3,460 research outputs found

    Gravitationally Induced Neutrino-Oscillation Phases

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    In this essay, we introduce a new effect of gravitationally induced quantum mechanical phases in neutrino oscillations. These phases arise from an hitherto unexplored interplay of gravitation and the principle of the linear superposition of quantum mechanics. In the neighborhood of a 1.4 solar-mass neutron star, gravitationally induced quantum mechanical phases are roughly 20% of their kinematical counterparts. When this information is coupled with the mass square differences implied by the existing neutrino-oscillation data we find that the new effect may have profound consequences for type-II supernova evolution.Comment: First Prize Gravity Research Foundation Essay (1996). Added two appendices. Appendix A: Erratum. Appendix B: Neutrino oscillations as a new energy transport mechanism for supernova explosions (taken from a 1996 JRO Fellowship proposal

    Visual SLAM for flying vehicles

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    The ability to learn a map of the environment is important for numerous types of robotic vehicles. In this paper, we address the problem of learning a visual map of the ground using flying vehicles. We assume that the vehicles are equipped with one or two low-cost downlooking cameras in combination with an attitude sensor. Our approach is able to construct a visual map that can later on be used for navigation. Key advantages of our approach are that it is comparably easy to implement, can robustly deal with noisy camera images, and can operate either with a monocular camera or a stereo camera system. Our technique uses visual features and estimates the correspondences between features using a variant of the progressive sample consensus (PROSAC) algorithm. This allows our approach to extract spatial constraints between camera poses that can then be used to address the simultaneous localization and mapping (SLAM) problem by applying graph methods. Furthermore, we address the problem of efficiently identifying loop closures. We performed several experiments with flying vehicles that demonstrate that our method is able to construct maps of large outdoor and indoor environments. © 2008 IEEE

    Quark fragmentation into vector and pseudoscalar mesons at LEP

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    Some data on the ratio of vector to vector + pseudoscalar mesons, V/(V+P), and the probability of helicity zero vector states, rho_00, are now available from LEP. A possible relation between these two quantities and their interpretation in terms of polarized fragmentation functions are discussed; numerical estimates are given for the relative occupancies of K and K*, D and D*, B and B* states.Comment: 5 pages, no figure

    The weight-inclusive vs. weight-normative approach to health: Evaluating the evidence for prioritizing well-being over weight

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    Using an ethical lens, this review evaluates two methods of working within patient care and public health: the weight-normative approach (emphasis on weight and weight loss when defining health and well-being) and the weight-inclusive approach (emphasis on viewing health and well-being as multifaceted while directing efforts toward improving health access and reducing weight stigma). Data reveal that the weight-normative approach is not effective for most people because of high rates of weight regain and cycling from weight loss interventions, which are linked to adverse health and well-being. Its predominant focus on weight may also foster stigma in health care and society, and data show that weight stigma is also linked to adverse health and well-being. In contrast, data support a weight-inclusive approach, which is included in models such as Health at Every Size for improving physical (e.g., blood pressure), behavioral (e.g., binge eating), and psychological (e.g., depression) indices, as well as acceptability of public health messages. Therefore, the weight-inclusive approach upholds nonmaleficience and beneficience, whereas the weight-normative approach does not. We offer a theoretical framework that organizes the research included in this review and discuss how it can guide research efforts and help health professionals intervene with their patients and community

    Improving model-satellite comparisons of sea ice melt onset with a satellite simulator

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    Seasonal transitions in Arctic sea ice, such as the melt onset, have been found to be useful metrics for evaluating sea ice in climate models against observations. However, comparisons of melt onset dates between climate models and satellite observations are indirect. Satellite data products of melt onset rely on observed brightness temperatures, while climate models do not currently simulate brightness temperatures, and must therefore define melt onset with other modeled variables. Here we adapt a passive microwave sea ice satellite simulator, the Arctic Ocean Observation Operator (ARC3O), to produce simulated brightness temperatures that can be used to diagnose the timing of the earliest snowmelt in climate models, as we show here using Community Earth System Model version 2 (CESM2) ocean-ice hindcasts. By producing simulated brightness temperatures and earliest snowmelt estimation dates using CESM2 and ARC3O, we facilitate new and previously impossible comparisons between the model and satellite observations by removing the uncertainty that arises due to definition differences. Direct comparisons between the model and satellite data allow us to identify an early bias across large areas of the Arctic at the beginning of the CESM2 ocean-ice hindcast melt season, as well as improve our understanding of the physical processes underlying seasonal changes in brightness temperatures. In particular, the ARC3O allows us to show that satellite algorithm-based melt onset dates likely occur after significant snowmelt has already taken place. © 2022 Author

    Rethinking the relationship between the observed, simulated and real Arctic sea-ice evolution

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    In this dissertation, I explore the large differences in Arctic sea-ice evolution between climate models and observations, and among individual climate models. First, I investigate the drivers of the long-term Arctic Ocean warming in a multi-model ensemble. I find that there is no consensus between the models about whether the excess energy is gained by the ocean through the net atmospheric surface flux or through the meridional oceanic heat flux. However, all models agree on the magnitude of the projected warming. The warming is small compared to the anomalies in the energy fluxes. This is because most of the energy gained through one energy flux is lost through the other energy flux due to a relationship between the magnitude of the increase in oceanic heat inflow and the increase in turbulent heat loss to the atmosphere. Second, I explore the feasibility of an observation operator for the Arctic Ocean. An observation operator translates the Arctic Ocean climate simulated by a climate model into a brightness temperature. The brightness temperature is the quantity directly measured by satellites from space. Hence, an observation operator enables us to circumvent the observational uncertainty currently inhibiting reliable climate model evaluation. Sea-ice brightness temperatures at 6.9 GHz are driven by the liquid water fraction profile inside the ice and snow, which is not resolved in most climate models. I show that in winter this profile can be described reasonably well by a linear temperature profile and a salinity profile prescribed as a self-similar function of depth. In summer, the melt-pond fraction is more important for the simulation of the brightness temperature than the internal structure of the ice. Third, I develop an Arctic Ocean Observation Operator for 6.9 GHz based on these findings. I compare brightness temperatures simulated from the output of an Earth System Model to brightness temperatures measured by satellites. The differences between simulated and measured brightness temperatures can mainly be explained by the uncertainty in the simulated state of the sea-ice concentration, the assimilation process, and the melt-pond parametrization. Differences attributable to biases in the observation operator itself are small. The operator is therefore a suitable method for climate model evaluation. In summary, I show different perspectives on the large differences in Arctic sea-ice evolution. On the one hand, I point out that the multi-model ensemble mean is not always representative for the simulated Arctic climate and should be interpreted with care. On the other hand, I introduce and develop an unconventional tool providing new opportunities for future climate model evaluation

    Percutaneous ct fluoroscopy-guided core needle biopsy of mediastinal masses: Technical outcome and complications of 155 procedures during a 10-year period

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    Purpose: To evaluate technical outcome, diagnostic yield and safety of computed tomo-graphic fluoroscopy-guided percutaneous core needle biopsies in patients with mediastinal masses. Methods: Overall, 155 CT fluoroscopy-guided mediastinal core needle biopsies, performed from March 2010 to June 2020 were included. Size of lesion, size of needle, access path, number of success, number of biopsies per session, diagnostic yield, patient’s position, effective dose, rate of complications, tumor localization, size of tumor and histopathological diagnosis were considered. Post-interventional CT was performed, and patients observed for any complications. Complications were classified per the Society of Interventional Radiology (SIR). Results: 148 patients (age, 54.7 ± 18.2) underwent 155 CT-fluoroscopy-guided percutaneous biopsies with tumors in the anterior (114; 73.5%), middle (17; 11%) and posterior (24; 15.5%) mediastinum, of which 152 (98%) were technically successful. For placement of the biopsy needle, in 82 (52.9%) procedures a parasternal trajectory was chosen, in 36 (23.3%) a paravertebral access, in 20 (12.9%) through the lateral intercostal space and in 17 (11%) the thoracic anterior midline, respectively. A total of 136 (89.5%) of the biopsies were considered adequate for a specific histopathologic analysis. Total DLP (dose-length product) was 575.7 ± 488.8 mGy*cm. Mean lesion size was 6.0 ± 3.3 cm. Neoplastic pathology was diagnosed in 115 (75.7%) biopsies and 35 (23%) biopsy samples showed no evidence of malignancy. Minor complications were observed in 18 (11.6%) procedures and major pneumothorax requiring drainage insertion in 3 interventions (1.9%). Conclusion: CT fluoroscopy-guided percutaneous core needle biopsy of mediastinal masses is an effective and safe procedure for the initial assessment of patients with mediastinal tumors

    An Autonomous Robotic System for Mapping Abandoned Mines

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    We present the software architecture of a robotic system for mapping abandoned mines. The software is capable of acquiring consistent 2D maps of large mines with many cycles, represented as Markov random fields. 3D C-space maps are acquired from local 3D range scans, which are used to identify navigable paths using A* search. Our system has been deployed in three abandoned mines, two of which inaccessible to people, where it has acquired maps of unprecedented detail and accuracy
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