56,605 research outputs found

    EcSeg: Semantic Segmentation of Metaphase Images Containing Extrachromosomal DNA

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    Dataset used to benchmark "EcSeg: Semantic Segmentation of Metaphase Images Containing Extrachromosomal DNA" by Rajkumar et al

    EcSeg: Semantic Segmentation of Metaphase Images Containing Extrachromosomal DNA

    No full text
    Dataset used to benchmark "EcSeg: Semantic Segmentation of Metaphase Images Containing Extrachromosomal DNA" by Rajkumar et al

    EcSeg: Semantic Segmentation of Metaphase Images Containing Extrachromosomal DNA

    No full text
    Dataset used to benchmark "EcSeg: Semantic Segmentation of Metaphase Images Containing Extrachromosomal DNA" by Rajkumar et al

    ecSeg Dataset

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    Raw and labeled images used to produce results for "EcSeg: Semantic Segmentation of Metaphase Images Containing Extrachromosomal DNA

    EcSeg: Semantic Segmentation of Metaphase Images Containing Extrachromosomal DNA

    No full text
    Dataset used to benchmark "EcSeg: Semantic Segmentation of Metaphase Images Containing Extrachromosomal DNA" by Rajkumar et al.THIS DATASET IS ARCHIVED AT DANS/EASY, BUT NOT ACCESSIBLE HERE. TO VIEW A LIST OF FILES AND ACCESS THE FILES IN THIS DATASET CLICK ON THE DOI-LINK ABOV

    A Dynamic Subfilter-scale Stress Model for Large Eddy Simulations Based on Physical Flow Scales

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    We propose a new definition of the length scale in an eddy-viscosity model for large-eddy simulations (LES). This formulation extends and generalizes a previous proposal [Piomelli, Rouhi and Geurts, Proc. ETMM10, 2014], in which the LES length scale was expressed in terms of the integral length-scale of turbulence determined by the flow characteristics and explicitly decoupled from the simulation grid; this approach was named Integral Length-Scale Approximation (ILSA). As in the original ILSA, the model coefficient was determined by the user, and required to maintain a desired contribution of the unresolved, subfilter scales (SFS) to the global transport. We propose a local formulation (local ILSA) in which the model coefficient is local in space, allowing a precise control over SFS activity as a function of location. This new formulation preserves the properties of the global model; application to channel flow and backward-facing step verifies its features and accuracy

    Large-eddy simulation of a separated flow with a sub-filter scale model based on the integral length-scale

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    A new sub-filter scale model for large-eddy simulations, which uses a length-scale proportional to the integral scale of the turbulence instead of the grid resolution to parametrize the modelled stresses, will be assessed in the prediction of the flow of a boundary-layer over a rough surface, which includes separation and reattachment

    Near Wall PIV-Measurements on the Windward Slope of a Hill

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    The turbulent flow over periodic hills was measured near to the wall, using planar Particle-Image-Velocimetry (PIV) at high spatial resolution. Our focus is on the near wall turbulence structure on the windward slope of the hill. For large-eddy simulation (LES) we suspect that, if this was not predicted accurately, it affects the prediction of the velocity profiles over the hill crest which in turn will affect the recirculation length downstream of the hill. Regarding the time averaged velocities, we were able to resolve the linear viscous region of the boundary layer. The velocity distribution and also the Reynolds stress does not comply with the law of the wall as it is valid for a turbulent boundary layer at equilibrium

    The implications of foreign aid fungibility for development assistance

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    A foreign aid or foreign lending policy that focuses exclusively on project financing may have unintended consequences, report the authors. New research shows that aid intended for crucial social and economic sectors often merely substitutes for spending that recipient governments would have undertaken anyway and the funds that are thereby freed up are spent for other purposes. If the aid funds something that would have been done anyway, traditional ways of evaluating the aid's effectiveness are not really accurate. Ifaid funds are fungible and the recipient's public spending program is unsatisfactory, project lending may not be cost-effective. If the recipient's public spending program is satisfactory, perhaps the donor should finance a portion of it instead of financing individual projects. One solution to the problem of fungibility, then, is that donors could tie assistance to an overall public spending program (in the recipient country) that provides adequate resources to crucial sectors. To make this kind of reform operational, the authors propose a new lending instrument: a public expenditure reform loan (PERL). A PERL would tie an institution's lending strategy to the recipient country's achievement of mutually agreed-upon development goals. Everyone agrees that better donor coordination is needed, but it has been difficult to achieve because some donors tend to prefer projects (usually with the national flag flying over them). By agreeing on a public expenditure program and financing a portion of it, the World Bank credibly ask other donors to do the same.Payment Systems&Infrastructure,Development Economics&Aid Effectiveness,Gender and Development,Decentralization,Economic Adjustment and Lending,Development Economics&Aid Effectiveness,Poverty Assessment,National Governance,Economic Adjustment and Lending,Public Sector Economics&Finance

    Energy dissipation and flux laws for unsteady turbulence

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    Direct Numerical Simulations of spatially periodic unsteady turbulence show that the high Reynolds number scalings of the instantaneous energy dissipation rate and interscale energy flux at intermediate wavenumbers are qualitatively different from the well-known u(t)3/L(t)u'(t)^{3}/L(t) cornerstone scalings of equilibrium turbulence where u(t)u'(t) and L(t)L(t) are time-dependent rms velocity and integral length-scales. Instead, they both scale as U0L0u(t)2/L(t)2U_{0}L_{0}\:u'(t)^2/L(t)^2 where L0L_0 and U0U_0 are length and velocity scales characterizing initial/overall unsteady turbulence conditions
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