210 research outputs found

    Curvelet Approach for SAR Image Denoising, Structure Enhancement, and Change Detection

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    In this paper we present an alternative method for SAR image denoising, structure enhancement, and change detection based on the curvelet transform. Curvelets can be denoted as a two dimensional further development of the well-known wavelets. The original image is decomposed into linear ridge-like structures, that appear in different scales (longer or shorter structures), directions (orientation of the structure) and locations. The influence of these single components on the original image is weighted by the corresponding coefficients. By means of these coefficients one has direct access to the linear structures present in the image. To suppress noise in a given SAR image weak structures indicated by low coefficients can be suppressed by setting the corresponding coefficients to zero. To enhance structures only coefficients in the scale of interest are preserved and all others are set to zero. Two same-sized images assumed even a change detection can be done in the curvelet coefficient domain. The curvelet coefficients of both images are differentiated and manipulated in order to enhance strong and to suppress small scale (pixel-wise) changes. After the inverse curvelet transform the resulting image contains only those structures, that have been chosen via the coefficient manipulation. Our approach is applied to TerraSAR-X High Resolution Spotlight images of the city of Munich. The curvelet transform turns out to be a powerful tool for image enhancement in fine-structured areas, whereas it fails in originally homogeneous areas like grassland. In the change detection context this method is very sensitive towards changes in structures instead of single pixel or large area changes. Therefore, for purely urban structures or construction sites this method provides excellent and robust results. While this approach runs without any interaction of an operator, the interpretation of the detected changes requires still much knowledge about the underlying objects

    The listener in music historiography, 1776-1928

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    Towards “The Nature and Secrets of Music”: W. C. Printz and the natural history tradition

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    The present article provides arecontextualization of Wolfgang Caspar Printz’s (1641–1717) landmark music history published in 1690 (Historische Beschreibung der edelen Sing- und Kling-Kunst). later commentators have read it as a primitive, naïve and even failed attempt at writing the history of music. Still, they seem to agree that the text, in virtue of its subject matter, forms part of a canon of music historiography. The present article will seek the interpretative key in the wider intellectual context, outside of the narrow confines of texts about the musical past. It will advance the thesis that Printz built his music historiography from elements of the natural history tradition. Two arguments support this thesis. First, it will be argued that the organization of the material in chapters XIv, Xv and XvI betrays the influence of a classical version of taxonomy closely associated with the natural history tradition. Secondly, that Printz’s inquiry into the purpose of music reveals his reliance on a concept of nature similarly rooted in natural history.The present article provides arecontextualization of Wolfgang Caspar Printz’s (1641–1717) landmark music history published in 1690 (Historische Beschreibung der edelen Sing- und Kling-Kunst). later commentators have read it as a primitive, naïve and even failed attempt at writing the history of music. Still, they seem to agree that the text, in virtue of its subject matter, forms part of a canon of music historiography. The present article will seek the interpretative key in the wider intellectual context, outside of the narrow confines of texts about the musical past. It will advance the thesis that Printz built his music historiography from elements of the natural history tradition. Two arguments support this thesis. First, it will be argued that the organization of the material in chapters XIv, Xv and XvI betrays the influence of a classical version of taxonomy closely associated with the natural history tradition. Secondly, that Printz’s inquiry into the purpose of music reveals his reliance on a concept of nature similarly rooted in natural history

    In memoriam Prof. Dr. rer. nat. Hildegard StrĂŒbing (8.5.1922 - 18.5.2013), with a complete bibliography

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    An obituary for Hildegard StrĂŒbing (1922 - 2013

    Thermal Critical Points and Quantum Critical End Point in the Frustrated Bilayer Heisenberg Antiferromagnet

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    We consider the finite-temperature phase diagram of the S=1/2S = 1/2 frustrated Heisenberg bilayer. Although this two-dimensional system may show magnetic order only at zero temperature, we demonstrate the presence of a line of finite-temperature critical points related to the line of first-order transitions between the dimer-singlet and -triplet regimes. We show by high-precision quantum Monte Carlo simulations, which are sign-free in the fully frustrated limit, that this critical point is in the Ising universality class. At zero temperature, the continuous transition between the ordered bilayer and the dimer-singlet state terminates on the first-order line, giving a quantum critical end point, and we use tensor-network calculations to follow the first-order discontinuities in its vicinity.Comment: 6 pages, 4 figures; supplemental material: 3 pages, 3 figures; v2: as publishe

    Finite-Temperature Dynamics and Thermal Intraband Magnon Scattering in Haldane Spin-One Chains

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    The antiferromagnetic spin-one chain is considerably one of the most fundamental quantum many-body systems, with symmetry protected topological order in the ground state. Here, we present results for its dynamical spin structure factor at finite temperatures, based on a combination of exact numerical diagonalization, matrix-product-state calculations and quantum Monte Carlo simulations. Open finite chains exhibit a sub-gap band in the thermal spectral functions, indicative of localized edge-states. Moreover, we observe the thermal activation of a distinct low-energy continuum contribution to the spin spectral function with an enhanced spectral weight at low momenta and its upper threshold. This emerging thermal spectral feature of the Haldane spin-one chain is shown to result from intra-band magnon scattering due to the thermal population of the single-magnon branch, which features a large bandwidth-to-gap ratio. These findings are discussed with respect to possible future studies on spin-one chain compounds based on inelastic neutron scattering.Comment: 10 pages with 11 figures total (including Supplemental Material); changes in v2: new Figs. S1 and S5, Fig. S3 expanded + related discussion + many smaller modifications to match published versio

    Pattern and Process: Evolution of Troglomorphy in the Cave-Planthoppers of Australia and Hawai’i ‒ Preliminary Observations (Insecta: Hemiptera: Fulgoromorpha: Cixiidae)

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    The evolution of troglobites comprises three distinct problems: cave colonization by an epigean ancestor, the evolution of troglomorphies, and intra-cave speciation. The study of cave-dwelling planthoppers has contributed much to our understanding of troglobite evolution and provides useful model systems to test various aspects of the theoretic framework developed in recent years. Most promising in this respect are taxa with several closely related but independently evolved troglobiontic lineages, such as on the Canary Islands, in Queensland/Australia and on the Hawaiian Archipelago. Closely related species often occur in caves with comparable ecological parameters yet differ in their age. Here we use comparative age estimates for Australian and Hawaiian cave cixiids to assess the dynamics of reductive evolutionary trends (evolution of troglomorphy) in these taxa and cave planthoppers in general. We show that the degree of troglomorphy is not correlated with the age of cave lineages. Morphological alteration may not be used to draw conclusions about the phylogenetic age of cave organisms, and hypotheses based on such assumptions should be tested in light of these findings

    Dynamical Signatures of Edge-State Magnetism on Graphene Nanoribbons

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    We investigate the edge-state magnetism of graphene nanoribbons using projective quantum Monte Carlo simulations and a self-consistent mean-field approximation of the Hubbard model. The static magnetic correlations are found to be short ranged. Nevertheless, the correlation length increases with the width of the ribbon such that already for ribbons of moderate widths we observe a strong trend towards mean-field-type ferromagnetic correlations at a zigzag edge. These correlations are accompanied by a dominant low-energy peak in the local spectral function and we propose that this can be used to detect edge-state magnetism by scanning tunneling microscopy. The dynamic spin structure factor at the edge of a ribbon exhibits an approximately linearly dispersing collective magnonlike mode at low energies that decays into Stoner modes beyond the energy scale where it merges into the particle-hole continuum.Comment: 4+ pages including 4 figure

    Automatic Shear Wave Splitting Measurements at Mt. Ruapehu Volcano, New Zealand

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    This thesis presents an automatic shear wave splitting measurement tool and the results from its application to data recorded in the vicinity of Mt. Ruapehu volcano on the North Island of New Zealand. The best methodology and parameters for routine automatic monitoring are determined and approximately 10,000 events are processed. About 50% of all S-phases lead to measurements of acceptable quality. Results obtained with this technique are reproducible and objective, but more scattered than results from manual measurements. The newly developed automatic measurement tool is used to measure shear wave splitting for previously analysed data and for new data recorded in 2003-2007. In contrast to previous studies at Mt. Ruapehu, we have a larger and continuous data set from numerous three-component seismic stations. No major temporal changes are found within the new data, but results vary for di erent station locations.
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