticity is 0 on the free surface. Here the vorticity may have infinitely many sign changes accumulating at the free surface, which makes this case particularly difficult and explains why it has been almost untouched by research so far. Our results are based on calculations in the original variables and do not rely on structural assumptions needed in previous results such as isolated singularities, symmetry and monotonicity.

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Improved crop yield forecasts could enable more effective adaptation to climate variability and change. Here, we explore how to combine historical observations of crop yields and weather with climate model simulations to produce crop yield projections for decision relevant timescales. Firstly, the effects on historical crop yields of improved technology, precipitation and daily maximum temperatures are modelled empirically, accounting for a nonlinear technology trend and interactions between temperature and precipitation, and applied specifically for a case study of maize in France. The relative importance of precipitation variability for maize yields in France has decreased significantly since the 1960s, likely due to increased irrigation. In addition, heat stress is found to be as important for yield as precipitation since around 2000. A significant reduction in maize yield is found for each day with a maximum temperature above 32 °C, in broad agreement with previous estimates. The recent increase in such hot days has likely contributed to the observed yield stagnation. Furthermore, a general method for producing near-term crop yield projections, based on climate model simulations, is developed and utilized. We use projections of future daily maximum temperatures to assess the likely change in yields due to variations in climate. Importantly, we calibrate the climate model projections using observed data to ensure both reliable temperature mean and daily variability characteristics, and demonstrate that these methods work using retrospective predictions. We conclude that, to offset the projected increased daily maximum temperatures over France, improved technology will need to increase base level yields by 12% to be confident about maintaining current levels of yield for the period 2016–2035; the current rate of yield technology increase is not sufficient to meet this target.

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The central sector of the last British–Irish Ice Sheet (BIIS) was characterised by considerable complexity, both in terms of its glacial stratigraphy and geomorphological signature. This complexity is reflected by the large number and long history of papers that have attempted to decipher the glaciodynamic history of the region. Despite significant advances in our understanding, reconstructions remain hotly debated and relatively local, thereby hindering attempts to piece together BIIS dynamics. This paper seeks to address these issues by reviewing geomorphological mapping evidence of palimpsest flow signatures and providing an up-to-date stratigraphy of the region. Reconciling geomorphological and sedimentological evidence with relative and absolute dating constraints has allowed us to develop a new six-stage glacial model of ice-flow history and behaviour in the central sector of the last BIIS, with three major phases of glacial advance. This includes: I. Eastwards ice flow through prominent topographic corridors of the north Pennines; II. Cessation of the Stainmore ice flow pathway and northwards migration of the North Irish Sea Basin ice divide; III. Stagnation and retreat of the Tyne Gap Ice Stream; IV. Blackhall Wood–Gosforth Oscillation; V. Deglaciation of the Solway Lowlands; and VI. Scottish Re-advance and subsequent final retreat of ice out of the central sector of the last BIIS. The ice sheet was characterised by considerable dynamism, with flow switches, initiation (and termination) of ice streams, draw-down of ice into marine ice streams, repeated ice-marginal fluctuations and the production of large volumes of meltwater, locally impounded to form ice-dammed glacial lakes. Significantly, we tie this reconstruction to work carried out and models developed for the entire ice sheet. This therefore situates research in the central sector within contemporary understanding of how the last BIIS evolved over time.

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This study reconstructs the depositional environments that accompanied both ice advance and ice retreat of the last British–Irish Ice Sheet in NE England during the Last Glacial Maximum, and proposes three regional ice-flow phases. The Late Devensian (29–22 cal. ka BP) Tyne Gap Ice Stream initially deposited the Blackhall Till Formation during shelf-edge glaciation (Phase I). This subglacial traction till comprises several related facies, including stratified and laminated diamictons, tectonites, and sand and gravel beds deposited both in subglacial canals and in proglacial streams. Eventually, stagnation of the Tyne Gap Ice Stream led to ice-marginal sedimentation in County Durham (Phase II). During the Dimlington Stadial (21 cal. ka BP), the North Sea Lobe advanced towards the coastline of N Norfolk. This resulted initially in sandur deposition (widespread, tabular sand and gravel; the Peterlee Sand and Gravel Formation; Phase II) and ultimately in deposition of the Horden Till Formation (Phase III), a massive subglacial till. As the North Sea Lobe overrode previous formations, it thrusted and stacked sediments in County Durham, and dammed proglacial lakes between the east-coast ice, the Pennine uplands and the remaining Pennine ice. The North Sea Lobe retreated after Heinrich Event 1 (16 ka). This study highlights the complexity of ice flow during the Late Devensian glaciation of NE England, with changing environmental and oceanic conditions forcing a mobile and sensitive ice sheet.

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This paper for the first time discuss the wind pressure distribution on the building surface immersed in wind profile of low-level jet rather than a logarithmic boundary-layer profile. Two types of building models are considered, low-rise and high-rise building, relative to the low-level jet height. CFD simulation is carried out. The simulation results show that the wind pressure distribution immersed in a low-jet wine profile is very different from the typical uniform and boundary-layer flow. For the low-rise building, the stagnation point is located at the upper level of windward façade for the low-level jet wind case, and the separation zone above the roof top is not as obvious as the uniform case. For the high-rise building model, the height of stagnation point is almost as high as the low-level jet height.