979 resultados para SINGULAR RIEMANNIAN FOLIATIONS


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Este artículo pertenece a una sección de la revista dedicada a innovación educativa, en este número a la audiencia pública. - Resumen tomado parcialmente de la revista

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Resumen tomado de la publicación. - El artículo forma parte de una sección de la revista dedicada a aulas hospitalarias

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Monogr??fico con el t??tulo: 'La lectura prioridad educativa: todos hacemos lectores'. Resumen tomado de la publicaci??n

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El t??tulo aparece en espa??ol y, a continuaci??n, el t??tulo traducido al ingl??s: ???Waldorf Education and Play in the Kindergarden. An Outstanding Theoretical Proposal'

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Monogr??fico con el t??tulo: "La formaci??n del profesorado desde distintas miradas: inclusi??n, g??nero y evaluaci??n".

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M. Lluïsa Faxedas, professora d'Història de l'Art Contemporani de la UdG i comissària de l'exposició "El gran dia de Girona, de Ramon Martí Alsina. Anatomia d'un quadre", ens parla breument de la importància d'aquest quadre dins la història de l'art català i de la seva recent restauració

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Sobre el creixement urbà, el desenvolupament i l'ordenació territorial de La Selva, comarca singular per la seva heterogeneïtat

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Descripció del bloc granític basculant, conegut amb el nom de 'Pedralta', situat entre els termes municipals de Santa Cristina d'Aro i Sant Feliu arrel de la seva caiguda per causes naturals, el 10 de desembre de 1996

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Numa altura em que a instituição escola alcança níveis de sofisticação cultural e organizacional inéditos, assistimos à implementação de uma liderança unipessoal, centrada na figura do Diretor de escola/agrupamento. Contudo, este novo rosto, erguido paradigma da nova gestão escolar, defronta-se com as múltiplas caras das escolas públicas, cada vez mais mascaradas face à imposição de um modelo de liderança unidimensional. Partindo deste cenário, focamos a nossa abordagem sobre: i) os traços que têm vindo a institucionalizar um perfil-ideal de liderança escolar; ii) até que ponto a liderança unipessoal servirá (melhor)como veículo de expressão de uma cultura escolar que se pretende reproduzir nas diversas escolas; iii) de que modo o rosto (Diretor) exercerá um efeito homogeneizador, marcando quadros de interação e lógicas de organização, sobre o quodiano das escolas. As questões enunciadas serão exploradas utilizando como dispositivo metodológico a análise crítica dos Relatórios de Avaliação Externa das Escolas produzidos durante o I ciclo avaliativo (2006-2011), com o objetivo de apreender os modelos implícitos de cultura de escola e de liderança e as suas implicações na reconfiguração do quotidiano das escolas.

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Moist singular vectors (MSV) have been applied successfully to predicting mid-latitude storms growing in association with latent heat of condensation. Tropical cyclone sensitivity has also been assessed. Extending this approach to more general tropical weather systems here, MSVs are evaluated for understanding and predicting African easterly waves, given the importance of moist processes in their development. First results, without initial moisture perturbations, suggest MSVs may be used advantageously. Perturbations bear similar structural and energy profiles to previous idealised non-linear studies and observations. Strong sensitivities prevail in the metrics and trajectories chosen, and benefits of initial moisture perturbations should be appraised. Copyright © 2009 Royal Meteorological Society

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The extent to which the four-dimensional variational data assimilation (4DVAR) is able to use information about the time evolution of the atmosphere to infer the vertical spatial structure of baroclinic weather systems is investigated. The singular value decomposition (SVD) of the 4DVAR observability matrix is introduced as a novel technique to examine the spatial structure of analysis increments. Specific results are illustrated using 4DVAR analyses and SVD within an idealized 2D Eady model setting. Three different aspects are investigated. The first aspect considers correcting errors that result in normal-mode growth or decay. The results show that 4DVAR performs well at correcting growing errors but not decaying errors. Although it is possible for 4DVAR to correct decaying errors, the assimilation of observations can be detrimental to a forecast because 4DVAR is likely to add growing errors instead of correcting decaying errors. The second aspect shows that the singular values of the observability matrix are a useful tool to identify the optimal spatial and temporal locations for the observations. The results show that the ability to extract the time-evolution information can be maximized by placing the observations far apart in time. The third aspect considers correcting errors that result in nonmodal rapid growth. 4DVAR is able to use the model dynamics to infer some of the vertical structure. However, the specification of the case-dependent background error variances plays a crucial role.

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In this article, we use the no-response test idea, introduced in Luke and Potthast (2003) and Potthast (Preprint) and the inverse obstacle problem, to identify the interface of the discontinuity of the coefficient gamma of the equation del (.) gamma(x)del + c(x) with piecewise regular gamma and bounded function c(x). We use infinitely many Cauchy data as measurement and give a reconstructive method to localize the interface. We will base this multiwave version of the no-response test on two different proofs. The first one contains a pointwise estimate as used by the singular sources method. The second one is built on an energy (or an integral) estimate which is the basis of the probe method. As a conclusion of this, the probe and the singular sources methods are equivalent regarding their convergence and the no-response test can be seen as a unified framework for these methods. As a further contribution, we provide a formula to reconstruct the values of the jump of gamma(x), x is an element of partial derivative D at the boundary. A second consequence of this formula is that the blow-up rate of the indicator functions of the probe and singular sources methods at the interface is given by the order of the singularity of the fundamental solution.